morphan: a new software tool to assess sandy...

4
DOI: 10.3990/2.189 Jubilee Conference Proceedings, NCK-Days 2012 MorphAn: A new software tool to assess sandy coasts Q.J. Lodder 1 and P.F.C. van Geer 2 1 Rijkswaterstaat, waterdienst, P.O.Box 17, 8224 AD, Lelystad, the Netherlands 2 Deltares, P.O.Box 177, 2600 MH, Delft, the Netherlands, [email protected] ABSTRACT We present a new software tool called “MorphAn” that enables easy assessment of sandy coasts. MorphAn provides the possibility to import data of various formats. The software pays special attention to coastal data provided in the so-called Jarkus format. Data can be analyzed with a GIS based map view. Simultaneously an overview of the profile development in time or a more detailed picture of the actual measurements is given. Furthermore, MorphAn includes the possibility to assess coasts for dune safety according the safety assessment rules VTV2006. The software program gives a graphically presentation of the calculation results of dune erosion according to the Duros+ and D++ model as well as calculation results of the normative erosion points. MorphAn also provides the possibility to calculate and visualize the momentary coastline (MKL) and the expected near future coast line position (TKL). The software is freely available and expected to become open source in 2012. INTRODUCTION This short paper will introduce you to a new and freely available software tool called “MorphAn”. MorphAn enables the user to assess the safety and beach development of sandy coasts. In 2008 the Dutch Ministry of Infrastructure and the Environment commissioned Deltares to start the build of a new software tool. The aim of this software is to support assessment of dune safety and beach development. Rijkswaterstaat plans to present MorphAn as its official and supported tool for assessment of dune safety in The Netherlands. From the start of the project, one of the main goals has been to release MorphAn as a freely available, preferably open source, software tool. At this moment, the beta version of MorphAn is freely available. Release of the source code is expected at the end of 2012. Data analysis, Dune safety assessment and coastal development assessment are the three pillars that form the basis of MorphAn. This paper will discuss the figures and tools included in MorphAn to support each of these pillars. DATA ANALYSES One of the most important aspects of assessing dune safety or coastal development is analyzing the data that is used to calculate a dune crest retreat point after a storm or momentary coastline. MorphAn offers the ability to import and analyze so-called jarkus measurements (yearly measurements of coastal profiles). A default jarkus dataset that includes most yearly measurements of the Dutch coast between 1965 and 2011 accompanies the software. Next to that, there is also the possibility to import user defined datasets or expand the default dataset with additional measurements. Once the data is imported, it is possible to specify a list of locations that is used in all operations throughout the program. MorphAn ignores all measurements at locations not in that list. To accommodate a thorough analysis of the imported data MorphAn provides various types of views that enable the user to analyze the data at different levels of aggregation and along the various dimensions in time and space. This section will introduce you briefly to the types of figures included in MorphAn. Map overview The map overview provides a GIS based map that gives a top view of the measurements in space and time. Figure 1 gives an example of the jarkus measurements at Texel for 2011. Blue lines represent the wet parts of the measurements, whereas the sandy colored lines represent dry measurements. Interpolated profile parts can be recognized by the tomato red colored lines. MorphAn also includes a time navigator to control the period that is presented on the map. Due to its GIS nature it is easy to expand the map by including for example shapefiles as is shown by including the Texel district boundaries and names in Figure 1. Transect side view The transect side view (Figure 2) shows a single jarkus measurement in the local coordinate system (RSP). The side view distinguishes wet measurements, dry measurements and the interpolated profile part with the same coloring as the map overview. Furthermore, the side view interrupts the plotted line whenever more than 10 meter separates the measured points. This enables visual assessment of the quality and origin of the jarkus measurements. Transects comparison view With the transects comparison view (Figure 3) it is possible to compare jarkus measurements in time for one location or in space for a specific year. This enables the user to look at profile development of a certain feature in time or space. Each measurement is now plotted by a single (unique) color. The tool offers various color scales to customize the image.

