laboratoire oceanographique de l1atlantique …

DFO - Lib/ I Mii- Ebb otheque

111 10028231

DEPARTMENT OF ENERGV,MINES AND RESOURCES MARINE SCIENCES BRANCH

MINISTERE DE L'ENERGIE DE MINES ET DES RESSOURCES DIRECTION DES SCIENCES DE LA MER

ATLANTIC OCEANOGRAPHIC LABORATORY BEDFORD INSTITUTE

LABORATOIRE OCEANOGRAPHIQUE DE L1ATLANTIQUE INSTITUT de BEDFORD

Dartmouth, Nova Scotia

Canada

WAVE CLIMATE OF THE CANADIAN ATLANTIC COAST

and

CONTINENTAL SHELF — 1970

by

H. A. NEU

AOL REPORT 1971-10

DECEMBER 1971

PROGRAMMED BY

THE CANADIAN COMMITTEE OF OCEANOGRAPHY

ATLANTIC OCEANOGRAPHIC LABORATORY

BEDFORD INSTITUTE

DARTMOUTH, NOVA SCOTIA

WAVE CLIMATE OF THE CANADIAN ATLANTIC COAST

AND CONTINENTAL SHELF - 1970

by

H.A. NEU

AOL REPORT 1971-10

DECEMBER 1971

(1)

ABSTRACT

Based on the synoptic wave charts issued twice daily by the

Maritime Forces Weather Centre, Halifax, the wave climate of the

Canadian Atlantic Coast and Continental Shelf was established for the

year 1970. The criteria and concepts for developing such a climate

are critically reviewed.

The results clearly indicate that the sea state conditions

along the coast and over the Continental Shelf vary greatly with season

and location. During the winter months, the wave energy was five to

six times greater than during the summer, and over Grand Banks it was

three to four times that over the Scotian Shelf.

The reason for this lies in the seasonal variation of the wind

with respect to its direction and strength. During the winter, strong

winds from the northwest are either directed off-shore with regard to

the southern coast thereby reducing the sea state by opposing the mid-

Atlantic waves, or are parallel to the eastern seaboard where they

generate large seas along the coast Of Labrador and over the grand Banks.

During the summer, winds are primarily from southwest along the southern

coast and away from the eastern seaboard. Since these winds are light,

wave action along both coastlines is very low.

In 1970, extreme wave heights over the Scotian Shelf were in

the order of 12.5 m, while over the Grand Banks they probably reached

18 to 19 m.

These results are essential for the design of structures and

for the planning and operation of off-shore explorations.

TABLE OF CONTENTS

Page

Abstract (i)

List of Figures (iii)

1. Introduction 1

2. The Atlantic Coast and Continental Shelf 2

3. Weather and Wind 4

4. Waves 6

4.1 Shoaling of Waves 6

4.2 Wave Observation Methods 8

4.3 Wave Data 10

4.4 Significant Wave 15

4.5 Extreme Wave 15

4.6 Wave Energy 16

4.7 Grid System 18

5. Results 19

5.1 Monthly Non-Directional Energy Distribution .. 19

5.2 Monthly Directional Energy Spectra 23

5.3 Monthly Directional Wave Statistics 24

5.4 Extreme Wave Heights 25

6. Conclusions 26

7. Acknowledgement 27

8. Appendix 28

LIST OF FIGURES

Page

1. Canadian Atlantic Coast and Continental Shelf 3

2. Mean Seasonal Atmospheric Pressure 5

3. Wave Refraction on the Scotian Shelf 7

4. Wave Refraction at Halifax Inlet 7

5. Wave Chart of 23 January 1970 12

6.• Wave Chart of 4 February 1970 13

7. Wave Chart of 27 December 1970 14

8. Statistical Distribution of Wave Heights 17

9. Significant Energy vs. Total Energy of a 6-hour

Sampling Period 18

10. Grid System and Codes of Wave Properties 20

11. Monthly Non-Directional Energy Spectra; January

to June 21

12. Monthly Non-Directional Energy Spectra; July

to December 22

I. INTRODUCTION

Canada has the longest coastline in the world, with a total

length of about 50,000 km. A large portion of it is along the Atlantic

seaboard, extending from the Gulf of Maine, at the Canada-U.S. border,

to the Arctic. Along this coastline stretches the Continental Shelf,

which is about 200 km wide off Nova Scotia, reaches out 500 km on the

Grand Banks south-east of Newfoundland, and then narrows to less than

100 km along the coast of Labrador. In general, the depths are less than

200 m, with the exception of the Laurentian Channel, which connects with

the Gulf of St. Lawrence,and Hudson Strait.

In recent years mineral exploration has increased in this area

particularly with respect to oil. Nearly all the available concession

rights have been acquired by oil firms, and several oil rigs are drilling

in the general vicinity of Sable Island and on the Grand Banks.

This exploration is faced with exceptional technological problems

with regard to the aquatic environment, especially the sea state. The

planning of the operation, the choice and design of drilling rigs which

can survive extreme storms and the knowledge of the occurrence of wave

heights which would limit drilling operations or threaten the platform,

all require reliable wave information.

It is well known that this type of information is scarce and

frequently non-existent. An investigation into the wave climate of the

Canadian Atlantic Coast and Continental Shelf thus became imperative to

provide systematic sea state information.

-2-

2. THE ATLANTIC COAST AND CONTINENTAL SHELF

As shown in Fig. 1, the Atlantic Coast and the Continental Shelf

are exposed to waves approaching the southern seaboard from the south-

west, south and east, and the eastern seaboard from the north and east.

Excluded from the investigation are the Bay of Fundy and the Gulf of

St. Lawrence which are partly protected by land. Fully exposed to wave

action from the south are Georges Bank at the entrance to the Bay of

Fundy, the Scotian Shelf, and the southern portion of the shelf off

Newfoundland. The Grand Banks, southeast of Newfoundland, are open to

nearly every direction, with the exception of a sector from the north-

west, while the east coasts of Newfoundland and Labrador are open to

waves from the Labrador Sea and the North Atlantic. The open sea dis-

tance, in all these directions, exceeds 3000 km. Storms rarely extend

over distances greater than 1000 to 1500 km.

When dealing with the wind-wave relationship, it is well known

and has been demonstrated by a number of researchers (Neumannl,

Bretschneider2, Darbyshire3 and others) that storm winds blowing over

such expanses, referred to as 'fetch', can generate exceptionally high

waves. In addition, swell waves, which may have originated outside

of the storm area - perhaps as far away as the South Atlantic - may

augment these wind-generated waves.

1. Neumann, G. "On ocean wave spectra and a new method of forecasting wind-generated sea". Tech. Memorandum No. 43, Beach Erosion Board, U.S. Army Corps of Eng., 1952.

2. Bretschneider, C.L. "Revised wave forecasting curves and procedures". Tech. Report No. HE-155047, Inst. of Eng. Research, Univ. of Calif., Berkeley, 1951.

3. Darbyshire, J. "The generation of waves by wind". Proc. Roy Soc. (London), Ser. A, 1952.

4o. 400

FIGURE 1: Canadian Atlantic Coast and Continental Shelf.

4

3. WEATHER AND WIND

During the winter months there is a strong outflow of very cold

Continental Arctic air into the Canadian Atlantic Region. Over the Gulf

Stream this encounters the moist warm air associated with the circula-

tion of the Azores High. The resultant great exchange of energy produces

frequent storm developments and these storms reach greatest intensity

between South Greenland and Iceland. A strong pressure gradient is

normally present, therefore, over the Scotian Shelf and Labrador Sea.

During the summer months, the temperature differential between

the Continental Arctic and the Maritimes air is much less pronounced

and consequently the polar front is less intense. Depressions forming

on this front rarely reach storm dimensions and the area of lowest

pressure is displaced northward towards the Davis Straits. Under these

conditions, winds over the Canadian Atlantic are generally moderate.

The average barometric pressure distributions, as shown in

Fig. 2, demonstrate this changing wind pattern. The geostrophic wind,

which is derived from these pressure distributions, is from the north-

west in the winter and blows along the coast of Labrador and off the

coast of the southern seaboard, while in the summer the opposite occurs.

However, the major difference lies in the greater strength of the winter

winds.

Clearly these wind conditions have a great effect upon wave

generation in both the coastal regions and the Grand Banks area.

40•

90.

-5

NOTE ATMOSPHERIC PRESSURE IN MILLIBARS MEAN SEA LEVEL PRESSURE OF PERIOD 1940 TO 1953 FROM ATLAS OF CANADA, OPT. OF MINES AND TECH. SURVEYS , 1957

FIGURE 2: Mean Seasonal Atmospheric Pressure

4. WAVES

4.1 Shoaling of Waves

Waves are modified on moving into shallower water. The

speed of a wave depends upon the water depth as well as upon the wave

length; the shallower the water, the slower the speed. Thus, wave

fronts must be bent when advancing at an angle into shoaling areas

because of the reduction of wave speed at the point of contact. This

behaviour is known as wave refraction. During the process, wave

energy may be concentrated or dispersed and, consequently, the wave

height increased or decreased locally. It is readily seen therefore

that heights and directions of waves in areas where shoaling occurs

are not directly related to the wave conditions in deep water.

According to the first order wave theory; waves shoal when

the depth of water is less than half the wave length. A 10-second wave,

which occurs frequently, begins to be affected when the depth is less

than 75 m, while a 14-second wave, which either results from a large

storm or is present as a swell wave, is affected when the depth is less

than 150 m. The depths on the Continental Shelf are usually greater

than 75 m and less than 200 m. It can be assumed therefore that most

waves, with the exception of very long ones, can move freely over most

of the Continental Shelf without being noticeably affected. This,

however, does not apply to some shallower areas on Georges Bank, around

Sable Island, and on the south tip of the Grand Banks, where depths are

less than 50 m.

66° 64° 63° 62° 61° 60° 59°

66' 65°

45°

44°

43°

PERIMI4 SECONDS DIRECTION FROM 180° SOUNDINGS IN METRES

9 190 290 Km

42°

FIGURE 3: Wave Refraction on the Scotian Shelf -

40'

30'

10'

64°00'

30' 20' 10' 63°00' 64° 00' 50'

40'

30'

44° 20'

10'

PERIOD 14 SECONDS DIRECTION FROM. 180°

SOUNDINGS IN METRES rioo

i~o, 10 20 Km

44° 20'

40' 10' 20'

FIGURE 4: Wave Refraction at Halifax Inlet

For a detailed analysis of wave conditions in these areas, the effect

of these shoals must be considered. An example of such a study for the

Scotian Shelf is shown in Fig. 3, where the Refraction Diagram of a

14-second wave approaching from the south is plotted.

Along the coast the sea bed generally rises landward from

a depth of 75 m in the last 10 to 20 km. Since the underwater topography

of this region is very irregular, the waves are modified greatly in

height and direction by shoaling and refraction. Such a modification

occurs at the entrance to Halifax Inlet, and is shown by the Fig. 4.

Thus it is obvious that wave observations performed in the

near-shore zone, with respect to wave height and direction of propagation,

are not representative of the sea state of the off-shore deep water region.

4.2 Wave Observation Methods

There are two ways of describing the sea state - one in

terms of power spectra, and the other with the characteristic physical

properties of the waves: their height, length or period, and the direc-

tion of propagation. The first is used primarily by scientists studying

the physics of waves, their relationship to the atmosphere, etc. It is

difficult and, in the opinion of the author, impracticable at present to

apply these data to a wave climate investigation. The second type of

description is more useful for applied scientists and engineers and also

more adaptable to a time series study.

In this investigation, waves are defined by the following

properties:

(a) Height - H, in metres

(b) Period - T, in seconds

(c) Direction - in degrees

There are four methods of obtaining these data. They are: hindcast-

ing from wind observations, direct measurement with wave gauges, aerial

surveying from satellites and visual observations from ships.

Hindcasting has been applied extensively in the past.

Its shortcomings, however, lie primarily in the fact that there are

insufficient meteorological observations made over the open ocean par-

ticularly with respect to varying winds and moving fetches. Furthermore,

the generation of waves and their decay is so complex and so little

understood that estimating the sea states from wind conditions can only

be performed by applying semi-empirical principles which do not provide

reliable or accurate results.

Direct surveying with wave gauges appears to be the most

logical method, yet it is confronted with extreme difficulties. Wave

gauges, exposed to the hazards of the open sea, have only short opera-

tional lives. For time series presentation and probability of occurrence,

pairs (or even more) of gauges would have to be placed at each location

in an attempt to ensure a continuous yearly record. For direct wave

height and energy comparisons along the coast and on the Continental

Shelf, hundreds of such groups would have to be operational for years.

This would be a monumental task. Furthermore, unless an even greater

number were used in special arrays, these gauges would provide no

information on wave direction, a property which is most important for

. coastal and open sea operations.

The third and potentially the most promising method of

obtaining wave data is that of surveying from satellites. Although the

author is not fully aware of the state of development in this field and

has no knowledge of a large-scale application of the method, it appears

- 10 -

that it may be available for general use in the late seventies or

early eighties.

In this paper, data obtained by the fourth method, visual

observations from ships, was used.

4.3 Wave Data

The Maritime Forces Weather Centre of the Canadian Weather

Service in Halifax, N.S., issues synoptic wave charts of the North

Atlantic twice daily based on observations taken at 0000 and 1200 hours

Greenwich time. The wave data for the charts are obtained from weather

ships, weather stations, Canadian and U.S. government ships, navies of

NATO countries and merchant ships. The majority of the data is obtained

visually and includes wave height, wave period and direction of propaga-

tion, to be transmitted in code.

On the average, the number of ships involved in reporting

the sea state is about 35 (varying from 20 to 60) depending on the season

and weather conditions. Occasionally, in areas far from navigation lanes

and observation ships, only few data may be available. Under these cir-

cumstances wave forecasting methods are applied and the results are

fitted into the observed wave environment.

A number of observations from the ships include information

on secondary waves, interfering with the primary waves. This is done in

order to differentiate between wind waves generated locally and the swell.

The wave chosen as being representative of such a sea state is obtained

by taking the square root of the sum of the component wave energies. The

second, third and ....nth

components are added to the first or prime one

in the ratio of their respective wave lengths. Since the wave length in

deep water condition is a function of the square of the wave period,

the composite wave height is derived from the following equation:

2 T H = H12 + T— T22 H 2 I. Tn2 H 2 4. 4. H 2 7 2 "T72- 3 • • • F2" n (1)

On a 24-hour basis, the data observed from ships and those

derived from regional forecasts are constantly reviewed by meteorolog-

ically trained personnel who continuously relate them to the past and

present wave-field and wind environment. Information which does not

fit into this pattern is rigorously checked for errors in observing,

reporting or communication and, if found faulty, discarded. In this

process, the wave data are subjected to a large measure of quality

control.

The data are then plotted on charts and lines of equal

wave height are drawn as shown in Figures 5, 6 and 7.

The charts issued twice daily form a time series of

12-hour intervals. From this sequence, the formation of storms, their

path and speed as well as their decay can be determined.

Winter storms passing along the coast of Nova Scotia have

speeds, on average, between 35 and 40 km per hour. The grid areas for

which the sea state is to be reported are approximately 200 by 280 km.

Thus, to avoid having storms pass through one of these grids without

being detected, the time interval should not be in excess of six hours.

This is achieved by estimating the location of the storm at 0600 and

1800 hours, thus providing wave information in the intermediate intervals.

roi GEOSTRONDC WIND SCUD NOWS.4201KTUNNW

T/h

D — DIRECTION T — PERIOD IN SEC

h — WAVE HEIGHT IN 1/2 METRES

— CONFUSED PERIOD

— ALL WAVE CONTOUR HEIGHTS IN METRES

4147, 411 41111111s 0

4!*

ICE •

•

4*

4s

nF 5/03

•

2/0

2/0

iwoas

WAVE DATA CHART

FOR 0000Z JAN 23 1970 SSUE0 BY MR WEATHER COM lIALIVAX

MATED SY CFN NALI1412 CANADA raw wineCTION

•11110•711011r.IMANDI• 011020•0110/110M110111.0Yea • RCM WM

20 40 60 SON . I -444111111111101 :l ANADIAN WEATHER SERVI 3/01 •

5/0

.ir

5/oi

- 12 -

FIGURE 5: Wave Chart of 23 January 1970

T/h

D - DIRECTION T - PERIOD IN SEC h - WAVE HEIGHT IN 1/2 METRES X - CONFUSED PERIOD

- ALL WAVE CONTOUR HEIGHTS IN METRES

/06 .

U.

CANADIAN WEATHER SERVICE

MID UT FLEET WIATNIA CENTRE HALIFAX RELATED ET CFN HALIFAX CANADA

WAVE DATA CHART

FOR 0000Z FEB a 1970

- 13 -

.1710101011al 01111101• Ova/OP =WINN, • CJIMa [011740 1%3

FIGURE 6: Wave Chart of 14 February 1970

- DIRECTION - PERIOD IN SEC - WAVE HEIGHT IN 1/2 METRES

- CONFUSED PERIOD

- ALL WAVE CONTOUR HEIGHTS IN METRES

. 40,1;), x/07.5/

• X/0 •

9/08. INOSTROPNIC WIND SCALE

1501AIS Olit NUMMI

10 AVM

20 40 100

CANADIAN WEATHER SERVICE WAVE DATA CHART

FOR 1200Z DEC. 27 1970 EYED WY FLEET WEATHER CENTRE HALIFAX

DILATED DT CFN HALIFAX CANADA

odlaNOUXICat NYCO • COMMON OP TIMIPOIT • Met

SON

. .70W •

- 14 -

FIGURE 7: Wave Chart of 27 December 1970

- 15 -

4.4 Significant Wave

As mentioned previously, the wave data used in this

analysis were generally derived from visual observations. According

to Wiegel4 and Ippen5 and their analyses of wave records, it has been

found that the wave properties obtained by visual observations are

equivalent for practical purposes to those of a wave defined as a

'significant wave'; the height (Haig) being the mean height of the

highest third of all the waves present in a wave train. Its period is

the 'significant period' (Trig).

This wave is considered to be representative of the sea

state for the six-hour sampling period. Its relationship to the

average (Hav) and maximum wave height (Hmax)

can be assumed to follow

a Rayleigh distribution as shown graphically in Fig. 8.

4.5 Extreme Wave

Besides the general description of the state of the sea

which the significant wave provides, it is of utmost importance to

coastal and off-shore operations to be able to estimate the extreme

wave height which may occur during the six-hour period. This relation-

ship has been investigated by a number of researchers (Wiege14, Ippen5

and Thom6). From their studies it may be concluded that for a recording

period of six hours, the ratio between the extreme wave height and the

significant wave height is about 1.8:1. This means that the maximum

4. Wiegel, R.L. "Oceanographical Engineering". Prentice-Hall Series in Fluid Mechanics; Chapter 9; Englewood Cliffs, N.J.; 1964.

5. Ippen, A.T. Editor "Estuary and Coastline Hydrodynamics", Chapter 3 by C.L. Bretschneider; McGraw-Hill Book Company, New York, 1966.

6. Thom, H.C.S. "Asymptatic extreme value distributions of wave heights in the open ocean. Journal of Marine Research, Vol. 29, 1971.

- 16 -

wave height can be obtained by multiplying the observed wave height,

which is equivalent to the significant wave height, by this factor.

4.6 Wave Energy

To evaluate the energy distribution and its seasonal and

directional variation over the Continental Shelf, the energy of the

six-hourly significant wave was calculated and integrated for non-

directional and directional presentation.

According to the wave theory, the energy per wave length

and per unit width of wave crest in the meter-kilogram-second system is:

1 E = -8- y Hsig2 • A • [mkg] (2)

where y is the specific weight of sea water, approximately 1.025, and

A is the wave length. In deep water, the wave length is proportional

to the square of the wave period.

A = 2- • T2 271.

= 1.56 T2 [m] (3)

where g is the gravitational acceleration, i.e. 9.81 m/sec2. Substitu-

ting this term into the energy equation, Eq. (2) provides the following

simplification:

E = 0.2 • Hsig

2 • T2 [mkg]

Over a six-hour period, i.e. for 21,600 seconds, the

number of waves which occur with a wave period T is:

- 17 -

H N = 33.3 percent Hmax.

FIGURE 8: Statistical Distribution of Wave Heights

n = 6.3600 T

Therefore the total energy per wave length and metre

wave crest for a period of six hours is:

En = 4.32 • 103 • H

sig2 • T [mkg]

In the analysis, waves were grouped with respect to

periods in intervals of two seconds; that is to say, the significant

period Taig

represents the period interval from Tsig-1

(sec) to

T+1 (sec). In Fig. 9, the relationship between the significant

wave energy (Esig)

and the energy of the entire spectrum (Etotal)

is

shown. The ratio is about 1 to 3.

Thus the total energy within a period of six hours can

be obtained by multiplying the significant wave energy by a factor of

three.

1,.....--Significant period

• —I/3E total

Etotai

sig.-1 (sec)// Tsig. (sec)

FIGURE 9: Significant Energy vs. Total Energy of a 6-hour Sampling Period

- 18 -

4.7 Grid System

A grid system, consisting of twenty-five by 21/2 degree

sectors, was placed over the area of interest. The sectors were grouped

in rows and numbered as shown in Fig. 10. They cover the Continental

Shelf to the 2000 m depth contour.

For convenience the sectors were named 'blocks'. For

each block and each six-hour time interval, the height, period, and

direction of the average representative significant wave were determined

from the published wave charts and the interpolated conditions. The

total number of representative waves for each block was 1460, covering,

as a time series, the entire year 1970.

The data were then grouped in their respective monthly

intervals, arranged for statistical purposes and the wave energy

evaluated for graphical presentation.

- 19 -

5. RESULTS

The results are presented in three ways:

(a) monthly non-directional energy distribution;

(b) monthly directional energy spectra; and

(c) monthly directional wave statistics.

It should be noted again that the energy evaluations are not

based upon the power spectra but upon the six-hourly significant wave.

5.1 Monthly Non-Directional Energy Distribution

The monthly total significant wave energy per metre of

wave crest for each block is shown in Fig. 11 and 12. The shaded areas

indicate the energy concentrations. The actual values in mkg/m can be

obtained from the scale attached to one of the blocks.

From this presentation, it can be seen immediately that

the wave energy along the Canadian Atlantic coast varies greatly with

time and location. As expected, the greatest energy concentrations

occurred during the winter months, January and December, and were,

particularly in the Grand Banks region, five to six times larger than

during the summer month of July. Thus, the energy density variation

is in good agreement and in phase with the weather and wind pattern.

More significant than the variation with season, however,

is the variation with location. With the exception of the summer months,

the energy concentration along the coast of Labrador and over the Grand

Banks was three to four times greater than over the Scotian Shelf. The

lowest energy density occurred in the Gulf of Maine. This is quite

surprising since it is known that severe damage has occurred to coastal

structures in the Yarmouth region. The reason for this may lie in

.c. I 2 3 O a0

8 POINT to DIRECTION SYSTEM WAVE HEIGHT

CODE HEIGHT - m

WAVE PERIOD

CODE PERIOD-sec.

0 0 - 0.5 <5 0 - 5 0.5-1.5 6 5 -7

2 1.5- 2.5 8 7 -9 3 2.5-3.5 10 9 -II 4 3.5-4.5 12 I I -13 5 4.5-5.5 14 13 -15 6 5.5-6.5 >15 >15 7 6.5-7.5 8 7.5-8.5 9 8.5-9.5 I0 9.5- >10

FIGURE 10: Grid System and Codes of Wave Properties

shoaling as indicated in Fig. 3. The highest energy concentration

occurred in December off the Labr ador coast, in Blocks H-7 and H-8.

Most of this area is covered with ice from February to mid-summer.

2 S r, MAY

En —m Kg / m

TOTAL ENERGY (SIGNIFICANT) PER 1 m CREST

- 21 -

FIGURE 11: Monthly Non-directional Energy Spectra; January to June

-22-

0 0 to

En —m Kg / m NOVEMBER

TOTAL ENERGY (SIGNIFICANT) PER I m CREST

FIGURE 12: Monthly Non-directional Energy Spectra; July to December

-23-

5.2 Monthly Directional Energy Spectra

These spectra are presented in the Appendix, in App. Fig. 1

to App. Fig. 12. They are plotted in groups of five blocks per page.

The energy of each block is divided into the eight point system, each

point representing the energy of the respective 45 degree sector.

The energy is plotted along the vertical axis and the wave periods

normal to it. The direction of wave propagation is along the E;1-axis

as indicated by the arrow. The periods (T), to which these energies

refer, are grouped in two-second intervals. The shaded area is the

integrated significant wave energy for each metre of wave crest. In

addition, the occurrence of these energies with respect to percentage

of time per month, is included.

The data cannot be discussed in detail because of their volume

but must be studied individually in the areas of interest.

A brief review, however, reveals the following general picture

for 1970. As already demonstrated by the non-directional energy

presentation, the energy level in January was extremely high, with peaks

primarily from the north-west and west; an exception being Labrador,

where energy came from the north and east. February and March show an

appreciable decrease, with more waves from the west and south-west.

In contrast, the following month, Aprillshowed an increase in energy

level which was experienced during the oil recovery operation from

the tanker Arrow in Chedabucto Bay (Neu7). The wave energy during this

7 NEU, H. A. "The hydrodynamics of Chedabucto Bay and its influences on the Arrow oil disaster." AOL Report 1970-6, Dartmouth, N.S.

-24-

period was primarily from the west and southwest. In the following

months, the waves decreased considerably; their direction being more

from the southwest. In the fall, the energy level started to increase

again, and in December was up to the level of January with waves from

the northwest, west and southwest along the southern seaboard and Grand

Banks. The energy from the southwesterly direction appears to be gen-

erated primarily through short but intense storms associated with

rapidly occurring weather disturbances.

In all these results, a remarkable agreement is displayed

between the state of the sea, on the one hand, and the wind strength,

direction and fetch, on the other. Where the winds are predominantly

offshore, it is not surprising that, on the average, relatively little

wave energy is transferred from the open Atlantic towards the Canadian

seaboard. Only swell with reduced energy and waves of severe weather

disturbances are usually able to enter the Continental Shelf region.

5.3 Monthly Directional Wave Statistics

The statistical analysis is also presented in the Appendix

and gives the most complete information on the sea state. Each block

contains 1460 individual wave data, each representing the 'significant'

sea state for a period of six hours. This information is grouped in

months, directions, heights, and 2-second period intervals. The number

of occurrences of a particular wave type is given numerically at the

intersection of the wave height and wave period.

The wave results of the analysis are given in App. Fig. 13

to 24.

-25-

5.4 Extreme Wave Heights

As discussed in Chapter 4.5, the ratio between the sig-

nificant wave height and the maximum wave height which may occur in a

6-hour period is about 1 to 1.8.

The wave charts of three large storms are shown in

Figures 4, 5 and 6, representing the wave conditions on 23 January 1970,

4 February 1970 and 27 December 1970, respectively. The first and the

last one were the year's most severe storms over the Grand Banks, while

the February 4th storm was the most severe one over the Scotian Shelf.

The storm of 23 January 1970 hardly touched the Scotian

Shelf. The centre of the wave field was located 600 km offshore and

extended over the southern part of the Grand Banks. In the Sable Island

area, the significant wave height was 3 to 4 m, while over the Grand

Banks it reached 10 m. The extreme wave heights were 5.5 to 7.5 m and

18 m respectively.

The storm which occurred on 4 February 1970, the day the

oil tanker Arrow grounded, affected primarily the Scotian Shelf. The

significant wave height was 7 m, and the extreme wave height in the

order of 12.5 m. Hindcasting, for the purpose of investigating the

storm during the disaster (Neu7), agrees with these figures. The storm

had little or no effect on the Grand Banks.

The storm of 27 December 1970 was similar in its wave

field pattern to that of 23 January 1970, though the December storm was

closer to the continent. The significant wave height at Sable Island

was 5 to 6 m and over the Grand Banks, 10 m. The respective extreme

wave heights were 9 to 11 m and 18 m. During the height of the storm,

-26-

an oil exploration platform near Sable Island experienced a maximum

wave height of 12 m. This is ten percent higher than reported herein

and may be caused by refraction. From these three storms, it can be

concluded that in 1970 the maximum wave height over the Scotian Shelf

was of the order of 12.5 m, while over the Grand Banks it was 18 m.

Shoaling could have caused still higher waves.

6. CONCLUSIONS

All three presentations, the non-directional energy distributions,

the directional energy spectra and the wave statistics, clearly demon-

strate the variation of the sea state along the Canadian Atlantic coast

and over the Continental Shelf with respect to time, location and

direction.

The most outstanding features are that during the winter, the

wave energy was five to six times greater than during the summer, and

the energy concentration on the Grand Banks and along the coast of

Labrador was three to four times that over the Scotian Shelf. This

latter fact indicates that the wave heights east of Newfoundland and

over the Grand Banks were, generally, nearly twice as high as those

in the Sable Island area. This ratio is also approximately indicated

by the comparision of the extreme wave heights which were 12.5 m and

18 m, respectively.

1970 was not apparently an exceptionally stormy year and it must

be assumed that a 100-year wave would be much higher, according to

probability statistics, of the order of 1;i while the wave energy would

increase by more than 2. The effect of shoaling is not taken into

consideration.

-27-

From this, it must be concluded that a structure such as an

oil drilling rig, which has been built for a design wave of 20 m, may

successfully withstand the sea conditions near Sable Island, but would

probably fail over the Grand Banks or off the Labrador coast.

Design concepts, safety standards and planning of off-shore

operations must therefore be reviewed carefully in the light of the

information submitted herewith.

7. ACKNOWLEDGEMENT

The author gratefully acknowledges the contribution of the

Maritime Forces Weather Centre and particularly that of M. R. Morgan,

the Officer in Charge. Without relinquishing the data and approving

their publication, this investigation would not have been possible.

Special mention is made of R. Walker for his untiring effort

in processing the data and preparing them for publication. I also

thank P. Vandall Jr. and others for their contributions to the project,

and E. S. Turner of the National Research Council for reviewing the paper.

11 It

ft I/

/I

It It

App. Fig. 14 a to g

App. Fig. 15 a to g

App. Fig. 16 a to g

App. Fig. 17 a to g

App. Fig. 18 a to g

App. Fig. 19 a to g

App. Fig. 20 a to g

App. Fig. 21 a to g

App. Fig. 22 a to g

App. Fig. 23 a to g

App. Fig. 24 a to g

" February

" March

" April

" May

" June

" July

" August

" September

" October

" November

" December

-28-

8. APPENDIX

The monthly directional energy spectra and the wave statistics

are given in this chapter. They are grouped as follows:

App. Fig. 1 a to e Directional Energy Spectra for January

App. Fig. 2 a to e

" February

App. Fig. 3 a to e It

" March

App. Fig. 4 a to e

I/

" April

App. Fig. 5 a to e

It

" May

App. Fig. 6 a to e

11

It

" June

App. Fig. 7 a to e

" July

App. Fig. 8 a to e

It

" August

App. Fig. 9 a to e

It

" September

App. Fig. 10 a to e

It

" October

App. Fig. 11 a to e

/I

11

" November

App. Fig. 12 a to e

" December

App. Fig. 13 a to g Directional Wave Statistics for January

0

NOTES:

I. E. • E..10-6

2. E. • 4.32•103.1,He•n TOTAL ENERGY(SIGNIFICANT)/(m CREST WIDTH IN mKgirn

3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H -*WE HEIGHT IN METRES 0. T - WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION 18 ALONG En -AXIS (SEE ARROW)

1. 91 21 El 0

1 91 CI 8 b

4 8 a la T

1 81 CI

71)

GRID SYSTEM

O

BLOCK:C2

to

s'o r

0

BLOCK:C4 4 R 12 16 T

APPENDIX FIGURE la: Directional Energy Spectra for January

1 91 Z1 8 b

N

NW

SW

55°

G

F 50°

45°

C

91 21 B

0

BLOCK:C8 4 8 12 18 T

BLOCK :C9 4 El a 16T

NOTES: GRID SYSTEM

I. Ed'• E,•10-6 2. E, • 4.32•103.7.H2.n TOTAL ENERGY(SIGNIFICANT)/1m CREST WIDTH IN mK9/m 3. n — No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H— WAVE HEIGHT IN METRES

5. T —WAVE PERIOD IN SECONDS

8. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.—AXIS (SEE ARROW)

APPENDIX FIGURE lb: Directional Energy Spectra for January

1 91 21

.L 91 8 21

NOTES: GRID SYSTEM

I. En° • En•10•e

2. En • 4.32.103•T•H2•n TOTAL ENERGY (SIGNIFICANT)/tm CREST WIDTH IN mKg/m

3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES

5. T — WAVE PERIOD IN SECONDS

6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En" —AXIS (SEE ARROW )

APPENDIX FIGURE lc: Directional Energy Spectra for January

1 91 Zi 9 9

5

rS! NOTES:

GRID SYSTEM

I. En • En.106 2. En • 4.32.103.T.H2.n TOTAL EAERGY(sioancamn/t m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES 5. T - WAvE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

BLOCK*E8

4 8 12 IS T

BLOCK : F7

4 8 12 IS T

1 91 21 8

APPENDIX FIGURE ld: Directional Energy Spectra for January

BLOCK: G8

4 8 a 16T

9

ICE COVER:23% OF TIME

5 sT 20

BLOCK: H7 4 8 12 18 T

I 2 3 4 5

NOTES' GRID SYSTEM

I. En • En010-8 2. En • 4.32•103.T•H2.n TOTAL ENERGY (SIONFICANT) m CREST WIDTH IN mKg/m

3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE

4. H- WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En -AXIS (SEE ARROW)

19.1 l 71 8

co- ICE COVER:25% OF TIME

En- • 4.

