photogrammetry is the science and technology of taking spatial measurements from photographs and...

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Photogrammetry is the science and technology of taking spatial measurements from photographs and preparing geometrically reliable derivative products. The techniques are based on the geometry of perspective scenes and on the principles of stereovision. Two kinds of photographs used in photogrammetry: aerial and terrestrial . Aerial photographs are usually acquired from aircraft but can also come from satellites, hot air balloons or even kites. Terrestrial photographs come from cameras based on the ground, and generally are used in different applications from aerial. There are two main data extraction methods used for analysing these photographs: a. Quantitative : that is size, length, shape, height, area, etc. b. Qualitative : geology, vegetation, drainage, land use, etc. Historically, the most common use of photogrammetry was to Photogrammetry

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Photogrammetry is the science and technology of taking spatial measurements from photographs and preparing geometrically reliable derivative products.

The techniques are based on the geometry of perspective scenes and on the principles of stereovision.

Two kinds of photographs used in photogrammetry: aerial and terrestrial.

Aerial photographs are usually acquired from aircraft but can also come from satellites, hot air balloons or even kites. Terrestrial photographs come from cameras based on the ground, and generally are used in different applications from aerial.

There are two main data extraction methods used for analysing these photographs:

a. Quantitative: that is size, length, shape, height, area, etc. b. Qualitative: geology, vegetation, drainage, land use, etc.

Historically, the most common use of photogrammetry was to produce hardcopy topographic maps, now it is used to produce a range of GIS data products such as DEMs, accurate raster images backdrops for vector data

Photogrammetry

Aerial photographs

- Vertical - Oblique

Vertical photographs most commonly used, but true vertical photographs are rare because of the angular attitude of the aircraft at the time of photography.

This results in slight (1-3º) unintended inclination of the optic axis of the camera, resulting in titled photographs.

However, for most practical applications, such photographs can be considered vertical photographs.

4-44-54-6

3-63-53-4

Block of Aerial Photography

Compiled into an Uncontrolled

Photomosaic

a.

b.

Aerial photographs

Aerial photographs: Some terminologyFiducial marks - Index marks, usually 4, at the center point of each side of an air negative or photo. These are rigidly connected with the camera lens through the camera body—which forms images on the negative. Usually are a hairline, a cross, or a half-arrowhead.

Principal Point - optical or geometric center of the photograph - the intersection between the projection of the optical axis (i.e., the perpendicular to the center of the lens) and the ground. Can be located by the intersection of lines between opposite side/corner fiducial marks.

Nadir - The nadir, also called vertical point or plumb point, is the image of the intersection between the plumb line directly beneath the camera center at the time of exposure and the ground. The nadir is important because relief displacement is radial from this point and is a function of the distance of the displaced image from it. Unlike the principal point, there are no marks on the photograph that permit to locate the nadir.

Isocenter - The point on the photo that falls on a line half- way between the principal point and the Nadir point.

Fiducial marks

Edge of format Fiducial axis

Lens

X axis

Plumb line

Principal point

NadirIsocenter

Y axis

Determination of nadir in oblique photos

Relief displacement is radial from nadir, and is a function of the distance of the displaced image from it. Unlike the principal point, there are no marks on the photograph that permit to locate the nadir.

However, in areas where tall and perfectly vertical objects (e.g., towers, smokestacks, electric poles, tall buildings, etc.) are clearly located on the photograph, the nadir point may be determined by projecting lines along the displaced edges of these buildings

Principal point

NadirIsocentre

Jensen, 2000

Exposure station #1

stereoscopic model

#2 #3

Direction of Flight

terrain recorded on three successive photographs

lens altitude above ground level, H

60% overlap

Coverage of photograph

Flightline of Aerial Photography

Flightline of Vertical Aerial Photography

20 – 30% sidelap

oblique photography may be acquired at the end of a flightline as the aircraft

banks to turn

Flightline #3

Flightline #2

Block of Aerial Photography

Flightline #1

20 – 30% sidelap

oblique photography may be acquired at the end of a flightline as the aircraft

banks to turn

Flightline #3

Flightline #2

Block of Aerial Photography

Flightline #1

Block of Vertical Aerial Photography

Jensen, 2000

Block of Vertical Aerial Photography Compiled into

Photomosaic

Columbia, SCOriginal scale = 1:6,000Focal length = 6” (152.82 mm)March 30, 1993

Jensen, 2000

4-44-54-6

3-63-53-4

Block of Aerial Photography

Compiled into an Uncontrolled

Photomosaic

a.

b.

