GLOBAL PRECIPITATION ESTIMATES BASED ON A TECHNIQUE FOR COMBINING SATELLITE-BASED ESTIMATES, RAIN-GAUGE ANALYSIS, AND NWP MODEL PRECIPITATION INFORMATION
Gj. Huffman et al., GLOBAL PRECIPITATION ESTIMATES BASED ON A TECHNIQUE FOR COMBINING SATELLITE-BASED ESTIMATES, RAIN-GAUGE ANALYSIS, AND NWP MODEL PRECIPITATION INFORMATION, Journal of climate, 8(5), 1995, pp. 1284-1295
The ''satellite-gauge-model'' (SGM) technique is described for combini
ng precipitation estimates from microwave satellite data, infrared sat
ellite data, rain gauge analyses, and numerical weather prediction mod
els into improved estimates of global precipitation. Throughout, month
ly estimates on a 2.5 degrees X 2.5 degrees lat-long grid are employed
. First, a multisatellite product is developed using a combination of
low-orbit microwave and geosynchronous-orbit infrared data in the lati
tude range 40 degrees N-40 degrees S (the adjusted geosynchronous prec
ipitation index) and low-orbit microwave data alone at higher latitude
s. Then the rain gauge analysis is brought in, weighting each field by
its inverse relative error variance to produce a nearly global, obser
vationally based precipitation estimate. To produce a complete global
estimate, the numerical model results are used to fill data voids in t
he combined satellite-gauge estimate. Our sequential approach to combi
ning estimates allows a user to select the multisatellite estimate, th
e satellite-gauge estimate, or the full SGM estimate (observationally
based estimates plus the model information). The primary limitation in
the method is imperfections in the estimation of relative error for t
he individual fields. The SGM results for one year of data (July 1987
to June 1988) show important differences from the individual estimates
, including model estimates as well as climatological estimates. In ge
neral, the SGM results are drier in the subtropics than the model and
climatological results, reflecting the relatively dry microwave estima
tes that dominate the SGM in oceanic regions.