0

BLOCK : H 5 4 8 12 161

APPENDIX FIGURE le: Directional Energy Spectra for January

45

• al'

oc

0

5 0 % OCC.

4

S- o0 0

0

BLOCK :C2

4, 49

4 0

191 21 B 17

8 12 16 T BLOCK:C4

(ib 4

% OCC

*

5 20

10

4 4

0

NOTES: GRID SYSTEM

I. En • En.10-6 2. E. • 4.32.103•T412.n TOTAL ENERGYISSINIFICANT)/1m CREST WIDTH IN mKg/m


4. H- WAVE HEIGHT IN METRES

5. T -WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) T. WAVE DIRECTION IS ALONG 0-AXIS (SEE ARROW)

191 El 8

APPENDIX FIGURE 2a: Directional Energy Spectra for February

1 91 31 8 V 1 91 31

191 SI S

7 I 2 3 4 5

NOTES: GRID SYSTEM

I. Eo.• E••10-

2. E. • 4.52•103.7.1.12.n TOTAL ENERGY (SIGNIFICANT) /1m CREST WIDTH IN mKo/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES

T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Eo.-AXIS (SEE ARROW)

191 SI 8

APPENDIX FIGURE 2b: Directional Energy Spectra for February

NOTES:

1. En • En•104 E. En • 4.32••O3•T•HE•n TOTAL ENERGY (SIGNIFICANT)/Im CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 11-HOUR REPRESENTATIVE WAVE 4. 11- WAVE HEIGHT IN METRES

5. 1-WAVE PERIOD IN SECONDS

8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

APPENDIX FIGURE 2c: Directional Energy Spectra for February

8

191 El 9

9 0

10: ICE

4 8 12 18 T

0

0 BLOCK:G7

o 4. . • ••■

A- 6 8 % occ.

,o(?. •

c'o

5- zo

10

8

3 4 5

S: GRID SYSTEM

NOTE

I. En'• 2. E,, • 4.32.103.1,H2.n TOTAL ENERGY ISIONIFICANT)/t m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES e. T -WAvE PERIOD IN SECONDS 6. DASHED LINE- PERCENTAGE OF OCCURRENCES (OCC.) T. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

APPENDIX FIGURE 2d: Directional Energy Spectra for February

APPENDIX FIGURE 2e: Directional Energy Spectra for February

O

NOTES: GRID SYSTEM

I. E•*• En.10-8 2. Fe • 4.32•103.1,H2.n TOTAL ENERGY (SIGNIFICANT)/1m CREST WIDTH IN mK9/m 3 n- No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES

T -WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En -AXIS (SEE ARROW)

1 91 21 8

0

A

ICE

5- et —20

—ID

0 4 8 12 16

1 91 21 8

•

4 8 12 16 T

0 1 91 V 8 b

1 91 21 9

NOTES:

I. En.• E1010-8 2. E• • 4.32•I03•T•H2•n TOTAL ENERGY (SIGNIFICANT)/1m CREST WIDTH IN mkg/m

3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES

S. T - WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) T. WAVE DIRECTION IS ALONG Ea.-AXIS (SEE ARROW)

APPENDIX FIGURE 3a: Directional Energy Spectra for March

5

BLOCK: C6

V

.3. ire • An

Cfr PO

. 20

• •

0 4.4 4 6

I 12 16T

f§ 51*

10

•

0

Ee o 4 06 % occ. r

8 1 , 1 .

IV

40

o

Mm

-33b % ,031"

ZS ,1/40

V

(./

BLOCK : C 10

6- -20 *

0 4 e isr

191 21 8 b

a

0

10 *

NOTES: GRID SYSTEM

I. 2.• • 200-6 2. E. • 4.32.103.7412.n TOTAL ENERGY (SIGNIFICANT) /1 m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6 -HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 6. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG fn.-AXIS (SEE ARROW)

o En° VI

AS°

‘■, % OCC. I

OZ 0

g

§4

APPENDIX FIGURE 3b: Directional Energy Spectra for March

%

NOTES: GRID SYSTEM

I. En • En.110-6 2. En • 4.32.103.T.H2.n TOTAL ENERGY(SIGNIFICANT)/1 CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En. -AXIS (SEE ARROW)

co

O

'030 % '2 2 • sr

.u3

6

Li

0 % N * 5- r7

20 e ti0

-

.- . 4. w

001 loll 4 8 12 16T

•4 8 16 T BLOCK:09

1 91 El 8 0

§3

% OCC.

• co

'000 % 2 o

u 0 •,

6. VI"

4; "bo

S- 42 -20 .

t 8

BLOCK:D6 BLOCK:07 fl-rte i4 8 112 1'13 T

O 4 8 M S T

APPENDIX FIGURE 3c: Directional Energy Spectra for March

o En. to

occ ce ,

a Cr

-o • • .0 st.

1. 91 ZI

0 Lit

51* 20

10

BLOCK : D 10 1111

4 8 12 16 T

q.0 •

1 91 ZI 8 0

N

AS'

C

9

•

NOTES: GRID SYSTEM

I • E: • En.1043 2. E. • 4.32.103.7• H2.0 TOTAL ENERGY(SIGNIFICANT)/to CREST WIDTH IN mKgio 3. n - No. OF OCCURRENCES OF 6 -HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES S. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En. -AXIS (SEE ARROW)

1 91 ZI 9

1 91 ZI 8

APPENDIX FIGURE 3d: Directional Energy Spectra for March

APPENDIX FIGURE 3e: Directional Energy Spectra for March

se

F se

O AS

c

5 0

NOTES: I. En'• En.10-6 2. 5, • 4.32.103.T.H2en TOTAL ENERGY (SIGNIFICANT) /1m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES

5. T - WAVE PERIOD IN SECONDS


N

NW

SW

O

GRID SYSTEM

—10

0 014„ 4 8 IS le T

02- 22 g

* N OCC

191 ZI 9 0

O

t g 5-0

—20

EA°

4 8 12 16 T BLOCK:H7

1 91 ZI 9

0 S

0

0).

BLOCK:GB

0

uU O aP

20

• 0

4414 4 8 I. I IA T

rs

43 IP

APPENDIX FIGURE 4a: Directional Energy Spectra for April

b 1. 91 21 8

0I

02

#

4; • 6L

w

0

NOTES: GRID SYSTEM

1. En • E,,•10-6 2. En • 4.32•101.7.142.n TOTAL ENERGY ISIGNIFICANT1/1 m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES


8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En" -AXIS (SEE ARROW)

12 18 T

W • 0D

O ti t 8

5

20

10

0 4 8

El 8 b

01

02 Qv v

N,

0

a

0

0 0

4,

BLOCK : C3

4 8 12 18 T

91 El 8

BLOCK:C4 4 8 12 181

5, ••••■

,30

0 :3 0

f§ 5 _I#

o E0

,

NOTES: GRID SYSTEM

I. Ea.• En.10-0 2. E. • 4.32.103.7442.n TOTAL ENERGY (SIGNIFICANT)/1 m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H— WAVE HEIGHT IN METRES 8. T—WAVE PERIOD IN SECONDS S. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.—AXIS (SEE ARROW)

4 8 12 18 T

APPENDIX FIGURE lb: Directional Energy Spectra for April

91 El 8

NOTES: GRID SYSTEM

I. En. • En•104

2. En • 4.32.1034,142.n TOTAL ENERGY(SIGNIFICANT)/lm CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 5-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES



APPENDIX FIGURE 4c: Directional Energy Spectra for April

.3 O

01,

ID

ive

0 SS -g 84

0 A

"bo i■

tl

S 8 5 *

20

O

ICA

4 8 12 14 T

1 91 El 9

t8

1. 91 21 8 0

O

0 •

al 8

0

„pa/ .

•

P 8 8 % occ. co

CD CT,

S - • 40 0

ICE

41.

8

A

,

BLOCK : F 8 BLOCK : G 4 8 12 18 T

970 % 0

...3

%

NOTES: GRID SYSTEM

I. En • Ea.104

2. E. • 4.32.1133.7.H2.n TOTAL ENERGY (SIGNIFICANNI m CREST WIDTH IN m8g/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 0. H- WAVE HEIGHT IN METRES 6. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG E:-AXIS (SEE ARROW)

1 81 21

104

0 BLOCK : E 8 4 8 12 1sT BLOCK:F7

4 8 12 18

5- * 20

APPENDIX FIGURE 4d: Directional Energy Spectra for April

5

BLOCK : H6 4 8 12 18 T

0

191 SI B 1 91 El B

BLOCK:H8 4 8 12 16 T

GRID SYSTEM NOTES: I. En • En.10-0

2. En • 4.32•I03•T•H2•n TOTAL ENERGY (SIGNIFICANT/it m CREST WIDTH IN mKq/m

3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. 7-WAVE PERIOD IN SECONDS

8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ed.-AXIS (SEE ARROW )

191 SI 8 1 91 al B 0

APPENDIX FIGURE 4e: Directional Energy Spectra for April

kT

I 2 3 5

1 91 71 8

1 91 21 8 0

1 91 21 8

GRID SYSTEM NOTES: i. En' • E,,•10-3 2. E,, • 4.32.103.T.H2.n TOTAL ENF-FIGY(SIGNIFICANT)/1m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES 5. T — WAVE PERIOD IN SECONDS

8. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.—AX1S (SEE ARROW)

APPENDIX FIGURE 5a: Directional Energy Spectra for May

'GM % 41.

0

191 21 8 V

50.

0 .0 • Ee * % Exc. 400,

45° to

3 5

GRID SYSTEM NOTES: I. Err • 410-5 2. E. • 4.32.103.7-H2.n TOTAL ENERGY (SRUBFICANT)/I m CREST WIDTH IN mKg/m 3.* n — No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H — NAVE HEIGHT IN METRES 0. T —WAVE PERIOD IN SECONDS 8. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC-) 7. WAVE DIRECTION IS ALONG En.—AXIS (SEE ARROW)

_ S ,4P. • A* V t

-,

4!7 510

* v zo

4:0

t ,6)

O 17 • 4 1

1.0 's?,14 ev

BLOCK:CB 0

4 8 ' IA 18T

APPENDIX FIGURE 5b: Directional Energy Spectra for May

1.91 31 8 O

BLOCK:06 4 8 12 M T

I 4 5 .9•

NO S: GRID SYSTEM TE I. E,P• E„.1o6 2. E. • 4.32-103.T.H2.n TOTAL ENERGY (SIGMFICANT)/1(11 CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En -AXIS (SEE ARROW)

1 91 31 8

1 91 31 B

APPENDIX FIGURE 5c: Directional Energy Spectra for May

GRID SYSTEM

.. I 2 3 4 5

NOTES:

I. E:• 2. E. • 4.32.105.7442.n TOTAL ENERGY (SIGNIFLCANT1/1m CREST WIDTH IN mKg/m

3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ea.-AXIS (SEE ARROW)

APPENDIX FIGURE 5d: Directional Energy Spectra for May

'DO % 0 0

BLOCK:F7 4 12 18 T

1 91 21 8

BLOCK : G 7 4 8 12 181

ICE COVER: 44%0F TIME

0

0 % OCC, .40,

ICE COVER : 32% OF TIME

\ 6

8 5 $

20

Ov O

BLOCK: E8 4 8 12 18 T

191 I 8 b

N

NW

SW

O

Y e

0

o Le 0,

4. Ye °CC.

46° CO

C N

' se '030 %

O •

4".

st)

5

GRID SYSTEM NERF_S: I. En • E..10$ 2. E, • 4.32.105.1,142.n TOTAL ENERGY (SIGNIFICANTI/Im CREST WIDTH IN mK9/m 3. it - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - %WE HEIGHT IN METRES 0. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES MCC.) 7. WAVE DIRECTION IS ALONG me-AXIS (SEE ARROW)

0 0

4,

BLOCK:G8 4 8 12 16T

1 91

8

1.91 El 8

91 21 8 0

1 91 21 8 17

APPENDIX FIGURE 5e: Directional Energy Spectra for May

N 5D° H

F 50°

SW

95°

c

5

NW

NOTES: GRID SYSTEM

I. En• • En.10-13 2. E. • 4.32.1133.7•H2.n TOTAL ENERGY (SIGNIFICANT) /1 m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES

5. T— WAVE PERIOD IN SECONDS

6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ed.—AXIS (SEE ARROW)

01

0 0

BLOCK:C3 4 B 12 167

1 91 El 1 91 El 9 t

•

o En 0

02

B 01, §e 00„

V fg 'bo

11/4 5 Se

•

e 0

99

4 8 12 16 T BLOCK:C2

Cl.

191 21 B

BLOCK : C 4 4 8 a 16 T

APPENDIX FIGURE 6a: Directional Energy Spectra for June

BLOCK:C9 4 51 12 167

NOTES: GRID SYSTEM

I. Ee • 4.10-e 2. E. • 4.32. 1031,142. n TOTAL ENERGY (SIONIP1CANT)/1m CREST WIDTH IN re143/m 5. n - No. OF OCCURRENCES OF 13 -HOUR REPRESENTATIVE WAVE 4. M - WAVE HEIGHT IN METRES

5. T - WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG E.° -AXIS (SEE ARROW)

APPENDIX FIGURE Directional Energy Spectra for June

BLOCK:D6 4 8 12 18 7

1 91 21 9 tr

BLOCK: D5 4 8 12 16

NW

SW

gdersili NOTES:

GRID SYSTEM

I. En • Eo.10-8

2. En • 4.32.104.T.H2.n TOTAL ENERGY (SIGNIFICANT)/ m CREST WIDTH IN mKgim 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H— WAVE HEIGHT IN METRES

5. 7 —WAVE PERIOD IN SECONDS 6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

191 21 13 0

4

m •

• aY

En

'000 leo 0

8 432

5 42 e

V

8

• Y0\

01' C'

(b4,

0 En.

IV

V el 8

- •

0 5- at

e ry0 20 •

er-, BLOCK D7

•

4 8 1 12 18 7

91 21 9 0

00

BLOCK:D8 4 8 12 M T BLOCK:D9 4 8 12 18 7

4

I>

0 4

APPENDIX FIGURE 6c: Directional Energy Spectra for June

N

NW

SW

5

so• 0

4

* 007

0

5 04

20 .

10

0 4 8 12 16 T

N

133 S if, .74.

BLOCK: DIO

.L 91 El 8 O

01

02

191 21 9 0


030 % 0 0 4-4111. en

°

En. In

4

111.11 I ?eit 0

✓ ° 01

• 02-

g

o . 8 %licc

BLOCK:F8

8- 0

-20 •'c

-10%

• Trt 1 o 4 8 12 M T

*" OBI

8 1 91 El

0

oo • e**

cf

• )

;.

0

02 * S


4 8 12 1ST

45°

NOTES: GRID SYSTEM

I. En'• En•10-6 2. 2, • 4.52.103.7.142.9 TOTAL ENERGY (SIGARFICANT)/1m CREST WIDTH IN rnM;gm 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES S. T -WAVE PERIOD IN SECONDS


APPENDIX FIGURE 6d: Directional Energy Spectra for June

0

a oho

U

6

BLOCK: G8

\ 5- 44

20

1.11

I I

■■■■ 4 8 12 M T

If

8 1 911 2,1 I' 0 1 91 Z1

.L.9I 21 8 P

BLOCK:H8 4 8 12 16 T

o I 3 4 5 CI)

NOTES: GRID SYSTEM

I. Eo.• En'10-6 2. En • 4.32.105.T.H2.n TOTAL ENERGY (SIGNIFICANT)/1 m CREST WIDTH IN mKgim 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES

5. T - WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En. -AXIS (SEE ARROW)

APPENDIX FIGURE 6e: Directional Energy Spectra for June

O .u3

Oa

de G

84

IV

1VOCP. •

5 al

BLOCK : C 2

191 al 9

0

0? ▪ S

50' SW

E. 4.. •I -41.

45" m 0.1

C N a)

-I,- , , co * ...1906. '030 % 8 2 •zr ,.. , -,.:.

• nTii '4-11 ■ 1 '0

4..P 0/ 0 .u3

4 5 l O 15,0 1 t§

9 *

ll o 4.

b 4, 5

•- • NOTES:

I. En'• En.10-5 2. En • 4.32.103.T.H2.n TOTAL ENERGY(SIGNIFICANT)/(m CREST WIDTH IN ml4a/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES

BLOCK: CI


8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW )

O

GRID SYSTEM ati

to

APPENDIX FIGURE 7a: Directional Energy Spectra for July

NOTES: I. E.`• 2. E. • 4-32.103.7-H2.n TOTAL ENERGY (SIGNIFICANT)/Im CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES

5. T - WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

GRID SYSTEM

4 8 12 M T BLOCK:C7

8 91 El

1 91 21 8

0.> O

o En•

g % %cc

/. ti •

5

•W

O

a32- 96, • .ug

§

•

1 91 21

1 91 ZI 8

APPENDIX FIGURE 7b: Directional Energy Spectra for July

191 21 B 0

BLOCK:C6 4 8 12 113 T

43,

ay % \

S 0 0 so # • ._ .'001 .P _to

..0.1

-0 '030 % 0 2

to 0 3

590 N

0 En°

% OCC. A

07

• it

BLOCK : D7 4 8 12 16

BLOCK:D9 4 8 12 16 T

4 5

NOTES: GRID SYSTEM

I. E:• En.10-0

2. En • 4.32•103.T.H2.n TOTAL ENERGY(SIGNIFICANT)/1m CREST WIDTH IN mKgirn 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS


1 91 El 9

BLOCK: D6

4 8 12 18 T

APPENDIX FIGURE 7c: Directional Energy Spectra for July

APPENDIX FIGURE 7d: Directional Energy Spectra for July

GRID SYSTEM NOTES: I. En.• En.10-6 2. E. • 4.32.1011,142.n TOTAL ENERGY (SIONIFICANT)/1 m CREST WIDTH IN enKo/en 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES


6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) T. WAVE DIRECTION IS ALONG En-AXIS (SEE ARROW)

191 21 9

J. 91 El 9 b

ICE COVER:IO% OF TIME

0 12 16 T

191 21 9

•

BLOCK : F7

to F.5

APPENDIX FIGURE 7e: Directional Energy Spectra for July

GRID SYSTEM

1 2 3 4 5

NOTES:

I. En.• E.•10-6 2. E. • 4.32•103•T• H2. n TOTAL ENERGY ISIGNIFICANNI m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES 3. T -WAVE PERIOD IN SECONDS

8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG EA.-AXIS (SEE ARROW)

8 1 91 21

0 .113

(1,

8 6 8 1 91 21

1 91 21 8 6

ICE

VQ

e

t 8 5 *

20

0

BLOCK: H5

lop% O o AA-

3

8 12 18

167 12 4 8 4 IS T 12 a BLOCK: H7 BLOCK:H8

AD 0 % OCC. 9,

ICE COVER:21S OF TIME

d• 46. '300 % O 0

5- it q.°

0

—10

O 1TI IIII

4 8 12 10 T

8 ;lb 4,1/4

/91 El 9

-•11c:

1,\ 3 4 5

0

0 * Oct..

4

O

at 9

0

BLOCK:C4 1

4 8 121 18 T

91 El 8 0

01 • •

/ 91 21 9 b

.14 % occ.

BLOCK:C5 4 8 12 18 T

5 20

A

sr

NOTES: GRID SYSTEM

I. En"• En.10-0

2. En • 4.32•103.1,H2.n TOTAL ENERGY (SIONIFICANT)/Im CREST WIDTH IN niKa/m 3. n — No. OF OCCURRENCES OF I3-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES 5. T — WAVE PERIOD IN SECONDS

8. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Er-AXIS (SEE ARROW)

APPENDIX FIGURE 8a: Directional Energy Spectra for August

NOTES: I. E..• En•106 2. E. • 4.32.103•T•H2•n TOTAL ENERGY(SIGNIFICANT)/)m CREST WIDTH IN mKo/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 3. T -WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG 0-AXIS (SEE ARROW)

GRID SYSTEM

APPENDIX FIGURE 8b: Directional Energy Spectra for August

APPENDIX FIGURE 8c: Directional Energy Spectra for August

N

NW

SW

46°

C

5

NOTES:

I. E.'• E.•10.6 2. E. • 4.32.105.7,112.n TOTAL ENERGY (SOMFICANT)/1m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H— WAVE HEIGHT IN METRES


6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En. —AXIS (SEE ARROW )

*it

GRID SYSTEM

to°

50°

01

OS-t-G

8

1 911 0

_ ,(

'000 % 0 0

BLOOK:D6

0

BLOCK:D8 4 8 12 16 T

1 91 DI 8

01

02

a2

0 0

% OCC • 5C1

u

0 8

.330 % .111-

0

0

ci? NOTES:

GRID SYSTEM

5- 0 20

I. En" • En.10-6

2. En • 4.32.105.7.1(2.n TOTAL ENERGY (SIGNIFICANT)/ I m CREST WIDTH IN mKp/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES BLOCK: DIO 4 8 12 5. T - WAVE PERIOD IN SECONDS 6. DASHED LINE- PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

3 4

16 T

BLOCK:ES 4 8 12 T

% OCC. N

N

C' l'OC'

*.;

0 „ „ 4 8 12 16 T

APPENDIX FIGURE 8d: Directional Energy Spectra for August

APPENDIX FIGURE 8e: Directional Energy Spectra for August

GRID SYSTEM NOTES:

I. En.• E••10-6 2. E• • 4.52.104•T• HG. n TOTAL ENERGY (SIGNIFICANT) /1 m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES

S. T —WAVE PERIOD IN SECONDS

8. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG 0—AXIS (SEE ARROW)

BLOCK : H 5 4 8 12 16 T

BLOCK: H7 0

4 8 12 I6 T

• •

1 91 21 9

5- )2

-20

4'. 4-

•

g 4'0 0 1\ 4. ,t5'

0 04 4

▪

G

8+ 0/

P 0 .og •

.45),

0

1 91 21 8 V

1 91 21 8

1 91 21 9

En. o

5

NOTES: GRID SYSTEM

I. En.• 4.1045

2. E. • 4.32.103.7.112on TOTAL ENERGY (S1ONIFICANT)/tm CREST WIDTH IN mKo/m 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES 5. T —WAVE PERIOD IN SECONDS

6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCCJ 7. WAVE DIRECTION IS ALONG En1—AXIS (SEE ARROW)

•

5 20

0

0 BLOCK:CI 4 8 12 16 T

1 91 1

/ 81 8 1 91 al 8

APPENDIX FIGURE 9a: Directional Energy Spectra for September

NOTES: 10 GRID SYSTEM

I. En•• En'1043 2. En .4.32•103.T.H2-n TOTAL ENF-RGY(SIGNIFICANT)/Im CREST WIDTH IN map/rn 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES



o o % ••■•

O

BLOCK:C7 4 6 12 16

91 al 9

4 8 12 18T

1 91 Z1 8 ty

•

BLOCK:C8

/C1C5' -I • 41,

0'

BLOCK:C9 1111

4 8 12 16 T

APPENDIX FIGURE 9b: Directional Energy Spectra for September

5- -20

0

BLOCK:DS 4 8 12 16 T

8 V 191 El

8 5-# -20 17 _

411k. , 4 8 12 ~ I6T

0

•

0

GRID SYSTEM

E0 • E0•10-6 E,, • 4.32.103.T.H2•11 TOTAL ENERGY (SIGNIFICANT) /1 m CREST WIDTH IN mKohn

3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES 5. T - WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

4 8 12 M T

APPENDIX FIGURE 9c: Directional Energy Spectra for September

1 2 3

oids1111100

95.

50°

qS

C

N

NW

SW

BLOCK : DIO

4 8 12 18 T

1 91 21 8

BLOCK:F8 4 8 12 le

p.

NOTES: GRID SYSTEM

I. En.• En.10-0

2. En • 4.32.103.7442.n TOTAL ENERGY (SIGNIFICANT)/1 in CREST WIDTH IN mKq/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 3. T - WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 1. WAVE DIRECTION IS ALONG En -AXIS (SEE ARROW )

1 91 El 8

APPENDIX FIGURE 9d: Directional Energy Spectra for September

191 ZI 8

0

"330 % °

.o3

qb

a020 V

16?

BLOCK:88

<1,

0 0

4 8 12 16 T

l'oc-'" ol•

8 4 12 161' BLOCK:H7 BLOCK:H8 4 8 12 16 T

NOTES: GRID SYSTEM

I. En • En.10-6 2. En • 4.32•103•T•H2.n TOTAL ENERGY ISIGMFICANN m CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 6 -HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES


6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Er:LANUS (SEE ARROW)

BLOCK:H5

4 8 12 M T

BLOCK : H6

4 8 12 16 T

APPENDIX FIGURE 9e: Directional Energy Spectra for September

APPENDIX FIGURE 10a: Directional Energy Spectra for October

GRID SYSTEM NOTES:

I. En'• En.10-5 2. En • 4.32•103.T.H2*(1 TOTAL ENERGYISIGNIFICANTI/Im CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES



191 21 0

4 12 167 BLOCK:C4

s'o '3

% 0CC.

5 0

V 20 0 RP

• IY

• 10 ti

BLOCK:C3 0

4 S 12 16 T

4 8 12 16 T

000 %

t§

5 0 0) w

0 0

191 21 H

•03

g 1lb 5 * 0

20

4 8 12 16T

I 2 3 4

BLOCK:C9 4 8 12 16T

GRID SYSTEM NOTES:

I. E: • E. 2. En • 4.32.1034.0.n TOTAL ENERGICSIGNIFICAMTVIrn CREST WIDTH IN 014/0

3. n - Ne. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES


G. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) T. WAVE DIRECTION IS ALONG Ee -AXIS (SEE ARROW )

APPENDIX FIGURE 10b: Directional Energy Spectra for October

J. 91

1 9

F. NOTES: I. E:• En•10-0 2. E. • 4.32.105•T•10.n TOTAL EMERGY(SIONFICANT)/Im CREST WIDTH IN rnSg/n) 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES 5. T —WAVE PERIOD IN SECONDS 6. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) T.. WAVE DIRECTION IS ALONG E..—AXIS (SEE ARROW)

GRID SYSTEM

APPENDIX FIGURE 10c: Directional Energy Spectra for October

BLOCK:ES

91 I 8 4

• 0

BLOCK : F7

NOTES: GRID SYSTEM

1. En • En•106 2. En • 4.32•103.T.H2.n TOTAL ENERGY tmaric.Altrn /1 m CREST WIDTH IN mIto/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. 7 -WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En° -AXIS (SEE ARROW)

APPENDIX FIGURE 10d: Directional Energy Spectra for October

.T+

NOTES: GRID SYSTEM

I. En'• En•I0-6 2. E. • 4.32•IOO•T•H2•n TOTAL EKRI3Y(SIONIFICANTIhm CREST WIDTH IN mKg/rn 3. n — No. OF OCCURRENCES OF 0-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES S. T — WAVE PERIOD IN SECONDS

13. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ee—AXIS (SEE ARROW)

BLOCK:He 4 8 12 1:17

APPENDIX FIGURE 10e: Directional Energy Spectra for October

APPENDIX FIGURE lla: Directional Energy Spectra for November

GRID SYSTEM NOTES:

1. En.• 4•10-8

2. En • 4.32•103.7412.n TOTAL ENERGY (SIGNIFICANT)/fm CREST WIDTH IN mKo/m 3. n - No. OF OCCURRENCES OF 8-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS 8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ed.-AXIS (SEE ARROW)

8 1 91 al

••■••

% OC C . A

B

4 8 12 18 T BLOCK:C3

N NW

SW

%0

4

BLOCK :C2 4 8 12 M T

0

4 01

•

00 on

* 0c,

N

990 % ° 5... 4-

191

0

o E0 u,

oz • a ot

.r,",

0

.000 •

(0•

O °'2.2 N

5 at

20 V

/ 91 21 8 0

co

1 91 21 8

,tetr

5- * t .12 20

•

4 8 12 18 T

4 8 12 16 T

191 2.1 9 0 MI 0

02•

g

01,

1 91 El 8

BLOCK:C9 4 8 12 16 T

1 91 21 B

• 02 e1-9

0

% OCC. .413,

*030 % 2

10 .03

NOTES: GRID SYSTEM

I. E. E,..10-6 2. 8, • 4.32•101.T.H2.4 TOTAL ENERGY ISIONIFICANT)/1 m CREST WIDTH IN mKpAn


4. H - WAVE HEIGHT IN METRES


6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.)

T WAVE DIRECTION IS ALONG En -AXIS (SEE ARROW)

BLOCK: C6

APPENDIX FIGURE llb: Directional Energy Spectra for November

0 I

NOTES: I. En' • En'10-6 2. En • 4.32.103.T.H2.n TOTAL ENERGY (ZIONIFICANT) /I m CREST WIDTH IN mKp/m S. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H— WAVE HEIGHT IN METRES 5. T —WAVE PERIOD IN SECONDS S. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.— AXIS (SEE ARROW 1

1.> 0

S_ 0

20 • u;

4 8 ' 12 161

1 91 21 8 4

44> •

„p0,

/106'. '030 % nh.

.u3

So

BLOCK:D7

ti

N

NW

SW

H 55'

G

F 50°

49°

C

5

GRID SYSTEM

0

0 8 37

20

10

4 8 12 16 T BLOCK:D8 0

5-

1'91 21 8 a

APPENDIX FIGURE 11c: Directional Energy Spectra for November

APPENDIX FIGURE lld: Directional Energy Spectra for November

GRID SYSTEM NOTES: I. En.• 2. En • 4.52.103•T• H2. n TOTAL ENERGY (SIGNIFIcANT)/ m CREST WIDTH IN m14/0 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H — WAVE HEIGHT IN METRES

T — WAVE PERIOD IN SECONDS 6. DASHED LINE— PERCENTAGE OF OCCURRENCES (OGG.) 7. WAVE DIRECTION IS ALONG En•—AX1S (SEE ARROW)

BLOCK: ES 4 6 12 16 T

0

0

O 0

el SI 9

a • 0

•

O, 02

# • 5 % °c

-

c

V

BLOCK: F8

OS C, §

▪

4 .• , • .430,

ei

53

Er+ o 104 '000 %

0

0 •

BLOCK : F7 4 '1'2 ' IST

• 20

1 91 21 8

1 91 21 8 1r

BLOCK: H7 4 8 12 16 T

"DO %

DI

kru3

• 0

0 C' tt 4 )4

P3 0,

7

NOTES: GRID SYSTEM

I. E. Ele1043 2. E. • 4.32•103.T.H2.n TOTAL ENERGY(SIGNIFICANT)/fm CREST WIDTH IN mKg/m 3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. 41 - WAVE HEIGHT IN METRES

S. T - WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Ee-AXIS (SEE ARROW)

APPENDIX FIGURE lle: Directional Energy Spectra for November

0 En.

1 91 ZI 14) 0

101 m 4:ro sn

02 Nq... 4

* G O_N4

fie

0

0

t),

BLOCK:CI

5

BLOCK : C5 4 8 12 18T

NOTES: S: GRID SYSTEM

I. En • En.10-6 2. En • 4.32•103.T.H2.n TOTAL ENERGY(SIGNIFICANT)/1m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H - WAVE HEIGHT IN METRES 5. T -WAVE PERIOD IN SECONDS 6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

APPENDIX FIGURE 12a: Directional Energy Spectra for December

BLOCK:C6 4 8 I2 18 17,

NOTES: GRID SYSTEM

I. En • En•10-G 2. En • 4.32•I03•T•H2•n TOTAL ENERGY (SIGNIFICANT)/1 m CREST WIDTH IN mlio/m


4. H - WAVE HEIGHT IN METRES

T - WAVE PERIOD IN SECONDS

8. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG a-AXIS (SEE ARROW)

BLOCK:C7

4 8 12 113

BLOCK:C8

4 8 12 18 T

APPENDIX FIGURE 12b: Directional Energy Spectra for December

191 21 8 4 1 0

01

OS -

se c 8i

fat at N

20 •

4 8 12 18 T

191 21 8

.43 0

0

191 21 8

GRID -SYSTEM

I. NOTES:

E:• E..10-9 2. E. • 4.32.105.7412.n TOTAL EKTERGY (SIGNIFICANT) / m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF -HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES

T -WAVE PERIOD IN SECONDS

G. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG En.-AXIS (SEE ARROW)

191 21 9 P 0

4

Se

0 61, 4

4- G oil

'550 % 0

to

BLOCK: D6

APPENDIX FIGURE 12c: Directional Energy Spectra for December

S 50°

E

NW

J1011*- 0441000

C

191 SI 9 t,

NOTES: GRID SYSTEM

I. E.' • E..10-8 2. E. • 4.32.103.7.H2.n TOTAL ENERGY (SIGNIFICANT) /1 m CREST WIDTH IN mKg/m 3. n - No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE 4. H- WAVE HEIGHT IN METRES

S. -WAVE PERIOD IN SECONDS

6. DASHED LINE - PERCENTAGE OF OCCURRENCES (OCC.) 7. WAVE DIRECTION IS ALONG Er-AXIS (SEE ARROW

APPENDIX FIGURE 12d: Directional Energy Spectra for December

/e,

BLOCK : H6

BLOCK:H7 4 8 12 16 T

NOTES: GRID SYSTEM

I. En' • En•10-8 2. E. • 4.32•103.T.H2.• TOTAL ENERGY (SIGMFICANT1/1 m CREST WIDTH IN mKg/m

3. n — No. OF OCCURRENCES OF 6-HOUR REPRESENTATIVE WAVE

4. H— WAVE HEIGHT IN METRES

6. T —WAVE PERIOD IN SECONDS

G. DASHED LINE — PERCENTAGE OF OCCURRENCES (OCC.)

7. WAVE DIRECTION IS ALONG En.—AXIS (SEE ARROW)

$ . .i

(b` OZ

N, cb C. * -g

* Nk 4 CE■

4' P

o En* cr. A• • I c'e 6'6

A

443, ° 0 ••• 8 % occ.