4-44-54-6

3-63-53-4

Block of Aerial Photography

Compiled into an Uncontrolled

Photomosaic

a.

b.

Geometry of Overlapping Vertical Aerial Photographs

Fiducial mark

y - a

xis

Line of flight

Principal Point of Photo #1

Ph

oto

1

Ph

oto

2

Principal Point of Photo #1 equals

Conjugate Principal Point of Photo #2

Principal Point of Photo #2 equals

Conjugate Principal Point of Photo #1

b.a.

c.

line of flight

stereoscopic model60% overlap

PP

CPP

PP

CPP

1

12

2

x-axis

Ph

oto

1

Ph

oto

2

PP1PP2

Principal Point of

Photo #2

Conjugate principal point: The point in the overlapping photo that is equivalent to the principal point of adjacent photograph

Fiducial mark

y -

ax

is

Line of flight

Principal Point of Photo #1

Ph

oto

1

Ph

oto

2

Principal Point of Photo #1 equals

Conjugate Principal Point of Photo #2

Principal Point of Photo #2 equals

Conjugate Principal Point of Photo #1

b.a.

c.

line of flight

stereoscopic model60% overlap

PP

CPP

PP

CPP

1

12

2

x-axis

Ph

oto

1

Ph

oto

2

PP1PP2

Principal Point of

Photo #2

Geometry of A Vertical Aerial Photograph

Obtained Over Flat Terrain

Ground points are denoted in capitals, the corresponding points on the image are denoted in small letters.

- X axis along the flight direction - Y axis perpendicular to X- Principal point - Origin

Exposure station Camera lens

Positive print/ transparency

Focal length (f)

Altitude ASL (H)

Elevation ASL (h)

SEA LEVEL

Negative (Reversal of tone and geometry

Geometry of A Vertical Aerial Photograph Collected Over Flat Terrain

Principal Point

Optical axis

Camera lens

Focal length, f

A B

a b

o

P

Positive print

Real-world object space

Image space

Altitude above ground level,

H

Exposure Station, L

Photographic scale

Scale (S) = Photo distance/ground distance = d/D

Scale (S) = f/H′OrScale (S) = f/(H – h)

Scale is dependent on the flying height ~ terrain clearance ~ terrain elevation

56.0’

0.112”

6’

0.012”

Geometry of A Vertical Aerial Photograph

Collected Over Variable Relief Terrain:

Geometric distortion

Average elevation above sea level,

h

Camera lens

Focal length f

Exposure station, L

A B

e go

P

Sea level

C

D

Highest elevation above sea level,

h max

Lowest elevation above sea level,

hmin

c d

Altitude above

sea level H

E

G

a bImage space

Object space

Average elevation above sea level,

h

Camera lens

Focal length f

Exposure station, L

A B

e go

P

Sea level

C

D

Highest elevation above sea level,

h max

Lowest elevation above sea level,

hmin

c d

Altitude above

sea level H

E

G

a bImage space

Object space

Þ Variation in the terrane elevation would result in scale variations across the photograph

Scale (S) = f/(H – h)

Þ Generally the average scale based on average height is given

Map vs Photograph

- On a map we see a top view of objects in their true horizontal (planimetric) positions (Orthographic projection)

- On a photograph they are displaced from their true map positions due to geometric distortions

(perspective projection)

• Objects at higher elevations (closer to the camera) appear larger than the corresponding objects at lower elevations

• Tops of the objects are displaced from their bases (relief displacement), which causes any object standing above the terrain to “lean” away from the principal point.

Map – Orthographic projection – No relief displacement

Photo – Perspective projection – Varied scale - Relief displacement

Measurement of Object Height From A Single Aerial Photograph Based on Relief Displacement

Principal point (PP)

d

Lin

e of

flig

ht

d

r

Lin

e of

fli

ght

r

d

Principal point

Given that the flying height is H

Measurement of Object Height From A Single Aerial Photograph Based on Relief Displacement

h = dH/r

d –relief displacement on the photographr – radial distance from the principal point to the displaced image pointh – height above datum of the object pointH – flying height above the same datum chosen to reference h

r

Negative

Exposure station, L

local datum

h

H

d r

H

=

d

h

h d

r =

H x

r = 2.23 in. d = 0.129 in. H = 2978.5 ft above local datum h = 172 ft

Principal point

Positive

f

A

B

a

b’

b

a’

o

o’

