Tuesday, 25 October 2005: 3:30 PM
Alvarado ABC (Hotel Albuquerque at Old Town)
Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR), TRMM Microwave Imager (TMI) and Visible and Infrared Scanner (VIRS) observations within the Precipitation Feature (PF) database have been analyzed to examine regional variability in rain area and maximum horizontal extent of rainfall features, and role of storm morphology on rainfall production (and thus modes where vertically integrated heating occurs). It was found that 9 percent of rain features extend to the edge of the PR swath, with edge features contributing 42 percent of total rainfall. However, the area (maximum dimension) distribution of features is similar to the wider-swath TMI up until a truncation point of nearly 30 000 km2 (250 km), so a large portion of the feature size spectrum may be examined using the PR as with past ground-based studies. This study finds distinct differences in land and ocean storm morphology characteristics, which lead to important differences in rainfall modes regionally. A larger fraction of rainfall comes from more horizontally and vertically developed PFs over land than ocean due to the lack of shallow precipitation in both relative and absolute frequency of occurrence, with a tri-modal distribution of rainfall contribution versus feature height observed over the ocean. Mesoscale Convective Systems (MCSs) are found to be responsible for up to 90 percent of rainfall in selected land regions. Tropics-wide, MCSs are responsible for more than 50 percent of rainfall in almost all regions with average annual rainfall exceeding 3 mm dy-1. Characteristic variability in the contribution of rainfall by feature type is shown over land and ocean, which may allow constraint on the development of improved convective parameterizations.
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