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- W2368793464 abstract "This paper studies a deep convection in warm sector and abnormal subtropical front caused by a cutoff low over East Asia in June 2009,by using cloud profile radar data from Cloudsat,temperature of black body from FY2C,atmospheric compositions from Aura/MLS,meteorological data from ECMWF and HYSPLIT4trajectory model.The analysis shows that,for the sake of the background of southern trough,there are two weaker rain bands from theinner fronts,while nearly 1000km scale deep convection occurs in warm sector.At the nearly mature stage of the low,the subtropical front induced by the cutoff low is abnormally developing throughout whole troposphere,which is due to the warm and humid air from southwest gathering along the subtropical front.After rapid eastward moving of the front into rain belt in warm sector,the strong ascending branch of thermal indirect secondary circulation across the frontal zone enhances deep convection at the colder part below the front.But it is difficult to sustain because the supplement of water vapor is blocked by the abnormal front.Furthermore,intense stratosphere-troposphere exchange occurs in the abnormal subtropical front zone due to the convective injection into stratospheric intrusions.On the scatter plot of ozone and water vapor these are two special gathering areas with both high(low)concentrations of the two species." @default.
- W2368793464 created "2016-06-24" @default.
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- W2368793464 date "2014-01-01" @default.
- W2368793464 modified "2023-09-24" @default.
- W2368793464 title "Stratosphere-troposphere exchange corresponding to a deep convection in warm sector and abnormal subtropical front induced by a cutoff low over East Asia" @default.
- W2368793464 hasPublicationYear "2014" @default.
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