1000 '330 % 8 1111111.111W • dp al 1.0 .113

APPENDIX FIGURE 12e: Directional Energy Spectra for December

1 2 1

4

a 12

NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE — IN DEGREES

H— WAVE HEIGHT IN METRES

T— WAVE PERIOD IN SECONDS.

— ONE OCCURRENCE REFERS TO A SIX HOUR MEAN

APPENDIX FIGURE 13a: Directional Wave Statistics for January

T <51 6 I 8 1 10 1 12 1 14 1>15 I 7 <5 1 6 1 8 I 10 I 12 I 14 1 >151 E

BLOCK: CI

H >10

9

tr) 8 N 7 N 1 5 ▪ 4 • 3 PI 2

>10 9

in 6

V 76 1 5

'en 4 r. 3 A 2

>10 9 8

0 cm 7 N 6 1 5 N 4 p- 3 52z

>10 • 9

8 Prit 7 N 6 I 5 in 4

71<5 1 6 1 6 I 10 1 12 1 14 I>i5 E 7 <5 1 6 1 8 I 10 1 12 1 141 >151 I

BLOCK: C3

T <S1 6 1 8 1 10 1 12 I A 1.15 E T <51 6 1 8 1101 12 1141>151 £

BLOCK: C 2

H >10

9 N 8 N (8- I 5 in 4

2

>10 9

fi) 8

1 5 'en 4 • 3 83 2

>10 9

to N 7

IS 'en 4 r- 3 D. 2

>10

fri 7

N 6 1 5 514

rci

745 1 6 18 1 101 12 1 141>15 E T<5I 6 I 8 I ioliz I t41>i5IE

BLOCK : C 4

N.

to

ro

112 5

° -1

57 5°

20

2 5°

- 24

7 5°

8,

9

g.) N

H

9 al a N 7 N 6 I 5

1,3 en 2

1

>10 9

1 5 N N, 4 o- 3 W 2 11

2 5°

-157

5°

20

2 5°

- 24

7 5°

4 3 1 9 1

1 1 2 2 3

1

22 5°

- 67

5°

112 5

° -1

57.5

° 29

2.5°

- 3

375°

2 2 1 12 10 2 9 1

1 2 1

1 2 1

4 19 4

7

2 2 6 2

in N 7

Lr) 4

N

J 5

A 32

>10 9

rs1 6 1 5

en 4 1, 3 (8 2

>10 9

in 6

N 7 6 I 5 N 4 r■ 3 5' 2

>10 o 9 ▪ B f7g, N 6 1 5

en 4 is:; gi 2

1

>10 9

in 8

0 N 7 N 1 5 N 4

3 52 2

>10 • 9

6

Pi 7 N 6 1 5

to 4

1 2 14 10 2 10 1

1 6 3 9 1

1 2 1

3 3 6 2

1 2 1 3 1

3 18 4 1

7

2

112.5

°-157

5°

202.

5°- 24

7 5°

2

5°- 33

7 5

2 64 1

1 1 1 1 2

2 1 1

1 3

2 1 1 3 1

17 16 1 7

23 4

2

2 1

1 1 1 1

3 1 1 1

2 1 3 1 8 12 1 6

1 1 2 2

1 3 2 15 14 9 1

1 5 2 3 1

1 5 3 3 1

1 1

2 2 1

NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES

H— WAVE HEIGHT IN METRES T— WAVE PERIOD IN SECONDS


APPENDIX FIGURE 13b: Directional Wave Statistics for January

71451 6 1 8 1 10 1 1 14 1.15 E 1' 451 61e110I12lKI.IME

BLOCK C5 TI45I oils 1 10I1214I.1512 71 4 51 6181101121141,151E

BLOCK: C6

1 3 1 3 1

22 5°-

67

5°

112 5

°-

i57

5°

202 5°

- 24

7 5°

rt-

112

50-1

57

5°

202

5°- 24

7 5°

H5

>10 9

N 8 N 7 ni I 5 in 4 ft: 3 2 2

I

SO 9

I 5 N 4 t- 3 ta 2

9

N7 2 6 1 5 th 4

4.) 3 2

>40 ▪ 9 w 8

7 1 5

4

Ft, :

H >10

9 ■11 8 C9 7

1

5 en 3

s0 9

N ;

(2.1 6 5

tn 4 4,3 tO 2

>10

9 ■n N 7 2 6 15

an

▪

2

9 al a

7 N 6 1 5

in 4

cri

1 3

2 2 4 7 1

14 18 1 1

2

2 1 2

1 7 1 7 10 2 6 1 1

3 1 1

1

2 1 2 1

1 2

1 3

1 2 2 4 10 1

14 16 1 1

1 4 9 2

10 7 1 3 1 1

1 2 2

1 9 6 1 6 2 2

22

5°- 67

5°

NO

N 7

1 5 tr, 4 r■ 3 u.2 2

NO • 9 ,n 8 N7 N 1 5

Fn 4

ri7-q

fr.-Tcr-i-rErr 10 1 12 1 14 >i 5 E 74516181101121141.151E

BLOCI< : C7

2 3 3

112 5

° - 1

57 5°

20

2 5°

- 24

7 5°

1

1 3 2

1 6 5 5 13 5 7 5 1 1

1 1 1 4 2 1

1 1 1

TI451 6181101121141.1511 r<51616101121141•IsIr

BLOCK C8

112

50-1

57 5°

390 9

N8 N C9 6 1 5 '64 I% 3 M2

>10 9

N8 N N. 6 1 5

1.11 4

2 32

>10 9

; 6

1 5 4

r, 3 2

s0 9

N 8 N 7

6 1 5

'N 4 1.- 3 _ 2

340 • 9 en 8

N6 I S in 4 n. 3

202

5°- 24

7 5°

1 2 4 3

2

2

1 1 1 1

8 7 1 6 4 3 2

2 1


H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 13c: Directional Wave Statistics for January

T 451.6191101121141.49 I 11<5161e1101121141.191s

BLOCK: C 9

T1<51 6 1 8 1 10 1 12 1 14 1,15 E T <S1 6 1 8 110 1 12 1 14 1.151 E

BLOCK: CIO

.10 9

NI 6 2 1 1 5 1 to 4 3 3

1 9

5 7

1 2 t-3 10 2

4 14

9 19

1 2 1

6 1 1

2 1 1

7 2 11 7 1

3 1 2

I12.

5°-1

57 5°

2

H .10

9 rn 8 N 7 cs.6

.1 5 gn 4 K 3 M 2

1125

°-157

.5°

H .10

9 al 8 N 7 Al 1

rg', 4 N 3 2 2

.10 9

3,

1 5 N 4 N 3 (5 2

T <5T 6 1 8 1 10 1 12 1 14 1.15 Tl<5 1 6 1 8 1 10 1 12 1 14 1.151E

BLOCK : D5

11.516161 101 121 141.15Z 1451 612110112 1 141.1512:

BLOCK: D6

H .10

9 3, 8 rs, 7

6

1 5 11/ 4

3 M 2

1 1 1

7 1 1 2 6

.10 9

• 1

.10 9

2

N 1 1 3 1 1 5 1 3 1 1 5 1 1 1 2 N 4 2 S 7 1 1 2 5 1 N 4 1 3 7 N 3 6 5 4 10 2 N 3 1 8 4 to 2 3 1 2 2 1 19 2 3 1 1

.10 9

N 6 8 7 N 6 1 5 to 4 N 3 '8 2

I

H2

5°-

157

5°

202 W-

247

5°

112 W

-157

.W

.10 • 9 41 8 g

6 I 5

in 4 3

rg 2

1 1 4 1

1 1 2 2 5 2 9 2 2 1

N 4 N 3 ul 2

.10 • 9

M 7 N 6 1 5 in 4

1 1 1 2 4

1 1

2 3

1

3 1

t•-•

.10 9

in 8 cm 7

cv 1 5 1

-a, 4 1 pN 1 N 3

N 2 1 4 1

202 5°- 24

7 5°

.10 9 8

N7 s

1 5 to 4 N

2

E

M 7 6 1 5

tn 4

.10 • 9 go. 8

2 1

1 1 4 1

In

.10 • 9 0. 8

6 1 5

31, 4 r■ 3 N 2

1 1 2

1 2 2

4 2 1

2 2 4 2 I -

2

2 3 5 8 1

16 19 2 2 2

1 1 2 5 1 4 1

1

1 3 2 4 1

>10 9

(7.1 6 1 5

in 4 r.,;) 3 0) 2

E

H 010

9 to N 7 N 6 1 5

rn 4 0z 3 M 2

20

2.5°- 24

7.5

°

202 5°- 247 5°

cm cm

112

.5°-

157.

5°

010 9

8

N 1 5

4 0. 3 <3 2

E

>10 9

U.) 71

.1 5 4

.10 • 9 07

ru 6

6 1 5

3 c3Z 2

010 9

rn N7

26 1 5 N 4

3 1.1 2

1

010 O 9 e

I, 3 cl• N 2

1 1 2

2 4 3 4 14 2 12 3 4 1 1

1 1 2 3

1 2 1 1

2

010 9

112

5° -

15

7. 5°

1 11

6 3 1

1 3 6 3 1

N fV ;

1 5 4

0. 3 2 1

2 4 8 1

6 14

4

2 2 4 3

1

1

1

1

1 5

1 2 2 3

10 7 2

• 1 5 1 1 1 6 1 1 3

11

2 5° -

15

7. 5°

2 1

1

5 1 1 6 1 1 1 • 4

112.5°-1

57.5

°

1.4

(N

▪

I

ppI

Nf

1 1 3

1 1 2 1 4 8 1 3 10 2 2 2 1

1

1 1 1

2 3 8

1 8 4 4 1 1

010 • 9 <1 8 V7 N g 1 5

En 4 3

ro 2

010 9

N 8 N ".6

5 in 4 r■ 3

010 9

1 5 N 4 0: 3 t02

010 9

th a

: 5

1, 4

010 9

1 1 5

th 4 1 1

1 3 7

10 4 : 5 1 1

010 9

rft a N 2 6 1 5

4

4) 3

V 7 6

1 5 4

N 3 N 2

>10 • 9

8

202 5°- 247 5

°

H .10

9 e

N 7

r! 5 in 4

(71 6

2

41

2 1 9 8 1 3 8 3 3 1

1

2 5 1 1

H

TI•c51 6 1 8 1 10 112 1 14 1015 E T <51 6 1 8 I io 1 12 1 14 1.151 E

BLOCK :D7 T <51 6 1 8 1 10 1 12 1 14 1015 E T <51 6 1 8 1 10 112 1 14 1 0151E

BLOCK: D8

71.051 6 1 8 1 10 r12 1 14 1015 E r.516151151121141,4511

BLOCK : D9 T<516181101121141015 E 71.516181101121141015 E

BLOCK: DIO

NOTES: ' — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES

H— WAVE HEIGHT IN METRES.


— ONE OCCURRENCE REFERS TO A SIX HOUR MEAN.

APPENDIX FIGURE 13d.: Directional Wave Statistics for January

20

2.5

- 2

4 7.5

°

H .10

9 th

1 5

N 61 6

u+4 7- 3

6,

.10 9

Ili 6 15 1 1 N 4 3 1 2 2 7- 3 4 8 3 3 14 (.5 2 4 3 3 7 8

2 11

2.5° -

15

7.5°

T <51 6 .1 8 1 10 1 12 1 14 1415 E T <51 615101121141.151E

BLOCK:E8

2 3 1 4

.10 9

th N 7 gl 1 5 N 4 r- 3 c' 2

410 o 9

I s Fr) 4

1"-.. 3 N 2

1 4 3 1

3

2 1 5

3 6 1 1

22

1 1 2 1

2 3 1

H .10

9 tn 8 NI 7

l'a! ( 71 7.11 6

I 5 rn 4 N 3

2 1

N 5 5

16 4 IS: 3 n

.10 9

112

5° -

157

.5°

410

e

E 7 I 5

rn 4 7., 3 6.1 2

1

T<51 6181 101 121 141.151 11451 6181 101 121 141.151X

BLOCK:F7

202 5°- 2

47.5

°

.10 9

7 N 6 1 5

'15 4 3 2 1

3 2 4 10 2 1 4 11 6 1

2 1 1 7 2 3 4 3

2

2 2 5 6 1 2

112

.5° - 15

7. 5°

T <51 6 I 8 I to 1 12 1 14 1415 E T € 5 I 6 1 8 110 1 12 1 14 I>151 I

BLOCK: F8

1

3 1

2

T <51 6 1 8 1 10 1 12 1 14 1.15 X Tic 51 6 1 8 1 10 1 12 1 14 1.151 X

BLOCK:G7

•

01

N

20

2.5°- 2

47

5°

H .10

9

'111 a N 67.6

5 tn 4

1

410 8

° lV; I 5 N 4 7: 3 t5 2

.10 9

th 8

: I 5

164

1

1 1

4 2 1

410

m6 g 7 N 6 15 514

1C1: 3 N 2

1 1 4

2

1 3 1

3 1 8

9 3

6 2 9 2 1 1/ 1

1 2 2 2 12 1 2 3 1




APPENDIX FIGURE 13e: Directional Wave Statistics for January

2 2 1 8 2 4 2 2

1 2 2 6 6 1 1

2 2 1

410 9

1 5 4

r-3 2

>10 9

fit a 01 7 61 6 1 5

'2 2

tn 4 7: 3

H .10

9

th a N 7 N 6

M 32

410 o 9 51 8

7 N6 I 5 e,) 4

2

2 6

3 5 1

1 1 4 4

4 12 2 1 4 8 4 1

1 2 I

1

3

NOTES' — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES




APPENDIX FIGURE 13f: Directional Wave Statistics for January

>10 9

ft') N 7

Ice covert

cc:. 6 1 1 1 5 2

8 1 1 2 3 fi) 4 3 9 1 2 14 e- 3 5 9 2 9 1 2 3 1 e2 2 8 1

1

258 of time t.: Ice covert 25% of time

1 en 3 NN 2 6

3 1 2

Tic 9 1 6 I 8 1 10 1 12 1 141>15 E T <sl 6 1 8 1 10 1 12 I 14 1 >151

BLOCK : G8 110 5 1 6 1 8 1 101 12 1 14 1 >15 E T <51 6 1 8 110 1 12 1 14 I >151 E

BLOCK: H5

Ti<51 618 1 101 12 1141>15 I 1o51 61 81101121141>1511

BLOCK: H6 11451 6 1 8 1 10 1 12 I 14 1.15 X T 451 6 1 8 1 10 1 12 1 14 1.151 I

BLOCK: H7

292

Y-3

37.

5°

ro

H >10

8 Ice covert 25% of time

1

Ice covers

1

25% of time

Ice covers 25% of time Ice cover.

3 1 1 7

1

25% of time

E

I 5 4

N 3 Lo 2 11

25°-

15

7.5°

22

V-6

75°

112 5°

-15

7 5°

fr? N 7 N 6

el 5 In 4 N 3

2

x

H .10

9 N 8 N 7 N6

01 4 1 1 4 2 3 1

1 3 1

5 1 10 5

6 1

48 7 N 6

1

N

▪

3 '2 2

2 1

Ice covert 23% of time

1

tD

112.5°- I5

7.5°

20

2.5°

- 24

7 5°

2


1 1 7 2 4 1


1

Ice covers 23% of time

3 1 1 8

2

Ice cover. 23% of time

1 3

2 6 3 1 2


1 2 6

•H >10

9 to 8 N CV 6 .1 5 u") 4

1.0 23

>10 9

in 8 N

67 1 5 tr, 4 N 3

2 112

5° -1

57 V

20

2 5°

- 24

7 V

29

2 5°

- 3

375°

H >10 9

111 8 N7 mr.6

5 0 4 N3 P2

I

tj 6 1 5 th 4 e- 3 • 2

>10 9

:I

N 616 15

N3 e2

I

>10

.1

• 9

1 M 7 N 6 1 5

en 4 N 3 7,, 2

>10 e 9

8

M 7 N 6 I 5 to 4 Is- 3 V N2

I

Ice covers 238 of time

23% of time

.10 9

(1 N

Ice covert

R 6 1 I 5 3 f,4 2 N 3 5 9 2 El 2 2 7 1

3

1 2 3 11

1 1

3 2

1 1 6 2 9 2

7 1

1 4 1 7 2

3 1 7 6

8 1

1 1 2

2 11 1 1 3

>10 • 9 0. N N 6 1 5

Pr) 4 N 3 61. 2

010 c 9

8

N 6 I 5

11-, 4

ri 1 4 1

2 1


1 1 7 2 5 1

Ice cover, 25% of time

1 2 6

3

3 2

1 4

1 9 4 6 1

340 9

I. 5 1174 9.: 3 M 2

610 9

e N 76 I 5 to 4 9: 3 (9 2

H

610 9

in U) Ni 7 19 8

5 1 to 4 1 7 1 5) 1 3 N... 3 2 10 2 lV 2 10 "" 2 it

6 1 2

>40

T 1 0,1 6 I 5 1 1 1 »4 4 2 rn 3 1

1.43

10 8 ni 2 1 1 1

I

T <5] 6 I 8 I 10 1 12 I 14 I >13 I Tc5I8I81101 12 1 1416151 1

BLOCK:H8

NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES

H — WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 13g: Directional Wave Statistics'for January

5 2 2 3 1

1 1 4

.51 6 1 8 1 101 121 141>15 14518181 101 121 141.151 z

H

BLOCK: C2

"2

2

2 1 1 1 1 6 4 1

>10 9

tai N..6 1 5

N 4

1

1

3

1

1 9 2

2

3 1 2 1 1 4 2 1

6

>10 9

6 7 V 6

1 5 rr? 4

w 2

1

3 3

2 1 1 8

1 1

1 S 1

1 1

T .51 6181101121141.191 T1 4 51 6 1 8 1 101 12 1 141.151E

BLOCK: C3 Ti35' 6 1 8 1 10 1 12 1 141.15 E 7 .51 6 1 13 1 10 1 12 1 14 1.151 Z

BLOCK : C 4

>10 9

tfr a

M: NN 1 5 1

1, 4 1 2 1 N 3 1 1

1 3 1 2 4 1 2 2 3 2 S 6 1 1 4 5

>10 9 e

M tv

'err.1 2

1 5 1 en 4 1 6 1 1 N. 3

2 2 N 2 2 2 1 1 1 1 1

202 5°

- 247

5°

>10 9

tile csi 7 (9 6 1 5 fr, 4 N. 3 • 2

>10 • 9 to 31 7

6 1 5

rn 4 3

it 2 1

1 2 3 1

1

2 1

1 1


H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS:


APPENDIX FIGURE 14a: Directional Wave Statistics for February

Tl<5 1 6 1 8 1 10 1 12 1 14 1>15 E 71.51 6 1 8 1 10 1 12 1 14 1.151

BLOCK: CI

112. 5

°-15

7.5°

H >10

9 tr) N1 7 0.1 1 rn 4

1 3 9 1 3 1 2 2 3 1

PA

112.5

° - 1

57. 5

°

e40 9

e lV

76 1 5 a, 4 N 3 tO 2

4 1 2 3 1

0 N

Pn

.10 e 9 In 8 31 7 6.1 6 1 5

Po 4 N. 3 cr N 2

.10 9 e

1 5 a, 4 N 3 9. 2

1

1 1 3 1

7 2 1

1 3 2 1

010 9

1 5 'er, 4 N. 3 ° 2

H >10

9 to N 7 N 6 1

fr, 4 N 3 2 2

1

to

112. 5

°-1

57.

5°

>10 9

°/ I 5 a, 4

3 '2 2

>10 a 9 tr,

IA 7 (..1 6 1 5 fn 4

if 3 N 2 1

2 1

1 1 1

3 1 1 2

10 1 3 1 3 1

2 4 4 1 2 1 2 1 1

2 1 11 6 1 2 1 1

2

1 1

2 3

6 3 1 2 1 2 1 1

1 3 2

2 1 9 5 1 2 1 1

: 2 1

ro 3

.10 9

6 8 ;

1 5 in 4 • 3 tO 2

al 8 N C\I 6 1

H >10

9

2

112

50-1

57.

5°

6 10

1 2 1

2 1 1

1 1 3 6 3

>10 9

i,8 N 7 in N 1 1 tO

2 1 5 1 1 1 2 1 2 3 N 4 1 1 1 1 3 1 3 1 r3 1 1 2 3 2 2 3 M 2 3 1 3

1 1 2

7409

e 1

1 1 5 1 1 1 1 1 g,4 3 1 1

1 2

1 3 1 r3 t02

2 11

6 1

1 2

2 1

2 3 1

3 2

112 5

°-1

57.

5°

0 9

to 8 N 7 N6 10 1 5

.1) 4 1 1 1

2 1

1 111

3 1 rn 2 1 1

>10 9

in 78 N 1 5 to 4 N 3 W 2

1

1 1 1

1 2 5 2

12 1 2 3 1

112 5

°-1

57.5

°

1 1 2 1

3 4

202.

5°-

247 5°

1 1 2 1

3

2 2

1 1 1 1

3 4

202.5°-

24

75 °

3

1 1. 3

1 1 4

1 1

>10 o 9 'n 8 N 7 cy 6 1 5

in 4 N 3

2 1

>109

toe N 7

6 1 5 to 4 n. 3

>10 9 8

0 N 1 5

4 r 3 e 2

>10 e 9 W1 8

7 N 6 1 5 tit 4 r3 ns 2

>109

N7 N 1 5 to 4 N

>10 o 9 41 8 01 7 1N1 6 1 5 in 4 1.4 3 it1 2

T<516181 101 121 141.15 E 7.516161 101 121 141>151£

BLOCK:C7 7 <5 1 6 1 8 1 10 1 12 1 14 1>15 .5 1 8 1 8 1 10 1 12 1- 14 1,151

BLOCK:C8

202

.5°- 24

7 5°

8,

1

202

5°- 24

7 5°

29

2 5°

- 33

75°

1 to 8 N 1

1 2 1 1 to 1 2 1 1 5 2 1

2 th 4 3 1 1 1 4 3 1 2 1 1 6 4 3 2 1 2 3 3 2 1 1 1 1 1

SO 9

; 1

1 1 5 in 4 1 1

1 8 1 ; 10 10 1 1 1 3

2 1 2 1

112.5

°-1

57.5

°

112 Y

- 15

7.W

H >10

9

H >10

9

h 8 N 7 N 6 I 5

in 4 'or*" 3 id 2

>10 9

• 8

11.1 8

1 5 to 4 h 3 10 2

1

1 1 2 1

1 4 1 1 2 2 3

1 1 2 7 1 10 7 2 1 2 1

>10 9

it ;8 N 7

1 5 11%, 4 r, E' 2

9 1.0 8

g 7 N 6 Is

Pit 4

'4 3 N 2

3 1 6 4 1 4

1 1 1 3 1

1

1 1

1

1 1

H

Tl<5 1 6 1 8 1 10 1 12 1 14 1.15 E T .51 8 1 8 1 10 1 12 1 14 1.151

BLOCK: C5 71<51 6 1 8 1 10 1 12 1 14 1).15 I 7 .5 1 8 1 8 1 10 1 12 1 14 1>151

BLOCK:C6



T— WAVE PERIOD IN SECONDS. — ONE OCCURRENCE REFERS TO A SIX HOUR MEAN

APPENDIX FIGURE 14b: Directional Wave statistics for February

1

7 1

2 2 1

$0 9

N 76

1 5 Er, 4 • 3 t5 2

1

s0

M 7 N 6 I 5 85 4 N it 2

2

$0 9

to 8

M N 6 1 5 N 4 pz 3 N 2

1 2 2 1 3

4 S 5 2 1

1 1

71.51 6 1 8 1 101 12 1 14 1.15 E 7 .51 6 1 8 1 10 1 12 1 14 1.151 2

BLOCK : C 9

.10 9

h

ON : 1 5

20

2.5°-2

47.

5°

a., 4

47 3 2 2 1 2

2 1 1 1 3 5 5 3 1 1 2 1 1 2 3.

112.5°

- 1

57.

5°

810 9

tV e

1 5 N 4 P 3 co 2 2

810 o 9 r 8

M 7 Ng 1 5

2

2 1 1 • 2 1

7145 1 6 1 8 1 10 1 12 1 14 1815 I T <51 8 1 8 110 1 12 1 14 18151E

BLOCK: C 10

V

1

2

112.5°

- 1

5 7. 5

.

H 810

9

h cv 7 0

2 N 1 1 5 3 &I 4 2 1 en 1 3 3 1 .nr.4 3 2 2 1 1 1 id 2 7 4 4

1

1 1 3 6 2 2 5 3 1 1 6 1 1

340 9

N N 7 N 6

5 `6)4 N 3 2 2

2 3 1 1 2 1

3 2 1 1 6 4 1

1

5 2 5 3 6

71< 5 1 6 1 8 1 10 1 12 1 14 1.15 E 7 <51 6 1 8 1 10 1 12 1 14 18151 2

BLOCK: D5

1 2

2

to

N

I 2

02

.5°-2

47. 5

°

74518181 101 121 141.151 74516181 101 121 141815

BLOCK: D6

810 9

52 6 1 5 N 4

N

4)

H 810

9

h N7 oe5 15 N 4 P.: 3 2 2

$0

e N 7 RI 8 1 5

*a., 4

4.3 3 2

1

$0 e 9

8

7 I 5 85 4 N 3 N 2

1

2 2 2 1 1

1 1 1 2

2 2 4 1 1 3 2 1

2 1 2 5 1

1 1 1

4 5 2 9 3 3 4 3

21 2 1

2

1 1

5 1

1 2

1 6 1 12 1 4 4 1

810 9

.7? 8 M 7 CV 6 1 5 854 N

2

810 9

1 5 Er', 4

3 .5 2

>10 9 8

M: 1 5 fk, 4

in 3 2

1 1 1 3 1

1 1 3. 2

H 340

9

h N 7 N

5 In 4 .' 3

2 z

1 1 2 5 1

1 2 1 1 3 2 2 1 3

1 1

2 1 2 3 1 3 1

1 2 1

2

fi.5161el101121141.15x 1.45161810112110,w2

BLOCK:D7 . T <5 1 8 1 8 1 10 1 12 1 14 1).15 I T <51 6 1 8 1 10 1 12 1 14 1.151 E

BLOCK:D8

>40 9

if) 8

; 1 5 N4

>10 e 9

N 7 N 6 I s No

v 3 N 2

H

>10 9

. 0,

11 1 5 N 4 >: 3

>10 9

N8 N 7 5, 1 5

Fr) 4 3

0 2

21

1 1 1 9 .9 8 1 1 1 2 1

1 4 1

1

1 1

1 1 3

1 5 1 1 2 1 2 3

20

2.5°- 2475°

I 12

5°-

157

5°

0 2

5 1

1 2 1

1 2 1 4 2 2 3 1 1

1 22

H >10

9 N 8 N N 1 5

1114

2 2

1 1 1 1

1 3 1 3 1

3 3

>10 9

N 8

Pi 76 1.5 N 4 H: 3 tn 2

.10 e 9 1,1 8 g 7

I s 4

612

>10 9

e 8

'(.1

1 5 fr', 4

2

1 1 2 10 1 7 8 1 1 2 1

99 R.

— a

7 11

2 5°

- 15

7.5°'

1 2 2 1

1 6 3 3 2 1 1 1

1 1 1

2 2 2

4 2

1

1 2 1 1 3

29

2.5°- 337

5°

Pn

112

5°-1

57. 5

°

pN

1 12

.5°-

15

75°

20

2Y

-247

5°

H 3.10

9

rn CM 7

5 <7 4

>10 o 9 51 V 7 N6 1 5

4

:

>10 9

15 N 4

3

1

>1Cs:

6 1 3 N 4

*2

1 2 1 1 2

1 1

1 1

1 2

1 2 1 2 5 5 5 3 3 1

3 8 1

3 1 2 2 6 2

2 1

8 4 1 6 3 4 1 3 7

1 1

1 2 1 1 1 3

1 1 2 4

2 6 5 2

2 2 1

1

3 1 1 2 6 2 1

1 2 1

>10 9

.en a

N ; I 5 N4 1 2

1 2 3 V: 3 6 6

2 2

>10 9

N 7 2 6 1 5 N4

3 51 2

>10 e 9 10 e V 7 N 6 1 5 704

3 N2

H NO

9 5

ni 7 N 6

5 <1 4

10 3 2

4,

71451 6 1 8 1 101 12 1 141 >15 X r<51 6 1 8 1 101 12 1 141.1513:

BLOCK:E8

112 5°

- 15

7 5°

202 5°

- 247

.5°

N 6 1 5

rn 4 >. 3 2 2

x

H .10

9 to N 7

.i0 o 9 ,11

NI5 5,4 1.■ 3 NI 2

410 9

rn 8 N ; I 5

11- 4

3 to 2

410 9

in

1 5 fr., 4 rt.: 3 522

1 E

4 2 1 5 3 2 10

3 3 9 2 6 8 1 1

1 1

1 1 1 3 2 4 1

1

3 1 1 1 2 3 2 1 1 2

T1.51 6 I 9 110 1 12 114 1.15 X T .451 6 18 1 10 1 12 114 1 >151 E BLOCK:F7

11 45 1 6 1 8 I 10 1 12 1 14 1415 X T <51 6 1 8 1 10 1 12 1 14 1 4151

BLOCK:G7

T1<51 6 1 8 1 10 1 12 1 14 1.15 X 11151 6 1 9 1 10 1 124 14 1.151 Z

BLOCK: F8

112.5°

- 1

57.

5°

H .10

9

In

to

A

.10 9

th 21 CV 6 1 5

'5, 4 Nz 3 e 2

>10 e 9

9 gi N 6 15

En 4

cs7,:

410 9

ai 6 1 5 g,4

2

N 7

j 5 trt 4

ICE ICE

ICE ICE

ICE ICE

ICE ICE

N 1

81

112 5°

- 1

57.

5°

225°

- 6

7.5

°

H .10

9 al 8 tse 7 N 6

5 to 4

5 >1 2

El

.109

• e ul

1 5 tn 4 It- 3 10 2

.109

roe '8 0.1 6 15 th 4 >: 3 to 2

.10 e 9 ‘r! e NT

6 1 5

Po 4

ti 32

1

2 2

1 4 1

1 5 3 2 11 1

1 1 1 1 3 2 4 1

2 2 1 1 2 5 2 3

4 2 7 2 6 9 1 1 2 1 1




Pn

APPENDIX FIGURE 14e: Directional Wave Statistics for February

1 5 en 4 ti 3 • 2

.10 9

>10

410 o 9 07 9 Pi 7 N 1 5

Pn 4 rt.: 3 V cy 2

ICE

ICE

ICE

20

2 5°-

24

7.5°

112.5°

- 1

57.

