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and N16 data for the years 2002–07. These results should facilitate comparisons with other sensors and datasets, and they include retrievals of annual accumulations of rain, snow, and convective and stratiform precipitation as well as two seasonal examples. Strong interannual variations are evident—in particular, in the Arctic where this algorithm successfully maps precipitation events for over four warm months each year despite extensive ice cover. Comparisons with Global Precipitation
and N16 data for the years 2002–07. These results should facilitate comparisons with other sensors and datasets, and they include retrievals of annual accumulations of rain, snow, and convective and stratiform precipitation as well as two seasonal examples. Strong interannual variations are evident—in particular, in the Arctic where this algorithm successfully maps precipitation events for over four warm months each year despite extensive ice cover. Comparisons with Global Precipitation
