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- W2361308574 abstract "By using the conventional meteorological observation data, automatic weather station intensive observational data, T213 physical quantity field, satellite images and radar echo data, a preliminary diagnostic analysis is made on the circulation background, satellite cloud images, evolution characteristics of precipitation echo and the physical cause of the continuous rainstorm in midsummer of 2008 in Hubei. The results show that the long-wave trough over mid-latitude is developing, moving eastward and southward slowly and inducing cold air moving southward with splitting small tanks converge with warm and moist air on peripheral of the stationary west Pacific subtropical high in the middle reaches of Yangtze river should be the cause of this process. During the heavy rain process, the middle and low level convergence and low-level jet from southwest offer enough water vapor for the rainstorm. The low-level warm advection and surface warm inverted trough afford great instability energy for the heavy rainfall. The fiercer confluence of both cold and warm air is beneficial to strengthen convection with the precipitation system moving eastward. And this is manifested as the generation, development and consolidation of multiple mesoscale cloud clusters in the satellite images. The Doppler radar products show that the precipitation echo of stratiform cloud is converted to the mixed one, with the occurrence and development of strong convection multicell echo." @default.
- W2361308574 created "2016-06-24" @default.
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- W2361308574 date "2010-01-01" @default.
- W2361308574 modified "2023-09-25" @default.
- W2361308574 title "Analysis on a Continuous Rainstorm Process in Midsummer of 2008 in Hubei Province" @default.
- W2361308574 hasPublicationYear "2010" @default.
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