5°

ICE

ICE

ICE

ICE

•

N

k

Pr)

2 2 1 10 3 4 14 1

ICE

.10 9

to 87

1

N

ICE c=i 6 15

of 4

15 3 2

.10 e 9 d! 8 g 7 0, 6 1 5 to 4 N 5 isit 2

>10 9

e

1 5 en 4

in 3 2

1 1 1

2 1 1

1 1 1

7 3 1

1 1 1

ICE

ICE ICE

ICE

ICE

H >IC

9

e N ? 0.1 6 1 5

in 4 r. 3 2 2

U)

112

5°-1

57. 5

° 20

2.5°-

24

7. 5°

U)

N 76

ti 3 N 2

>10

9 ; 6

1 5 in 4 N 3 6' 2

.10 9

in N 7

6 1 5

en 4

:

3 2

6 1 1

2 3 12 2

3 4 1 2 1

1

2

U) to V)

112

5° -1

57. 5

° 20

2 5'-

247 5

°

H .i0

9 81 8 N 7 N 1 5 <I 4 N 3 2 2

>10

9

1 5 a, 4 r— 3 (5 2

>10

e N 7 2 6 1 5 rn 4 N 3 N 2

.10 9

7 N 6 1 5 th 4 N N 2

ICE ICE

ICE

ICE

ICE

ICE

ICE

ICE

H .10

9 tr1 e tv

‘1 5 In 4

.10 9

o 8

1 5 4

:

.109

e .e ( 1 5

11,4 N 3 8.) 2

112

.5° - 15

7.5°

202.5

°- 2

47

5°

IAf

N

.10

: g 7 N 6 1 5

11 4

4: 3 N 2

3 1 7

5 1 1

3 2 14 3

4 6 1 2

4 3 1 I

1 1 1

2 2 10 4

3 12 1

1

3 3 2

T1<51 6 1 8 1 10 1 12 1 14 1.15 1 T <51 6 1 8 1 10 1 12 1141>I51 I

BLOCK:G8 T <51 6 1 8 110 1 12 1 14 1.15 T <51 6 1 8 I 10 1 12 1 14 1.151 Z

BLOCK:H5

T <51 6 1 8 1 10 1 12 1 14 1.15 I T <51 6 18 110 1 12 1 14 1.151

BLOCK: H6 T <51 6 18 1 101 12 1 14 1.15 I 71451 8 1 8 1101 12 1141,151 1

BLOCK: H7 NOTES:

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H — WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 14f: Directional Wave Statistics for February

N 6

5 .11 4

3 en 2

3 1 7

5 1 1

to to

?r)

E

8 7 cm I 5

4 3 2

XI

>10 • 9 ▪ 8 gl7 N • I 5 b4

N2 2

in N

N

NN

4

>83 9

en e 8

6 7 .•.! 6

I 5 fr.,4 r-40

3 2

E

1 3 1 1

1 1

4 2 13 3

4 3

1

1

1

1 1 1

4 4 11 1

3 9 1

1 .1 1 2 3 2

7 451 13191101121141,15 E T14518181i01121141,451E

BLOCK: H8





APPENDIX FIGURE 14g: Directional Wave Statistics for February

3 2 4

2

1 14 4 9 2

7 4 1 O 1

112 5°-1

57.5

°

H 5110

9

IN N 6 I 5

in 4 ▪ 3

2 4 1 3

rn

H

AO 9

trt ° N 7 N 6

3 id 2

11 7 1 11 3

tr! N 6

5 N 4 N 3 co 2

AO 9

0 N 7 N 6 I 5 N4 N3

>10 e 9 qe g 7 01 I 5 I74 N 3 N 2

112 5° - 15

7.5°

rn

Pn

1 2

10 9 8 1

>10 9

1

2

2 14 3 10 2 1

1 7 4 1 3 1

5110

9

N 7

I 5 N 4 IN 3 Ia 2

>10 9 a

0 N 7 N 6 I 5 N 4 .„N 3

2

11 7 1 12 3 1

10 6 1 7 1

8) 8)

to

112.5° - 15

7. 5°

H 210

9

e N 7 N I 5

3 pH 2

H >10

9

en 8 N

I 5 to 4

1 3 1 1

1 3 9 12 2 5 1

1 / 2 3 2

>I0 9

,a0 III 6

I 5 rt, 4 1

2 N 3 2 5 1 1 2 1 1° 2 7 11 2 14 1 4 4 2 3

112.5°

- 15

Z 5°

1 4 1 1

1 1 3 2 2 2

P I 5 GI 0 N 3 N 2

rksi 81811011211415115 E T <51 8181101(21141.(51x

BLOCK:C3 T45 18! 6 1101121141,15 E T451 818110112 114IA51E

BLOCK: C4

5110

e 9 .0 9 g 7 0.1 6 I 5

4 N 3 ct 2

>10 9

c2 a 0

61 6 V

I 5 "r5 4 1

0 5 1 IN 3 ‘..) 2

3 14

5 8

8 1 1

1 5 1

4 1 1 2

>10 9

tt 6

'8' 7 N 6 I 5

ft., 4 3 2

1 1 1 1

1 1

1 1 1 1

5 3 9 1.13 2 2

T 45 I 6 1 13 I 10 1 12 I 14 1>15 E T 4 51 6 I 9 1 10 I 12 I Hi I >151 E

BLOCK:CI 11<s 16161MI 12 IMIA5E 7451 61 almlm104 1>IWE

BLOCK: C2


H — WAVE HEIGHT IN METRES. T_— WAVE PERIOD IN SECONDS


APPENDIX FIGURE 15a: Directional Wave Statistics for March

2 1 2

1

1 2 2 2

3 1 2

>10 9

in 8

c0J 76 1 5 N 4 I- 3 'I' 2

>10

cCii N 6 1 5 a) 4

14 3 N 2

X

>10 9

csi)

I 5 rn 4 r, 3 (0 2

H >10

9

I 5

'en 8 cv 1 N 6

in 4 3

K., 2

112

5°-

I57

5°

202.

5°- 2

47 5

°

2

11€51 6181 101 121 141.152 14516181 101 121 101>1512

BLOCK: C5

1 1 1 4 2 3 6 2 1 2 2

1 1 1 3 1 1

1 6 1

1 2

1 1

6 2 3 1

1 2 1 1 3 2

1 3 1

5 1 12 2 2 1 1

292 5°

- 337

5°

ir N

5,

112

5°- 15

7.5°

1 1 1 6 3 1 4 3 3 2

2 6 3 1 1

1

3 5 1

1

T €5 1 6 1 8 1 10 1 12 1 10 1.15 I T €5 1 6 1 8 1 10 1 12 1 14 1>151 I

BLOCK: C7

th

1 1 1 2 1

6 1 0 3 1 1 3 2

112.5

°-157

. 5°

1 5 N 0 r- 3 40 2

1 5

N 8 N 1 N 6

in 4

>10 9

op 8

1 1

3 3 1 2 3 1

1

112.x

-15

7.5°

>10 e 9 ul 8 V7 N 6 Is 0,4

r.4 3 IQ 2

1145 1 8 1 8 1 10 1 12 1 14 1>15 E T 451 6 1 8 1 10 1 12 1 14 1 >151 E

BLOCK: C6

rn 10

rn

H >10

9 8

cv

eI5

in 4 tri 5 id 2

>10

57 8

ck, ; 15

4 3 2 •1

• >10

e 9 10 B7 As 6 1 5

4

:

11 451 6 I 8 110 112 1 14 1>15 E T €51 6 1 8 1 10 I 12 1 14 1 3451 E

BLOCK:CS

>10 9

Es? 6

1 5 tn 4

'13 23 3 2 1

4 2 6 1 1 1

1 1 5

1 1 1

3 1 1 1

3 1 7 3 4 3 2 1 2 1

.2 2 1 1. 1

1 1 1

1 2 2 3 2 4 1

1

2 2 2

1 1 2 1 3 2 2

>10 9

in 6

N 6 1 5 in 4

N 3 ul 2 20

2.5°

- 247

.5°

>10 9

N ;

1 5 a" 4 3

>10 9

06

1 5 N 4 rz3 e 2

H >10

9

N N 1 ,s1 j 5 10 4 .1:;;; 3 id 2

>10 9 e

V7 N 6 1 5

4

0 3 N 2

1 5 3 0 2 5 2 1 1

1 1 4 2 3 3 1

2

1 1 1

2 1

1 1 ,3 1 1 2 1

1 2 1 4 1 3 8 2 2 1

2 3 8 3 2 1 1

8 2 2 1

.2 3 3 1 8 3 1 1

3 1 3 3

H 310

9 In 8 N 7 N 6

2 4

310 9

V. 76

1 5 in 4 m 3 .9 2

1

310 9

in 0 N 7 N 6 1 5 th 4 M 3 • 2

1

>10 e 9 m V7 Ng I 5 rn 4

T<5 181 13 1 101 12 1 141>15 E 7.5 1

BLOCK:C9

H

e

10 1

In

NN N

II,

1

1 6 2 6

1

>10 9

in N 7 N g

5 41 4 IA 3 2 2

2 3

2 3 1 2

1

1 3

1 7 5 1

1 1 1 1

2 1 1

1 1

310 9

1V 7 6

I S th 4 M 3 (5 2

1 3 6 2 5 2 1

1 1 3 1

2 3 1 2

1 1

3 3 1.

310 9

rf? 07 Is fh4 N3 na

2 1 1. 2 4 1 1 1

1 1

3 1

1 1 3 1

>10 e 9 tr! 8 V 7 N I9

274 M 3

1

1 1 1 5 2 5 2 2

1 1 4

2 2 2 1

61810112114 1 ,1511 TI<5I 6 I 8 1 10112 I 10 1.15 x 1.51 61 6 1 0112 1141 3151

BLOCK:CIO 2

rn

1 1 1 5

1 4 1

1125°

-15

7.5°

1 1 2 4 3 5 1 1

112

.5°-1

57.

5°

N

1 2 1

5 2 6 2 3

1 3 1 3 4 2

1

6 3 1

1 11 1

2

2 7 1

2 2

1 2 1 1 5 2 1 1 4 1

H >10

9

e N 7 Ng

J 5 O 4

2

>10 9

1 5 rn 4 M 3 8:1 2

in

11

2 5*

- 15

7 5

*

20

2.5°- 247

5°

29

2.5

°-

337

5°

H 310

9

tr1 a N ? N 6 I 5 04 My P2

In ri

112.5*

-15

7.5°

310 9

••1 N 6 1 5

fr', 4 m 3 62 2

X

>10 9

in N 7 0 6

5 a., 4 N 3 m 2

>10 e 9 tr! e V7 N 6 1 5 of 4

N 3 2

>10 9

al 7

N 15

'3, 4 M 3

2

1 4 1

4 6 3 3 2

2 4 1 8 5 1

11 1

1

6 4 2

1 1 4 2 4 7 1 3 1

5 1 1 8 5 1 1

>10 e 9

e

N 6 1 5 b4 r5 2 N2 2 2 1 2

1 1 2

1 1 7 1

2 1

1 1 1 1 7 2 1 3 -1.

2 2 11 2 3 1 1

1' <5 1 6 1 8 1 10 1 12 1 14 1.15 E 7 .5 1 8 1 8 1 10 1 12 1 14 1.151

BLOCK:D5 11<5 18181M1 12 1 141m5 E T1.5 18181M1*1i41m51

BLOCK:D6





APPENDIX FIGURE 15c: Directional Wave Statistics for March

N6 1 5 in 4 en 3 NI 2

1 2 2

2

H 510

9 a, a N

PI7 N 6 Is

4

.10 9

e 8

1 5 to 4 H. 3

>10 9

in Ht 7 2 8 1 5

et, 4 H- 3

2

>10 e 9 In

1 2 4 3 9 2 5 2 2 2

1 1 2 1 2 4 1

1

1 1 1 2 1 5 2

2,0

2.5°- 24

7.5°

r.z 2

1 1 6 1

6 3 4 3

1 5 4 2 2

1 1 2 1 1

5 2 2

2 2 I. 1

N

42

112 5°

-15

7.5°

Fr;

>10 9

to 8 N 2 8 1 5

4 3

'1.3 2 1

H >10

9 al 8 N 7 cv 6 I 5

rn 3 2

510 9

111 6

1 5 et, 4 r. 3

1

410 o 9 N M 7 Hi 6 I5 ft, 4 r3 V cv 2

1 1 3 1 2 3 1 1 1

tr)*

• N 0 N

1 3. 2 1

6 2 2

1 1 2

4 1 2 1

1 1 9 3 4 3 3 1 3

3 1 5 4 4 2 1 2

1 5 1 2 2 2 3.

1 3 2 1

1 5

H >10

9

fh N 7 • 6

to 4 r3 M 2

>10 9

6

1 5 er, 4

,0 2

>10 9

tfl 8 N

8 1 5

et, 4 1.4 3

2 1

410 e 9 ‘11. e

7 N 6 I 5 in 4

r..; 3 . CV 2

3 3 1

1 4 2 1 1

1 1 2 4 5 5 1 2 1

3 1 5 2 1 1

3 2 6 3 2

U)

en

re)

Tn

112 5

° - 15

7 5

°

>10 9

tri a lV ; 1 5 et, 4 H: 3 t0 2 11

25°

- 15

7. 5°

>10 e 9 01 a

7 N 1 5 al a I, 3 V cu 2

In

sr N

202.5

°- 247

.5°

N 7

>10 9

the

N6 1 5

1, 4 t: 3 1.12 2

1 7 1 6

2

1 2 1 2 1

2 4 3 1 1

E

H >10

9

e N 7 HW6

5 43 4

M 2 P.: 3

1 6 1

4 6 2

2 1 2 1 6 1 2 1

2 2 5 4 4 1 2 1

2 2 2 5 2 2 3.

3 1 1 2 5 1

1 4 3 6 2

1 3 2 1 1 4 1

1 2

3 3 2 3 1

1 1 2 3 3

T <5 1 6 1 8 1 10 1 12 1 14 1.15 E 7 .5 1 6 1 8 1 10 1 12 1 14 14151 2

11451 6 1 8 1 101 12 1 141.15 I 7.51 6 I a 1 101 12 1 14 14151E

BLOCK:D7

BLOCK:Da

TI.516161 101 121 14IH15 I 7.516181 101 121 14141512

7 .51 13 1 8 1 10 1 12 1 141415 E 71.51 6 1 8 1 10 1 12 1 14 1>151

TI.516161 101 121 14IH15 I 7.516181 101 121 14141512

7 .51 13 1 8 1 10 1 12 1 141415 E 71.51 6 1 8 1 10 1 12 1 14 1>151

BLOCK:DIO BLOCK: D9

BLOCK:DIO BLOCK: D9

NOTES: NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES

H — WAVE HEIGHT IN METRES. H — WAVE HEIGHT IN METRES.

T— WAVE PERIOD IN SECONDS. T— WAVE PERIOD IN SECONDS.

— ONE OCCURRENCE REFERS TO A SIX HOUR MEAN — ONE OCCURRENCE REFERS TO A SIX HOUR MEAN

APPENDIX FIGURE 15d: Directional Wave Statistics for March APPENDIX FIGURE 15d: Directional Wave Statistics for March

&.! a co 7 N 6 ICE j 5 0 4 N 3 M 2 1 3

1

1

1 2 1 4

N N N 6

1 5 4 1

N 3 2 5 2 M 2 4 1 3

1 1

112

5 °-1

57.5

°

1 5 th 4

El

1 1 1 1

11 2 1 2 1

1 1 4 1 3

1 1 6 3 1 2 2

1 5 2 4 3 1

1 1 1

T <51 6 1 B 110 1 12 1 14 1.151

1 3 1 7 1 2 2 3 1

<51 6 1 8 1 10 1 12 I 14 1.15 E

BLOCK: E8

H >10

9

ICE

>10 9

in a ;

1 5 a, 4 N 3 w 2

>10 9

re/ 5 co 7 0 N 6 1 5 th 4

ICE 5) N

ICE

ICE ICE

l 'E

>10 e 9

411 g N 6 1 5

Pn 4 r: 3 ct 2

I <5 1 6 I B 1 10 I 12 114 1.15 E T <51 6 1 8 1 10 112 1 14 1.151 E

BLOCK: F7

202.

5°- 24

75°

>10 9

ONE 7 N 6

I 5 fr) 4 1,: 3 N 2

El

T

202.

5°-2

47.5

°

>10 9

I 5 ▪ 4 ts 3 0 2

ICE ICE 5,

H

1 2 3 1

>10 9

11? a N 7 1,1'.

5 rn 4 N 3 22

ICE tO ICE

H >10

9

&I a cv 7 csi

5 5) 4 N 3 2 2

1 1 6 1 4 2 3 1 1

>10 9

1 5 ICE ICE l4

1 N 3 2 1 45 2

3

>10 9 e N

N 1 5 ICE NN

ICE 1, 4 5, 1 3 5 4 ul 3 2

1pV

2

112.W

-157

.Y

&I V. 6 I 5

th 4

.10 9

31 9 N 7

6 1 5

fb N 3 `n 2

>10 9

1125°-

157

5°

202

5°- 24

7 5°

1 2

1 1 8 3 5

1 4 1

3 1 1

>10

: 7

N6

1 5 4

I 5 al 4 N 3 .4 2

71<5 1 1 8 1 10 1 12 1 14 1.151 E 7 <5 1 6 1 8 1 10 1 12 1 14 1.15 E 71.51 6 1 8 1 10 1 12 I 14 1.151 I

BLOCK:G7

[Er 3 2 1 5 2 3 3 3 3 1 1

6 1 8 1 10 1 12 1 14 1.15 E 7 451 6

BLOCK:F8

>10 e 9

e 4,

F4 76 I5 ICE ICE

th 4 5,

H





APPENDIX FIGURE 15 e : Directional Wave Statistics for March

H >10

9 an N 7 N 6 j 5

4 3 2

1 1 1 2 2 1 3 2

610 9

the N 0 N 6 1 5 rn 4

rr;

>10 9

1 5 a, 4 r- 3 tO 2

2 1 2 4 3 1

1 4 1 1

112.5

°-1

57. 5

°

6, to to

1 1

1 1 5 2

2 2

112

5°—

57.

5°

.10 9

8

• 7

tV 6

1 5 rn 4 N._ 3

2

H 610

9

t11 8 N 7

22

5°—

67 5°

eu 4,

tla

N 6 1 5

an 4

23

ICE

1 1 1

6 5 1 4 1

ICE

ICE

ICE

ICE

ICE

>10 9

a? 7 N 6 1 5

en 4 IT 3 N 2

El

71.5 1

1

1

ICE

an

1 trt

1615 E 7 451 6 18 1 10 1 12 1 14 1.151 E

BLOCK: H5

>10 • 9

7 .4 6 I 9

11 4 3

X' 2

to

O'

aA

ICE ICE 1 3

1 3 1 1

2

1 1 1 5

1 1 1 1 2

1 2 4 1 1 1 1

H 610

9

th 8 N N 6

e! 5 0 4 N3 2 2

111 1, 1.1

610

111 :

1 1 5

; 1 5 ICE

2 2 an 1 1 2 tr) 4 4 2 1 2 1 5 1 2 2 4 1 tpH 2

1 1 1

8 1 8 1 10 1 12 I 14 1615 X 7 451 6 1 8 1 10 1 12 1 14 1.15i 114 51 8 1 8 I 10 112 1 14

BLOCK:G8 H

ICE 6,

ICE

610 9

t0 N 7

I

an

co

PR 0 4 2 1 2 1 2 5 2

122 1 2 2 1 3 1 1

>10 9

ICE

rn

an ICE

610 9

&I 1;

1 5 fh 4

V/

1

3 1 2 2 1 '8 2 2 5 1 4 2 1 2 1 1 X

610 9

al em 7

ICE N ICE 1 5 rn a, 4 1 an

1 4 lV 2 2 1 1 1 5 5

• i 2 4 1

>I0 9 8

eq 76 1 5 N 4 N 3 El 2

>10 e 9 0 8

g 1 5

an 4

71 691 8 1 8 1 10 1 12 1 N 1615 491 6 1 8 1 10 112 1 14 16191 X

BLOCK:H6 4516113110112 1 14 1615 714 51 6 I B 1 10 1 12 1 14 1 6191£

BLOCK:H7

NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 15 f : Directional Wave Statistics for March

1

1 1

2 3 1 2 1 1 5 1

>10 9

the

1 5 4

N 3 8/ 2

>10

to: N 7 6 1 5

rn 4

01*3

N 2

1 1 1 5

1 1 2 1 1 1 3.

1 2 0 1 1 1

1 3 2

S 5 1

2 5 2 1 2 1 1

2 1 4 2

2

to to

112.5°

- 15

7. V

•

NN

2 1 2 2 1 2 2

>10 9

1'71 tS 6 1 S th 4 N 3 8 2

j 5 18 4

6 /2 2

>10 9

tr) 8 Cm 7 N 6

11.051 sIaItol 12114 1 >15 I 71 m51 6 I 9 110 1 12 1 141>151

BLOCK:H8




APPENDIX FIGURE 15g: Directional Wave Statistics for March

6 1 1 12

1 4 1 7 1

2 .6 1

1 1

4 4

T 45I6181101 121 141015 E 11<51 61 B 1 101 121 141,151E

BLOCK:CI H

>10 9

al N 7

a, 4

M 2 1

112

5°-

15 7

202 5°

- 24

7

71<5 16181 101 121 81 1.15E 74516191 101 12 1 1418151E

BLOCK:C3

11451 8 I B 1 10 1 12 1 14 1015 E 7451 8 1 8 1 10 1 18 1 141.151

BLOCK:C2 H

>10 9

.1 5 117 4 Is: 3

>10 9

1 5 rr, 4 P 3 67 2

N B 1 5

',en 4 N 3 tn 2

>10

al 7 N6 15

4

71 < 5 1 6 I 8 I 10 1 12 1 NI 1.15 E 7 <51 6 1 8 1 10 1 12 1 14 1 0151

BLOCK:C4

>10 9

rfl 8 N 7

Fr1 N 7 N. 6

M 2


H— WE HEIGHT IN METRES

T1- WAVE PERIOD IN SECONDS. — ONE OCCURRENCE REFERS TO A SIX HOUR MEAN

I1 S

APPENDIX FIGURE 16 a : Directional Wave Statistics for April

4 3 1 4 1

H >it)

9 to a N 7

6 3 1 4 2

1 6 2 8 1

1 6 1

4 1 1 14

2 2 6 1

1 2 3 4 2

5 4 1 12 1

112.5

°-15

7.5°

N

rn 2

M

at

in

N

rn

N

al

2

•

r.g

>10 9

51j 6 1 5 th 4 r- 3 W 2

>10

7 K6 1 5 th 4 I- 3 D 2

>10

ft)

Si 7 N 8 I 5

07 4

'4 3 N 2

>10 9

a)

5 N 4

2

0 N 7 N 1 5 a, 4

['A

>10 9

ul 8 01 7 N6 15

en 4

N%1* N O

H >10

9 en 8 N ? N 6 rs1 6

I 5 >1 4

> en 2 7 1 1

6 6 1 12 1

18 1

5 1 7 1

2 2 2 4 3 1

4, trO

112. 5

°-1575°

20

2.7

-24

75°

1 1

2 5 1 7

2 1

3 6 6 1.

2 3 3

1 1

4 6 1 6

2

1 1 3 2

1

1 1 1

1 1 1

3 4 4 2 1

1 1 2 1

4 4 1 8 1

1 1

3 4 3 4

APPENDIX FIGURE 16b: Directional Wave Statistics for April

1 3 1 1

4 6

T 4516' 18 I 101 12 1 14 1.15 I 7 451 61 B 1 10 1 12 I 14 1.15

BLOCK:C5 71451 6 1 8 1 10 112 114 1.15 E 7 4516161 10 1 12 1 14 1 3431

BLOCK:C6

1

1 1 2

I12.

5°-1

57

5°

2

1 7 1

8,

1 2 1 3 1 2

3

1 1 1 1 4 1 S 3

1 1 1

H 3,40

9 h

7 N 6 I ,r) 4

3

2 2

310 9 8 7

1):' I 5 rn 4

t.r3 :

>to 9

o e

7 N 6 1 5 to 4 r: 3 in 2

112

5 °-1

57.

5°

292 5°

- 3

375°

H >10

9 th a

7 N 6

5 61 4

3 2 2

• 310

9 to a (21 ; 1 5

4

3 2

.10 .9

IA

15 1h 4 N: 3 in 2

.10 e 9 ,r! e

tN~ B 1 5

PA 4 3

N 2 1

1 5 1 2 1 3 1

2 1 7 7 1 1

2 1

1 2

1 1 4 1 6 1 1 1

.10

a, p1 7

2 1 5

in 4

a 3 N 2 1 1

2 3 1 1

1 2

1 3 1 1

2 1

3 2 21 1 2 1 3 1

7 8 1 1 2

1 1 3

3 1 2 4 1

2 1

1 2

2 1 1 1 1 1 7 4

1 1 3 2 1

2

71451 6 1 8 1 10 1 12 1 14 1.15 I T 451 6 1 8 1 10 1 12 1 14 1.151 E

BLOCK: C7




T 451 6181101121141.15E T 451 6 1 6 1 10 1 12 1 10 1.151

BLOCK: C8

1

3 3 3

1

2 2 4

4 1 1 1

2 1 1 6

6 2 1 4 1

1 1

1 1 1 2

H >10

9 111 5 N 7

1

.10 9

in a f. u. ; I5 rn

.10 9

15 in 4

3 ▪ 2

.10

Si 7 N 6

I5 GI 4 r3 N2

IA

112.

5.-

157

5°

a, 4

N 3 'n 2

.10 e 9

V7 N 6

8

I 5 &•) 4 ▪ 9 Xt. 2

1 5 ,n 4

;

>10 9

N

1 5

N 6 1 5

=04

H

9 in 5 N N 6

5 s", PA

2 1

si0 9

111 ; • 6

1 1 1 2 1 1 1

3 4 3 4 1 1

1 2 3

4 3 3 1

1 1 2 1

1 8 1 o 1

1 2 1 1 3 1 2 1 1 1 4 3 6 1

1 1 1 2 5

4 4 2 2

1 1 5 3 2 3 4

1 1 2 1 3

6 1 1

2 1

.1 2 3 2

1 2

4 3 2 2

x 7 51 6 1 8 1 10 1 12 1 14 1 015 /

BLOCK: C9

010 ▪ 9 81

V 7

I s Pt, 4

2 1

2 2 1

T <51 818 1101121141015

1

1 2 5 5

2 2 1 4 1 1

1

N 2

2 5°

- 67

5°

1 5 Eh 4

H $0

9 in cv 7 N 6

r. 3 2 2

1

NO 9

o8 IV ;

1 5 a, 4

3 tD 2

1

0109

toe N 7 0 NI 6 1 5 th 4

3 2 1

1 2 3 1

1 3

1 1 1 1

1 1 1 2 1

1

2 5

4 4

421

1

1 1

2 4

1

1 1 a 1 1 2

1

2 3 3 1

H 010

9 tr) 8 N 7 cv 6

ol 5 10 4 „.,P4 3 id 2

010 9

al 6 I 5 u, 4 F 3 tD 2

010 9

al 0 cv 7 0.1 6

1 5 ti, 4

in 3 in 2

010 0 el

9

1 5 a, 4 P.; 3 N 2

1 1 1

1

4) to to

3 2

1

7 3

5 2 2 1

1

1

1 1 3

1

3 2

2 4 1

4 3 1

1

In

23 1

3

1

2

3

2

1

1 1

1 3 3

1

trt

V

1 4

2 1

1

1 1

1 2 1

1

1 1

1

3 1

1 2 2

1

71051 6 1 13 1 101 121 141 >15 X 1.51 6 I B 1 101 12 1 14 1.151 /

BLOCK:CIO

T <51 6181 101 121 141015 2 T1451 6 1 61 10T12 1 14 I.151

BLOCK: D5 TI 451 8 1 8 1 10 1 12 1 14 1.15 I T 461 6 1 8 110 1 12 1 14 1.151 I

BLOCK: D6




APPENDIX FIGURE 16c: Directional Wave Statistics for April

rN

1.4

pN

1125-1

57. 5

°

e V7 01 8 1 5

a, 4 3

iru 2

H

1 1

010 9

al cv 7 Nr6

5 to 4 2

1

1 3 1

0109

N 8 IV ;

1 5 1 1 fh 4 1 2

2 1 .1 3 1 1 1 1 5 3 1 ce 2 4 3 4

4 1 1

NO 9

01 N 7 0 N6 1 5

11, 4 .1 3

2

010 o 9

112 5

°-157

. 5°

0109

N 7 Es 15

11,4

>40 9

1 5 A.) 4

3 2

H $0

9 ret N

I s N6

104

2 4

2 1 2

1

2 1 1

2 2 4

1 1 2

2 5 3 1 4 1

1

1 4 3 5 3 4 4

2 1

8 1

1 5

3 1 5

2 5 3 6 1 1 3 4

1 2 1 1 1 4 1

1 7

2

9

;}, 76

1 5 2 1 1 a,4 2 1 1

1 2 1 ti 3 1 2 1 1 6 6 2 ID 2 7 4 3 2

2 1 1 1

112.

V-1

57V

2 2 2

6 6

22.5°- 6

7 5°

11

2.5°-1

57. 5

°

ri tD

N

I

H >10

9 N oi 7 CM 6

j 5 In 4

In3 2 1

>10

1 1 2 1 1 6 1

3 2 1

2 1 1 2 1 3 1 1

9 2 2 1

2 1 2

2 2 2 1

1 2

1 1 1

1 6

3

1 2 1 3

1 1 1

2 1 1 1

3. 2

1 2 2 1 3 2 7 1 1

20

2 V

-24

7.5°

1

1 2 1

1 3

2 1 3

3 3. 1

1 2

1 1 1

20

2 V

- 2475°

>10 e 9 to

PI 7 N 6 I 5

in 4

4- 3 N 2

1 5 tr, 4

3 2

>10 e 9 1n B

I 5 b 4 1.:3 N 2

1

H >10

9

rc? a oi 7 N 6

.1 5 1,1 4

H >10

9

31 8 oi 7

2 ts.i 6 to 1 3 1 5 1 2 3

1 3 31 4 2 1 ro 2 3 4 1 1::-; 3 4 5 1 1 3 5 1 HS 2 2 3 5 1

1

>10 9

1 N 78 2

1 1 N 6 1

1 5 1 2 a, 4

3 1 1 3

6 24

3

4 5 2 tO 2 4 5 1 5 2 1 2

112.

5°-1

57. 5

°

>I0 9

• e , 113 6. I 5 a,4 r- 3 w 2

20

2 5°

- 2

475°

112

5°-1

575°

20

2 V

- 247

V

>10 9

0 N 6 Is

Ir., 4

E' 1 2 7 1

1 1 5 3

2 3 1 1 1 4 1 1 2

>10 9

ff. / N 7 (Csi 6 1 5

4

ri) 23

1 1 1

4 3

2 1 3 1

2 2 5 1

M

>10 e 9 0. B

7 N 6 I 5 in 4

7 <5 I 6 1 8 1 10 1 12 1 141>15 E 1*

>10 t. to 01 7

1 6 1 I 5 2

N 4 1 1 22

2 3

X' 2 2 3 1 2 2

1 2

1

1 1 1

<51 6I s 1 10 1 12 1 14 1.151 T <51 6 I 8 1 10 1 12 1 14 1.15 E T <51 6 1 8 110 1 12 1 14 1,151

292 V- 337

5°

H .10

9

111 5 os 7

22

>10 9

. 8

1 5 4

N 3 1.0 2

71<51 6181 101 121 141.15 / 74516181 10I121 141>1511

BLOCK:D7 71.51 6 1 B 1 10 1 12 I 14 1>15 E 7 <51 6 I B 110 112 I 14 1.151

BLOCK:De

BLOCK:D9

BLOCK:DIO


H— WAVE HEIGHT IN METRES. T— VINE PERIOD IN SECONDS.


APPENDIX FIGURE 16d: Directional Wave Statistics for April

BLOCK:FS BLOCK :G7




APPENDIX FIGURE 16e: Directional Wave Statistics for April

2

1 4 1

1 3 1 1

240 9

ej 76 1 5

th 4 3

W 2

.10 9

N 7 N 6 I 5

in 4 3

In 2

1 1 1

1 2 3

2 1 2 1

1 NN

112Y

-157

.5°

8 1 10 1 12 1 14 19151 E T1 45 1

1 1

.10 9

in 8 07

13 1 5

en 4 3

tr) 2

a-10 9 8

6 I5

trt 4 3 2

1 1

2 2 1 3 4 1 4 1 2 2

6 I 8 1 10 1 12 1 14 1915 I T 451 6 1

BLOCK: E8

1 2 2 5 9 1

1 1 2 4 2

1 2

3 2 2

3 7 8 1 2 1

1 2 2 1 1

N

T1451 8 1 6 1 10 1 12 1 14 1915 T 4 51 6 1 8 1 10 1 12 1 14 1 9151

BLOCK: F 7 H

910 9

e N 7 N 6 1 5 ICE

p.; 49 ICE

1 1 th 4 r3

2 2 1 2

910 9

in a 1,

1 tt 76 I 5 ICE ICE rr, 4 rz 3

1, N

1 1 1 W 2 1 1 1

toe

N

2 1

ti

3 2 1 1 6 2 1 1 1 2 1

.10 9

en N 7 lN 1 5 a, 4 I,: 3 tv 2 4

2

1

£

3 4

1 3 4

2 2

1

4418

9

al 7 N 6

1 5 1", 4

3 04 2

1

ICE 0'

1,

ICE

451 6 1 8 1 10 1 12 1 14 19151 E 71451 8 I 8 I 10112 114 1915 T 4 51 6 1 8 1 10 1 12 1 14 1 2451

540 9 e

0 N 7 N 6 1 5

4 rte

.3 tr, 2

910 9

'in ;

H .10

9

1°P a N 7 N 6 1 5 ai

T1451 6 1 6 1 10 1 12 1 14 1915 I T

.10 9

N6 Is rn 4

3 N 2

.1a .10

;.1 :

1 5 to 4 rz N2

a-10 9

in a ;

1 5 th 4 P 3 4:0 2

H eqo

9

e N ? N 6

j 5 1v 4 r 3 2 2

1

>to 9 e

KJ), 7. 1 5

4)2 11 4 r■ 3

ICE

ICE

ICE

ICE

ICE

ICE

ICE

ICE

1 1 2 5 8 1 1

2 1 1 1 2 2

1 2 1

ICE ICE

2 3

3 3

H

T <51 6 1 8 I 10 1 12 1 14 1.15 E T <51 6 1 a 1 101 12 1 14 1.151

BLOCK:H5

au) 9

0 a 8

EV 76 1 5 N 4 r- 3 W 2

6,10 9

N 6 1 5 4

>10 ▪ 9 Ins

N 6 1 5 11 4 a 3 N 2

1

H 340

9

13 N 7 N, 6 el 5 0 4

.10 9

Et,. 76 1 5

1.6 4 N 3 w 2

040

9

; 1 5

N3 2

112.5°- 1

57 5°

•

V

in in

Ki rel

U) 5,

010 9

6 I5 574 N3

71.51 6 1 8 1 101 12 1141.15 1 1451 6 1 8 1101121141.151E

BLOCK: H6 7 < 51 816101 121 141.15 Z 7.516181101121141.151E

BLOCK:H7 NOTES:

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 16f: Directional Wave Statistics for April

3 1 1

1 1

2 3 1 2 2

1 0 2

1 7 2

4

1 1 1 1 1 2 3

2 6 S 2

1 1

1 3 1 1

112.

