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- W785054721 abstract "Because the real atmosphere is non-uniformly saturated, the generalized potential temperature is introduced. The convective vorticity vector, which can depict the occurrence and development of mesoscale deep convective systems, is modified and re-derived in a nonuniformly saturated moist atmosphere (C*). Then, a case study is performed for a frontal rainfall event which occurred near the middle and lower reaches of the Yangtze River in China. The diagnostic results of C* show that, in the lower troposphere, the vertical component of C* (C*z ) can diagnose developments and movements of precipitation and convection better than those of Cm (Cmz, in saturated moist flow) and C (Cz, in dry flow). C*z is a good predictor for precipitation analyses as well." @default.
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- W785054721 date "2009-01-01" @default.
- W785054721 modified "2023-10-18" @default.
- W785054721 title "Diagnostic Analyses of the Modified Convective Vorticity Vector in Non-uniformly Saturated Moist Flow" @default.
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- W785054721 doi "https://doi.org/10.1080/16742834.2009.11446788" @default.
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