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## PowerPoint Slideshow about 'Photogrammetry' - zoie

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Presentation Transcript

Introduction

- Photogrammetry: the science, art, and technology of obtaining reliable information from photographs.
- Two major areas: metric, and interpretative.
- Terrestrial and aerial Photogrammetry.
- Uses of Photogrammetry: topographic mapping, determine precise point coordinates, cross sections, deflection monitoring, and many other applications.
- Why Photogrammetry?

Aerial Cameras

- For precise results, cameras must be geometrically stable, fast, have efficient shutters, sharp lenses
- Single-lens frame cameras: figure 27-2
- most used format size is 9”, focal length 6 in
- components: lens, shutter, diaphragm, filter, focal plane, fiducial marks.
- shutters can be operated manually or automatically.
- The camera could be leveled regardless of the plane orientation.
- Exposure station and principal point.
- Camera calibration.

Aerial Photographs

- True Vertical: if the camera axis is exactly vertical, or near vertical.
- Tilted Photographs
- Oblique photographs: high and low
- Vertical Photos are the most used type for surveying applications

Geometry of Vertical Photographs

- Figure 27-6
- Define: image coordinate system (right handed), principal point, exposure station.
- Measurements could be done using negatives or diapositives, same geometry.
- Strips and Blocks.
- Sidelap (about 30%), and Endlap (about 60%), why?

Scale of a Vertical Photograph

- Figure 28-6
- Scale of a photograph is the ratio of a distance on a photo to the same distance on the ground.
- Photographs are not maps, why?
- Scale of a map and scale of a photograph.
- Orthphotos
- Scale (s) at any point:

f

S =

H - h

f

- Average scale of a photograph:

Savg =

H - havg

If the f, H, and h are not available, but a map is available then:

photo distance

X map scale

Photo Scale =

map distance

Ground Coordinates from a Single Vertical Photograph

- Figure 27-8
- With image coordinate system defined, we define an arbitrary ground coordinate system.
- That ground system could be used to compute distances and azimuths. Coordinates can also be transformed to any system
- In that ground system:
Xa = xa * (photograph scale at a)

Ya = ya * (photograph scale at a)

Relief Displacement on a Vertical Photograph

- Figure 27-9
- The shift of an image from its theoretical datum location caused by the object’s relief. Two points on a vertical line will appear as one line on a map, but two points, usually, on a photograph.
- In a vertical photo, the displacement is from the principal point.
- Relief displacement (d) of a point wrt a point on the datum :

r h

d =

H

where: r is the radial distance on the photo to the high point

h : elevation of the high point, and H is flying height above datum

- Assuming that the datum is at the bottom of vertical object, H is the
- flying height above ground, the value h will compute the object height.

ra/R = f/H

Or: ra *H = R * f ----(1)

rb/R = f/(H-h)

Or: rb * (H-h) =R * f ---(2)

Then from (1) and (2);

Or

ra *H = rb * (H-h) then;

D = rb - ra = rb *hb /H

Flying Height of a Vertical Photograph

- Flying height can be determined by:
- Readings on the photos
- Applying scale equation, if scale could be computed
- Example: what is the flying height above datum if f=6”, average elevation of ground is 900ft, scale is 1”:100ft? Is it 1500’?

- Or, if two control points appear in the photograph, solve the equation:
L2 = (XB - XA)2 + (YB - YA)2

then solve the same equation again replacing the ground coordinates with the photo coordinates.

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