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.

Instrument Details
- Radar
- Earth Science > Land Surface > Topography > Terrain ElevationEarth Science > Spectral/engineering > Radar > Doppler VelocityEarth Science > Atmosphere > AltitudeEarth Science > Cryosphere > Sea Ice > Sea Ice ElevationEarth 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
Unpublished
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