Upload: others

Post on 18-Aug-2020

1 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: MorphAn: A new software tool to assess sandy coastsproceedings.utwente.nl/189/1/Lodder12morphan.pdf · DOI: 10.3990/2.189 Jubilee Conference Proceedings, NCK-Days 2012 MorphAn: A

DOI: 10.3990/2.189

 

Jubilee Conference Proceedings, NCK-Days 2012

MorphAn: A new software tool to assess sandy coasts

Q.J. Lodder1 and P.F.C. van Geer2 1Rijkswaterstaat, waterdienst, P.O.Box 17, 8224 AD, Lelystad, the Netherlands 2Deltares, P.O.Box 177, 2600 MH, Delft, the Netherlands, [email protected]

ABSTRACT

We present a new software tool called “MorphAn” that enables easy assessment of sandy coasts. MorphAn provides the possibility to import data of various formats. The software pays special attention to coastal data provided in the so-called Jarkus format. Data can be analyzed with a GIS based map view. Simultaneously an overview of the profile development in time or a more detailed picture of the actual measurements is given. Furthermore, MorphAn includes the possibility to assess coasts for dune safety according the safety assessment rules VTV2006. The software program gives a graphically presentation of the calculation results of dune erosion according to the Duros+ and D++ model as well as calculation results of the normative erosion points. MorphAn also provides the possibility to calculate and visualize the momentary coastline (MKL) and the expected near future coast line position (TKL). The software is freely available and expected to become open source in 2012.

INTRODUCTION

This short paper will introduce you to a new and freely available software tool called “MorphAn”. MorphAn enables the user to assess the safety and beach development of sandy coasts.

In 2008 the Dutch Ministry of Infrastructure and the Environment commissioned Deltares to start the build of a new software tool. The aim of this software is to support assessment of dune safety and beach development. Rijkswaterstaat plans to present MorphAn as its official and supported tool for assessment of dune safety in The Netherlands. From the start of the project, one of the main goals has been to release MorphAn as a freely available, preferably open source, software tool. At this moment, the beta version of MorphAn is freely available. Release of the source code is expected at the end of 2012.

Data analysis, Dune safety assessment and coastal development assessment are the three pillars that form the basis of MorphAn. This paper will discuss the figures and tools included in MorphAn to support each of these pillars.

DATA ANALYSES

One of the most important aspects of assessing dune safety or coastal development is analyzing the data that is used to calculate a dune crest retreat point after a storm or momentary coastline. MorphAn offers the ability to import and analyze so-called jarkus measurements (yearly measurements of coastal profiles). A default jarkus dataset that includes most yearly measurements of the Dutch coast between 1965 and 2011 accompanies the software. Next to that, there is also the possibility to import user defined datasets or expand the default dataset with additional measurements.

Once the data is imported, it is possible to specify a list of locations that is used in all operations throughout the program. MorphAn ignores all measurements at locations not in that list.

To accommodate a thorough analysis of the imported data MorphAn provides various types of views that enable the user to analyze the data at different levels of aggregation and along the various dimensions in time and space. This section will introduce you briefly to the types of figures included in MorphAn.

Map overview The map overview provides a GIS based map that gives a top

view of the measurements in space and time. Figure 1 gives an example of the jarkus measurements at Texel for 2011. Blue lines represent the wet parts of the measurements, whereas the sandy colored lines represent dry measurements. Interpolated profile parts can be recognized by the tomato red colored lines. MorphAn also includes a time navigator to control the period that is presented on the map.

Due to its GIS nature it is easy to expand the map by including for example shapefiles as is shown by including the Texel district boundaries and names in Figure 1.

Transect side view The transect side view (Figure 2) shows a single jarkus

measurement in the local coordinate system (RSP). The side view distinguishes wet measurements, dry measurements and the interpolated profile part with the same coloring as the map overview. Furthermore, the side view interrupts the plotted line whenever more than 10 meter separates the measured points. This enables visual assessment of the quality and origin of the jarkus measurements.