5°-1

57

5°

>10 • 9

N6 1 5

a, 4

V 3

N 2

04

to N 7 N ,!

16; 3 M 2

.190

11i 16 1 5

in 4 3

W 2 1

.109

Fp 0

N 7 8

I 5 11,4 N in 2

TI .c 5 1 6 1 8 1 10 1 12 1 14 1.15 I T <51 6 1 8 1 10 1 12 1 14 1.151 2

BLOCK:68

H 340

9

1 1

2 2 1 1 8 1

1

1 3 1 1 2 1

3 2 2 1 2

H 240

9 a) cU N I 5 0 4 N 5 IR 2 ty

112

V -

157.V

2

1 6 4 1 2 1

ICE

ICE

ICE

ICE

ICE

1 4 2 1 1

1 2 2 3 1 2

ICE

ICE

ICE

2 1

1 1 1 3

7 2

1 1 1 3 3 1 2

4 7 5 2 1 4

1

1 4 1 3

1 2 2 1 1

ICE

ICE

ICE

ICE

2

4 1

2 2 1 9 2

>10 9 0 a

1 g in 4

:

>10 9

13

1 5 a., 4

X

>10 9

in 9 N 7

6 1 5

fe, 4

trZ;):

>10 • 9 0 6

7 N 6

1 •

1 5 5 1 to 4 1 2

N 3 2 4 1 2 3 1

a

7 <51 6 1 8 1 10 1 12 1 141 >18 E

4 2 3

1 3 1

1 2 3 3 1 5

1 7 6

1

1 7 4 1 3

N N 6

1125

°-1

575°

4,

NN

N

in

ro

71451 6 1 8 1 10 1 12 1 141>131 E

BLOCK: H8



— ONE. OCCURRENCE REFERS TO A SIX HOUR MEAN

APPENDIX FIGURE 16g: Directional Wave Statistics for April

112V

-157

.5°

3 2 2

T5 5, 4 N 3 ■1) 2

110 9

in 8

15 a, 4 N 3 el 2

4 1

110 9

! 1 5

4 N 3 `n 2

: 1

4, N

N

110 e 9 Lc) 8 N7 N 6 1 5

Pn 4 1", 3 N 2

10 4 1 1

U.)

2 2

10 2 2

1

>10 e 9 III N T N 6 I5

Pn 4 N 5 N

1 1

10 3

202.5

- 2

47.

7451 6 1 8 110112 1141.15 I 71<51 6 1 8 110112 11411151 z BLOCK:CI

71.01 8 1 8 1 10 1 12 1 14 1115 E 7 <51 6 1 8 1 10 1 12 1 14 11151

BLOCK:C2

H 110

9 !

Nr

.50 9

I a

M

110 9

in N 7

110 9

N 87 V 6 1 5

in

N

In tO




APPENDIX FIGURE 17a: Directional Wave Statistics for May

110 9

N 8 fV : 1 5 '- 4 N 3 0, 2

>10 9

fr.> 6 N7 86 1 5 5,4 N3 e2

>10 9

N7 N 6 1 5

N 3

H 110 9

rn N 7 N I 5

1114 N 3

2

E

3 2

7

2 6 2

1 3 5 9 1

19 2 2 2

T <51 6 I9 1 10 112 1 14 1115 E T<51 6 1 8 1 10 112 1 14 11151E

BLOCK:C3

2 1 3 1 1

1 3 1

<51 6 1 8 1 10 112 1 14 1.1511 71.51 6 1 8 1 10 1 12 1 14 1.15 E 7

BLOCK:C4

1 4 2

112.5

° - 15

7.

112 - 1

57. 5

°

fro

H 1(0

9 ih 8 NI 7 N6

1 3 M 2

>10 9

in 8

15 5) 4 N 3 t0 2

.10 9

; I5

4

mo 96 Ein

6 15

1.) 4 N 5 N 2

2 2 1 4 11 2 1 1 15 3 3 2

5 3 7

1 1 3 1 2 3 3 1

1 1

4 2

5 3

2 5 2

15 6 2

3

1

in

2 1 1 2 1

12 3 19 4 3 1

N 6 5

117 4 3

2 2 11 6

5 2 2

2 1 18 9 2 1

2 1 12 1

1 1 2 1

1 8 3

7410

9 to oi 7 .... 1 5 g, 4 r: 3

UI

1 rn

202

5°- 247

.5°

H .10

9 u,8

1 5

N 7 N 6

lb 4 5 2

MO 9

in N 7 0 N 1 5

a, 4 3 2

.10 e 9 4't g N 1 5 al 4 r: 3

2

H

9 fn 8 oi 7 N

M 2

5 .7 4

5

7410

9 ! 6

1 5 a, 4 r- 3 to 2

.10 9 8 117

N 7 gi 6 1 5

I}, 4 3

4' 2

.10 • 9 41 8 M 7 N 6 1 5

4 r: 3 ol 2

1 3 2 9 4 3

6

1 4 1 5 1

5 1

2 2 2

3 2

1 1 1 5 1 2 3 2

24 2

1

5 2 1 5 3 1

24

2 2 1 1

10 4 1 1 4 7 1

1 2 3 7 3 1

1 1 1 2 1. 5 1

2 1 1 5 1 1

6 1 10 1

1 2 1 1 6 1 2

3 3

4

1

ru

tf) 1

N

N

Pn

`0

▪

. yyI

NN

H .10

9 th N 7 N

J 5 5

2 a

7410 9

a ;

1 5 al 4 r-to 2

.10 9

h N 7 N 6 6 1 5

4 N 3 el 2

>10 • 9 6? 8

N

N 8

1 5 814

3

H .10

9

N 7 N 1 al 4

5

5 M 2

7410 9

11? 1 6

I 5 11.) 4

.10 9

7 N 6 15

1, 4

7410 e 9

8

g 15

11 4 1:4•-: 3 ni 2

1 4 6 2 9 1 2

1 1 11 3 1

7 1 1

2 5 1 1 1

2 3 8 S 1

1 3 2 1 2

1 1 3 2 3

2 3

1 1 3 9 3 6 3 1

10 2 2 1 7 2 1.

1 3 3 6 5 2

6 2 4 3

6 7

1 2

2

1 5 1 3

1 1 1 2 2

T 451 6 1 8 110 1 12 114 1.15 E 71451 6 1 8 1 10 1 12 1 14 174151 2

BLOCK: C5 714516181101121141.151 7 4 516181101121141.151E

BLOCK: C6

T 451 6 1 8 1 10 1 12 1 14 17415 X 71451 6 1 8 1 10 1 12 1 14 1.151 X

BLOCK: C7 71 4 5 1 6 1 8 1 10 1 12 1 141.15 I 7 4 51 6 1 13 1 10 1 12 1 14 1.151

BLOCK: C8 NOTES:

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 17b: Directional Wave Statistics for MEW

H

9

in

H .10

9

0 7 N N6 tD

I s j 5 N4

1.0 4 1

15

1 3 4

In 4 N 3 2 2 2 1

4 1 10 1 1 5 1 1

,90 .10 9 9

if3 *1 8 7 V 6

15 I s 1 11,4 1 2 IN 4 1 2

2 1 2 2 1 3 3 2 0 2 3 3 2 1 1 9 2 2 1 W2 7 2 2 2

3 1 2 1 1 3 1 I

.10 9

tr1 w 7 2 6

1 5 N 4 N 3 52 2 3

4

3 2 1

1 1

3 5

1 1

.0 9

g* 7 0 6 15 N4 N3 0 2 1

4 4

3 2 4

1

I 12

5' -15

7. 5

°

1 4 1 4 5 2 9 2 2

1 1 3 1 8 6

13 1

2 1 7 2 2 1 3

2

.10 .40 • 9 tn e

g N 6

1.14 V7 0.1 6

I 5 Is GI 4 b4 N 3 3 N 2 1 2 0.12

3 1 1 1 3 2

491 6151101121141,05 E T45I 6151101121141>1512

BLOCK:C9 T195I 8 1 8 1 10 112 1141>15 E T 951 6 I 8 I 10 1 12 I 14 1.151

BLOCK:CIO

112.5*-1

57

5°

qN

H

?s,

,90 9

th 0 7 0 N.6 PA J 5 1

1 3 1 1 7 2 9 5 3 8 3 1 4 5

H .10

9 N6 0 7

6 S

N4 1 3 2

I

1 1

3 1 3 2 1 2

4 2 5 1 2 1 5 3

8,

112.Y

-15

7.W

>10 9

"l 411 6 I 5 N 4 N 3 15 2

1

5 3 1

1 2 1 4 4 1

2 1 5 2 1

'11 6 I 5 N 4 N 3 '5 2

.10 9

h 8

0 N 7 N 6 I 5 N 4 N 3 12 2

.10 • 9 0.

7 N 6 I 5 h 4

v 3 3 0 2

.10 9

• to e7

8 1 2

1

1

110 9 8

15 N 4 N 3 52 2

4 1

11 1

tn

3 2

2 1 2

3 3

510 9

91

V 7 Ng I 5 N 4 9: 3 V cy 2

1

1 1 2 3 3

I

•

V

yyI YS

r•O'

Tpc51 6 I 8 1 101 12 I 14 1,95 I 7 <SI 6 18 I 10 112 1141>151 X

BLOCK:D5 71551 6 18 I 101 12 1 14 1.15 X T 961 6 18 I 10 1 12 I 0 1.01

BLOCK:D6



— ONE OCCURRENCE REFERS TO A SIX HOUR MEAN .

APPENDIX FIGURE 17c: Directional Wave Statistics for May

6 6 2

2 2 1

3 2 1 4 2

43 2

1 7 1 1 1

1 4 12 1 6 3

6 9

4 1 4 1 1 7 1 1 1

1 1 2

In to

hI

112.5

° -

157.

5°

202.V

. - 247

5°

3 1 3 1 6 3 3 1 4 2

1

S3 1

4 7 4

10

3 3

1 2 7 4 1 1

1 2 2 5 1

In

PA

112

- 15

7. 5°

H >10

9

al N N 6

h 4 N:3 M 2

>10 9

2i? 67I

I 5 6 4 N. 3 w 2

H .10

9 al N 7 61 6

>10 9

111 6

I 5 fr., 4

>10 9

NI 13 I 5

4

512

Si 7 N 6 '5

11 4

:

j 104 .z 3

g

>10 e 9 e

.10

N 6 1 5

P-, 4

a 3 N 2

1 S 5 2

1 2 4 6 2 9 2

1 2 1 1 1 6 4 1 1 5 2 1

1 2 1 13 1 2 1

3 2

H

V7 N 6 1 5

.h 4 i■ 3 N 2

0 N 7

1 5 64

3 2 2

• 9 'n 6

>10 9

th

,1 5 64

1023

N 7 N6

.10

ti

1

0: 1 3 5 2 7 3

>10 9

et

N

1 5 6 4

.10 9

0 N7 N6 15 N .)

I 5 114 N: 3 N 2

21

>10 9

rc.1,73

112.

5°-1

57.

5°

I 5 to 4 rs w

3 2

4 9 1 9 2

2 3 2 2

1 3

4 3 8 2 1

1 8 1 2 2 6 3

6 1 10

2 1 2025°- 247

5°

2 5 1 1 5 1

4 2

N

202.

5°- 24

7.5°

<S1 13 1 8 1 10 1 12 1 141>15 2 11 4 51 8 1 8 1 10 1 12 1 14 1.151 2

BLOCK:D7 11 4 5 1 6 I 8 r 10 1 12 1 141>15 2 T <51 8 1 6 I 10 1 12 1 141>1311

BLOCK: D8

451 6 1 8 1101 12 1 141>u E 71 4 5 I 6 1 8 1 10 1 12 1 141>151 t

BLOCK: D9 71.51 6 I 6 '10 I 12 I 141.15 E T 451 21211011211413.121

BLOCK:DIO NOTES:

— DIRECTION INTO WHICH WAVES PRORAGATE— IN DEGREES H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


tQ

APPENDIX FIGURE 17d: Directional Wave Statistics for May

1 3 8 1 6 1

.10 9

6 N 7 oi I 9

1? 4 ICE

5 2 8 4 4

5 1 1

1 1 2

.10 9

rn (71 `4 6 I 5

rb 4 N 3 55 2

ICE

112.5.

-15

7.5°

N

N N

N

>109

• 9

1 2 1

1 8 6 2 1

2

1 1 1 2 4

E3178

1 5 4

r- 3 W2

1

>109

oi 7 N6 I 5 N 4

E

>10 9

9•2 a

N7 N 9 1 5

in 4 1`... 3 V N 2

ICE

112

5°-1

57.5

°

0" N s 1 5 'lb 4 o: 3

2

>10 e 9 rn 8 N7 N 1 5 in 4 o: 3 N 2

ICE

ICE

3

3 3 1

2 5

ICE

ICE

ICE

ICE ICE

>10 9

trI N

1 5 a, 4 7- 3 '5 2

7

1 9

2

1 4 3

7 8 6

6 1 1

1 1

ICE

>10 9 e Ni

RI 6 1 5

N3 "5 2

1 1 6

1

1

2

X

1 1 4 3 6 1

112.5

°-

157

5°

202

5°- 247

5°

>10 • 9 11 9 N7 N 6 I 5 rn 4 dr 32 29

2 5°

- 3

375°

H >10

9 ,n 8 os 7 N 9

5 0 4 .

3 2 2 6 1 3

H .10

9

rfl e N 7

in 4 7- 3

.40 9

• 8

CI' 6 I 5 tr, 4

3 '15 2

N7 N

I 5 rb 4

>10 9

10 8

1 5 to 4 N 3 N 2

I

112

5° -

157

5°

N

N

pN

292

5°- 337 5°

ICE

ICE

1 23 2

1 5 3 1 1

ICE

ICE

ICE

ICE

H

T<5 16181 101 121 141.15X T14516161161121141,451X

BLOCK:GS 11.5 1 6 1 8 110 1 12 1 14 1>15 I T >51 6 1 8 1 10 1 12 1 14 1.151

BLOCK: H5

T <51 6 1 8 I 10 I i2 I 14 1.15 E T1<51 6 I 8 I 10 I 12 1 14 1.151 E

BLOCK: H6 NOTES:

71.51 6 1 8 1 10 I 12 1 14 I 2.15 X T <51 6 1 9 I 10 1 12 1 14 I .15i

BLOCK: H7

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES

H — WAVE HEIGHT IN METRES.


APPENDIX FIGURE 17f: Directional Wave Statistics for May

3 9 1 1

>10 9

th

c-v- 67 1 5 N 4 es 3 to 2

>10 • 9 to 9

if+ 7 NI 6 I 5

to 4

'7.7;

>I0 9

to 6 NO 7 N 6 1 5 to 4

3 2

H >10

9 in 8

1 5 111 4

N 7 N 6

tiri 3 01 2

1 1

10 7 1 8 3

3 1

2 2 10 1

20

2.5

°- 247 5°

112.5°

-15

7.5°

22

.5°- 67.

5°

71.51 6 1 8 I 10 112 1 14 1.15 I 71 4 51 6 1 8 1 10 112 1 14 1.151 Z

BLOCK:E8

2

2

1 3 1 2 6

11 1 1

H >10

9 al 8 of 7 ,%1 J 5 47 4 ri 3 id 2

Ice coves. 44% of time

27

Ice covert 44% of tire

1 1

3 4 1 3

>10

>10 9

r e N - 6 1 5 N 4 ez 3 ED 2

gi 6

>40 9

N a N 7

1 5 in 4

"' 3 2


2 3 3 1

.11 : e 0

7 tg

6 id I5 I

0) 4 al r.: 3 gri 2

1 E

Ice covers 44% of time Ice clovers 444 of time

2

In ti 10

112 V

-15

7. V

N


6 2 6 1


1 1 1 3 7 5 1 1





APPENDIX FIGURE 17e: Directional Wave Statistics for May

T 491616 I 10 1 12 1 141>15 I 71 431 6 1 8 1 10 112 1 14 13451 r

BLOCK: F8


1 2 2 1 6 2 1


1 1 2 4 4 1 1


1 1 2 2 3


3 7 2 8 1 3 3 1

1 1


11 2


3 2

1 2

>10 ▪ 9 In 9 to

1 5 I a, 4 ez 3 Nsr 2

1 I


In

7.011318 1101121141.15 E 7 451 8181101121141.151E

BLOCK:G7

>10 9

NC)* 78 e 1 5 N 4 rz 3 w 2

I

In se se

gi

112

.5°-1

57.

5°

H >10

9 N 8 tv 7 N I s h 4 >1 3 2 2

>10 9

o e N 7 N 6 1 5

11, 4


1 1

5 7 1 6 3

1 3 6 1 2

>10

67 I 5

Po 4 1.z 3 N 2

H >10

9

N 1 5 to 4 e4 3 M 2

1

>10 9

; 1 5

a, 4 e- 3 tO 2

I

>10 9

rit a ;

1 5 rn 4 rz 3 w 2

1

2 2 9 1

2 1

men

N

‘17

1

112

V -1

57.

V

4

1 3 1

4 7 12 1 1

71 4 1 6 1 8 1 10 1 12 1 14 1 .15 £ T 8 1 8 1 101 12 1 141.15 3 451

BLOCK:F7

2 1 5 2 1 1

1 2 4 2 5 1

1 7

2 8 1 1 3 1

1 1

1 9 0 1

3 1 1 3

2 2 1 2 3

H

0

en

N N

V

1

pN

>10 9

■A 8 cv 7 N 6

3 2 3 7 1 3

.10 9

N 8 DI 16 I 5 3, 4 N 3 to 2

N 7 6 1 5

GI 4 N 3 N 2

.1 5 07 4

M 3 07 2

Tcsle le I 1011211417.15 E r<5161511011211413.1512

BLOCK: H8




APPENDIX FIGURE 17g: Directional Wave Statistics for May

>10 9

&) N N I 5

lb 4

to to

>10 9

al 6 N 7 N 1 5 an 4

3 3 3 1 2

24 2 2 29 11 2 20 3 1

.10 .10 9 9

rn t}1 :

al 6 T5 1 5

4 4 N. 3 W 2 1 1

1, 3 'D 2 1

14 1 1 3 1 13 11 1

.10 9 e

N7 E 16 N 4 rz 3 ° 2

2

>10 9 B

N 7 N6 16 rn 4 rz3

2

010 9

7 6 1 5 GI 4 ...1•4 3 t3.I 2

.40 e 9

g N 6 I 5 en 4

R

1 1

1 2 1 8 2

2 1 1

2 1 1 1

2

112

.5°-15

7.5°

tD

112

5°-I5

7. 5

°

NN

In

1 1 1

1 2 2 1 5 1 2

3 1 25 12 1

3 1

1 4 1

2 1

2 1

6 2 1 4 2

3 1

2 2

6 6 i 30 9 1 2

3 1

112V-1

57

5°

202 5°- 24

7 V

112.5°-1

57.V

2

02

.5°- 24

7. 5

°

90

2

>40 9

I 5 fk, 4 P 3 (.0 2

>10 9

th 8 N 0 N I 5

in 4 3

2 2

>10 • 9 ,11 5

7 N 8 1 5

rn 4 1;i 3 N 2

.40 9

ih 87

1 5 N 4 ts: to 2

.10 9

8 NN I 5

'en 4

2

.40 9

0. 8

I 5 rn 4

1 1

2 2 11 3

J. 1

1

1 2 13 3

H

H

T1.51 616 1101121141.15 I 145I 8 I B I 114 141.4512

BLOCK: C I T<5161131101121141.152 1•<5141611011211413.1512

BLOCK: C2

Ti<51 6 1 8 I 10 112 1141.15 2 T <51 8 1 8 110112 1 14 >151 I

BLOCK: C 3 71 ..5 I 8 I 8 1101 12 I 14 1.15 2 T <51 6 I B 1 10 1 12 1 141.151

BLOCK: C4




APPENDIX FIGURE 18a: Directional Wave Statistics for June

1 1 6 2 2 9 1

11 2 7 3 2

; 2

1 2 1 6 6 25 4 4

1 3 3

H >10

9

1 2 2 7 2 2 7 1 1

2 1 2 1

2 1 2

1 1

1 2 9 7

24 4 2

4 2

N

112 5

°-1

57.5

°

to a Ni Rs

• 9 e

N7 N6

1 5 an 4 rz 3

2

>10

202.

5°- 2

47. 5

°

NN

tn

1 5 in 4 N 3 RI 2

>10 9

in N 7 N a

j 5 N 4

M 3 2 1

>109

in 8 0 N 8 1 5 a, 4

N.3

2

N7

>10

Ng

N6 I S

in 4 rA 3 ro 2

.10 9

N 8 t•-1 76

tO

1 5 tb 4 n3

112.5

°-15

7.5°

rn NN 1,

to

112.5

°-15

7.5°

N

1

H >10

9

*1 8 7

N 6 ; 5 in 4

2 1

.10 9

in .1

1 5 N 4 H. 3 1.0 2

>10 9

N7

6 1 5 a,4 N 3

2 1

>10 • 9

a IN 7 N 6 1 5

in 4 3

N 2

H >10

9

in 6 N 7 N

1 1174

M 2 1

>10

N

76 1 5 in

2

.109

in 8 N 7 R 1 5

*a, 4 N 3 N 2

zt

>10 . 9

M 41/41 6 I 5 0-) 4

3 2

1

1 1 1 1 1

13 1 3 1 2

2 1 2 8 10 3 13 1 1

5 8 4 9 4

1 2

3 2

2

3

2 2

1 1 1 11 2

3 2

3 1 2 1 12 9 3 1 11 3

21

4 7. 7 8 1

1 1 1 2 2 2

1 1 1

1

3

3 2

H

T <51 6 1 8 1 10 1 12 1 14 1.15 E T > 51 8 1 8 1 10 1 12 1 14 I >is' X

BLOCK:C5 Tl<5 1 6 1 8 1 10 1 12 1 141.15 I 'I* >51 6 1 8 1 10 1 12 1 141>151

BLOCK:C6

T <51 8 1 8 1 10 1 12 114 1.15 I T <51 8 1 8 -1 10 1 12 1 14 1.151 E

BLOCK: C7 11<5 1 6I 8 I 10 1 12 1 14 1.15 E T>51 8 1 8 1 10 1 12 1 141>1511

BLOCK: C8


14— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 18b: Directional Wave Statistics for June

1,

2

2


H— WAVE HEIGHT IN METRES. T — WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 18c: Directional Wave Statistics for June

H >10

9 in a N N

1 in 4

4,

to 1

11.- 3 4 4 22 15 6 15 14 6

4 1

H >10

9 °

0.1 6 5

in 4 N 3 M 2 4

4 3

4,

to

3 19 2

5 IS

1 7 3

>10 9

eV 7

1 5 tn 4 I,: 3

>10 9 a

rni ; 1 5

4

(-3

2

>10 e 9 • a N 6

I s 4 3

CV 2

>10 9

e to N 76

1 5 ▪ 4 r- 3 W 2

1

>10 9

in r1 7 :i N 6 1 5 tn 4 s: 3 ▪ 2

1

>10 e 9 ul

NG 1 5 ill 4

14 3 N 2 1

T .51 6 1 8 1 10 1 12 1 14 1.15 E 71.51 6 1 8 1 10 1 12 1 14 1.151

BLOCK:C9 1.51 8 1 8 1 10 1 12 114 1.15 E T .51 6 1 8 1 10 1 12 114 1.151 I

BLOCK:CIO

T <51 6 1 6 1 10 1 12 1 141.15 E T1.51 8 1 8 1 10 1 12 1 14 1>151 E

BLOCK: D5 T1451 8 1 6 1 10 1 I2 1 14 1.15 E T .51 6 1 9 1 10 1 12 1 14 1.151 E

BLOCK: D6

112.5

°-15

7 5°

20

2.5°

- 247

5°

112.5

° - 157.

5°

5,

N

k N N

3 1

1 7 1 2

13 1 1

112 5° - 157.

5°

H >10

9

al N 7 N

N 4

22

>109

ez. 3

rp;

I 5 rn 4 t•Z 3 W 2

I

H >10 9

Fr) a N 7 N 6 .1 ,1-1 4

3 1" 2

>10 9 8

6 1 5

fh 4 t- 3 (0 2 5 1

4 1 1 1

2 5 6 1 34 2 2

4

>10 e 9 ‘7! a M N 6 15

en 4 1%1 3 N 2

2

>109

r1./ 8 8

7 N 1 5

*Er, 4 3

n 2

El

.93 . 9

e N 8 15

rn 4 r" 3 N 2

1

>10

N9

fit 9 7

6 1 5 N 4 N 3 al 2

112.5

° - 157.

5°

Fr,

8

O'

1

7 I 2 9 1 1

; 2

8 1 7 1 1 1

4 2 1

2

2

3 1 3 7 7 2 4

3 1 5 2

1 2 2 I

2 1 2 7 7 2 2

3 1 2 5 1 1

1 2 2

1

H H

N6

117 Iii 7

1 1

7 <5 1 6 1 6 1 101 19 1 14 1>15 E T1.51 6 1 8 1101121141>m1

BLOCK: 010 T c5 16161 101MI 1413.15E 7 ,0 16181 101121 Mi 0.151E

BLOCK: D9

>10 9

?II N N 6 I Nn q

1,3 to

>10 9

N 8 N 7 N6

ei 5 1n 4

iA wr"

3 2 2 1 2 2 1.; 3 3 2 1 .1 1 3 2 2 9 2 1 8 9 2 10 3 1 13 10 3

3 2 21 2 5 2 14 2

2 1 1

3 1 1

2

16 b 4

3 N 2

7.5 18191 MIMI 141>15 E 7• 48 18161 MIMI 141>151E

BLOCK :D7 TI.c51 6 IS I IO 112 110.15 E TI.51 6 I 6110112 I MI>1612

BLOCK : D8

292 5°- 33

7 5°




APPENDIX FIGURE 18d: Directional Wave Statistics for June

>10

15

0-3

1

a, 78 9

112

5°-1

57.5

° 20

2.5°

- 24

7 5°

3 8 9 1 9 1

>10 9

1 5 N 4 t 3 W 2

4 1 2 3 7 1 1 2

H >10

9

al 8 N 7

rn

63 1

N

1

pN rn

>10 9

0 7 00 6 1 5 rn 4

tn 3 2

J 5 4

1.■ 3 2 2

1 6 7 2 5 3, 1

7 3 15 13 4 1 2 1

1 1 4 3

1 1 2

sw

1 12.5

° -1

57. 5

° 20

2.5°

- 24

7.5°

H >10

8 in 8 N N 6 1 of 4 04 3 M 2

>10 9 3/ . 2

N e 1 5

4 0.3 3 02

>10 9

tc.3 5

E 1 5

4 3

'n 2

: 0 1 8 2

13 20 7 1 3 1

4 1 2 3 7 1 1 1

1 1 2 3

1

1 3 4 3 1 2 1

2 2 1

N 6 1 5 a, 4 0.: 3

2

>10

>10 O 9 t.11 Si 7 N 6 1 5

En 4 0- 3 N2

>10 0 9 61 a N7 N 6 1 5

Po 4 1,, 3 N2

3 7 4 1 4 1

1 1 3

2

10 4 2 10 3

.10 9

H •to

9

ft') e N ? N

j 5 074

er)

▪

•

el 2 1

81

er e N.

1 5 N 4

3 1 8, N

47 2 3 1 1 1 13 3 I

71051 6 1 B 1 10 1 12 1 14 1.15 E T 0 51 8 1 8 1 10 1 12 1 14 10151 I

BLOCK: E8


1 1

Ice covers 45% of tine

1

Ica cover. 45% of time

3 3 1 1 5 2

Ice covers 05% of tile

10 3 2 1 9 7

Ice covers 45% of tire

1 1

H $0

9

al 8 CV 7 N 1 5 th 4

112. 5

°-1

57.

5°

men

81

15 1.1 4

it :

71 <5 I 6 1 8 1 10 1 12 1 14 1.15 E 71051 6 1 9 1 10 1 12 1 14 17151 E

BLOCK: F7

$0 9

oc 7 19 6 15

fe, 4 3 2

I

>10 e 9 el 9

6



3 3 1

>10 9

• 9 N 7

ti 6 1 5 a, 4 N 3 W 2

9 3


010 9

rft 67 1)1. 6

1 5 N 4 N 3 1.0 2

j 5 in 4 N 3

H >to

9

rt1 N 7 cV 6

010 9

al 8

1 5

"/ 2 1

al 4 N 3

8 3 2 12 4

1 3 3 1 9 3 1

1 3 1 1 1 2

01 13 81

M 7 l- M 7

N6 6

1 5 1 1 5

&I 4 al Go 4

f■ 5 N 3

gi 2 3 1 cli 2

1 1 I

7 051 8 I B 110112 1141015 I 7 051 6 1 B 110112114101513:

BLOCK: G7

010 • 9

1

a, (93

ts- sr

NN

8 N

8, N

Pfl


1 1 2 2 1 7 1

010 9

. L4, 1 5

4 N W 2

1

Ice cover. 30% of tine

4 5 3 7 4

H >10

9

j 5 07 4

tft 8 ?

N 6

tor*" 3 07 2

1 I

1 r6

NN

•

10

71051 6 1 8 1 10 112 114 1015 E T 051 6 1 1 10 112 1 14 10151E

BLOCK: F8

>10 9

rg 7 N 6 1 5

Tr, 4

"' 3 2

I

>10

>10 9

rn 8 N 7

6 1 5 fr, 4

3 N 2

010 • 9 07. 9

NN ; I 5

fn 4

it 3 N 2

11 10 2 1 2 8 32 1 1

2 2 3 1 1

Ioe covers 30% of time

1

Ice covers 30% of tie*

1 1 1

1 2 1 3

3 1 1

2 1

1 19 5 2 1 1 9 10 1

Zoe covers 3011 of time

Ice covers 30% of tiro


4 3 9 3

Ice cover. 30% of tier

1 1 2 4 1 2

1 2 1

71.51 6 1 8 1 10 1 12 1 14 1.15 E 7 .5 1 6 1 8 1 10 I 12 I 14 1.151 X

BLOCK:G8

71.5 1 6 1 8 1 10 1 12 1 14 1.15 X T .51 6 1 8 1 10 1 12 1 141 .151 X

BLOCK:H5

1 2 3 2

2 3 2 1

.10 9

e 41 7 c=j 6 1 5 N4 f■ 3 10 2

.10 9

N 7 gi 6 1 5

4 1.; 3 N

.10 e 9

RI 7

1 5 F174

H .10

9

N 7 01 6

I,: 3

ICE

ICE

ICE

ICE

7 12 9 11 4

a

rn

H .10

9 'in 8 N 7 N 6 e) 5 O 4

P2

H >10

9 N8 es.i 7 N 6

8 In 4

3 2

ICE ICE

1 5 er', 4

14; :

X

112 5

° - 1

5 7. 5

° 20

2 5°- 24

7 5°

010 9

1 5 N 4 0: 3 1.8 2 2 3 1

9 1 1

.TO 9

in 8 0 N7

N 6 1 5

4-1 2

.10 9

al 8 O 7 N 1 5

'N 4 P 3 4:2 2

ICE ICE

ICE ICE

2

010 .10 e 9 o 9

O 8 N m e ai m g 7

7 1... CV 6 m cv 6

1 5 I 1 5

rn 4 :7 Z-, 4 ft: 5 t- 3 X' 2 E I

x2 ,

. .

ICE ICE

2 3 5 1

.10 o 9

M 7 0.1 6 I 5

4 5

V N2

X

H eq0

9

0, 6 1 (.04 %.

112 5

° - 1

57. 5

° 20

2 5°

- 24

75°

>io 9

ff.> 8 76

1 5 • 4 7. 3 tg,

>10 9

in 8 01 7

R, 6 1 5 N4 1.■ 3 42 2

7 10 1 5 9 4

1 6 5 10 1

1 3 2 3 2 2

2 S I 10 3 1

4 1

292.

5°-

337

5°

202.

5°- 24

7.5°

11

2.5° - 15

7.5 °

1 I I

7 5 10 2

3 2 6 1 3 1

in

1

202

5 °- 2

47. 5

° 11

2 5.-

157

.5°

ICE

ICE

ICE

ICE

1 2 1

3 3 2

7 4 7 3

•3 1 3 6 1 6 1

112

5° -

157

5°

202 5

°- 2

47. 5

°

7 12 3 8 4

cj 6 1 5 th 4 5- 3 W 2

510 9

Uf e

1 5 N 4

r?;

510

In 8

15 4 3 V

AI 2

2 2

510 9

1 0 1 9 1 1

2

2 1 3 2

T <51 6 1 8 1 10 1 12 1 14 1515 E T <51 6 1 8 1 10 1 12 1 14 1 5151 E

BLOCK: H8




APPENDIX FIGURE 18g: Directional Wave Statistics for June

1 9 3

MO

N 9 '' 47) 7 cv 6 I 5 in 4 ▪ 3 X 2

.51 6,I B I 10 I 121141.15i 14 518181101121141.151E

BLOCK:CI

111

N

112.

5°-1

57.

