| | The first echo is reflected by the ground surface, hence by treetops, high-voltage transmission lines or roof ridges, the last echo mostly by the land underneath. A Digital Surface Model (DSM) is generated by the selection of the first echo. The last echos are the starting point for generating the Digital Terrain Model (DTM). Given reflectors, such as house roofs or roads, both echos are identical. A feature distinguishing the principle of laserscanning from terrestrial surveying, but also from photogrammetry, is that no selection of single prominent points takes place during measurement. The acquisition of areal data of extensive terrain is to the fore. Laserscanning is highly cost-effective in this connection because the processing sequence of the data can be very largely automated, from the acquisition in flight, through the evaluation, all the way to the end product of the elevation model.
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