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The Airborne Topographic Mapper (ATM) measures topography to an accuracy of ten to twenty centimeters by combining measurements from an airborne laser altimeter and GPS (Global Positioning System) receivers. The ATM has demonstrated this accuracy at distances as great as 1000 kilometers from any base station. The current ATM instruments (ATM2 and ATM3) and their predecessors have a history going back to the mid-1970s. The instruments commonly fly aboard the NASA P3-B based at Wallops Flight Facility, Virginia. ATM2 has also flown aboard several twin-otter (DH-6) aircraft. A major task of the ATM over recent years has been the measurement of the Greenland ice sheet with the goal of determining changes in the ice sheet elevation. Other uses have included verification of satellite altimeters and the measurement of sea-ice thickness. The altimeter often flies in conjunction with other instruments and has been used to measure sea-surface elevation and ocean wave characteristics. 

This is a digital elevation model of Mt. Erebus.
Image Caption

This is a high-resolution Digital Elevation Model (DEM) of Mount Erebus in Antarctica captured by ATM at 2x2 meter resolution. Credit: https://atm.wff.nasa.gov/

Instrument Type

Altimeters

Instrument Subtype

Lidar/Laser Altimeters

Specifications

Resolution

Spatial

Varies

Spectral
Varies by instrument model
Temporal

Varies

Frequently Asked Questions

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