5°

>10 9

V. 76 5

N 4

t'i3

SO 9

tn N 0 N 1 5 a., 4 N 3

2

3 2

4

5 4

1 4

tr) 67

In

2 1 1 3 4 2 7 3 1 2 33 4

H

9 &le N 7 N 6 I 5 in 4

4 22

r.0 3 2 1

2 1

I12

.5°-

15

7.5°

T <51 6 1 8 1 10 1 12 1 14 1.15 E 714 51 8 1 s 1 lo 1 12 1 14 1 >151 2

4,

sD

.10 9

is7

3 2,

I S tr. , 4

202.5°- 247

5°

H >10

9 'th 8 Ds 7 N I 5

31 4

>10 9 e

M 7 N I 5

Pn 4 ▪ 3 N 2

SO 9

O B

I 5 pr, 4 N 3

2

: 3

4 2 1 1 2 21 5 1 1

1 3 2 32 5 2

4

3 1 2 3 1

BLOCK:C2

3 Hi 2

1 7 2 2 17 2 1 1

2 1 6 1 4

BLOCK: C3 BLOCK:C4

14 MO

9 trl N 7 N 6

5 07 4 N 3

2

SO 9

N a N 7 N 8 1 5 in 4 N 3 D2

SO 9

in 6

1 5 a., 4 1- 3

SO o 9 0

418 87

7 r- in

N 6 In

IS I

ik ) 4 in P A 2

3

I 1 2 4 1

I

I E 71.51 61 8 I 10 1 12 1 141.15 I 71.51 6I B 1101121141>151E 714518181101121141.15E 71.51 6181101121141.151E

1 2 1

1 4

2 5 5

19 11

4 1

112.5°

-15

7.5°

rt,

SO o 9 31 8 M 7 N 6 I 5 to 4

3 Di 2

H >10

9 al N 7 N

ol 07 4

112 5°

-157

5°

SO 9

1 5 4

El

>10

N 7 6

1 5 4

10 3 2 2

7 3 1 1 16 4 1

3 3 1 34 10 1

4

1 3

2 11 1 4

1 1 2 1




APPENDIX FIGURE 19 a: Directional Wave Statistics for July

1 2

Pei 3 In 2 1

1 7 2 2

15

>10 9

rn 6 mi N 6

5 Lr1 4 Pn

T1451 6 1 8 1 10 112 1 14 1.15 X 7 <51 8 1 8 1 10 1 12 1 14 1.151 X

BLOCK: C5

112 V

-157

5°

ol

pNN

202 5°

- 247

V

.10 9

N o 8

; 1 5 th 4 es 3

2

.10 e 9 in 8

7 N6 1 5

rn 4

:

>10 9

N 8

8 7 N 6 1 5 N 4 es 3

3 3 5 3 1

25 14

3 1 2 7 2 1

2 2

1 2 7 1 1

1 5 N4 es 3 1

4 2 8 1 1

up 2

1 2

1 1 1

112 5

°-15

7.5°

.10 9

frt e N 7 E 5 1 5 tr, 4

N 3 E' 2 1

o 9

" 6 1 5

Pn 4

X

4 1 5 1

1

4

71451 6 1 8 1 10 112 1 14 1.15 X 7 <51 6 1 8 1 10 112 1 14 1.151 X

BLOCK: C7



T— WAVE PERIOD IN SECONDS. — ONE OCCURRENCE REFERS TO A SIX HOUR MEAN.

APPENDIX FIGURE 19b: Directional Wave Statistics for July

3 4

1 2 1 8 1

e•10 e 9 q 8 M 7 im 6 1 5

rn 4

.10 9

rn (.11 6 1 5

tn 4

if;

1

.10 9

• 8 Ni

5 N4 N 3 w2

1 X

2 4 5 2

202.

5°- 24

7 5°

11

2.5°-

157.

5°

1 3

2 2 5 5 2 1

12 11 2

12

7 <51 6 1 8 1 10 1 12 1 14 1.15 X 7 <51 6 1 8 1 10 1 12 1 14 1.151 X

BLOCK: C6

.10 9

N 7 cso 6 1 5 N 4 N 3 M 2

,9 6

.10 9

N 7

1 5 1, 4 N 3

•1

.10 9

112.5

° -15

7.5°

;

1 5 N4 N 3 W2

1 6 1 2 11 2 1

2

.40 e 9 ul 8 M N 6 2 I5 Po 4 es V N 2

te)

T1.51 6 1 8 1 10 112 1 14 1.15 <51 6 1 8 1 10 112 1 141>151

BLOCK: C8

1 5 2 1 9 1

2 13 6 28 5 2 1

71 < 51 6 1 8 1 101 12 1 14 1.15 E 745161 8 1 101 12 1 141.151E

BLOCK:C9 H

>10 9

rtl 8 0.1 7 N 5

04

1

.10 9

tn N 6

e 5

Y7 4 • 3 63 2

9 in 8

MI 76 1 5 N 4 isz 3 52 2

>10 o 9 0 8

7 MI 6 1 5 in 4

1

714 51 6 1 8 1 10 1 12 1 14 I.t5 I 7 .451 6 1 8 1 10 1 12 1 14 1,151

BLOCK:D5

7 451 6 1 8 1 10 1 12 1 14 1.15 I 7 < 51 6 1 8 1 10 1 12 1 14 1.451 X

BLOCK:C10 H

>10 9

N 7

1 5 10 4

7 <51 6 1 8 1101 12 1 14 1.15 E 7 < 51 6 1 8 1 10 1 12 1 14 l>151 E

BLOCK:D6

j 5 6




APPENDIX FIG= 19c: Directional Wave Statistics for July

N

Pn

N

67

20

2.5°- 24

75°

1125° - 15

7. 5°

8)

PR

1 5 4

1, 3 ° 2

1 11

25°-

1575°

.10 9

0 o 8

7 N 6

1 5 ?n 4

1 6 t■ 3 °

1 11 8

1 1

3 7 1 2 1

12 8 2 13 5 1 1

2 11 6 2 9 1

.10 9

111 a

IA 7 03 1 5 fb 4

51 3

>10 e 9

B g NI

I 5 fn 4 1". 3 DJ 2

>10 9

i0 8 Da 7

19 4 3

'12 2 1 2

M 7 N 1 5 th 4

3 & 2

1

>10 • 9

6

1

1 3 1 2

2

1 3 1 2

1 14 8 2 11 4 1

6 5 1

2 2 2 3 2

to to

7 1

I125°

-15

7.5°

20

2 5°

- 247 5°

292 5

°- 3

37

5°

5 3 2 28 3

S 2 3 25 13 1

2

3 3.

21

2 2 1.43

1 5 th 4

: 1

>10 • 9 0 8

6 1 5

rn 4

20

2.5°

- 247 5°

6,

rn

8)

iy 11

2.5° - 15

7.5°

1

4 2 4 1

6 1 3 21 2

1 2

2

6 2 3 1 33 12

3




APPENDIX FIGURE 19d: Directional Wave Statistics for July

14 H

1410

NO

9 9

in 8 N tn 8 N 7 p N 7

CY 6 t0 N8

J 5 J 5

,11 4 Pn 117 4 N N 3

2 2

3

5 5

11451 8 1 8 1 10 1 12 1 14 17.15 E T 451 8 1 8 1 10 1 12 1 14 17.151

BLOCK: D8

N 1 5

4 N 3 gi 2

1

71451 6 1 8 1 10 112 114 17.15 I T 451 6 I 8 1 10 112 114 13451

BLOCK: D7

74516181101121141745Z 74518181101121141.151£

BLOCK: D9 7145 1 6 1 8 1 10 1 12 1 14 1 7.15 I T 451 6 1 8 1 10 1 12 1 14 17.151E

BLOCK: DIO

NO 9

& 8 Lt 7

6 1 5

f.r, 4 N 3 0 2

112.5°-1

57. 5

°

NO 9

III a

0 N 7 44 1 5

To 4

112

.5° -

157.

5°

20

2.5° - 2

47.

5°

8)

H No

9

01 ? N6

5 al 4 04 3

22

H

9 17 8 N N

riz ! 5 47 4

M 2

1 1 1 6 1

16 2 12 8 2 14 6 2

10 11 2 14 5 1 1

1410 9

1 5 ro 4 N 5 0 2

1410 9

LO

1 5 rn 4 N 3 2 2

NO

9

V 7

N

1

8

7.10 o 9 q a tn g 7 N N 6 I5 1 6 4 th r;t: 3 1 N 2

E

MO

N 1 5

en 4 N. 3 N2

If

04 04

310 9

6

1 5 rn 4

5 w2

m09

8 1 N 6

1 5 rt, 4 N 3 El 2

Pn

• V

1 N 2

2

4

NO 9

tO a fV; 1 5

11) 4 I, 5 to 2

NO 9

h; 2 6 1 5 fi) 4 N 5

2 1

10 29 3 2

5 2 2 1 1

1 1 5 2 6 1

1 2 1 3 3

9 19 2

1 3 2 7 1

2 2 7 4

2 1 10 8 2 6 1 1 5 3 2

1

1 3 1 2

2

15 En 4 N 3 N2

1

2

3

3 1 2 2

1 1 2 1 1 2

3

1 8 7 1 7 1 1

2

1 4 1

za 3 2

1 1 6 2

4 1 7 1

2 1

.40 9


1 1 8 1


5 1 1


3 1


4

>10 9

:1 8 1 5 in 4 N 3 47 2 11

2.r-

157W

.10 9

!

15


1 7 3 2

Ice cover: 10% of time

1125°-

157.

5°

th 4

010 9 B

CI 7

I 5 1,5 04 3 er N 2

6 15 64

NZ

>10

7 8 I 5 a, 4 0- 3 cr

>10 9

• a

: I5 4

IN 3 ID 2

H sip 9

6 N 7 N 6

N 5 WI 4 3

2

>10 9

0 • 6

N

1 5 tr', 4 N 3 v0 2

H

4 25

2 1 3

10

12 10

3 3

1 2

.10 9

ra a

? 0.1 6

in 4

1

1 6 27

2 1

1 2

8 11

3 1 3 1

4 13

2 1 3

0

N N

4

1 1

>10 9

• 41

8

15 6 4 N 47 2

1 5 11

1 1 3 2

I. IA N

4

1 1

I

>10 9

re) a

S 7 cv 8 15 in 4 N 3 'n2

>10 • 9

a

cv 15 6 4 N cv 2

2 7

2 1

6

V Pl

2

.10 9

16 B cm 7 2 5

64 N5 e2

I

>10 9

V7

15 4

tz 3 cv 2

1

3Si

1'0

2 1

2 10 1 1 4 1 7 1

T

H >10

9 k os 7

ci 5 cn 4 S.: 3 M 2

El

451 6 I B I 10 I 12 I 14 1.15 2 714 61

BLOCK:E8 6 I B 1 10 1 12 1 14 1.151 2

H 210

9 16B oi 7 N 6

s! 5 41. 4

3

21

T145I 6 1 B 1 10 112 1 14 1215 E T 451 6 1 8 110 112 1 14 I.151 Z

BLOCK:F7

1 6 24

2 1 2

4

10

11 10

3 2 3 1

Ice cover. 10* of time

5 10 1 23 3


2 3 1 10 1

T 451 8I B 1 10 1 12 1 14 1215 E T 451 8 1 8 1 10 1 12 1 14 1.151 2

BLOCK:Fe 1.1451 6 1 8 1 10 1 12 1 141,15 E T 451 8 1 0 I 15 I 12 I 141 2451

BLOCK:G7

NOTES • — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES



APPENDIX FIGURE 19e: Directional Wave Statistics for July

Ice ammo ;1% of time

1 2 6 1

H 010 9 B

N 7 ce 6

5) IA 10

4) 4 N 3 2 2 5 9 1 4 3 1

20 3. 13 1

1 6 1

112.5°- I

57.V

2

02

.5-2

47.

5°

T1451 6 1 8 110 1121141.15 I Te51 8 113110 11211410151E

BLOCK: G8

010 9

l; III 6 1 5 r- 4

3 (.0 2

I

2 4 2

010

W RI 7 N 6

1 s in 4 N 3 N 2

1 5 1 I

N N6 1 5 • 4 N 3 .11 2

I

1 7

4 2

2 1 7 1

N 6 ICE j

04 143 M2

1

>10 9

1V 7

1 5 tr', 4 r3 1°2

1 I

010 9

to 0 N 7 N 1 5

fr., 4 N 3 Le 2

I

so • 9 W

N

I5 in 4 N 3 te 2

I 11.51 eIeIlo 1 12 1 141015 I T45 16181 10 1 12 1 14 1.151

BLOCK: H5

to

N

71.51 6 1 8 1 10 1 12 1 14 1.15 5 T 451 6 1 8 1 10 1 12 1 14 1,451

BLOCK: H6 T1451 6 1 8 1 10 1 12 1 14 1015 I T .51 6 1 8 1 10 1 22 I VI I >191

BLOCK: H7




APPENDIX FIGURE 19f: Directional Wave Statistics for July


3 1 1

1 6 2

1 1 3 2 1

H .93

9 Ice covers

1 1

21% of time tai 7

I in 4

3 2 4 24

8 2 4

8)

10

3 11

3 1

I

Ice covers

4 2

2111 of time

>10 9 e

Eli ; I 5 [1,4

10 2 1 3

1 8 1

1 4 5

I

2409

rp a

N■ 8 15

1, 4

3 2 1 7 2

I


2


1 1 4 1

N

of

1 a,

>10 e 9 08 g 7 N

15 al 4

te 2

I

112

V-1

57.

5*

H *10

9

th 8 N 7 te 1

in 4 r 3

2z

N L°. 6

I 5 rr, 4 N 3 tO 2

9

rrt e (cc:: : 1 5 th 4 N 3 tn 2

Al 6 5

N 3 611 2

I

)40 • 9

e

010 9

)40

I

I

112

5°-

157.

5°

5, N

to

IM

Ice cover. 21% of ties

4 2 18 3


1 1 3 1

ICE

ICE

ICE

ICE

ICE

ICE

ICE

1 8 1

1 1 6 2 2

1 6 112 5

.-15

25°

V

2

2

>ID

1,1 ,1 Al T 6 I 5 a, 4 ••• 3

2

.10 9

0 e

(13;

Is 11„4

el) 2

MO 9

&)e

N T 5

th4

02

1 2 7 3 1

3 1 3 1

2 1 5 1

H

5 3 1 11

3 8 1 1 19 4

22 5°-

67 5°

.10 9

rn N ?

6 1 5

4 3

es 2

1.1<51 6 1 8 1 10 1 12 1 14 11.15 I T 451 6 I 8 110 1 12 I 14 1.151 E

BLOCK:H8

KITES: — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES



APPENDIX FIGURE 19g: Directional Wave Statistics for July

2 3

2

112 5

°- 1

5Z 5°

202 5°- 247

5°

2 4 1 16 10 4

4 5 26 2

1 1 2 2

2 1

22

5°- 67

5°

112

5° -

157

5°

20

2 5°- 24

7 V'

.10 9

N 7 N6

2

.10 9

• a

;

1 5 4

f, 3 2

.405

in 8 N 7 N6

1 5 N 4 1- 3 `-r-' 2

>10 e 9 ‘17 V7 N 6 1 5

Pr) 4

;

H

.10 9

th 8 N N 6 1 5

fn 4

M 3 yl 2

.10 9

to 8

EY 76 1 5 -, 4 r 3 t° 2

>10 9

&) N7

6 1 5 to 4 r, 3 Li'. 2

>10 ▪ 9 0 Si 7 " 6 1 5

al 4

2 3 12 9 4

2 4 29 4 1

1 4 2 1 1

1 1 12 2

3 1

1 3 5 1 2

1 2

2 1

H >10

9 N 8 N N 6

1 5 1 4 1 1

1 3 a 1 1 4 8 1 2 2 12 4 3 10 2

24 12 1 10 7 1 21 7

225°

- 67

.5°

202 V

-24

7 V

T <51 6 1 8 1 10 1 12 1 14 1.15 E 7 <51 6 1 8 1 10 1 12 1 14 1 >151 X

BLOCK:C3

It 2 ts 3

>10 9

1 5 4

I, 3 10 2

1

.10 9

N M 76 I 5 to 4

1

>10 • 9 to. V7

I 5 en 4

2 3 4 6 1

2 1

2 6 1

2 1

2 3

7 <51 6 I 8 1101 12 1 14 1.15 I 7 <51 6 1 8 1 10 1 12 1 14 1 >151 2

BLOCK: CI 7 <51 6 1 8 1 101 121 141.1512 T1 4 51 6 1 E1 1 101 121 141.151E

BLOCK: C2

I 5 In 4

3 w 2

.i0 9

In•8

N 6 I 5

11,4

1

>10 e 9 'n 8 N7 N 6 I 5

87 4

it; : 1

74516181 101 121 141.1512 11.7 516181 101 121 141.151E

BLOCK: C 4

NOTES — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES

H — WAVE HEIGHT IN Ml I Ktb.



APPENDIX FIGURE 20a: Directional Wave Statistics for August

1 1 4 6 4 1

112.

5°-1

57 5°

3 2 2

202.5 - 247 V

2 2

2

1 6

N 7

T1<5 1 6 1 8 1 10 1 12 1 14 1.15 I T <51 8 1 8 1 10 1 12 1 14 1.151 E

BLOCK:C7 T <8 1 6 1 8 1 10 1 12 1 14 1.15 E T <51 6 1 8 1 10 1 12 1 14 1.151 I

BLOCK:C8





APPENDIX FIGURE 20b: Directional Wave Statistics for August

2 4

.10 o 9 N

N 7 6.1 6

1 5 fr', 4 r-g'2

1 5 En 4 ... 3 N 2

.10 9 8

N 7 c4ii 6

71.51 6 1- 8 1 10 1 12 1 14 1.i5 I T

BLOCK:C5

22 5°

- 67

5°

112

5° -

157

5°

3 7 7 9

2 2 2

1 1

in 8 N 7 csi 6

I N4 3 1 3

6 7 5 3

4 1

1 4 1

1

.10 9 8

,7 6

1 5 Fr, 4 r- 3 W 2

1 1 5 8 4 8

2 I

>10 9

in

07 N 6 1 5 rn 4

r;-; 1

1 3 2 1

1 I 6 1

2

>10

a 9 41 N7 N 6 I 5 N4

Cr• 3 N 2 1

<51 18 1 8 110 1 12 114 1 .151 T <51 8 18 1 10 1 12 1 14 1.15 E

H >10

9

T <51 6 16 110 1 12 1 14 1.151

BLOCK:C6

112

5°-

157.

5°

202

5°-

24

7 5°

In 10

1 5 N 4 r- 3

2 2

2 7 1 4 9

H HO

9

ot N6 1 5 N 4 - 7 3 . .7 2

1 1 1 3 3 11 5 4

Ho 9

th 7 111 6

1 1 1 3 7

1 2 3

5 7 1 14 8

1 2

2 1 1 2 1

H .10

1 1 2

1 5 4 1 6 1 7 15 1 5 10 1 8 2 10 4

112 5°

-15

7 5°

>to o 9

g 7 6

1 5 fh 4 1":„... 3 & 2

.10 9

N 7 2 6 1 5

4 3

Ez 20

2 5°

- 247

5°

2

9

e N 7 N 1 5 N4

.10 9

111 87 11.1 6

1 5 N 4 r- 3 W 2

7 1 6 2 2 7

3 I 2 1

2

N

112

.5.-

15

7.5°

In 141.' N N

fpV

N

t"n

En

1 1 7 1

5 II. 1 7 3

2 I 4 3

10 14 1 10 4 1

1 7

3 2 2 7 1

2

>10 9

52 6 1 5 rn 4

3 '5 2

>10 9

h e Ni4

(.1 6 1 5

11, 4 3

u7 2

N7 N6

>10 . 9

B

1 5 N4

Q N 2

H .10

9

?s, a NI 7 1•1

5 N4

1 5 in 4 6. 3 Ct 2

1

.10 e 9 al

7 6

292

5° -

337

5°

20

2 5°

- 2

47

5°

1 12

5°- 15

7 5°

0,

5 5

10 16 2 2 1 8 6

1 1 2

1 1 1 4

TI<516113 I Wm' 141.151E 7 4 5 16181 101 12 1 141.151E

BLOCK : C 9

3 2

202

5°- 24

7.5°

71451 6 1 6 1 101 12 1 14 1.15 X T 451 6 I 9 1 101 121 141>151 E

112 5

°-1

57. 5

°

rn

.10 9

in 8 N N 6 I 5

Iz

.10 9

N 8 NI 7

1 5 to 4

>10 9

1"1 N 6

I 5 rs., 4 rs 3 W 2

.10

3 i (9

M 7 N 1 5 in 4

ri 32

1 2

1 1 10 1

3 11. 4 2

1

1 2 1 7 2 1

4 6 1

13 12 2 2 1 11 7

BLOCK: CIO

2 3

a a

8 1

T <5 1 6 1 8 1 10 1 12 1 14 1.15 X Tl<5 1 6 1 8 1 10 12 1 14 .151 E

BLOCK: 05

NI

225°

- 67

5°

1 12

5° - 157

5°

20

2 5°

- 24

7 5°

>10 o 9 to

Si 7 N 6 I 5

in 4 O3 2

>10 9

to 8 N 7 N 6

in 1 5

N 3 in rn2

1

>10 9

to o 8

(11 ;

1 5 a, 4 r– 3 '5 2

>10 9

in a 0.1 7

6 1 5 a, 4 r..1 3 • 2

1 1 1 1

1 7 10 7

2 2

4 3 18 8 1

3 9 4 7

1 2 2 1

a 2 1

>10 9 ▪ B

68 7 • 6 1 5

lb 4 6.: 3 N 2

1

>10 e 9 In

all 7 N 6 I 5

er, 4

: 1

TI 4 5 1 61 8 1101 12 I 14 1.15 E T 451 6 I 8 I 10 1 12 I 14 1.151 E

BLOCK: 06

202

5°- 24

7 5°

I 1

2 5°- 15

7. 5°

a

o 9

to 8 ;

I 5 ▪ 4

H >10

9 N 8 N 7 N 6

5 10 4 N 3

2

X

>10 9

if', C-11 ;

1 5 4

6- 3 'D 2

N 6 I 5 to 4

;

9 in N 7

X

H >10

9 to° a cv 7 NI 6 I 5

r11 4 tr:i 3

2

2

1 2 2 6 1

3 7 17 6

3 3 6 9 6

3 8 6 8 1

12 1 9 1

4 2 1

1

1 3 3 1 5 2 1

112

5 °-1

57. 5

°

N

5, loV

9 rn 8 0.1 7 01 6 I s N-4 e- 3 2 2

>10 9

N 8

I 5 tr, 4 r. 3 w 2

>03 9

:I8 8 7 N 6 I 5 ro 4 t. 3 52 2

1 3

112.

5e-1

575°

202 5°- 2

4 75°

IA

>10 • 9 d!

N6

I 5 014 tz N2

z

)40 9

ai 6 1 5 rn 4

3 co 2

1

>10 9

O 7

s 15 rs, 4 rz 3

2

£

1 1 6 1

8 6 6 1

1 1 6 5 5 1 a

1 1

2

3 1 1 1 3 1

>10 e 9 el 0'1 N 6 I 5 al a

3 N 2

1 1

5 2 6 8 7 3

1 1 6 1

9 10 1 13 6 1

4 7 5 1 8

3 1

1 3

1 3

2

9

8 11 1 3 1 10 7

a,

112

5° -

157

5°

202 5°

- 247

5°

292 5°

- 3

375°

H NO

9 1.1.1 8 m7 m6

l 5 10 4 Pz 3 M 2

1 11

2.5°

- 15 7

. 5°

202.5°- 24

7 5°

29

2 5°

- 337

5°

>10

N7 26 1 5

'er, 4 3 LT) 2

9 111 Pi 7 N 6 1 5 ti)

3 N2

H >10

9

5, 4 3

'in 8 N 7 N 6 I 5

n 2

>10 9

a-) 1 1.,1

N 1 5 a, 4 I, 3 w 2

>10 9

51 5 N cc:3 6 1 5

4 to.: 3 '12 2

>10

N

• 6

SI 7 N 6 I5 to 4 1, 3

2

2 3 2

1 11

5 11 5 3

1

1 5 3 1 5

3 8 1 1

11 12 1 2 1 1 12 8

1 1 9

4 10 3 0

1 2 4

1

1

H H

TI <5 1 6 18 110 1 12 I 14 1.15 T <5I 6 18 110 1 12 1 14 1.151

BLOCK: D7

T <51 6 1 8 1 10 1 12 I 14 1T•13 I T.51 6181 10 1 12 1 14 1 >151

BLOCK:D8

-11.5161e110 z T.5161elmlmimi.orz

BLOCK:D9 T <51 6 1 8 110112 1141.15 T.51 6 1 6 I 10Ii2 1141.151 X

BLOCK:DIO




APPENDIX FIGURE 20d: Directional Wave Statistics for August

2 5 2

2 4 1 1 1

BLOCK: F8 BLOCK: G7

3 10 1 5 2

1 3 2 1 1

4 4 4 1

225°

- 67

5°

>10

In 8

7 N 6 1 5 in 4

ri.76

T1.51 6181101121141.15 X 1.516181101121141.1512

1:b

N rs.1 6 1 5

i■-", 3 ro 2

112 5

° -1

57 5

° 20

2 5°

- 247

5°

292

5° -

337

5°

>10 9

N 8 N 7

6 1 5 f}-, 4 r- 3 co 2

>10

N 7 2 6 1 5

4

Lin ;

1

4 6 1 13 6 1

2 8 11

12 4

1 4

2 1

BLOCK: E8

N7 N 6 1 5 tn 4

X 71.5 1 6 1 8 1 10 1 12 1 14 1.15 X 7 .51 6 1 8 1 10 1 12 1 14 1.151

>10 o 9 n 9

22 5°

- 67

5°

112 5

° - 1

57.5"

202

5°-

247

. 5°

>10 9

in 8 7

0 CV 6 1 5 fc., 4 6- 3 I'2

>10 9

:I 8 N ;

1 5 fr., 4 r- 3 W 2

1

1 2 2 1 3

2 1 9 9 3

1 7 4 2

3 8 6

2 5 1 3 1 1

BLOCK: F7

8 9 1 6 2

22

5°- 6

7 5°

11

2 5°

-15

7 5°

22

5°-

67 5

° 11

2 5°-

157

5°

5) pN

202 5°

- 2

47 5

°

1 5

H >10

9 in 8 OJ "

10 4

2 2 is: 3

>10 9

1 5 fg, 4

;

>10 9

in 8 0 N 7 N 6

1 4

O. 3 D 2

1 3 10

11 3

3 a 5 1

1 1 2 4 2 4

1 1 6 2

5 2

ccg 6- en 7 N 6 N 6 In 1 5 I Is I 554 u, in 4

N 2 1

3 2 : Xi 1 3

11 < 5 1 6 1 8 1 10 112 1 14 1.151 I 7 <51 6 I 8 1 10 112 1 14 1 >121 2 T1 <51 6 1 8 1 10 I 12 1 141.15 E 7 .51 6 1 8 1 10 1 12 1 14 1 >151 2

NOTES: —7 DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H— WAVE HEIGHT IN METRES T— WAVE PERIOD IN SECONDS


APPENDIX FIGURE 20e: Directional Wave Statistics for August

>10 e 9

e

2 2 2 2 1

H >03

9 to 8 01 7 N 6 1 5

Fr) 4 Pi 3 ^l2

>10 9

Lo

>10 9

to t-s-'i N 6 1 5

4 6- 3 u' 2

>10 9

trl 8 cv 7 N 1 5 ?, 4 7, 3 tr' 2

2 2 6 4 1 3

1 2 1 2 3

2 1 1 5 5 3 1

1 1 3 6 2 1

1 7 9

13 6

2 2 1 I 1





APPENDIX FIGURE 20f: Directional Wave Statistics for August

20

2 5°- 2

47 5

°

112 5°

-15

7 5

°

22 5°

- 67 5

°

2 2 5 0 2 3

1 2 1 2 3

11451 618 1101121141415 Z T 451 6 1 8 1 10 1 12 1 14 14151 £

BLOCK :68

3 6 5

>10 9 e

N 7 6

1 5 N4

92

Zi

H >10

9

th N 7 (%1 6 1 5

fc.) 4

15'7; 3 en 2

>10 9

= 6 1 5

'en 4 r- 3 (.0 2

•

1 6 0 7 3

112.5°-1

57

5°

•

N

N oN

1451616101121141 >15 7451618110112118 1 >151

BLOCK: H5

1 4 3 1 1

/

3 2 5 2

1 1 2 8 2

5 1 3

202 5

- 2

47

5°

T14516181101121141/15 70516181101121141.1513:

BLOCK: H6

112

5° - 15

7. 5

°

>10 e 9 (r)

292 5°-

3375°

7 N 6

15 4

4- 3,, N

9,

>10 9

fit 6 N 7

1 5 a, 4

3 ,n 2

>10 9

1 5 en 4

H >10

9

N N 7

6 j 5 4") 4 1.- 3

2

1 6 2

3 2

1 1 7 2

4 1_

1 3

7 5 1

1 2 3 1

2 1 8 10 1 7 2

1 1 1 9 2

2 3 8 1 1

1 5 2 2 1

>10 9

th 8 ;

I 5 a, 4 5- 3 07 2

410 9

fh

N 7 6 16 N4 5: 3 N 2

>10 e 9 5.1 8

N 6

I 5 1, 4

a 3 N 2

H >109

el 5 47 4

?n e N i N 6

M 2 N43

Zi

1 1 1 1 5 2 2

2 1 5 1

3 2

1 8 10 2 6 1

112.5 -

15

7.5

°

In ri (0

7051 s I 81101121141.15 Z 1145161811011211414.1512:

. BLOCK:H7

2 1 5 5 5 1

1 1 1 2 2 4

2 1 2 2 1

>I0 9

N

1 5 en 4 N. 3 tO 2

>10 9

r08 N 7 R 6 I 5

en 4 5- 3 “2 2

1

SIo

9

`' 7 6

1 5 4

r,3 3 2

>10 e 9 44

017 N 5 1 5 in 4 it 3 cu 2

1 W 9

2 1 3 3 2 4

1 8 2

5 1

>10 9

Ehe N 7 N 6 I 5

&') 4

2

I

22 5°- 67

5°

112 5

° - 1

57 5°

20

2 5°

- 247

5°

11<5 I 8 1 8 . 1 10112 1 141>15 I 11..51 616I10I12I14IM5It

BLOCK: H8

>10 9 th a Es.! 76 I 5 fs, 4

t' :

>10 9

to N 7 0 cc. 6 I 5 N 4

3 92 2

I

1 2 1

7 3

>10 • 9

s

N6

I 5 to 4

N 292

5°- 3

37 5°

2 4 7 1 1

2 1 1 2 1 3

1 6 10 1 6 1

2 1 6 5 1 3 1

2 2 1 2 3 1 4

1 6 1

4 1


H— WAVE HEIGHT iN METRES.

— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 20g: Directional Wave Statistics for August

_ —

2 3 1 8

112 5

°-157

5°

20

2 V

- 24

7 5°

1 3 1 10

3 3 1 6 1

1 12

32. 1

112

5°-1

@75°

20

2 - 24

7.5°

r-

4 3 3 15 4 3 1

6 1 1 1

53 2

19

71<51 6 1 8 1 10 I 12 1 14 1>15 E 71<5 1 6 1 8 1 10 1 12 1 14 1 >19

1 7 1 1 1

Tl<616161101121141.16 E r<516181101121141.15

H >10

9

e tu

2 2

5 8) 4 r•Z 3

>10 9

6 76

1 5 N 4 ft.. 3 19 2

>10 9

fi) e N 7 N6 I_ 5 a, 4

3 D2

>10 e 9 tn a

ONi ? N 6 1 5

rn 4 1.■ 3 N 2

H

>10 9

N 6 j 5 in 4 M 3 M 2

$0 9

N 8

ti , 1 5

4 r, 3 Wa

>10 9

a, 8 N 7 N6 1 5

a, 4 P 3 e 2

>10 o 9 t0 6 • 7 N 6 1 5

iO4

2 6 2

2 18 1

3 2 1 6 1

11

7 2 2 16 4 3

4 1

9 7 1

22 V

- 67

5°

1125

°-15

75°

20

2 5°

- 247

5°

292

5° -

337

V

H >10

9

N 7 N6

ol 5 6 4

2 2• 3

>10 9

o 8

1 5 N 4 r, 3 O 2

- 1

>10 9

6 5 N 7

6 1 5 to 4 it- 3 ul 2

0

1.12 5°

-15

7 V

20

2 5°

- 247

5°

H >10

9 N a N 7 N 6 1 th 4 M 3 M 2

1

>10 9

:I 8 cs, 76 1 5

'en 4 r- 3 10 2

1

>10 9 8

O 7 N 6 1 5

4 tt- 3 e 2

1

>10 o 9

7 N 6 1 5

1h 4

14 3 N 2

1 10 4 1

>10

a 9 to a

g 7 N 6 I 5

in 4

1 2 1 1 2 1 1

9 2

2 3 5 1

17 3 2

4 3 11 1

2 1

1 1 1

4 4 2 16 3 2

1 1 7 2 1 8 1

1 1 9 5

3 2 1 11 1

8 2

BLOCK: CI

BLOCK: C2

71<5 1 6 1 8 1 10 1 12 1 14 1.15 I 7 <5 1 6 1 8 1 10 1 12 1 14 1.151E

BLOCK : C3

T1.51618 1101121141.15 E T.516181101121141,1511

BLOCK: C4



T— WAVE PERIOD IN SECONDS


APPENDIX FIGURE 21a: Directional Wave Statistics for September

I 6 1 8 1 10 1 12 1 10 >15 E T <5 1 6 1 8 1 lo 12 1 14 1.151 I

BLOCK :C5

1 5 tr, 4

3 (5 2

>10 9

r0 8 N 7 196 1 5 rr, 4 r- 3 e2

>10 o 9

a 7

111 6 1 5 N 4

: 1

T<516181101121141.153 T<51 618110112114130513

BLOCK : C6

>10 9

‘1' ;

H >10

9 ,n* a N N6 I s tn 4

A 1,

32 1 £

1 5 N 4 4

▪ 3 2 11

2 5°

-15

7.5°

2

02

5°- 24

7 5°

2

92

5°- 3

375°

>10 9

a, 8 Ni 2 6 I 5 a-, 4 r. 3

2

>40 o 9 el

R41 N 6 1 5

in 4 3

ct 2

ti IO

112

5°-

157

5°

202

5°- 2

47 5

° 29

2 5°

- 3

37 5°

2 2

1 2 3 5 1

2 2

4 5 2 5 1

1 2 4 7 1

2 1 1

3 3 13 1

4 9 2 1 14 2

1 1 3 4

1 4

5 10 2 10 2

2 4 9 2

1 4 1

3

1 1 5 5 1

2 4

.40 9

tr' 8 N N 6 1 5 tr.,4

t-3 2

>10 e 9

T N6 I 5

4

9 N e N N 6

1 5 0 4

P. 3 2

1 5 N 4 N. 3 t17 2

H .19

>10 9

22 5°

- 67

5°

112

5 °-1

57

5°

2 S 1 7

1 2 4 7 7 1 6

2 1 2 1 4

3 1 1

2 2

3 1 3 2 8 7 1 5

112 5

°- 1

57

5°

4

2 2 1 1 4 1 1

1 1 1 3

11 4 7

2 3 3

4 2 2 2

;

T <51 6 1 8 1 10 1 12

1 1 1 2 2 6 3 2 4

3 2 5 1

3

14 >15 3 71451 6 18 1 10 1 12 1 14 1,451

BLOCK: C 7

H >10

9 f'n N 7 N 6

j 5 ,r1 4 rin. 3 >I 2

>10 9

N 7

1 5 4

r- 3 W 2

>10 9

Y7

C1; ( 1 5 in 4

>10 e 9 In

7 N 6 1 5 1

En 4

(11 2 1,- 3

202

5°-

247

5°

2

3 1 2

11<51 6 1 8 1 10 112 1 14 1.15 E T <51 6 1 8 1 10 1 12 1 14 1,451 X

BLOCK: CS




APPENDIX FIGURE 21b: Directional Wave Statistics for September

MO 9

N 76

w

I 5 • 4 r- 3

3.10 9

fn N 7 2 6

6 9 7 2 4

1 5 2

4 1 4 3 1 3 1

610 9

in ° N 76

I 5 II, 4 rs 3 W 2 11

2 5°

-1

57.

