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- W2040580930 abstract "Abstract A case of the heavy rain vortex which occurred during the period 14–15 July 1979 is studied using a limited-area mesoscale numerical model. This is a representative example of a group of warm southwest vortices that often form over the eastern flank of the Tibetan Plateau after the onset of the summer Indian monsoon. Some common features of the dynamic structures exhibited both by the simulation and by observations are discussed. The developing vortex is noticeably detached from the polar frontal zone. A 180° phase shift exists between the upper and lower layer vorticity fields. In the boundary layer, a pronounced northward transport of mass and moisture is connected with an intense upward motion near and to the east of the 700-mb vortex center, whole the southward cold advection is insignificant. The vortex originated and rapidly developed in a stagnation region on the lee side of the plateau. The presence of the stagnation region not only removes local dynamical energy sources from the environm..." @default.
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- W2040580930 date "1987-07-01" @default.
- W2040580930 modified "2023-10-16" @default.
- W2040580930 title "Study of a Heavy Rain Vortex Formed over the Eastern Flank of the Tibetan Plateau" @default.
- W2040580930 doi "https://doi.org/10.1175/1520-0493(1987)115<1370:soahrv>2.0.co;2" @default.
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