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- W2388387029 abstract "Using MM5,a mesoscale model,the sea breeze front(SBF) inducing a rainstorm process in Beibu Gulf on 5 June 2008 was simulated.The results show as follows.(1) The model successfully simulated the area,intensity and time of rainfall.The heavy precipitation process was caused by an SBF in a small-scale circulation system under the environmental background field with such synoptic scale systems as a high-altitude ridge,southwest monsoon,and low-level jet.(2) From sunrise to 14: 00,two relatively hot,humid airstreams separately from the Indian Ocean and South China Sea encounter relatively dry inland cold air in the coastal areas of Beibu Gulf.The warm ocean advection superimposed,increasing temperature gradients.With the accumulation of warm air,instable energy increases the stimulated convection,resulting in sea breeze frontogenesis.A precipitation zone is located roughly between two axises of unstable energy.The energy axis weakened continuously while moving inland,the intensity of precipitation diminished.(3) The vertical scale of this SBF is about 5 km,with convection mainly occurring in the 950～800 hPa layer,and a horizontal scale of about 40～60 km,belonging to a mesoscale system in the near-surface layer.(4) The intensity of SBF is decreasing during the process of its movement from coastline to inland.The thickness of the air flow demonstrates a bulge,i.e.the structure of a head feature.In the head part there is a relatively dry zone that is surrounded by nearly saturated moist air and corresponds with the updrafts center." @default.
- W2388387029 created "2016-06-24" @default.
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- W2388387029 date "2012-01-01" @default.
- W2388387029 modified "2023-10-17" @default.
- W2388387029 title "NUMERICAL SIMULATION STUDY OF A SEA BREEZE FRONT INDUCING A RAINSTORM PROCESS IN BEIBU GULF" @default.
- W2388387029 hasPublicationYear "2012" @default.
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