Handout (2.3 MB)
The objective of this study is to estimate the rainfall rate (R) and total rainfall produced by a storm on 18 July 2010. We will first use an algorithm based on the differential phase shift (ÔDP) to correct Zh and ZDR for attenuation and differential attenuation. In the next step, we use three different relationships between rain rate and polarimetric variables ( R(KDP,ZDR), R(Zh,ZDR), R(KDP) ) to calculate an instantaneous rain rate map. Finally we calculate the total rainfall produced by the storm and use ground observations for validation of the method. This will allow us to determine the best rain rate algorithm according to rain regime (convective, stratiform).
This work was partially funded by MIT Lincoln Laboratory's NEXRAD Enhancements Program for the FAA.
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