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- W2361289711 abstract "Gust front is often produced by mesoscale convective system and produce low altitude wind shear that can be hazardous to aircraft operations.A gust front,produced by a severe mesoscale convective system happened in Nanjing on 29 June 2006,was examined.The gust front structure was analyzed with single Doppler radar data and surface mesonet data collected in Nanjing region.When gust front occurred,some physical features were obviously observed by surface mesonet,including wind direction change,wind speed increase,pressure intensifying,temperature descending,and then the rainfall.These were compatible with classical gust front theories.Refraction was figured out by using pressure,relative humidity and temperature.This parameter zoomed when gust front arrived,and dropped slowly when gust front moved away.Because rearward of convective system after the leading edge was very moist,refraction kept high for a time.The reflectivity and echo height of gust front were stronger than those of both sides resulted from radar observation data.The distance between gust front and leading edge extended from 5 to 10 km.Wind field simulated from radar observation radial velocity showed faster wind at upper level than at low level,and the center of large velocity area at upper level was anterior.Rear flow could been seen from the simulated wind field at low level.The feature of gust front showed in radar observation was obviously intensity composed shear line.Using this feature,an auto detection method was designed,which could availably detect gust front.Combinatorial shear line indicated the development and track of gust front." @default.
- W2361289711 created "2016-06-24" @default.
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- W2361289711 date "2009-01-01" @default.
- W2361289711 modified "2023-09-24" @default.
- W2361289711 title "Analysis of a Gust Front Process in Early Summer of Nanjing Region" @default.
- W2361289711 hasPublicationYear "2009" @default.
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