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《Geo-information Science》 2003-01
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Mining Eastward-moving MCSs Features over the Tibetan Platean

GUOZhongyang 1,2LIN Hui1JIANG Jixi3HUANG Qian3FANG Zhaobao1(1 Department of Geography & Joint Laboratory for GeoInformation Science,The Chinese University of Hong Kong,Hong Kong;2 Department of Geography,East China Normal University,Shanghai 200062;3 National Satellite Meteorological Center, China Meteorological Administration, Beijing 100081)  
In this paper, we automatically trace the movement routes of MCSs over the Tibetan Plateau using GMS infrared black body temperature (Tbb) in summer of 1998, while the MCSs are classified according to their move direction.Based on this, the relationships of eastward-moving MCSs features over the Tibetan Plateau and its environment physical field values are obtained using decision tree technique. Results indicated that in 400hPa, when the gravity center location of MCSs is near 100°E, the south east ward moving MCSs that has moved out of the Plateau is only related to the height and temperature over this constant pressure surface;the northeast ward moving MCSs is only related to the height and potential pseudo equivalent temperature; further more, the eastward-moving MCSs that has already moved out of the Plateau mainly depends on four physical values of constant pressure surface height, divergent, vortex and the potential pseudo-equivalent temperature. While in 500hPa, the northeast ward movement of MCSs are mainly influenced by K index and water vapor flux divergent when they lie west to the 104°E, however, to the eastward or southeastward moving MCSs, they are influenced by more factors in this layer.
【CateGory Index】: P458.2
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