Comparison of TRMM Microwave Imager Rainfall Datasets from NASA and JAXA

Author:

You Yalei1,Wang Nai-Yu1,Kubota Takuji2,Aonashi Kazumasa3,Shige Shoichi4,Kachi Misako2,Kummerow Christian5,Randel David5,Ferraro Ralph6,Braun Scott7,Takayabu Yukari8

Affiliation:

1. a Earth System Science Interdisciplinary Center, and Cooperative Institute for Climate and Satellites, University of Maryland, College Park, College Park, Maryland

2. b Earth Observation Research Center, Japan Aerospace Exploration Agency, Tsukuba, Japan

3. c Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan

4. d Graduate School of Science, Kyoto University, Kyoto, Japan

5. e Colorado State University, Fort Collins, Colorado

6. f NOAA/NESDIS/STAR, College Park, Maryland

7. g Laboratory for Atmospheres, NASA Goddard Space Flight Center, Greenbelt, Maryland

8. h Atmosphere and Ocean Research Institute, The University of Tokyo, Tokyo, Japan

Abstract

AbstractThis study compares three TMI rainfall datasets generated by two versions of NASA’s Goddard Profiling algorithm (GPROF2010 and GPROF2017) and JAXA’s Global Satellite Mapping of Precipitation algorithm (GSMaP) over land, coast, and ocean. We use TRMM precipitation radar observations as the reference, and also include CloudSat cloud profiling radar (CPR) observations as the reference over ocean. First, the dynamic thresholds for rainfall detection used by GSMaP and GPROF2017 have better detection capability, indicating by larger Heidke skill score (HSS) values, compared with GPROF2010 over both land and coast. Over ocean, all three datasets have very similar HSS regardless of including CPR observations. Next, intensity analysis shows that no single dataset performs the best according to all three statistical metrics (correlation, root-mean-square error, and relative bias), except that GSMaP performs the best for stratiform precipitation over coast, and GPROF2017 performs the best for convective precipitation over ocean, based on all three metrics. Finally, an error decomposition analysis shows that the total error and its three components have very different characteristics over several regions among these three datasets. For example, the positive total error in GPROF2010 and GSMaP is primarily caused by the positive hit bias over central Africa, while the false bias in GPROF2017 is largely responsible for this positive total error. For future algorithm development, results from this study imply that a convective–stratiform separation technique may be necessary to reduce the large underestimation for convective rain intensity.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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