Transects comparison view With the transects comparison view (Figure 3) it is possible to

compare jarkus measurements in time for one location or in space for a specific year. This enables the user to look at profile development of a certain feature in time or space. Each measurement is now plotted by a single (unique) color. The tool offers various color scales to customize the image.

Page 2: MorphAn: A new software tool to assess sandy coastsproceedings.utwente.nl/189/1/Lodder12morphan.pdf · DOI: 10.3990/2.189 Jubilee Conference Proceedings, NCK-Days 2012 MorphAn: A

162

Figof conDu

Figsidelanlinewet(tom

Figmeameacom

2

gure 1. An examthe imported j

ntains a layer thtch cadastre (h

gure 2. An exae view shows d (sandy coloree) and interpolt and dry meamato red line)

gure 3. An exaasurements ovasurements formpared.

mple of a map ijarkus measurehat shows the dttp://kadaster.n

mple of a trandifferences be

ed line), measulated profile paasurement when

ample of a traver a certainr one year o

in MorphAn shoements for Texdistricts of Texenl/)

nsect side viewtween measure

urements taken farts that are usn assessing the

ansect comparin period on over multiple

owing an overvxel. The map ael according to

in MorphAn. ements taken ffrom a vessel (bsed to connecte complete pro

son plot in whone location, locations can

view also

o the

The from (blue t the ofile

hich or

be

Figure developcertainbar tra

Figure measuraccreteThe rerelative

Figure indicatmeasur

Jubilee

4. An examplepment at one l

n height regionsaveling offshore

5. An examrements. Greened (or have beed parts indicae to the first me

6. An examplete the last yearred in that parti

Conference Pr

e of a time staclocation. Browns of the profile. .

mple of a difn shows the paeen nourished) ate locations weasurement.

e of a time histor in which a chicular part of th

roceedings, NC

ck representation and blue colThe blue part c

ifference plot arts of the prosince the first

where the prof

tory plot. The change of the bhe profile.

K-Days 2012

on of the beachlors accentuateclearly shows a

between twoofile that havet measurement.file has eroded

colored patchesbathymetry was

h e a

o e .

d

s s

Page 3: MorphAn: A new software tool to assess sandy coastsproceedings.utwente.nl/189/1/Lodder12morphan.pdf · DOI: 10.3990/2.189 Jubilee Conference Proceedings, NCK-Days 2012 MorphAn: A

Ju

TimT

in tcerthigfeatFigoffs

TimV

a cchashoDuchashorefemeana

TimT

cropatoccusethro

Duseextrthismeyeathe

MDurimpcalcNexmo

TMoassretrthe

Otooon samComrelaresucalcthro

ubilee Conferen

me stack vieThe time stack vtime at a certatain distance

ghlighting of sptures in the pr

gure 4 for exafshore.

me differencVisualization ofertain location

anges in the baows these differe to its couplin

anges in time iows a nourishmerence year anasurement the

alyzed.

me history vTime history fiss-shore profilches. The colo

curred in that per gets an idea oough time.

DUN

Dutch dune safee of Duros+ foreme storm eves extreme evasurements ove

arly variation ose fifteen years

MorphAn incluros+ model andplements Durosculation result xt to the Durodel (Deltares, 2

To support deorphAn also essment rules reat points (R) third worst poi

One of the addls is the abilitya map as wel

me feature asmbining the catively easy. Fults on the mapculated erosionough the results

ce Proceedings

ew view is another

ain location. Inhigher than tpecific heightsrofile becomes ample shows th

ce view f the morphologcan help the u

athymetry. The rences as green ng with a timeis quickly visument just belond changing thdevelopment o

view igures (Figure le at one locator represents thparticular part oof the depth at w

NE SAFETY

fety assessment for calculating ent. To assess vent needs ter a period of

of the beach prs is considered tudes a model tod visualize the rs+). Figure 7 s

for an indivis+ model, Mor

2010). etermination ofproduces Rt-d(Figure 8). Anin time (t) for

int as the normaded values of My to interactivel (Figure 9). Ts the previoualculation resu

