Reprocessed, Bias-Corrected CMORPH Global High-Resolution Precipitation Estimates from 1998

Author:

Xie Pingping1,Joyce Robert2,Wu Shaorong2,Yoo Soo-Hyun3,Yarosh Yelena3,Sun Fengying2,Lin Roger2

Affiliation:

1. NOAA/Climate Prediction Center, College Park, Maryland

2. NOAA/Climate Prediction Center, College Park, and Innovim, LLC, Greenbelt, Maryland

3. NOAA/Climate Prediction Center, College Park, Maryland, and Wyle, Inc., McLean, Virginia

Abstract

Abstract The Climate Prediction Center (CPC) morphing technique (CMORPH) satellite precipitation estimates are reprocessed and bias corrected on an 8 km × 8 km grid over the globe (60°S–60°N) and in a 30-min temporal resolution for an 18-yr period from January 1998 to the present to form a climate data record (CDR) of high-resolution global precipitation analysis. First, the purely satellite-based CMORPH precipitation estimates (raw CMORPH) are reprocessed. The integration algorithm is fixed and the input level 2 passive microwave (PMW) retrievals of instantaneous precipitation rates are from identical versions throughout the entire data period. Bias correction is then performed for the raw CMORPH through probability density function (PDF) matching against the CPC daily gauge analysis over land and through adjustment against the Global Precipitation Climatology Project (GPCP) pentad merged analysis of precipitation over ocean. The reprocessed, bias-corrected CMORPH exhibits improved performance in representing the magnitude, spatial distribution patterns, and temporal variations of precipitation over the global domain from 60°S to 60°N. Bias in the CMORPH satellite precipitation estimates is almost completely removed over land during warm seasons (May–September), while during cold seasons (October–April) CMORPH tends to underestimate the precipitation due to the less-than-desirable performance of the current-generation PMW retrievals in detecting and quantifying snowfall and cold season rainfall. An intercomparison study indicated that the reprocessed, bias-corrected CMORPH exhibits consistently superior performance than the widely used TRMM 3B42 (TMPA) in representing both daily and 3-hourly precipitation over the contiguous United States and other global regions.

Funder

NOAA/CPO Climate Monitoring and Observation Program

NOAA/CPO Ocean Climate Observation Program

National Oceanic and Atmospheric Administration

NOAA/NESDIS/NCEI Climate Data Record Program

Publisher

American Meteorological Society

Subject

Atmospheric Science

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