Topic 13 Flashcards
(30 cards)
terrain models and GIS
perhaps the most important type of raste data used in GIS is terrain data often referred to as digital elevation models
aquiring terrain data
there are three common ways to collect terrain/elevation data
ground based
airborne direct measurement tech like Lidar
photogrammetric methods
ground based surveys
GNSS and total station surveys can ve used to collect elevation data on the ground
airborne LiDAR surveys
direct measurement of earths surface features
bare-earth models reveal terrian
terrain data from photogrammetry
resurgence of this technoque with advances in digital (softcopy) processing, high-resolution satelittle imaging and drones
photogrammetry
science and technology of making measurements from aerial photographs, drone photographs and satelittle imaged
museum artifacts
data models
(3)
three common ways to represent terrain
raster digital elevation models (DEM)
triangualted irregular networks (TINS)
elevation contours
spatially quantized (raaster) no smooth and continuous (box steps)
dem raster models
most common type of terrain data
sun is walys in the Northwest or Northeast
TIN model (vector)
surface model created from vector data using tesselation of triangles that store elevation attributes at the vertices
has advantages over raster
constructing DEMS and TINS
Lidar and photogrammetry
ground surveys
contouring
usually relate to elevation
create vector representation of breaks
can be done for nearly any feature at interval or ratio scale
isolines
used for visualization
isolines
different lines types
contours = isolines for elevation
visualizing terrain: contours
important way to visualize terrain data, partiularily for static maps
visualizing terrain: hill shading
DEMs and TINs are very useful for geovisualization where terrain interpolation is important
hillshade are also known as shade relief maps
hillshading a DEM
automatic shading
can change elevation of the sun
heights and slopes of surfaces used as input
unidirectional vs multidirectional
light from one direction or multiple directions
class values vs colour ramps
colour ramps = hypsometric tinting
colours end
vs a gradual gradient change
Eyton (1990) colour stereoscopic effect
the use of colours and how more complex colour schemes can be harmful to viewer
visualizing terrain : vertical profiling
interpret changes in elevation
3D rendering of digital surfaces
have become very sophistaced in recent years, and provide a realistic view of terrain surfaces and features
slope and aspect measurements
key measurements that can be performed on terrain models
slope computations
Raster DEMS
computation is the ratio of two components
vertical component
window distance
convert to % or to degrees
change in elevation over distance (derivative)
aspect
direction of slope (derivative)
compass usually from the North
surface curvature
terrain, changing slope over space
first derivative of slope