Furthermore, sep is synchronizn and the Rt-ds a fun job to do

s, NCK-Days 20

r way of lookinn this plot eachthe previous ys in the profile

more visible. he movement

gical change beser understand time differenc(accretion) or r

e navigator devalized. The exa

ow NAP. By he year of thef the nourishm

6) show the detion in time byhe last year inof the profile. which the profil

Y ASSESSM

rules (TRDA2dune erosion dune safety, duto be calculfifteen years. T

rofile, the thirdthe normative eo calculate dunresults in order shows a represidual measuremrphAn also imp

f the normativdiagrams as n Rt-diagram plr a certain locaative dune crest

MorphAn with rely display the This map repreusly discussedults with otherelection of oneed with the repdiagram. This o.

012

ng at measuremeh year is plotteyear. Due to e, developmentThe time stackof breaker ba

tween two yearthe effect of la

ce view (Figurered (erosive) arvelopment of thample in Figurholding the sa

e compared jarment in time can

evelopment of y plotting colon which a chaWith this tool le actively chan

MENT

2006) prescribe at the end of

une erosion dueated for proTo incorporate d worst result oerosion point. ne erosion with

to inspect thementation of sucment at Amelaplements the D

ve erosion podescribed in lots the calcula

ation and identit retreat point. respect to existcalculation res

esentation uses d map overvi

data thereforee ore more of presentations of

makes naviga

ents ed a

the t of k in anks

rs at arge e 5) reas. hese re 6 ame rkus n be

f the ored ange

the nges

the f an e to

ofile the

over

the m (it ch a and. D++

oint, the

ated ifies

ting sults

the iew. e is

f the f the ating

Figure calculaThe figbounda

Figure The noMorphAinvalidqualificmore ex

Figure is couptime. Tnormat

7. Representatation using Dugure also incluary profile.

8. Visualizatioormative retreaAn also disti

d (red) and cation is just axamination bef

9. Map overvipled to a time

The MorphAn otive retreat poin

tion of the resuros+ at Amelaudes the calcul

n of the calculaat point is visuinguishes betw

valid (green)a first pointer tfore trusting the

ew of the calcunavigator, wh

verview also innts.

Lodder

ult of a dune safand as includedulated additiona

ated retreat (R)ualized as a sqween questiona) calculation to the results te result.

ulated retreat phich allows scrncludes a layer

and Van Geer

163

fety assessmentd in MorphAn.al erosion and

) points in time.quared symbol.able (orange),

results. Thisthat need some

points. The maprolling through

that shows the

t .

d

.

. , s e

p h e

Page 4: MorphAn: A new software tool to assess sandy coastsproceedings.utwente.nl/189/1/Lodder12morphan.pdf · DOI: 10.3990/2.189 Jubilee Conference Proceedings, NCK-Days 2012 MorphAn: A

164

Nthe beaas tby

Figposthe detthe

Figat AMKthe

FigTheMKgretrenww

4

COASTAL

Next to dune sadevelopment o

ach position is tthe volume of the difference

gure 10. Repressition (MKL) as

volume betwermining the MMKL position.

gure 11. RepresAmeland. Morp

KL points by plopredicted coas

gure 12. Map ove map also incKL relative to teen bars. This lnds in the kustl

ww.kustlijnkaart

DEVELOP

afety assessmenof the coastlinethe momentary sediment betwbetween these

sentation of thes included in Mween the uppMKL position.

sentation of the phAn also incluotting an orangstline TKL.

verview of the ccludes a layer the basic coastllayer looks simlijnkaartenboekt.nl

