Abstract

This paper revisits the problem of finding a parametric form for the rain drop size distribution (DSD) which (1) is an appropriate model for tropical rainfall, and (2) involves statistically independent parameters. Using TOGA/COARE data, the authors derive a parametrization which meets these criteria. This new parametrization is an improvement on the one that was derived by Z. S. Haddad et al. (1996) using TRMM ground truth data from Darwin, Australia. The new COARE data allows the authors to verify that the spatial variability of the two "shape" parameters is relatively small, thus confirming that this parametrization should be particularly useful for remote sensing applications. They also derive new DSD-based radar-reflectivity-rain-rate power laws, whose coefficients are directly related to the shape parameters of the DSD. Perhaps most important, since the coefficients are independent of the rain-rate itself, and vary little spatially, the relations are ideally suited for rain retrieval algorithms. It should also prove straightforward to extend this method to the problems of estimating cloud hydrometeors from remote-sensing measurements.

Keywords

Parametrization (atmospheric modeling)RadarParametric statisticsRemote sensingRain rateParametric modelComputer scienceMeteorologyEnvironmental scienceAlgorithmMathematicsGeologyStatisticsPhysicsRadiative transfer

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Publication Info

Year
1997
Type
article
Volume
35
Issue
3
Pages
532-539
Citations
111
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Ziad S. Haddad, David Short, Stephen L. Durden et al. (1997). A new parametrization of the rain drop size distribution. IEEE Transactions on Geoscience and Remote Sensing , 35 (3) , 532-539. https://doi.org/10.1109/36.581961

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DOI
10.1109/36.581961