Linked from

The 43 pages that link to LiDAR, each with the reason it gives.

• LaserRelated: Short laser pulses or modulated beams reveal range and shape from return signals.

• SurveyingRelated: Laser scans produce dense three-dimensional measurements of land and structures.

• Rayleigh scatteringRelated: Molecular backscatter can contribute to lidar signals in clear air.

• Inverse-square lawRelated: Its return signal strength depends partly on distance-related spreading and target geometry.

• ScatteringRelated: Scattered returns locate targets and reveal aerosols or cloud particles.

• CanopyRelated: LiDAR can map canopy height and the forest’s three-dimensional structure.

• Mie scatteringRelated: Atmospheric lidar signals depend on scattering by airborne particles.

• PhotodetectorRelated: Its receiver detects returning light to estimate range and construct measurements.

• Atmospheric windowRelated: Laser wavelengths are chosen to pass through the atmosphere and interact with targets.

• Forest degradationRelated: LiDAR can reveal changes in forest height and vertical structure that canopy-cover maps miss.

• Archaeological surveyRelated: Its terrain models can reveal subtle archaeological features beneath forest cover.

• Digital elevation modelRelated: Laser returns can provide dense elevation samples for terrain grids.

• AtmosphereRelated: Lidar detects atmospheric aerosols, clouds, and winds from a distance.

• Specular reflectionRelated: Specular returns can dominate when a target surface faces the laser.

• TopographyRelated: Airborne LiDAR can measure ground elevations beneath vegetation to map terrain.

• Autonomous vehicleRelated: Lidar-based systems contrast with approaches that rely primarily on cameras.

• Laser spectroscopyRelated: Laser spectroscopy can identify atmospheric molecules in range-resolved lidar measurements.

• Strike-slip faultRelated: Bare-earth LiDAR can reveal subtle scarps and offsets along strike-slip faults.

• Orbital rendezvousRelated: Lidar can provide precise range and shape measurements during close approach.

• Spectral line broadeningRelated: Atmospheric lidar can use broadened returns to estimate temperature and wind.

• Atmospheric opticsRelated: Atmospheric lidar uses backscattered light to profile clouds, aerosols, and other atmospheric layers.

• Laser diodeRelated: Laser diodes can serve as emitters in compact or pulsed LiDAR systems.

• Atmospheric absorptionRelated: Absorption at laser wavelengths can affect lidar signals and enable gas measurements.

• Fiber laserRelated: Fiber lasers can supply compact, stable sources for lidar instruments.

• Avalanche photodiodeRelated: Avalanche photodiodes convert faint return light into electrical signals.

• MesosphereRelated: Lidar reveals mesosphere temperatures, winds, and thin ice clouds from the ground.

• GeomaticsRelated: Laser ranging produces dense three-dimensional observations of surfaces.