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1 A dual-polarization radar hydrometeor classification algorithm for ...

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329330331332333334335336337338339340341342343344345346347348349350351Modifications to this <strong>algorithm</strong> necessitated (a) new procedures, (b) new membership betafunctions, and (c) a variable weighting system <strong>for</strong> each precipitation category. These three stepssubstantially increased the <strong>algorithm</strong>’s ability to distinguish different precipitation categoriesaccording to literature examples of these features, decreased its reliance on external temperaturedata to make <strong>classification</strong>s, and allowed it to work well on a variety of <strong>radar</strong> plat<strong>for</strong>ms.This <strong>algorithm</strong> assumes ice or mixed-phase precipitation is occurring somewhere in thedomain so an appropriate convective warm-season <strong>algorithm</strong> should be consulted under otherconditions. Non-meteorological echo must be removed a priori. A 5 dBZ reflectivity and 7-10 dBSNR threshold was also used to avoid mis<strong>classification</strong>s at echo edges due to nonmeteorologicalZ dr increases.a) Algorithm proceduresAs is typical <strong>for</strong> many HCAs, <strong>classification</strong> is per<strong>for</strong>med on each pixel without knowledge ofdecisions made <strong>for</strong> nearby pixels or how the <strong>radar</strong> variables trend with height and time. Park etal. (2009) suggests that HCA per<strong>for</strong>mance can be optimized if indivi<strong>dual</strong> <strong>algorithm</strong>s aredeveloped <strong>for</strong> each major precipitation regime. It may be unrealistic to design a single <strong>algorithm</strong>(or single set of MBFs) to handle convective, strati<strong>for</strong>m, warm, and cold-season precipitation.Our HCA methodology is demonstrated during a strati<strong>for</strong>m freezing rain event in centralOklahoma with the C-band OU-PRIME <strong>radar</strong> in Norman, OK (Palmer et al. 2011). The nearbysoundings <strong>for</strong> this event are shown in Fig. 3, which exhibit a strong temperature inversion and acold surface layer from 15 UTC until 21 UTC. Fig. 4 shows the 2.4° PPI of OU-PRIME C-bandpolarimetric <strong>radar</strong> variables through the melting layer of strati<strong>for</strong>m precipitation when METARreports indicated freezing rain at the surface. A DGZ of enhanced K dp and Z dr with reduced ! hvappears aloft toward the southwest. This particular <strong>radar</strong> scan was used to verify that the16

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