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- W2373961570 abstract "Aim To analyze climatic causes between the situation in winter of historic typical wet cold pattern and that of historic typical dry warm pattern so as to provide basis of short-term climatic trend forecast in winter.Methods Use the climatic statistical diagnosis analysis and climatic dynamics analysis method.Results Typical wet cold pattern and typical dry warm pattern in winter have contrary features in the circulation situation,surface pressure field,the horizontal wind field at lower layer and so on.Conclusion The typical wet cold pattern has the 500hPa general circulation characteristics of the long stable existence of the blocking over Ural mountain and Aral Sea low trough,the activity of lower pressure in Tibetan Plateau,Aral sea low trough splitting cold sir converged with warm humid air in Shaanxi Province,stronger Mongolia high,accompanying continuous southward intrusion of cold air.The typical warm dry pattern has 500hPa general circulation features of two troughs one ridge distribution in mid-latitude Europe and Asia,low trough over the northwest Europe and Okhotsk,stronger pressure ridge over Siberia and Balkhash,which formed high east low west circulation situation,weaker Mongolia high-pressure system." @default.
- W2373961570 created "2016-06-24" @default.
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- W2373961570 date "2010-01-01" @default.
- W2373961570 modified "2023-09-23" @default.
- W2373961570 title "The comparative analysis between the typical wet cold climate and the typical warm dry climate in winter in Shaanxi Province" @default.
- W2373961570 hasPublicationYear "2010" @default.
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