J1.5
Atmospheric diabatic heating distributions derived from a combination of satellite sensor data
William S. Olson, Univ of Maryland Baltimore County, Greenbelt, MD; and T. S. L'Ecuyer, M. Grecu, G. Gu, X. Jiang, and M. G. Bosilovich
Satellite estimates of atmospheric latent+eddy heating (Q1-QR) and radiative heating (QR) are combined to yield estimates of the large-scale diabatic heating, or apparent heat source (Q1). The latent+eddy and radiative heating estimates rely on cloud and precipitation information from TRMM Microwave Imager (TMI) data, with additional cloud information supplied by the TRMM Visible and Infrared Scanner (VIRS) and clear-air environmental properties from NCEP reanalyses. Comparisons of the diabatic heating estimates to those derived primarily from the TRMM Precipitation Radar (PR) and from rawinsonde diagnostic budgets are favorable, although some biases due to differences in sampling and the limited sensitivity of the TMI are noted. The addition of an approximate Q1-QR estimate for non-precipitating regions leads to mean heating from precipitating/non-precipitating Q1-QR and mean cooling from QR in the troposphere that are roughly balanced over the TRMM domain.
Recently, an eleven-year database of diabatic heating has been constructed using TRMM observations from 1998-2008, as part of NASA's Energy and Water cycle Study (NEWS) program. Initial applications of this dataset have been the delineation of the seasonal cycle in the tropics/subtropics, the distribution of heating anomalies associated with the phases of ENSO, and the progression of heating in the Madden Julian Oscillation. Preliminary comparisons of satellite heating estimates versus model-based heating and dynamical fields from the Modern Era Retrospective-Analysis for Research and Applications (MERRA) will be presented at the conference.
Joint Session 1, Measuring the Water Cycle From Space
Monday, 27 September 2010, 3:30 PM-5:00 PM, Capitol D
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