PP B′D

H

h

r

d

O

R

ΔLOB′ ~ ΔBAB′

Þ D/R = h/H

or, on the scale of the photograph

d/r = h/H

d = rh/H

Measurement of Object Height From A Single Aerial Photograph Based on Shadow Length on Level Terrain

shadowL

Measurement of the Height of Objects Based on Shadow Length

h

a

tan a = adjacent

opposite

= shadow, L

height, h

h = L x tan a

Sun’s rays

Object Height Determined by Shadow Length

0.119” 59.1’

0.241” 119.65’

0.119” 59.1’

0.241” 119.65’

Image parallax

Apparent change in relative positions of stationary objects caused by a change in viewing position

Objects closer to the viewing position appear to move with respect to the objects farther away

Eye base

Distance to the object

Parallax angle

Parallax

Parallax: Look at apparent motion of object against distant background from two vantage points; knowing baseline allows calculation of distance:

distance (in parsecs) = 1/parallax (in arc seconds)

1 parsec ~ 3.3 ly

Image parallaxObjects closer to the aircraft-mounted camera (that is, at higher elevation) would appear to move with respect to objects at lower elevation when the position of the air craft changes in successive exposures.

These relative displacements or parallax form the basis of stereo viewing (depth perception)

PP1 PP2a b

Parallax = a –b

Parallax on overlapping vertical photos

Parallax displacement occurs parallel to the line-of- flight

In theory the line-of-flight should be parallel to the fiducial x axis. In reality, there is a slight offset - the true flight direction is along the line joining the principal point and the conjugate principal point.

The line-of-flight for a stereopair defines the photocoordinate x axis. Line drawn through the principal point perpendicular to the flight line defines photocoordinate y axis.

Parallax of a point (Pa) = xa – x′a , wherexa is the measured x coordinate of the image point a on the left photo of the stereopairx′a is the measured x coordinate of the image point a on the right photo of the stereopair

A

aL

xa

ax

o

fa′

a′x

o′x′a

f

hA

hA

XA

L′

O

AX

xa

axo

L

a′xo′x′a

L′

xa

axoa′x

x′a

L

DATUM

Parallex = Pa = xa - x′a

+

==

>

H

A

aL

xa

ax

o

fa′

a′x

o′x′a

f

hA

hA

XA

L′

O

AX

xa

axoa′x x′a

L

DATUM

Parallex = Pa = a′xax = xa - x′a

Lo = Focal length = fLL = Air base = B

H

Δa′xLax is similar to the ΔLL′AX

Therefore,

aA

aA

A

a

X

xx

P

BfHh

P

BfhH

hH

f

B

P

MA

LO

LL

aa

M

DATUM

Parallex = Pa = a′xax = xa - x′a

Lo = Focal length = fLL = Air base = B

H

Now ΔLoax is similar to the ΔLOAAX

Therefore,

a

aA

a

aA

aa

AaA

AA

a

AXA

x

P

yBY

P

xBX

f

PBf

x

f

hHxX

hH

f

X

x

LO

Lo

AO

oa

)()(

M

OA

ya

A

aL

xa

ax

o

fa′

a′x

o′x′a

f

hA

hA

XA

L′

O

AX

YA

A

aL

xa

ax

o

fa′

a′x

o′x′a

f

hA

hA

XA

L′

O

AX

DATUM

H

a

a

aA

a

aA

aA

p

Hph

p

yBY

p

xBX

p

BfHh

M

OA

ya

Parallax Equations

Where:Δh - Difference in the elevation of two points whose parallax difference is ΔpH′ - Flying height above the lower pointPa – Parallax of the higher point

x = - 0.267”

x = - 0.270”

Fid

ucial lin

e fro

m P

ho

to

4

-4

x = - 3.606”

x = - 3.82”

F

id

ucial lin

e fro

m P

ho

to

4

-5

p = 0.511”

p = 0.30”

c.

b.

c.

a.

Photo 4-5

Photo 4-4

Methods of Measuring Stereoscopic x-parallax from

Overlapping Aerial Photographs: • Measurement Using Fiducial Lines (a,b) • Measurement Based on Superposition (c)

Photo 4-5 Photo 4-4

dp = 0.211”

PP 4-5

PP 4-4

b’

a’

b

a

b

a

x = - 0.267”

x = - 0.270”

Fid

ucial lin

e fro

m P

ho

to

4

-4

x = - 3.606”

x = - 3.82”

F

id

ucial lin

e fro

m P

ho

to

4

-5

p = 0.511”

p = 0.30”

c.

b.

c.

a.

