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- W2357978049 abstract "Based on the NCEP/NCAR 1°×1°reanalysis data,conventional meteorological data and automatic observations,the two strong convective weather processes caused by cold vortex on June 17,2010 and May 31,2005 were analyzed.The three-dimensional structure characteristic analysis showed that cold vortex and strong convective weather were all located in southwest quadrant of 4-7 latitudes departing from the center of the cold vortex.The greater inclination of positive vorticity column was more advantageous to the hail weather generation.Low-level convergence,high-level convergence,and strong vertical velocity were favorable for hail weather occuring.If temperature advection on 500 hPa and 850 hPa in the southeast quadrant of cold vortex were warm,convective weather would mainly bring precipitation,but if temperature advection on 500 hPa in the southeast quadrant of cold vortex was cold,and warm on 850 hPa,convective weather would mainly bring strong wind and hail.And there was good corresponding relation between the low-level strong frontogenesis region and strong convective weather areas.North side of the positive frontogenesis function center often occurred a wide range of hail weather.Strong convective weather generation in the two weather processes were due to the superposition of the ground cyclonic convergence center and temperature frontal zone.The ground cyclonic convergence center played a well dynamic lifting role in the thunderstorms trigger and development processes." @default.
- W2357978049 created "2016-06-24" @default.
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- W2357978049 date "2012-01-01" @default.
- W2357978049 modified "2023-09-22" @default.
- W2357978049 title "Analysis on Structure Characteristic of Two Cold Vortex Processes" @default.
- W2357978049 hasPublicationYear "2012" @default.
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