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Instrument

D2P
Delay-Doppler Phase-monopulse Radar

The Delay-Doppler Phase-monopulse (D2P) Radar is an airborne radar altimeter developed by Johns Hopkins University Applied Physics Laboratory (JHU/APL). It was designed to demonstrate improvements in satellite radar altimetry and to reduce risks for future flight programs. It uses delay/Doppler and phase-monopulse radar techniques to measure the distance between the altimeter and the surface. It operates at 13.9 MHz and altitudes from 300 to 12000 meters. At a flight altitude of 6000 meters, D2P has a Doppler bin separation of 25 meters. D2P has been used to measure sea ice elevation and snow depth.

NASA's DC-8 flying laboratory passes Antarctica's tallest peak, Mount Vinson, on Oct. 22, 2012, during a flight over the continent to measure changes in the massive ice sheet and sea ice. Credit: NASA/Michael Studinger (Photography courtesy NASA Images)

Instrument Details

Radar
Earth Science > Land Surface > Topography > Terrain Elevation
Earth Science > Spectral/engineering > Radar > Doppler Velocity
Earth Science > Atmosphere > Altitude
Earth Science > Cryosphere > Sea Ice > Sea Ice Elevation
Earth Science > Spectral/engineering > Radar
Full Column Profile
N/A
25 m
13.9 MHz
Currently unavailble
  • Keith Raney

  • Keith Raney

  • JHU/APL

  • NASA Instrument Incubator Program

  • Currently unavailable