Tropical Rainfall Distributions Determined Using TRMM Combined with Other Satellite and Rain Gauge Information

By Robert F. Adler, George J. Huffman, D. Bolvin, S. Curtis, E. Nelkin. 2000

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WHERE ARE THE MOST INTENSE THUNDERSTORMS ON EARTH (2006, background): “There are numerous papers describing the improved quantitative estimates of precipitation and its variability (e.g., Adler et al. 2000, 2003; Nesbitt et al. 2004), the diurnal cycle (e.g., Negri et al. 2002; Nesbitt and Zipser 2003), the partit ioning between convective and stratiform precipitation…”
Surface Fluxes and Tropical Intraseasonal Variability: a Reassessment (2008, methodology): “The TRMM 3B42 product we use here incorporates several satellite measurements, including the TMI and TRMM precipitation radar to calibrate infrared measurements from geostationary satellites (Adler et al. 2000).”
The Evolution of the Goddard Profiling Algorithm (GPROF) for Rainfall Estimation from Passive Microwave Sensors (2001, background): “An example of this overestimation occurred during the Third WetNet Precipitation Intercomparison Project (PIP-3) intercomparison (Adler et al. 2000).”