LiDAR (Light Detection and Ranging) transmits laser pulses (typically near-infrared, ~1064 nm) and measures the round-trip time to derive precise distances to reflecting surfaces. When mounted on aircraft with GPS and inertial navigation, LiDAR generates dense three-dimensional point clouds with centimeter-level vertical accuracy. Unlike passive imagery (2D), LiDAR directly measures elevation and can record multiple returns per pulse -- first return from tree canopy, intermediate returns from branches, last return from the ground -- enabling separation of vegetation from terrain.
While radar uses microwave pulses, LiDAR uses laser pulses -- highly focused beams of light, typically at 1064 nm (near-infrared) for topographic mapping or 532 nm (green) for bathymetric mapping. The fundamental measurement is the precise round-trip travel time of each pulse, giving distance with centimeter-level accuracy.
An airborne LiDAR system integrates three components: the laser scanner (firing 100,000 to 1,000,000 pulses per second), a GPS receiver (providing aircraft position to centimeter accuracy), and an inertial measurement unit (recording aircraft orientation). Together these produce a georeferenced 3D coordinate for every return, generating a point cloud with densities of 1-100+ points per square meter.
The multi-return capability distinguishes LiDAR from other elevation technologies. A single pulse encountering a tree is partly reflected by canopy, branches, and ground. Full-waveform systems record the complete return signal for even finer vertical decomposition. This allows creation of both a Digital Surface Model (including canopy) and a Digital Terrain Model (bare earth) -- the difference being the Canopy Height Model.
Applications span forestry (canopy height, biomass), flood modeling (high-accuracy terrain for hydraulic simulation), archaeology (revealing structures beneath forest canopy), urban modeling (3D city models), and coastal erosion monitoring. Space-based LiDAR (ICESat-2, GEDI) extends these capabilities globally at lower point densities.