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- W2371845405 abstract "The fields of geopotential height,anomalous change of high-level jet-stream,helicity,divergence and stratification conditions as the circulation dynamical structure in course of the sand-dust storm occurrence in southern Xinjiang in spring of 2003 are analyzed based on observed data and T213 data.The results show that(1)the polar cold air entering into Tarim basin caused sand-dust storms in large extent because of eruptive development of Iran high and Ural ridge pile up;(2)The eruptive and violence development of west cold Siberian high pressure principally caused strong sand-dust storms;(3)The jetstream over South Xinjiang caused by anomalous change of high jetstream resulted in ground gale by descending momentum,which are one of the dynamical conditions of sand-dust storm;(4)The distribution feature of helicity over the sand-dust storm area is negative at the high level and positive at the lower,which implied that the strong rotating ascend is another one of the dynamical conditions of sand-dust storm;(5)There is a vertical structure with convergence at lower level and divergence at upper level over the sand-dust storm area,this is favorable for occurring strong wind near ground and rising stream;(6)The case of sandstorm is a strong convection process,when the air stratification is convection neutral or instability,but all with strong development of baroclinic instability.Cold air and warm air meet strongly;there is energy collecting period before sand-dust storm,and the period is very short." @default.
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- W2371845405 date "2006-01-01" @default.
- W2371845405 modified "2023-09-26" @default.
- W2371845405 title "Circulation Dynamical Structure of Sand-Dust Storm Caused by Cold Air Crossing Mountains in Southern Xinjiang" @default.
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