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- W2393878503 abstract "In order to find out the development mechanism of Shaanxi regional heavy rainstorm and improve the accuracy of forecasting,with NCEP 1°×1°re-analysis data,FY-2E-by-hour TBB data and conventional meteorological observation data,the regional heavy rainfall in Shaanxi province on 28th July 2011 are analyzed by synoptic and dynamical methods.Results show that the main influences to system are 500hPa westerly trough,west pacific subtropical high,700hPa and 850hPa shear.Low level large wind speed and far distant typhoon influence maybe strengthen the rainstorm magnitude.Storm area has strong energy front and convective instability,precipitation occurs on the greater value side of 850hPa temperature-moisture energy.Water vapor mainly comes from the bay of Bengal and Typhoon external.Convergence center and divergence center downwards are the signal of strong precipitation to happen.Specific humidity below 850hPa increasing rapidly has guidance on forecast of Weihe river valley rainfall." @default.
- W2393878503 created "2016-06-24" @default.
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- W2393878503 date "2012-01-01" @default.
- W2393878503 modified "2023-09-23" @default.
- W2393878503 title "Analysis on a Regional Rainstorm in Shaanxi Province in 2011" @default.
- W2393878503 hasPublicationYear "2012" @default.
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