5°

202 5°-

24

7 5°

3 4 6 13 4

1 1 4- 3 N 2

2

2 S 5 11 4 1

1 1 1 2 3 1

1 1 2 1

112 5°

-157

5°

202 5°-

24

7 5°

H >10

9 e

N 7

eI5 ▪ 4

N 6

✓ 3

2 2 1

610 9

rel e O 7 r 2 6 I 5

4 rz 3 tn 2

1

610 9

7 N 6 I5 a, 4

N. 3

N 2 1

1 5 rs, 4

0- 23 1

610 9

1

4 5 2 1

2 1 3 6 1

1 3 13 2

1 3

4

2

2 1 8

1 1

5 6 2 5

1.

N

3 14 1 13 1

3 2 2 1

1 1 1 3 1

1 1 2 4

1 4 10 4

1 1 1 3 4 2

112.5°-

157

5°

202.5°- 247

5°

292 5°

- 337

5°

1 2

1 1 12

4 11 2 12 1

1 3 3 2

2 1

H >10

9 VI N 7 N 6

112

5° -

157

.5°

1 1 3 1

4 1 4 4 1 2 1 1

in

aA

5 in 4 1.;) 3 M 2

1 5 a, 4 P.. 3 12 2

X

>10 .10 ▪ 9 e 9

o 6 in t'8

in M 7 CM 7

N6 .1 N6

I 5 I 1 5

.31 4 ,,,, rn 4

E r-: 3 X 2

1

E X

T <5 I 6 1 8 1 10 1 12 1 14 1.15 E T <51 6 1 8 1 10 1 12 1 14 1.151 X

BLOCK: C9

3 2

3 1 3 1

22

5°-

67 5

°

1 1

T <5I 6 1 8 1 10 I 12 1 14 1 615 X T1451 6 I 8 1 10 1 12 1 14 1.151

BLOCK : C 10 H

MO 9

th 8 N 7 N 6

2 2

610 9

fh (-11 I 5 a, 4

p- 3 1D z

610 9

e N 7 2 6 1 5 ro 4 p- 3 12 2

X

2

>10 • 9 IP 8

7 N 6 I 5

Eh 4 N 3 X 2

1

71.51 6 1 8 110 1 12 1 14 1 .15 E T <51 6 1 8 1 10 1 12 1 14 1.151 E

BLOCK: D5 T <5) 6 1 B 110 112 1 14 1.15 E 11451 6 1 8 1 10 1 12 1 1416151 X

BLOCK:D6

I 5 10 4 N 3


H— WAVE HEIGHT IN METRES. T — WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 21c: Directional Wave Statistics for September


H — WAVE HEIGHT IN METRES



APPENDIX FIGURE 21d: Directional Wave Statistics for September

112.5

° -1

57. 5

° 20

2 5°

- 24

7 5°

g3 rr,

T <51 8 1 El I 10I 12 1 14 1.15 E Tl< 5 1 8 I 1 10 1 12 1141.151 £

BLOCK:D7

1 1 2

202

5°- 24

7 5°

7 <51 618 I 701 12 1141,15 E Ti<51 61 8 I 101 121 141,151£

1 12Y

-157

Y

292

5° -

337

5°

26 I 5 5, 4 rs n 2

.10 9

N 7

22

5- 67

5°

9

; I 5 1

5, 4 1 7- 3 1 3 w e 8 12

5

>63 e 9 ul

N 7 6

I 5 in 4

O :

H

9

111 cv

I N 6

A 2

th 4 I.- 3

2 2 4 1 1 1

1 4 3

1 2 1 7 5 1 1 1 1

1 2 2

6 2 1 3

1 8 6 7 2

BLOCK: D9

H MO 9

tn 8 N 7 N 6

In 5 In 4 w, A 2 4

a

1 2 1

2 1 2 9 3

O : V7 N 6 I 5

4

O • 2

71 <5 I 6 I 8 1101 12 I 14 1.15 I <51 6 1 8 r 10 1 12 I 14 1.151 £

BLOCK:08

1 2

40 9

112. 5°-

157

5°

202 5°

- 247 5°

.10 9

ih

0 N 15

Tn 4 ▪ 3 'n 2

3 1 4

1 1 1 2 1 8 4 1 1 1 1

H NO

9 in 8 N 7

I rn

N 6

N 3 2 2

2 2 1

3 1 1 2

1 7 6 8 3

292 5

° - 337 5°

N N 1 5, 8 N

112 5°

-157

. 5°

26 I 5 5, 4 r-

z

H09

in N

21

.10

H09

I 5 rr, 4 1••••3 W 2

1 1 3 1

1 2

4 1

2 3 9 7 4

1I 2 1

1 3 1 3 2 9 3 1 4 3.

>10

o 9 in

N 6 I 5 in 4

1

7 <51 6 I 8 I 10 I 12 1 141.15 E T <51 6 I 8 110112 1 14 1.151 £

BLOCK:DIO

MO 9

117 ;

I 5 4

r- 3 W 2

9 in 8 tv 7

I 5 rr, 4

N 3 e 2

>10

in 093

7 N 6 I 5 N4

H >10

9 in a N C■1 6

o 5 N 4 r-

A 2

1 3 1 2

3 2

1 2 2 6 7 1 8

1 2

3 1 6

292 5

° -

337

5°

1 5 4

1 1 2 2 7 5 1 a

1 3

3 1

2 2 2

T <51 6 1 8 1 10112 1 141>15 £ T <51 6 1 8 1 10 1 12 1 14 1 >151 £

BLOCK: E8

225°

- 67

5°

112 5°

-15

7. 5°

>10 9

in 8

20

2 5°

- 24

7 5°

N 7 C96 1 5

4 r 3 _2

0.1 6 1 5 th4 'A 3

2

>10 9

tn

N 6

I 5 tr, 4 ✓ 3 432

>10 o 9 In

ON 7 N 6 1 5

al 4 N. 3 N 2

1 5 4 6

1 1

11 2 1

4 11 9 1

5 3

2 3 6

10 9 1 4

1.5161131 101 121 141.15£ 1<516181 101 121 141.151E

BLOCK: F7

2 1 3 1

292

5° - 337

5°

>10 e 9 In

M 1'1 6 1 5

in 4

H >10

9 al 8 N 7 N 6 1 5

111 4 1•■ 3 P2

2409

e tn.

I 5 tn 4 ✓ 3 t0 2

26 I 5

1

>1:

rn 8 151 7

.f'n 4 r- 3 u" 2

In

ID

tn 11

2.5°

-15

7.5°

20

2 5°- 24

7 5°

22

5°- 67

5°

112 5

° -1

57 5°

202

5° -

247

5°

1 1 3 1 4 6 1 2

2 1 2 6 1 4 8 3 2 3

1

1 1

4

: 3

1 1

14 4 2

1 2 5 6 5 7 1 3

1 3 1 2 2 2 1 2 2

2 1 3 1 5 1

1 1 2 1 2

9 8 1 1

APPENDIX FIGURE 21e: Directional Wave Statistics for September

>10 O 9 01 8

617

1 5 4

:

>10 9

1 5 rn 4

3 (0 2

>11:91

e

1 5 tn 4

H >109

tn° 8

N 6 1 5

in 4 s: 3 2 2

2 1 1 9 10 9 2

2 2 2 1 2 1

2 2 7

>8) 9

'en 6.1 7 2 6 1 5 th 4

3 2

10 • 9 In

m 7 rs.1 6 I 5

in 3

N 2

9 8 7 6 5 4 3 2 33

7 5°

-22

5°

.40 9

< 8

,176

1 5

✓ 3 W 2

1 4 3 6

2 1 1 11 11 6 1

3 1 1 3 1

292.

5°-

33 7

5°

202 5°- 24

7 5°

112 5°

-15

7.5°

2

2 5°

- 67

.5°

2 2

2 2 1

1 1 12 4

5

5 7 7 8 1 4

111 4 e- 3

2 1

>10 9

N 57

1 5

M 3 >4 2 1

2 1 3 1 4

4 6 1 2 7

T1451 6 1 8 1 10 1 12 1 14 1.15 E T <51 6 1 8 110 1 12 114 1.151

BLOCK: G8 H

>10 9

N e N 7

>10 9 8

51i76 I 5 ft', 4 1, 3 ‘1) 2

.10 9 e

0 N 7 0.1 1 5 0., 4 t■ 3 N 2

.10 o 9 ul 8g 7 N 6 I 5

N 4 V 3 csi 2

11451 6 1 8 1101 12 1 14 1.15 I T 451 6 I 8 I 10 I 12 I 14 1 >15 I

BLOCK: H6

NOTES:

7 <51 6 1 8 1 10 1 12 1 14 1.15 E 145I6181 10 I 12 I 14 1.161 I

BLOCK: H5 H

.109

° N 7 N

ol 5 In N: 3 2 2

.10 9 ° ;

1 5 4

t- 3 W 2

.10 9 e

0 7 N 6 I 5

4 o- 3 'I' 2

.10 9

NM 7

1 5 11 4

Na

71 4 5 1 6 1 8 I 10 112 I 14 1.15 E 714 51 6 I 8 I 10 I 12 1 141>151 I

BLOCK: H7

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H— WAVE HEIGHT IN METRES T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 21f: Directional Wave Statistics for September

22 5- 67

5°

112 Y

-157

5°

1- N 1 N

112. 5

°-1

57

5°

202.

5°- 24

75°

N6 .1 5 111 4

3 In 2

•

: 8 N7 N 6 1 5 474

112

5° -

157 5°

20

2 5°- 24

7 5°

4,

1 7 5 7 2

1 3 6 5 3 1

1 1 1 1 3

1

2 2 1 6 9 1 6 3

1 6 1

rs,

61

112

5°-I5

75°

20

2 5°- 24

7 5°

.10 9

N 137 6

1 5 tn 4 t-3 (6 2

.10 9 e

1 5 tr, 4 I- '2 2

>10 • 9 W

2

7 N 6 I 5 in 4 IN 3

H TIO

9 rn 0.1 7 N

I 5 th 4 t- 3 t0 2

>10 9 8

M 7 N 6 1 5 rr, 4

E

>10 o 9 'O9 S4 CY 6 1 5 -l 4 1- 3

2 1

1 1 6 6 7 1

1 1 5 7 2 1

1 5 7 2 1

1 1

1 2 3 3 1 5

1 1 1 3 1 3 8

2

1 1 3

1 1 4 5 4 1

1 1 1 2 5 2 1 1 1

5

2 1 1 6 2 4 8 4 1 1

2

1

1

1 1 2

1 3 2 7 8 1

1 1 2 1 1 2 2 1 2 2

2 1 1 3

1 1 1 4 1 4 6 1 1

4 1 3 6 2 3 7 1 2 2

1 3

1

1 1

6

1 1 1 3 6 2 3 1

2 2 1 6 10 1 5 2

5

1

4 2 4

1 2 1 4 4 7 1 2

2 2 1 7 3 4 6 2 1 1

1 1

1 1

H >10

9

22 5°

- 67 5

° 11

2 5°

-157

5°

20

2 5°

- 2

47 5

°

N cv 7 N , 6 1 5

'.10 9

in 8 Esi; I 5 1 2

fr, 4 3 3 1 1 3 ko 2 5 5 1

'10 .9

*we

F:11 ; I 5

0 1 '1 es. 3 1 1 2 "" 2 4 2

1 1

'.10 o 9 0.8 V 7 cv5 I 5

to 4

71.516181101121141,ME 745I6181101121141..1511

BLOCK: HS


H— WAVE HEIGHT IN METRES. T— WE PERIOD IN SECONDS.


APPENDIX FIGURE 21g: Directional Wave Statistics for September

TI 9 5 1 6 1 8 1 10 I- 12 1 14 1.15 E T'.516181101121141'.151 3:

BLOCK: CI

3 2 1 17

8 14 5

>10 9 e

N 7

1 5 en 4

3 12 2

1

202.

5°-

247

5°

ID

ri•c51e1e11011211e 1.15 E r<316181101121141.telE

BLOCK: C2

N

in 5 Lrl 4

M2 rs 3

112 V

-1

57. V

>10 9

▪ 8 7

c=j 6 1 5

fb 4 es 3 ID 2

.10 e 9 (0 a

? N I5

IN 4 1,- 3 X' 2

9 15

5

1 4

10

12 1 1 3 7

1

11 1

1 6 2 1

1 3 1

6

iy

1125

°-157

5°

112.

5 °-1

57 5°

>10 9

0

11)

N

5, AI 6 1 5

'en 4 3

In 2 1

202.

5°- 24

7 5°

0 0 0

H .10

9 N N ? N I50

111 4 re: 3 2 2

.10 9

N • ; 1 5

f'n 4 r• 3 '5 2

.10

M 7 6 15 al 4

cri.■ : 1 I

1 4 1 5 6

11

6 1 4

1 1 3 1 2 3

11 1

4 2

1 1 2 1 4 1 8 7 1

3 3

2 2 13

.40 9

N 87 6

1 5 a, 4

(71 :

el0 9

:I N 1•1 6 1 5

rei 3 en 2

.10 9

,n9 N

1 5 a., 4

3 tn 2

.10 . 08 V7 " 6 1 5 al 4 r- 3 'X 2

2 1 1 4

10

1 2 1

7

2 6

H .10

9 rn 9 N ? N

5 91 4 • 3 M 2

1 I

.10

N N 6

6 5

rn 3

N c

I

.10 9 7e

111 6 I 5 a, 4 rs 3 19 2

.10 9

04: 1 5 a, 4 e. 3 • 2

2 2 7 5

10 2

11 1

In

202

T-2

47

5°

112

5° -

157

5°

14 5

1

13

2

1 4 1 3

>10. • 9

7 N 6 1 5 in 4

3 N 2

S 4 5 2 1 1

22

5°- 67 5

°

2

1 2 4 1 3 1

1 1 6 6 2

13 1 I 12

5°-

157

5°

20

2 5°-

247

5°

2 3 2

2 1 2 1

1 1 1 1 3 2 1 1

3 2 1

12 4 8 1

'10 9

N N 7 N 6 1 5 in 4

3 In 2

em0 9

e 8

IS 3_, 4 r- 3 18 2

>10 9

in 6

x

1 5 N 4 r- 3

>10 9

of 6

N 7 6

1 5 GI 4 1, 3

2 1

11

2 5°

-157

5°

202 5°- 247

.5°

>10 9

1 5 4

tZ 3 '8 2

1

>10 9

in

CZ 16 1 5

4 tz 3 8.) 2

1

2 7 5 3

13 1

3 4 1 6 2

2 1 1 1 2 2 2

2 1 2 2

11 3 9 2

2 2 1 2

2

2 6 2 4 2 2 6

1

4 5 3

1 3

1 3 1

24 3

3

1 2

1 1 5 5 4 7 1

11 3

2 2 2

112 5

°- 1

57

5°

20

2 5°- 247

5°

29

2 5°

- 3

37 5°

3

4

1 1

6 3 10 3 1 5 1

1

4 7 4 5 1 1

10

k

2

2 1 2 4

1 12.5

°- 1

57.

5°

20

2 5

°- 2

47 5

0

1 1 1

1 1 1 6

2 2 2 1 2

1 2 2 2

4 8 4 6 1 5 1

1 5 rn 4 r'n 3 WI 2

H >10

9

tr! 8 N 7 N 6

.10 9

N 7 = 6 1 5 • 4 • 3 w 2

.10 9

318 N 7 26 1 5 a., 4 1, 3 02

>10 • 9 0. 01 7 N 6 1 5 in 4

N3

2

H >10

9

N N N 6 .1 5 113 4

2 2 1

.10 9

H V 6

I 5 4

▪ 3 ig 2

>10 9

N 8 7

N 6 1 5

4 r3

V2

.40 e 9 6 01 7 N 6 1 5 fr', 4 1, 3 gi 2

1

T1 <5 1 6 1 8 1 10 1 12 1 14 1.151 I T1.51 6 1 8 1 10 1 12 1 14 1.15

BLOCK: C5 T <51 8 1 8 x10 1 12 114 (>15 I T <5I 6 1 8 1 101 12 1 14 1.151

BLOCK: C6

Ti<5 16181 101 121 141.15II 71.516181 101 121 141.151E

BLOCK:C7

NOTES:

7 <51 6 1 8 1101 12 1 14I>15 I T <51 6 1 6 1 101 12 1 14 1.151 E

BLOCK: C8

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES



APPENDIX FIGURE 22b: Directional Wave Statistics for October

3 5 2 2

2 3 1





3 1

APPENDIX FIGURE 22c: Dire cti onal Wave Statistics for October

N N 6 1 5

MO 9 8

;

1 5 tr, 4 N3 w 2

MO 9

to

(0J 76 1 5

50 4

g 7 NI 6 1 5

tO 4

:

X

T11.5 I 6 1 8 1 10 1 N 1 14 1.15 X T <51 6 1 8 1101 12 1 141>15l Z

BLOCK: C9

tO 4 1:-.1 3 rn 2

>10 o 9 'n6

Ti<516181101121141.15 X T<5-1 8181101121141.151E

BLOCK : D5 11.51 6181101121141>15 I 1.516181101121141>15

BLOCK: D6

rn

112.

5* - 15

7.5*

20

2 5°

- 24

7 5°

0

P

N 1 2

N N 6

8 0 4 N 3 2z

Is

N3 W 2

NI 7 ic.1 6 1 5 rn N 3 '2 2

H MO

9 u,8

>10 • 9 41 a Si 7 N 6 I 5 in 4

: rs*,. 3 N 2

>10 9

>10

El

21 rko I 6 1 6 1 10 112 I 14 1,15 T <51 6 1 6 110 1 12 I 14 >151 2

BLOCK: CIO

in

In pN

2 2 3 1 2 1

4 4 8 3 4 4 1 1

3 2 5

1 1 5 4 1

3 4 3 1

1 2

1 7 1 1 0 2 3 1 3

1 2 a 1

MO 9

rn (aI ;

1 5 4

A 3 W 2

2 2

1

2

1 7 1 4 4

11 2

0

2

6 1

6 3 7 3

0

N N

1 1

1 3

3 1 2 1

2 1 1

5 1 5 1

3 2 2 9 3 9 1

H MO

9

8 N 7 N 6

j 5 in 4

rn3 2

H >10

9 to N 7 CV j 5

4

;

El

>10 9

'in 8 ;

I 5 a, 4 A

>10 9

in N 0 m6 15

522

>10 o 9

e 7

1 5 Pn 4 I., 3 X 2

10

In

.10

5N 7 2 6 I 5 th 4 N 3 '2 2

1

9 '81

N6 I 5

en 4 N 5 N 2

1

1 1 1

2 1 5 1

1

2 2 2 1 9 4 7 1

1 2 1

1

t 3 5 1

3 2 1

1 1 2 2

1 1 3 1 3 1

2 5 6 5 5 2 2 1

1 1 1 1

2 5 2

4 2 1 3 3 1

1 1 3 3 1 7 1

1 1 2

2 1 4 5 1

>10 9 e

cst ? 6

1 5 11.., 4

5 in 2 2

02

V- 24

7 5°

20

2 5°

- 247

5°

112 5

°-1 5

7 V'

112

5°-1

575°

29

2 V

- 337

5°

292 5°

- 33

75°

1 1

5 4 1 3

5 2

Yi

H >10

tel • ? NI 6 1 5 th 4 fI3

1

1 2 4 2

>10 9

to 57 6

5 'a, 4 rs: 3 W 2

>10 o 9 Eno

Mil Nu 6 1 5

4 3 2

1 1

3 1 1 6 1

1 1 3

1 3 2

5 5 2 1 2

1 1

3 2 7 1 1

1 1 4 1 4

4 5 6 4 5 3 4 2 1

1 1 1

3 1 4

1 3 6 7 2 4 3 4

1 1 1 4

5 1 1 2

1 1 2

1

1 3. 1 3 6 1 1

Tl<5 1 6.1 8 1 10 I 12 I A 1.15 Y T <51 6 1 8 1 10 1 12 1 14 1 >151

BLOCK :D7

1

1 4

10 2 1

1 3 1

1

4 4 2 5 1

1 1 3 1

1

5161 91 101 121 141.151I 11<516181101 121 141.152 1 4

BLOCK: D8

292.

5°-

337

.5°

202

5- 2

47 5

° 11

25°-

157

.5°

>10 9

'en 87

IS N 4 ID 3 ID 2

1

.109

N 8 cV 7 (9 6 1 5 rn 4

N 3

42 2

>10 o 9 11/

M CV 6 1 5 In 4 r- 3

2

H

>10 9

e! 8 4

Fr) 8 Cu 7 Csl 6

wAi 3 1.1 2

2 1 1

1 2 4 1 5

1 2

1 3 6 7 8

10 1

3 1

1 4

1 1 6 2 2 8 6 1 1

112

5°-1

57.5

°

>10

I S 4

ts 3 2

>10 9

in 8

O 7 cs., 6 1 2

4

i23 2

>10 o 9 0. 8 Pi 7 N 6 1 5 274 1:3; 3 N 2

1

:11

N

2

2

3 2

2 3 1 4 1 3

H

10

In

iy

51

1

3 1 5 4 1 1

2

1 5 3 7 2 1 6 2

H >I0

9 Fele N (s.1 6

eI5

4 5

2 2

>10 9

rr, 7 1 5 fn 4

5 W 2

1

>10 9 8

0.1 7 6

1 5 4 3 2

>10 e 9

e

M 7 N6 I 5 in 4

sc:3 ▪ 3

1 1 3 4 1

3 1

1 3

2 3 1 1.

4 2 1 2 2 1

1 3 2

>10 9

8 ,1J

I 5 tr, 4 r- 3 W 2

010 9

toe

0 N7

me

15 .64 N3 o 2

6

2 1 5 2

1 3

22 73

5 1 1

1 3 B

1 2 7 5

2

3 3 1

1 1 1

1125°

-1575°

202 5°- 24

7 5°

H >10

22

5°- 67

5° 9

tn N 7 N 6

1 1 4 9 1

202 5°-

24

7.5°

H >10

9 8

N 7 N6

I 5 N 4

23

>10 9

IJ 7 = 6 I 5 N 4 N 3 W2

6,

to

Ri

112.

5°-

1 57.

5°

>10 • 9

a V7 N 6 I 5

rn 4

2 5 8 1 2

2 1

2 6 5 1

2

1 1 1 1 1

1 1 1

2 2 2

4 3 1 1 2

1 7 4 2

2 4 2 1

>10 o 9 0 6

7 N 6 I 5

fn 4

;7;

1 1

1 2 8 3 1

2 1 3

2

4 1 7 1 1 1

4

2 4 2 1

Rb R1

112

5° -

15 7

5°

H >10

9 in cv 7 N 6 is 0 4 N 3

2

>10 9

tn CY. 6

I 5 th 4

3 ° 2

In N

T <51 6 I 8 I 10 I 12 I 10 1.15 X T <51 6 I 8 1 101 12 I 14 1.151

BLOCK: F8 T145161111 101 121 141.15X 8 8 110 1 12 1 14 1.151 E1 151z

BLOCK: G7




H >10

9

N 8 N7 MI 6

1 5 0 4

3 2

4 2 2 4 2 5 9 1 1 4

20

2 5°- 247 p°

>10 9

ti/ N7

6 15

4 N 3 4/ 2 2

02.x- 24

7 5°

1 1 1 2 1

2 1 2 1

1 1 5

Si 7 cs, 6 I5 th N 5 N

▪

2

>10 o 9 '

N 6 I 5

rn 4 N st& 2

>10 9

:I 8 ;

I 5 4 3

w

1 1

6 8 1 1

1 3 1

1 2 5 4 1

1 1

1 2 4 3 1

3 1

3 5 4 1

6 3 9 1

5 3 1 1

2 3 2 3

1 2 1 1

2 1

TI45 I 6 I 8 I 10 I 12 I 14 1.15 X TI 4 5I 8 I 8 1101 12 1 14 1.151

BLOCK: E 8 TI<5 I 6 I S 1101 12 1 141.15 E T <51 6 I 8110112114100013:

BLOCK: F7

APPENDIX FIGURE 22e: Directional Wave Statistics for October

N

A

th

202

5°- 247 5°

11

2 5

°- 1

57

5°

225°

- 67

5°

1 2 1

3 1 2 1 2

1 3 2 4 2 1

4 3 1 3 3

2

H

9 to N 7 I 5 dl 4

3 en 2

4

6 1 6 1 1

6.10 9

?„,

(I' 1 5

4 D. 3 'D 2

.109

rn a

5 11, 4 5 3

1 7 3 1 .r;-3 : 7 6

2

1 1 10 2

7 1 5 3

240 9

I 5 N 4

3 W 2 11

2 5 °

-15

7.5°

.10 • 9 4? SI

5 I 5

In 5

A 2 1

1 2 3 5

10

1 1 2 2

2 2 1 2

1 2

4 7 4 4

2 1 3

1 8 9 3

292 5°

- 3

375°

71.51 8 I 8 1 10 1 12 I 14 1.i5 E T <51 6 1 8 I 10 I 12 1 14 1 6.151 I

225°- 67

5°

112

5°- 15

7.5°

2

025°- 247

5°

• 9 in 8

Mi 6 I 5

C1 4 D. 3 it 2

H

9 N 8 N 7

1 5 65 4 D.3

2

MO 9

; I 5 g, 4

C15

2 1 1 2

1 6 1

1 3 3

10 1

1 4

7 2 4

2 6 1

2 6 6 2

2 3 1 2

3

3

6 2 7 1 1

112.

5°- 15

7. 5°

202

5°- 24

7 5°

fN

Pr)

6.10 9

N 8 ;

15

,n 4

.10 9

rn EN 7

e 1

a„ 4 1, 3 E) 2

H .10

9

I 5

to N (6 5

N 4 Dz 3 2 2

1 7 2

1 9 2 4 4

1

3 3 2 8 1 4 6 1 2

1 1 4 2 2

2

4,

N

.10 • 9 65 8

I S in 4

3 X 2

T <5 I 6 1 8 I 10 I 12 1 14 1.15 Z T <51 6 1 9 I 10 I 12 I 14 1.15

BLOCK : G 8 T <5 1 6 1 8 I 10 1 12 I 14 1.15 E T <51 6 I 9 I 10 1 12 I 14 1.151 X

BLOCK : H 5

1

1 1

BLOCK: H6

.10 • 9 65 8 N7 5.1 1 5

th 4

: 1

7451 6181101121141,15 E T<51 6181101121141.151/

BLOCK: H7


H — WAVE HEIGHT IN METRES T WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 22f: Directional Wave Statistics for October

>10 9

N 8

;

I 5 rn 4 r. 3

2

>10 9

to N 0 N 6 I 5

1.0 4

II .10

9 to 8 cv 7 04 6

4,

tO I 5

11)4 1 3

4 7 3 .0 2 2 6 2

1

2 1

1 8 3

1 7 1 4 3

1

112

5° —

157.

5°

?. 2 5 2 2 4 3 1

4 3 2 7 2 4 2 1 2

20250

_247

5e

2 1 1 2 1 2 2 2

1 1 1 1

P

an

.10 e 9

OM 7 CM 6 1 5 to 4 14- 3 N 2

110 101 12 I 141e.15 I T 45I WI 1 114 141.15IE

BLOCK:HS




APPENDIX FIGURE 22g: Directional Wave Statistics for October

2 3 2

9 2 12 5 1

H H

+10 9

to N N 6 1 5

3,4 >11..- 1,1 2

H

2

2 2 3

N

U1

3 3

3 1 1

.10 9 B

N 7 N 6 I 5 to 4 f•Z 3 2 2

2 2 1

2 3

113

1 1 3

3 1 1

74616161161121631.16z 1,616161631121631>I6rz

BLOCK: CI

7 <51 6 1 8 1 10 1 12 1 14 1>15 E T .51 6 1 8 1 10 1 12 1 14 1 >151 E

BLOCK:C2

>10 9

N N

510 9

N. N

N 6 N 6 1 5 5 1

111 4 1 Pn Ln 4 1 1 r- 3 2 1 9.: 3 1 2 102 2 1

1 5 22 2 1 2

1

>10 >10 9 9

• 8

V. 76 511 6

1 5 1 5 fr) 4 4 r■ 3 r- 3 1 1 up 2 15 6 1 2 2 3 2 5 4 1

1

>10 >105 9

;he N 7 6, 7 RI 6 (C1 6 1 5 1 5 3, 4 1

" 4 1

1`3 u) 2

25 2 12

2 3 ti5 :

2 6 3

9 15 1 7

>10 >10 • 9 in 8

N 7 V 7 1,1 6 N 6

1 5 1 5 N 4 1 1 fl) 4

'774 32 13 1 3 3 V r- 3 N 2 10 3 5

2 5 1

7F-5-1- 67 8 1 10 1 12 1 14 1.15 755 1 6 1 8 1 10 1 12 1 14 1 9151 E <51 6 1 8 1 10 1 12 1 14 1 >15 E

BLOCK: C3

NOTES: —DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES




APPENDIX FIGURE 23a: Directional Wave Statistics for November

112 5

° - 1

57 5°

112.5

° -

157

5°

202

5°- 24

7 5°

202.

5°- 247

5°

292

5 °- 33

75°

292

5°-

337 5°

7 <51 6 1 8 1 10 1 12 1 14 1 >15. X

BLOCK: C 4

>10 9

1 5 fr., 4 r- 3 W 2

•

>10 9 B

V 0 N 7

N N 6 1 15

tO fe, 4

6 1 N N 6 1 1 ;1 - 1 23 7 1

6 1 9 4 9 2

>10

111 V 7 N 6 I5 tn 4 r- 3 • 2

>10 9

to 8 N 7

1 5 N 4 r- 3 E 2 20

2 5°- 24

7.5°

1125

° -

157.

5°

1 5 fb 4 r- 3 tp 2 11

2 5°

-15

7.5°

29

2.5°

- 33

75°

"0 9

• 8 ,

N

>10 • 9 in 8

N 7 6

1 5 to 4 1.- 3 N 2

4 3 3 2

1 10 1 9 6

1 2 5 3

3 6

4 3 6 2

3 4

7 2 12 6

3 3 1

1

1 1 2 2 5

1 7

11 4 11

2 4

1 2 23 5 4 1

7 .51 6 1 8 1 10 1 12 1 14 1.15 E T .3 1 6 1 8 1 10 1 12 1 14 1.151 Z BLOCK: C5

22 5°-

67

5°

112 5

° -1

5 7 5

° 20

2 5°

- 247

5°

en

.10 9 rn 8 N 7 N 6 1 5 in 4 rti3 In 2

£ >10 9

I 5 ar, 4 re 3 w 2

>10 o 9 to 8 N 7 N6 I 5 in 4 re5 X 2

>10 9 fn 8 N 7 2 6 1 5 N 4 re. 3 ▪ 2

33 2 3 1 1 3 1 1 2 1 1 2 1 3 1 1

31 2 1 1 1 1

1 12 2 3 3 1 6

1 4 8 1 2 1 2 71 1 1

112

5° -

157 5°

T.51 6 1 8 1 101 121 141.151E T.516181 101 121 141.151E BLOCK: C7

>10 9 .