Photo 4-5

Photo 4-4

Methods of Measuring Stereoscopic x-parallax from

Overlapping Aerial Photographs: • Measurement Using Fiducial Lines (a,b) • Measurement Based on Superposition (c)

Photo 4-5 Photo 4-4

dp = 0.211”

PP 4-5

PP 4-4

b’

a’

b

a

b

a

Principal point 4-5x axis

y ax

is

Principal point 4-4

'30.178"55.3

'3000"211.0

"211.0"339.3"55.3

"339.3)"606.3("267.0

"55.3)"82.3("27.0

'

'

a

b

a

x

bbx

aax

p

Hph

p

xxp

xxp

The height of the Senate Condominium in Columbia

d=0.247”

Xb’=-3.606”

Xa’=-3.82”

Xb=-0.267”

Xa=-0.270”

r=4.164”

'95.177"164.4

'3000"247.0

r

dHh

Flying height above the base of the building – 3000 feet

Parallax measurement

+ +++PP1 PP2

x x′

d

D

Parallax = x – x′ = D - d

Ground Control Points

A point on the surface of the earth of known horizontal and vertical location (i.e. fixed within an established co-ordinate system and datum) which is used to geo-reference image data sources, such as aerial photographs, remotely sensed images, and scanned maps.

When mutually identifiable on the ground and on a photograph, GCPs are used to establish the exact spatial position and orientation of a photograph relative to the ground

Historically GCPs have been established through ground survey techniques, now a days GPS are more frequently used.

Accurate ground control is essential to all photogrammetric operations because photogrammetrical measurements can only be as reliable as the ground control

FLIGHT PLANNINGParameters:• Focal length of the camera to be used• The film format size• Photoscale desired• Size of the area to be photographed• Average elevation of the area to be photographed• The overlap desired• Side-lap desired• Ground speed of the aircraft

Based on the above parameters, mission planner decides:• The flying height above the datum• the location, direction, and the number of flight lines to be made• the time interval between exposures• the number of exposures on each flight line• the total number of exposures for the mission

FLIGHT PLANNING

Area to be photographed

North

16 km

10 km

Camera characteristics:• f = 152.4 mm• Film format = 230 mm

Photoscale: 1:25000End-lap – 60%; side-lap 30%

Average elevation: 300m

Beginning and ending flight lines should be along the boundaries

Aircraft speed – 160 km/hr

Direction of flight lines?N-S

Flying Height?H=f/s + Mean elevation = 0.23/(1/25000) = 4110 m

Ground coverage per photo?= film format size/scale = 0.23 m/(1/25000) = 5750 m on a side

Ground separation between photos (in the flight direction)?

Advance per photo = 40% (60% overlap) = 0.40*5750 m = 2300 m (Between photocentres)

Time between exposures?= 2300m/160 km/hr = 51.75 s

FLIGHT PLANNING

Area to be photographed

North

16 km

10 km

Camera characteristics:• f = 152.4 mm• Film format = 230 mm

Photoscale: 1:25000End-lap – 60%; side-lap 30%

Average elevation: 300m

Beginning and ending flight lines should be along the boundaries

Because time can set in seconds, the number is rounded off. Recalculate the distance between photos?51 sec/phot * 160 km/hr = 2267 m

Number of photos?

= 16000 m per line/2267 m/photo + 1 +1 =9.1 (use 10)

Flight line separation?

30% sidelap = separation of 70% of the coverage = 0.70 * 5750 m = 4025 m between flight lines

Number of flight lines?

= 10000/4025 +1 = 3.48 (use 4)

Adjusted flight line space? = 10000/(4-1) spaces = 3333 m

Total number of photos?= 10 photos per line + 4 lines = 40 photos

Principles of Remote Sensing : NR –603

• Atmospheric windows and effects, corrections• Multispectral systems• Characteristics of important remote sensing systems: LANDSAT, IRS,

ASTER, SPOT; • High resolution sensors• Hyperspectral sensors• Thermal systems• Microwave systems• Geostationary systems (?)• Interpretations and applications - agriculture, forestry, land-use

mapping, geology, water resources etc etc.

• History and development of remote sensing• Electromagnetic radiation - nature and sources, interaction

with matter and atmosphere

… and Arial Photography/Photogrammetry.