In a LiDAR system, pulses of light travel to the ground. They return and are detected by the sensor giving the range (a variable distance) to the Earth. Hence, how they earned their name of Light Detection and Ranging.
In the end, LiDAR delivers a massive point cloud filled of varying elevation values. But these elevation values can come from the top of buildings, tree canopy, powerlines and other types of features. A DSM captures the natural and built features on the Earth’s surface.
A DSM is especially useful in 3D modelling and is relevant in telecommunications, urban planning, aviation and forestry. This is because objects extrude from the Earth, which is particularly useful in these examples:
Runway approach zone encroachment – In aviation, runway obstructions in the approach zone can be examined with a DSM to ensure no collisions.
Vegetation management – Along a transmission line, overlaying a DSM to see where and how much vegetation is encroaching.
View obstruction – Urban planners use DSM to check how a proposed building would affect the viewshed of other residents and businesses.
What is a Digital Elevation Model (DEM)?
A digital elevation model is a regularly-spaced bare-earth raster grid referenced to a common vertical datum. When you filter out non-ground points such as bridges and roads, you are left with a smooth digital elevation model. The built (powerlines, buildings and towers) and natural (trees and other types of vegetation) aren’t extruding in a DEM.
When you void vegetation and man-made features from elevation data, you obtain a DEM. A smooth, bare-earth elevation model is particularly useful in fields of study such as hydrology, soils and land use planning/safety. Here are examples how a DEM can be used in GIS:
Hydrologic modelling – A DEM is used to delineate watersheds, calculate flow accumulation and find out flow direction.
Terrain stability – Areas prone to avalanches are high slope areas with sparse vegetation, which is useful when planning a highway or residential subdivision.
Soil mapping – DEMs assist in mapping soils which is a function of elevation (as well as geology, time and climate).