CAO Fang, LI Yunying. 2011: Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event. Torrential Rain and Disasters, 30(1): 30-37.
Citation:
CAO Fang, LI Yunying. 2011: Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event. Torrential Rain and Disasters, 30(1): 30-37.
CAO Fang, LI Yunying. 2011: Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event. Torrential Rain and Disasters, 30(1): 30-37.
Citation:
CAO Fang, LI Yunying. 2011: Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event. Torrential Rain and Disasters, 30(1): 30-37.
Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event
Taking an excessive heavy rain event which occurred in Guangxi on 12 June 2008 for example,based on the surface precipitation data and the LAPS 0.045°×0.045°data collected in the SCHeREX,the meso-scale disturb
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