|Coverage||Global Ocean (90N-90S, 0-360E)|
|Time Period||July 1987 - Present|
|Resolution||2.5 x 2.5 degree, monthly|
Window channel observations from passive microwave radiometers have been used to estimate rainfall since the launch of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave/Imager (SSM/I) in July of 1987. Over radiometrically cold ocean regions, changes in brightness temperature due to the absorption/emission by liquid hydrometeors at frequencies below the 50-60 GHz oxygen absorption band is directly related to rainfall. While this approach doesn't work over radiometrically warm land surfaces, scattering by precipitation size ice particles at frequencies above the oxygen absorption band can be used to estimate rainfall. Microwave sounding channel data have also been used to estimate rainfall going back to 1979 from the Microwave Sounding Unit (MSU) on board NOAA's TIROS-N polar-orbiting satellite in October of 1978. Although MSU provides a longer data record than SSM/I, poor spatial resolution of the sensor along with limited precipitation information have limited it use primarily to enhance coverage prior to SSM/I in the merged CMAP product.
This dataset is one of the intermediate products from version 2 of the Global Precipitation Climatology Project (GPCP) merged rainfall dataset.
The SSM/I emission dataset provides rain estimates over ocean regions only and is based on the retrieval algorithm by Wilheit et al. . Because emission-based passive microwave retrievals rely on having a radiometrically cold background, such techniques cannot be applied over radiometrically warm land regions. The SSM/I emission dataset is one of the component rainfall estimates used in the GPCP merged dataset [Huffman et al., 1997].
This dataset and other GPCP intermediate datasets are available through either of the following sources.