Titlebook: Intense Atmospheric Vortices; Proceedings of the J Lennart Bengtsson,James Lighthill Conference proceedings 1982 Springer-Verlag, Berlin He

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书目名称Intense Atmospheric Vortices影响因子(影响力)




书目名称Intense Atmospheric Vortices影响因子(影响力)学科排名




书目名称Intense Atmospheric Vortices网络公开度




书目名称Intense Atmospheric Vortices网络公开度学科排名




书目名称Intense Atmospheric Vortices被引频次




书目名称Intense Atmospheric Vortices被引频次学科排名




书目名称Intense Atmospheric Vortices年度引用




书目名称Intense Atmospheric Vortices年度引用学科排名




书目名称Intense Atmospheric Vortices读者反馈




书目名称Intense Atmospheric Vortices读者反馈学科排名

nuclear-tests

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Influence of Environmental Conditions on the Genesis of a Tropical Stormel basic flow has an impact on the latent energy supply which is essential for genesis. The upper level basic flow has to be coupled with the phase speed of the low level incipient disturbance. The low level cyclonic shear of the basic flow is conducive to storm genesis.

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The Numerical Experiment on the Contribution of Landed Typhoon to the Rainfall in North China adjacent sea areas. Furthermore, some of typhoons may generate heavy rainfall in North China when they are interacting with the cold air of westerlies. Such kind of rainfall process is considered as “indirect” typhoon rainstorm, which constituted the majority of the heavy rainfall (≥100 mm.day.) an

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Estimation of Radial Distribution of Eddy Viscosity in a Mature Hurricaneibution of tangential velocity in a mature hurricane. It is an extension of a previous paper by EVANS and DAVTES (1979), which was concerned with the vertical distribution of the eddy viscosity components. Over most of the region between the eye boundary and the position of maximum tangential veloci

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The Factors Determining Radial Flow and Eye Formation in an Intensifying Tropical Cyclonend at the same time the moist static energy sink. On the other hand, surface transfers determine the angular momentum sink and the moist static energy source. It was pointed out by Pearce [1981] that whether or not intensification can occur depends crucially on the vertical distributions of the mois