Why collect elevation data?
Topography is important for describing:
POINT CLOUD
A ‘cloud’ of points in 3D space
-represents 3D surface made of 100s to millions of points
Simple data structure
Can be converted to other formats:
LIGHT DETECTION & RANGING (LiDAR)
a laser pulse is emitted and the time of reflection from the earth’s surface is recorded
-knowing speed of light can calculate distance
lidar can capture multiple ‘returns’
-last return represents ‘bare’ earth
commonly used in: geology, glaciology, forestry, archaeology, conservation
AIRBORNE LiDAR SCANNING
Requires:
Typically:
STRUCTURE FROM MOTION (SfM)
point cloud creation from photos
photogrammetry
-terrestrial/aerial
no lasers but instead
Requires:
SATELLITE APPLICATIONS
all techniques can also be applied from satellites
LiDAR: ICESat-1, ICESat-2 (since 2018)
Radar: Shuttle radar topography mission (SRTM), Tandem-X
Photogrammetry: Aster, Worldview
Airborne scanning advantages and disadvantages
Advantages:
Disadvantages:
TERRESTRIAL LiDAR SCANNING
Requires:
Typically:
Airborne laser scanning advantages and disadvantages
Advantages:
Disadvantages:
Terrestrial laser scanning advantages and disadvantages
Advantages:
Disadvantages:
SfM advantages and disadvantages
Advantages:
Disadvantages:
Radar advantages and disadvantages
Advantages:
-can detect surfaces through clouds, independent of weather and works at night
Disadvantages:
-not as high resolution
Imaging by Radar
Across the image swath the angle changes because of elevation and therefore a phase variation is measured across the swath. Two satellites are needed. Example: Tandem-X satellite mission