PMENT ASS

nt, MorphAn ofe. A widely usecoastline positi

ween two elevate two levels. W

e calculated moMorphAn. The bl

per and loweThe blue dashe

MKL point in tudes the calcuge line. The gre

calculated MKLthat expresses

line (BKL) by milar to the prek published by R

SESSMENT

ffers tools to ased indicator forion (MKL) defition levels divi

While assessing

mentary coastllue area visualizer boundary fed line represe

time for a locatlated trend of een dot represe

L and TKL poins the trend of means of red asentation of MKRijkswaterstaat

T

ssess r the fined ided

g the

developlocationexpectewith a not the10, 11 results.MKL kustlijnEnvirondevelopdevelop

As mpotentithis massess assessmto expalike inautomaAlthoukustlijnresults creatin

HowMorphAerosion(SteetzcommuEarth f

In t“Morphdevelopexpectesupportdune saTRDAcoastlinpossibihear alwe did

Deltaretusse

Dano RVrieimpaEngi10.1

TRDAexpe

Henk S

line izes for

ents

tion the

ents

nts. the

and MKL

t at

Jubilee

pment of the cn are often used coastline poreference coas

ere should be nand 12 show th. Figure 12 also

position andnkaarten producnment (www.kpment of Morppment and dete

FUTU

most users wial for further d

moment equippidune safety ac

ment rules has aansion of the funcluding a natically determugh there is no nkaarten produ

can be writteng these maps.

wever, there are An. One can t

n models like Xzel, 1993), bunication with for example).

this paper, wehAn” to facilitpment of sandyed to become ts data analysiafety according2006 and assesne. At this ilities for expal ideas about thnot think of ye

es (2010), Ontenrapportage SB

Roelvink, Ad Rs, Robert McCaacts on beachineering, 5016/j.coastalen

2006 (2007erisenetwerk wa

Steetzel (1993).

Conference Pr

coastline these sed to calculateosition (TKL) istline (BKL) adnourished at thahe way MorphAo contains a rep

its relation ced by the Min

kustlijnkaart.nl).phAn, it also prmining the TK

URE DEVEL

ill experience,development ofing MorphAn ccording to an a high priority. unctionality to

nourishment damine the best

direct couplinuced by the mn in an output

also possibilitithink of includXBeach (Roelvut also expaother programs

CONCLUS

e presented a tate analysis any coasts. The soopen source ats in various wto the Dutch assment of the demoment, Mornding the func

he possibilities et.

REFEREN

twikkeling detaBW-Duinen. De

Reniers, Ap vanall, Jamie Lescihes, dunes an56(11–12),1133g.2009.08.006.

7), Techniscaterveiligheid.

Cross-shore Tr

roceedings, NC

positions in timte a trend and in a future yeads to the decisat particular lo

An represents thpresentation of t

to the TKnistry of Infrast. As the ministplans on asses

KL with MorphA

LOPMENT

, MorphAn of the supportedwith the neceexpected new Next to that, acalculate beach

database and period for t

ng between Moministry, in futu

format that ca

ies for adding nding interfaces vink et al., 2009anding the cs (export of res

SIONS

new softwarand assessmentoftware is freelyt the end of 2

ways as well asssessment rulesevelopment of rphAn still octionality. We to expand Mor

NCES

tailtoest duineneltares, 120212

n Dongeren, Jaainski (2009), Mnd barrier isl

3-1152, IS

ch rapport

ransport during

K-Days 2012

me at a certaindetermine the

ar. Comparisonion whether orcation. Figures

hese calculationthe trend of the

KL similar toructure and thetry initiated thessing the MKLAn in future.

T

ffers a lot ofoperations. At

essary tools toversion of the

attention is paidh development,a module to

trend analysis.orphAn and theure calculationan be used for

new features toto other dune

9) or DurosTAcapabilities ofsults to Google

re tool, calledof safety and

y available and012. MorphAn assessment ofs denoted in thethe momentary

offers lots ofwould love to

rphAn in a way

n 2011 (D++),24-003).

ap van Thiel deModelling storm

lands, CoastalSN:0378-3839,

duinafslag,

g Storm Surges.

n e n r s n e o e e L

f t o e d , o . e n r

o e

A f e

d d d n f e y f o y

,

e m l ,

,