10th Conference on Satellite Meteorology and Oceanography

P5.1

Development of the PM-1 AMSR amd TMI land precipitation algorithms

Jeffrey R. McCollum, NOAA/NESDIS, Camp Springs, MD; and R. R. Ferraro

The PM-1 Advanced Microwave Scanning Radiometer (AMSR) is a new passive microwave instrument that will fly on NASA's Earth Observing System (EOS) PM-1 satellite, planned for launch in the year 2000. The PM-1 AMSR instrument is a modified version of the AMSR built for deployment on the Japanese Advanced Earth Observing Satellite-II (ADEOS-II). Precipitation is one of the many atmospheric, land, and oceanic parameters that will be estimated using AMSR data.

The PM-1 AMSR land and ocean rainfall algorithms are being developed separately, but the final global rainfall algorithm will be unified such that both land and ocean instantaneous rainfall estimates will be produced using the Goddard Profiling Algorithm (GPROF). The GPROF produces instantaneous rainfall estimates from the weighted average of rainfall rates from different hydrometeor profiles created from a cloud model database. The profiles used for estimation are chosen so that the observed microwave radiances match those obtained from radiative transfer calculations with the cloud model output. For the unified PM-1 AMSR algorithm, different profile databases will be used over land and ocean.

The databases used in this algorithm are selected to satisfy specified objectives. The initial database is chosen from cloud model output cases that result in relationships between rainfall rate and brightness temperature similar to those of the current FNMOC operational SSM/I land rainfall algorithm (that was developed at NESDIS). This database is then modified based on considerations such as location, season, and convective/stratiform classification, with the objective of providing the most realistic set of candidate profiles for the given situation. The results of this study are applied to SSM/I, TMI, and AMSR algorithms (all in the GPROF framework), as the same cloud model output cases are used in calculations of microwave brightness temperatures for the different frequencies and resolutions of each of these three sensors.

Poster Session 5, Retrieval of Atmoshperic Profiles and Constituents: Part II
Wednesday, 12 January 2000, 3:00 PM-5:00 PM

Next paper

Browse or search entire meeting

AMS Home Page