•

13 ; 1 5 N 4 • 3 W 2

202

5°-

24

7 5°

910 9

CCX N6

2

1 5 rr, 4 re, 3 11

>109

0 N7 Ne 15

1 3 2 4 1 3

1 2 2 2

22 6 2 1 2 2 1

H 910

9 rr, 8 N 7 N 6 1 5 in 4 3 In 2

£1

2 26 1 2 1

2 32 8 1 3 3 1 21 1 6 3 1 5 1 1

11 2 3 1 1 3 2 1

>10 9 N 8 N 76 1 5 in 4

>10 9 isr,8 N 7 6 1 5 an te• 4 3 8/2

910

el 5 .4

9

e N 7 N 6

3 E

20

2 5°

- 24

7 5°

22 5°

- 6

7 5°

11

2 5°-

157

Y

910 e 9 8 1 5 In 4

841 N 6

1 11 4 2 7 2

2 2 3 1 6 2 1 1 1

1 22 2 3 1 1 1 4 1

1.

1 13 1 2 1 1

4 1 21 1 4 2

>10 o 9 0. 9 g 7

6 2

1 5 1

Fn 4 Pn

f43 /4 2 1 1 2 2 2

T1.5 1 6 1 8 1 10 1 12 1 14 1.15 E T 451 6 1 8 1 10 1 12 1 14 1.151 E BLOCK:CS

to N

Pn pN

112.

5° -

157

5°

>10 9 4'1 8 N 7 2 6 15 To 4 N 3 2

H 910

9

e Ni

fr. ) 4

N 6 1 5 2 2

910 9 N 8 N 76 I 5 th 4 3 87 2

3 16 1 1 1

1 2 1 3 1 2 4 63 1 3 1 1

1 1 12 1 5 2 2 2 1 1 1

1 1 5 1 1 3 1 2 1

1 2 1 4

2

T.5161131 101 121 14 1.18 2: 1.516181 101 121 141.151E BLOCK C6


H — WAVE HEIGHT IN METRES. T— WAVE PERIOD IN' SECONDS.


APPENDIX FIGURE 23b: Directional Wave Statistics for November

292

5°- 33

75°

71..5 I 6 1 8 1 10 1 12 1 14 1815 E T

>10 9

en N 7 N 6

rn

ID 2 1 I 5 3 1 4 'rn 4 2 1 4

1 1 N 3 1 2 2 2 1 M 2 3 4 1 2 2 1

1 1 1 2

>10 9

8 ;

1 5 4 2 1

1 8 n- 3 1 5 1 4 3 1 2 1 1 4 2 2 2

>40 9

of El N 7 0 N 8

1 I 5 1 2 6 4 6

1 er, 4

1?-; 5 11

4 1

1 1 1

4 7

4 1 1 4

3 1 2

tD

1125

°-1

575°

20

2 - 24

7 5°

112

5 °-

157.

5°

202 5°- 24

7 5°

>10 o 9 41 5 M 7 N 2 1 5

1 h 1 2 1 1 3 1 2 2 N 1

1 5 1 gi 2 1 2 2 1 1

<51 13 1 8 1 10 1 12 I 14 1.151 I Tl<518181101121141.15 E 1<518181101121141.151E

H +i0

9 B

(s, N 6 I 5

en 4

In 3 ro 2

1 2 1 1

1 3 2

4

1 1

1 3 1 8 1 2

1

1 1 3 2 2

2

>10 9

N

1 5 rr, 4 N. 3 48 2

810 9

of e (01 7 NI 6 I 5 th 4 1- 3

2

>10 e 9 Lc) 8

M 7 ni 6

r- 3 NI 2

H

>10 9 B

N 7 N 1 5 1

1 1 an 4 1 3 rn 1 1 2

2 2 2 1

4 3

1 3 5

2 1

1 1 2 1

112.5

° -

157.

5°

202 5°

- 247

H >10

9

tr! 8 N 7 N 6 o! 5

4 • 3 n 2

>10 9

I}, 8

;

1 5 ▪ 4 r- 3 W 2

>10 9

N 7

I 5 ▪ 4 ▪ 3 422

>10 o 9

e ONE 7 N6 I 5 ho

X' 2

112 5

° -1

57.

5°

202 5°

-24

7S°

1 3 2 1

11 2

1 4 2 3 2 3 2 1 1

1 1 3 2 1

1 13 1

810 9

0.1 o 8

7 .c\-1 6 1 5

er, 4 n• 3

2 1

.10 9

N

iCZ ; I 5

'en 4 N 3

>10 e 9 ▪ e

IS Po Ii 3 N 2

1

12 3

1 2 1 1 1 1

2 1 2

2 1 1 7 3

2 2 1 3 1 6

6 2

12 3 1 3 1 1 1 1

7 1

2 2 1 12 3

3 " 4

3 2 3 1 1 3

1 9 2 2 1 2 1

BLOCK: C9

BLOCK: CIO

71.c 5 I 6 I 8 I 10 1 12 I 14 1.15 E T <51 8 1 8 1 10 I 12 1 14 1.151 E

BLOCK: D5 T <51 8 1 13 1 10 I 12 I 14 1.15 E 7 <51 8 I 8 110 1 12 I 14 I >151 2

BLOCK: D6



T — WAVE PERIOD IN SECONDS.

— new OCCURRENCE REFERS TO A SIX HOUR MEAN.

APPENDIX FIGURE 23c: Directional Wave Statistics for November

N6 1 5

N 4 I, 3

N 2

T45161131101121141.151 1<518181101121141r1513:

BLOCK: D7

112 5

° - 1

57. 5

° 20

2 5°

- 24

7 5°

H .10

9 N8 N i Of 6 1

1 5 1 1 2 5

th 4 rz 3 2

1 3 6 2

2 1 M 2 1 6 1

a10 9

in 8 0 N 7 N6 15 N4 3

5 4 1 tt!.2 2 8

1 2 1

6 1 7

>10 9

N 6 ai 76

1 5 2 N 4 2

1 p- 3 1 3 '8 2 2 1 1 3 2

.10 0 9 c! a

N 6

g

1 5 in 4

3 2

El

1 1 2 2

< 5 1 8 I 8 110 1 12 1 14 1.15 E T <51 8 I 8 110 1 12 114 1,151E

BLOCK: D8

112

5° -

157.

5°

292.

5°- 33

75°

H .10

9 N8 N 7

I 5 N 4

3 f^2

2

3 1 7 2 7 2

N6

.10 9

N8

1 5 N 4 r- 3 '8 2

>10 9

Ne N 7 R., 6 1 5

N 4 r- 3 w 2

3 1 2 3 3

3 1 5 1

4 2

3 2 3

2 1 1 5 2

10

3 2 1 5 1 2

1 1 5 3 1 8 2

2 1 5 1 1 2 1 1

1 6 1

2

4 2 7

7 2 1 112

5.-1

57 5°

112.5

° - 1

57. 5

°

1 5 N 4 r- 3

2 1

202

5°- 24

7 5°

>10 9

N 8 •

O

2 4 0 2 N 3 2 1

11 2 5 1 1 3

H >117

9

N B N 7 N 6 1

3 1 5 2 3 N4

23. 4

1 3 2 1 1 2 Fe 1 2 1 2 2

1 1 2

2 1 1

1 1 1 3 1 5 1 1

2 1 1 1 1 1

5 6 3 1

1

2 3 2 12 4

4

3 2 1 1 4 1 2

.10 9

N6 N ? m e

j 5 4

r- 3 P. 2

040 9

NB

1 5 N 4 r- 3 W 2

ri0 9

N 8 . cv 7 N 6 1 5 N 4 r: 3 u") 2

.10 o 9

6 1 5

2 4 2 1

6 1 1.4 3 N 2

2 1

1 2 4 2 1 2 6

1 1

6 1 8 1 10 112 1 141 >151 E 11<51 8181101121141>15 E 7451 6191101121141,151 E

BLOCK: D 10

292

5'' - 337

5°

1 1 2

Tl<5 I 6 1 8 1 10 112 1 14 1.15 E TI.51

BLOCK: D9

>10

9

8 7 • 6 1 5 N4

6J2 2 1 3 1 2

NOTES: — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES H— WAVE HEIGHT IN METRES. T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 23d: Directional Wave Statistics for November

2 2 5 5

1

1

2

2 4 4 4

3 4 4 1 2

2

NINES: — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES



3 2 5 5 1 1 2

APPENDIX FIGURE 23e: Directional Wave Statistics for November

T <51 6 1 8 1 10 1 12 1 14 1.15 E T <51 6 1 8 1 10 1 12 I 14 1.151 I

BLOCK: E 8 H

>10 9

tn e N 7 cv 6

'64 r- 3

>10 9

N :

1 5 g, 1- 3

2

>109

Frt e N 0 N 6 1 5

en 4

D t■ 3

2

>10 e 9 to

7 N 6 15 in 4

17:, 32 11 <5 1 6 1 8 1 10 1 12 1 141.15 I T <51 6 I 8 1 10—F12 1 14 1>151

BLOCK: F8

11.516181101121141.153: T1<51 6 1 8 1 10 1 12 1 14 1.15 E

BLOCK: F7 H

>10 9

?c, a 0i 7

,1 5 01 4

2

>10 9

IV 7

1S en 4 r- 3 (0 2

0 mi 7 N 1 5

'en 4

to v.: 32

>10 e 9 01 8 V7 N 6 I5

rn 4

'4 3 N 2

El

T <51 6 1 8 1 10 1 12 1 14 1>15 I Tl<51 6 1 8 1 10 1 12 1 141>151 I

BLOCK : G7

1

A2

'en

N

In

N 6

a 9

>10 9

h

1 1

1 10 1 2 1 1

202.

5°- 24

75°

•

>10 9

*

•

8

IO

112 5°

-15

7 5°

20

2 5°

- 247 5°

01 4

H

>10 9

tn N 7 0.1. 6 c! 5

Lt; 3 14 2

IA IO

112.5

°-15

7.5°

>10 9

N 'Yr EY 6 1 5

eh 4

>10

7 0

9 h 8

N 6 15

en 4 tz 3 9- 2

>10 e 9 01 6 V7 N 6 15 rn 4 r 3 N 2

1 5 N 4

3 (.0r.

2

>10 9

'en 8

0 01 7 N 6 1 5 N4 r. 3 52 2

1

>10 e 9 ,n

I S in 4

N 2

2 1 1 1 2 2 a

1 1 1 1 1 3 2 1

11 1

2 3 4

11

23 2

1

1

1 1 1 2 1 3 S 1 2 1

1 1 1 3 5 3

1 2 6 4 24

4 2 2 3 7 1 3 1

1 1 1

2 2

1 1 6 3 1 3 5 2 2

1

1 4 2 2

1 1 1

2 9 1 2 1

2 1 3 5 4

1 1 1 1 1 5 3 9

1 1 1 2

1 3 3 4

1 1 2

1 1 S 2 4 1 1 •

1 1 8 3 5 5

2

1

1 1 1 5 5 1 2

H >10

9 8

? rm 6 1 th 4 N 3

2

.10 ' 9

.1, '71 fsj 6 1 5 N 4 N 3 (02

>10 9

:18 N7 26

1 5 N 4 7- 3 N. 2

E

H

1 3

2 2 1

2

10

3 2 1

1 7 3

3 3 1

>10 9

h tv 7 4%1 1 5

N5 2a

1 3 1

1 1 1 2

1 3

Zi

1 1 1

4 2

1

1 1

1 1

0 4 7 1

1

>10 9

N 6 7

rj 6 1 5 N 4 1.3 10 2

1 3 1

2 1

1 1

1

10 2

9 5

9. N

Epp

2 3

1

3

>10 9

in 8

8 7 N 6 I 5

4 N 3

12 :

>10 o 9

>10

Ln 8 : g 7

6

N 6 IS

In 4 2 1 1 5

4 1 2 1 3 3 1

1 N 2 3.

5 1

71.51 6 1 8 1 10 1 12 1 14 1>15 E 71.51 6 I 8 1 10T12 1 14 1 >15 2: 7451 6 18 110

BLOCK:G8 H H

1

3 1

112 5°

- 1

57.V

1 1 3 2 1 1

gl 2 7

1 1 7

1

1

.40 9

rn.° N N 6

c! 5

11") 4 ■•• 2 23

1

1 1 3 3

4 2 1

1

10

112.5°-

15

7. 5°

N 1

O

N

2

1121141>I5 E r<51sieliolal,41,•151E

BLOCK: H5

>10 9

rn. N 7 Iv 6 1 5 fr) 4 t■ 2 2

2 2 1 9 6 1 1 1

4 5 3 8 6

1 1 2 1 1 2 1

3 3 7 3 2 3 1

8 4 4 1

112 5°

-1575°

20

2 V

- 24

7 V

112.

5 °-1

57

5°

.40 9 • 6

v 76 I 5

fr., 4 r. 3 10 2

.40 9

a,

1 5 iO 4 74 3 tn 2

>10 o 9

e

g 7 A.1 6 I5

Pt! 4 P.: 3 N 2

1

2 2 2

3 2

2 1 7

2

3 2 2 6 3 3

1 3 2

>10 9

:I

I 5 4

7- 3 ° 2

1

>10 9

rrt N 7 0 N 6 1 5

er, 4 3

52 2

>10 5

LH

N6 I 5 al 4 N N 2

1 1

1

1 13 10

1 1 7 0 2 8 5

2

1 5

1 1 4

S

TI <51 6 1 8 1 101 12 1 141.151 E Ti<51 6Ie1101 121141,151Z

BLOCK: H6

NOTES:

7 .51 6 1 8 I 10 1 12 1 14 1.15 E 7 .51 8 1 13 I 10 1 12 I 14 1.151E

BLOCK:H7

— DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES H— WAVE HEIGHT IN METRES

1— WAVE PERIOD IN SECONDS. — ONE OCCURRENCE REFERS TO A SIX HOUR MEAN

APPENDIX FIGURE 23f: Directional Wave Statistics for November

H 2.10

9

co co

1 1 6 1 2

3 2 2 2 8 1 1 2 2 1 3

1 1 1 1 4 1 5 2 3. 1 2 1 8 8 1 1 2

5)

9

O 7 m8 1 6 5, 4

24

7.5°

N 6

5 0 4

2.10 0 9

e

I to 4 0.2, 3 N2

1 1 1

7 0 1 3 3

2 2

1

3. 1

4 2

71051 8 1 8 1 10 1121 14 12.15 1i "T 051 6 1 6 110 1 12.1 14 12.1518

BLOCK : H 8

ACRES: — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES

H— WAVE HEIGHT IN METRES. T NAVE PERIOD IN SECONDS.


APPENDIX FIGURE 23g: Directional Wave Statistics for November

2

1 1 6

H >10

9 tn 8

? N

1 5 al 4

1 2

1,

RI 12

3 12 12

4 6 1

1

>ea 9

tf! ; N 6 1 5 th 4

6 7

1

2 1

57

Cd 1 2

12 11

9 6

1

>10 8

ro 8

7 th

0.1 6 1 5

1 5, 4 1 1 1 3 1 1 1 5 8

6

11 3 1 12 5 1 12 3 1 El

>10 e 9 01 e N7 N6

5 1174 N5 V N2

>10 9

a7 8

>10 • 9 • e N6

15 r, IQ 3 N 2

H .10

9 tn 9 N 7 cv 1 5

tr) 4 N 3

2

112.5*

-15

7.5°

8 N N

1 5 4 3

(1N

7 2

>to 9 B

0 N 7 N 6 1 5

in 4

6 1 7 2 1

3 1

13 5 1

1 1

1 1

1 1

1

1

1 1 5 3 6 2 3 6 2

8:

T .5 1 6 1 6 1 10 1 12 1 14 1.15 I 7 91 6 1 8 1 10 1 12 1 14 13151

BLOCK: C 4 11<51 6 1 8 1 101 12 1 14 1.15 1 1451 6I 8 1 10 1 12 1 14 1.151 1

BLOCK: C 3

>10

rg1 :

7 6 15 rn 4 N 3 N 2

4 4 1

9 N 7 N 6

el 5 al 4 I,: 3 2 2

1) to

p4

1

4 1 5 9 5 2 1

3

1

1

310 9

&?

1 5 th 4 rz 3 (0 I

2 4 a

3 3 3 4

&-)

tcia 1

8 2

1 6 3 3 7 1

>10 9

V

1

>10

r11 : al 7 N I5 8-3 4

3 2

4

N(1 N

1

8

Rt

3,40 9 N7 0 616 15 5,4

6 1 5

4

H >10

9 8

N 7 N6 1 5 IN 4

M 2 P., 3

>10 9

0017 7

N 6 I5 N 4 r. 3

2 1

H >10

9

1

1 2

3 1 5 2

5 3 1 1

5 1 1

3 1 3 1 1 7 4 3.

1 2

1 4 5 5 1 3 6 3 1

1 4

2 47 2

2 1

7 <51 6 1 8 1 101 12 1 14 1.15 E T <5I 6 1 8 1 10 1 12 1 14 1315

BLOCK : CI T <5 16 1 8 1 10 1 12 1 14 1315 1 7 .51 8 1 8 1 10 1 12 1 14 1 3151

BLOCK: C 2




APPENDIX FIGURE 24a: Directional Wave Statistics for December

1 1 1

1 1 1 1

1.1 m5 1 6 1 8 1 10 1 12 1 14 1.15 E , T <51 6 1 8 1 10 1 12 1 14 1.151 E

BLOCK: C5

z 451 slelieliolt41.13 E r<313131431131141.431z

BLOCK: C6

T <51 6 1 8 1 10 1 12 114 1.15 E T >51 6 1 8 1 10 1 12 1 14 1.151 E

BLOCK : C 7

T <5 18 1 8 1 10 1 12 1 14 1>15 E T <51 8 1 8 1 10 1 12 1 14 1 >151 E

BLOCK: C8




APPENDIX FIGURE 24b: Directional Wave Statistics for December

sr N

51

1 5 114

H >10

tr, 8 ai ? Cm 6

>10 9

V 6 1 5 N4

3

1 2

3 2 3 1 2 12 2

112.Y-

157.Y

9) to to

1 1 2 2 1 5

1 3 1 4 9

3 2 3 2 5 7 1 6 4 1 2

1 1 1 3 5 7 1 7 3 1

1 1 1 1

1 1 1 2 2 1 2

0 3 2

1 1

1 1

3 1 1 1 1 1 1 1 1

2 1 2

H >10

9 8

OJ7 N 6 1 5 rn 4 1n1 ••• " 2

1

>10 9

rn EY: 6 1 5 to 4 ▪ 3

2 1

4)

A II

2r-

157.

5°

5, 2 1

2 2 1

1 3 2 6 3 5 3 1.

9 eO' 1 N 6 1 5 rn 4

3 2

>10

01 7

1 5 en 4

w2

3

>10 9 ;

1 5 in 4

3 W2

1

>10

>10 9

rn 8 (11; I5 u,4

3 c.0 2

>10 9

N8 1 5

lb 4 3

55 2 1

>10 e 9 cri: 8

E ; 1 5 4

14 3 N 2

1

H >10

9 th 5 N 7

2 1

N j 5 In 4 P.: 3

H >10

9 th 0„, N 6 15

rn 4

5 1 1 2 4 5 5 3

1 1

1 1 1 7 7 2 1

1 1

1 2 1

2 1 1 1 2 2

1 5 2 3 2

2 3

1 2 2 5 4 1 3 8 2

3 1 1

2 1

3 3 1

1 5 2 2 4 2

1

1 2

1 1 3 4 5 3 1

1

1 1

2 2 7 7 1 1

>10 9

N I5

N 4

;

a10 e 9 8) 9

I 5 11 4

3 N co 2

>10 9

rn

ck: I 5 a, 4

'n ▪ 3

2 1

1 2 1 2 7 4 1 3 1

1 2

3 1 1 1 1

2 1

1 3 1 1 5 5 1 3 1

2

1 1

1 1 a

NOTES — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES



APPENDIX FIGURE 24c: Directional Wave Statistics for December

.10 e 9 • s

M 7 N 6 1 5

?17 4 Is: 3

XI i■ri 2

1 2

7145 1 6 I 8 1 10 I 12 1 14 1.15 E T <51 6 I 8 1 10 I 12 I 14 1.151 I

BLOCK: C9 1l<51 6 1 8 1 10 1 12 1 14 I>15 E T <51 6 1 8 110 112 1 14 1.151 E

BLOCK: CIO

H >10

9

a N 1 N 1 2 I 5 1 1 1 1 6 n4 3 0 6

1 6 2 2 4 1

>10 9

in 8 ti 76

2 1

1

1 5 2

2 1 n4 2 1 1 1

1 3 1 7 2 6 9 tO 2 4 1 2 1

2

.40 9

in 6 0 N 7 N 6 cs,

1 5 4 1

in 3 in 2 1 2

a 1

2 1 1

7 2

112 5°-

I5

7. 5

°

fr)

1

1 1 1

1 1

4 1

9 a

N N

1 5 al 4

1 11 0 0

1

4 3

1 I

2

3

H 3.40

1 1 2 1

3 1 1 2

1 1 1 1 1

1 1 2

10 2 0 1

N, ,1 5 07 4 ti 3 el 2

1 2

Pn

112.

5°-

157

.5°

1 2 1

240 e 9 al al 7 N

I5 11 4

ri :

3

H '40

9

N 7 N6 1 5

07 4 3

2 2

H

9 a, N 7

810 9

in a ;

1 5 er, 4 r, 3 42 z

1 1 5 2 7 S 1

2 2 1

1 5 9 1 4

1

1 1

1 2 1 1

1<5I6181 101121 141.15E 74516181 101 121 141.152

BLOCK: D5

en

2 I5

81 4

kJ' 2

T <51 8 1 8 I 10 112 I 14 1.15 E T <51 8 I 8 I 10 112 I 14 1.151

BLOCK: D6

.10 . 9 e

I s rn 4

s imr 2

>10 • 9

s

1 5

12 4

2 1 8 3 1

2 1

.10 9

in a t%.1. ; 13 a, 4

3 to 2

0 0 1

1

1 2 3 4 8

2

1 1

1

12

1 1 3 7 3

1 1 2

1 1 1

2 1

>10 9

0 N 15

4 17

1

2

24 1

rn

4.1 1 2 2

1 1 1 2

1125

- I5Z

5°

112.

5°-1

57

.5°

.10 9

n 9 ;

1 5 rn 4

3 10 2

3.10 9

N 6 15 a, 4

tn 3 2

2 2 2 3 1

3 2 1 0 9 1 2

2 6 5 1 1 2

1 1

2

1 1

1

1 1 1

3 1 1 1 2 1

1 4 2 3 6 2 1

2

1

1 1 1 1

1 1 2 1 1 1

1 2 4 2

2 4 7 4 2

In

10

H 7.10

9 N a N 7 N

11

25°

-15

7.5°

.10 9

:38 N 7

6 I 5 a., 4 7. 3 u22

51 lV

710 • 9 In e SI 7 N 6 1 5

fh 4 7- 3 N 2

g 7 N 6

I5 to 4 N 3 N 2

>72 e 9 e

1 5 a, 4 1, 3 87 2

5 0 4

12 3 2

.10 9

• e al 7 V. 6 1' ▪ 4 7: 3 to 2

.10 9

5n8

0 N 7 N 6

5 to 4

3 m") 2

11

2 5°

- 1

575°

2025- 247

.5°

0

3 1

H >10

rn 4

9 ▪ 8 cs, 7 N 6 1 5

1 3 5 7 3 2

1 3

1 1 9 6

2

1

1 2 1

2 1 2 4 4 2 7 3 2

1 2

1 1 7 8

1

1 1 1

1 2 2 1

3 1 1

2 1

1 2 1

1 5 2 1 1 5 3 1

1 3

1 3 3 9 1

1 1 1

2 1 2 3

1 8 1 2 5 1

1

H

1 2 8 3

1 1 4 5

1

710 9

51 8 ni 7 N6 j 5 0 4 IN 3 r;3 2

2 1

1 1

1 1

2 3 2 1

1

1

4)

2

1 2 7 3

1 2

4

1 1

1

1 3 10 3 8

D.10 9

:I 8 V;

1 5 5f 4

tr'r; 23 1 1

2

1 9 5

; 1 1

2 1 5 1

1 1 3 9 4 1 1

>10 9

51 8 CM 7 RI 6 1 5

4 3 2 2

02 5

°- 2

47

5°

IN 3

.10 9

rn. (01$1 7 N 6 1 5 ▪ 4 7- 3 'LI 2

E

9

th a N 7 62 6

5 5f 4

2 a

s 340

9 ▪ 8

;

1 5 N 4

3 t8 2

1

H 510

202 5°- 247 5°

112

5° -1

57.

5°

to 1 1 1 2

1 4

3 2 1 1 1

7 1 2

29

2 5°- 3

375°

T1451 6 1 8 1 10 1 12 1 141>15 £ 7 <51 6 1 e 1 10 1 12 1 141>151 £

BLOCK: D7 71<51 6 1 8 1 101 12 1 141.15 £ 7<51 6 1 8 1 101 12 1 141.151 £

BLOCK: De

.:10 710

to : to tO 9

In7 7- M 7

N6 2 N6

1 5 I 1 5

ro 4 in 5f4

a3 3 I 3

N X 2

1 II 717.-5-1-6 18 1 10 1 12 r 14 1>15 T <51 6 ! 8 110 1 12 1 14 1.151 7 <51 6 1 8 110 1 12 1 14 1.15 Z T <5I 6 1 8 1 10 1 12 1 14 1- .151

BLOCK : D9 BLOCK: DIO NOTES:

— DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES H — WAVE HEIGHT IN METRES.



APPENDIX FIGURE 24d: Directional Wave Statistics for December

>10 9

clj 1 5 th 4

3 W2

010 9

m e N RI 6 1 5 r , 4 r- 3 "2 2

>10 • 9 to

Pi 7 N 6

3 1 3 1 5 5

2 1 1 1

2 3 5 4

1 3 3 1 1

1

010 9

fh 8 N 7 R. 6

1 5 4

52 2

>10 • 9 0 6

Si 7 N 6

gl 2

1 5 rn 4 P- 3

H 010

9 th .4 7

1 5 tr, n- 3 M2

>10 9

al 8 V 76

1 5 4

n- 3 W 2

1 1 1

1 3 1 6 5 1

1 2 3 2 3

112 Y-I

57

W

1. 2 8 3

a a 5 1 33

1,15 I 7 .51 6 1 8 1 10 1 12 1 14 1 >151 ;

BLOCK: F7

112

5°-1

57.5

°

tD

81

N N

Fa

N

in r, M lo

1 FP

E

1 2 3 2 1 1 3

2 10 3 4 3

1 2 2 2 1 1

2 1 2

2

H

2 1

1

2

1

2 2

1 22

o51 6 1 8 1 10 112 1 14 1>15 E

BLOCK:E8

010 9

N 8 N 7 N 6

N

10 1 2 1

j 5 10 4 3 3 1

3 1 1...4 3 1 0 1 1 4 0 2 3 1 4 3

1. 1 1

>10 9

1 1 1

a., 8

1 3 ; 2 3 1 1 5 1 1 2 1 2 4

2 4 1.■

24 1 3 2

3 2

W2 04 2 1 1 1

10 2

>10 9

in N

6 11 1 1 1 5 2

2 1 3 'en 4 3 2 1. 1

1 1

'2 2 3 1 1 1

>10 9

0 8 1 1 7 1 1

N 6 1 1 5 1 1 1

2 1 1 2 1 2 1

rs 1 2

1 2

1 2 1

2

1 6 1 8 1 10 1 12 1141>151 E T1451 6 1 8 1101 12 1 14 1 >15 E 710 51 6 1 6 1 10 112 1 14 1,451

BLOCK: 07

NOTES* — DIRECTION INTO WHICH WAVES PROPAGATE—IN DEGREES

H — WAVE HEIGHT IN METRES T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 24e: Directional Wave Statistics for December

H 010

9 to 8 N ? N 6 .1 5 0 0 1, 3 0 2

2

2 0

7 1

I 5 Pr) 4

Tic 5 1 6 1 8 1 10 1 12 I 14 1 >15 E 7

112

5.-1 5

7 5°

1 4 7 4

202

5°-

247

5°

2

0 2 1

4 2

>10 9

N N ? N

1 5

2

1 2 tr, 4 1 2-; 1 3

8 1 M2 5 6 1

>10 9

1 in 713

3 3 C=1 6 1 5 1

3 1 U, 4 1 2 S p- 3 1 2 4 W 2 5 5 2 1

>10 9

th 8 N 7 ia 6 1

1 5 1 tr., 4 1

[?; ; 2 3

1 1

1

>10 9

P s W 7 N 6

1 5 al 4 1.- 3 X 2

, ; 11.51 6 1 8 I 10 1 12 1 14

H

112. 5

°-1

57 5

° 20

2.5°

- 24

75"

T1 c 1 6 I 8 110T12 1 14 1.i9 I T 0 5

BLOCK:F8

202

5°-

247

5°

1 3 1

1 3

2 3 3

2 2 2 1 4 2 3

52

2 2

1 1 2 2 1 10 1 1




APPENDIX FIGURE 24f: Directional Wave Statistics for December

H >10

9

tn 8 N 7 N 6

5 04

Si 5 M 2

>10 9

1 2 1

3 3 1

< 8 , N 6 1 5 1 1 fr, 4 2 1

3 4 1 w 2 6 2

3

>10 9

in 8 N 7 1 1 C9 6 1 1 1 5 1

41,4 1.- 3 .2 2

2 2

1

1 .15 E T <5 1 6 1 8 1 10 1 12 I 14 1,151 I

BLOCK:G8

H >10

9

En 8 N 7 N6

T <5 I 6 1 8 1 10 1 12 I 14 1>15 E T <51 6 1 8 110 1 12 1 141>I51

BLOCK:H5

225°

- 67

5°

.10 o 9

N 7 6

I 5 1 In 4 1 1

3 1 2 1

Tl<5 1 6 1 8 1 10 1 12 1 14

MO 9

ni ; 2 1 1 5

2 1 in 4 1 1 2

2 11

2

t•-• 3

0:1 2 1 5 4

1 2

1 7

3 2 2 1

1 1 5 1 2 6 1

>10 9

in 8 N 7

1 1 R 8 1 2 1 5 1 2 1

1 N 4 1 3 1 r: 3 1

1 1 D 2 1 2 1 1 3 3 1

>10 o 9

4.) 1 1 8 2 1 1 1

1

1 N 7

6 I 5

2 3.. 1 1 1

4 2 rn 4 1 2 1 3 2 1 3 1

1 : 2 3 3 3

112 5°

-157

5°

202

5°- 24

7 5°

112 5

° -15

7.5°

20

2 5°

- 247

. 5°

292.

5°- 33

75°

BLOCK: H6

H

1 1 1 2

.1) Ir to

2 2 5

1

2 1 3

>10 9

N e 0.1 7 C46 j 5 <1 4 tz 3

2 2 1

1 3 4 1

iy 1 2 5 3

2 1

1 1 1

1

1

O 7 N 6 15 N 4

N 3 '41 2

>10 o 9 gl 8 Si 7 N 6

1 5 b 4 r- isri 3

2 1

Tl<5 1 6 1 8 1 10 112 I 141>15 E T <51 6 1 8 1 10 1 12 I 14 1'151

1 5 a, 4 I• 3 0 2 11

2.5° -

157.

5°

H >10

9

8 N 7 cs, 6

I 5 in 4 f z 3 <1 2

>10 9

N 8

1 5 N 4

3 102

>10 9

in 8

v 76

292 5°

- 337

5°

T <51 6 1 8 1 101 12 1141>15 £ T <51 6 I 8 I 10 1 12 1 141 >151 E

BLOCK: H7

112

5° -

157

5°

202

5°-

247

5°

292

5°- 337

5°

>10 9

r0 8

ir6 1 5

202

5°- 247

5°

4 3

E.) 2

>10 o 9 cncs, 6

cs 7 0.1 Is

En 4 r- 3

2 1

1 2

1 1 2 3 1 1 2 3 3

1 1 2 2 1 2 2 2 1

2 1 1

1 1 3 1

2 4 4 1

1 3 1 1 3 1 1 7 1 1 2 5 1

2

3

4 3

1 3

2 1

1 2 4 3 1 1

2 1 2 1 1

2 2 2 2 4 5

2 1 1

1 1 2 2 9 1 1

1

1 1 1

1 1

1 1

1 - 1 1 1 2 1 2 1

H >10

9 in 8 cv 1 2 N 6 VI

5 si 4 3 In' 3 5 3 1 H•c 2 1 1 5 1

3 1 E

112 Y

-157

.5°

to r- N

N pN

Fr)

>10 9

N 8 7

I 5 4

2- 3 W 2

>10 9

to 8

4

2 4 4

1 1 2

1 1

1

0 N 7 1 1 cv 1 1 2 I 5 1 1

fe, 4 r- 3 1

1

g'2 1 3 1 1

NO 9

In 8

ccill cv 6 I 5 1 1 1

?r, 4 3 3 t, 3

I 1 2

1

1 E

r<516161101121141.162 r<516181101121141.1512

BLOCK: H8

NOTES' — DIRECTION INTO WHICH WAVES PROPAGATE— IN DEGREES

H — WAVE HEIGHT IN METRES T— WAVE PERIOD IN SECONDS.


APPENDIX FIGURE 24g: Directional Wave Statistics for December

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