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《Plateau Meteorology》 2004-06
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Analysis and Satellite Monitor of A Developing Process of Hail Cloud

ZHANG Jie~1,LI Wen-li~2, KANG Feng-qin~1, QU Yong-xing~1, SONG Xu-ying~1 nce, Lanzhou Institute of Arid Meteorology, China Meteorological Administration, Lanzhou 730020, China; 2. Lanzhou Central Meteorological Observatory, Lanzhou 730020, China)  
Weather process, energy conversion and reflectance character of a hail cloud in visible and middle infrared bands are analyzed by using the satellite, radar and some observed data including surface and upper air, aiming at a convection process of regional hail generanting on September 21, 2003. The result showed that, accompanying the exchange of atmospheric energy, the convective cool cloud cells in areas of Lake Qinghai to the east move toward the precess of east to combined warm clouds brought by the warm tongue in westsouth of Qinghaihu on the same day, which formed hail and rainstorm weather. The reason is that there are a instability atmosphere layer and effect of surface heated. 1 The cloud developed peak at 17:00, at that time, the lowest temperature of cloud top is -44℃, critical temperature of hail generant is -39.2℃, critical bright-temperature is 221K. (2) Horizontal gradient of temperature of hail cloud is between 20~35℃/50km, it means that character of hail intensity is with hail and without disaster. 3 The effective radius of cloud particle is larger and optical thickness of aerosol is large, which were reflected by CH1 and CH3 reflectance.
【Fund】: 科技部社会公益研究专项"西北地区人工防雹消雹技术"项目(2002DIB10046)资助
【CateGory Index】: P458.121.2
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