HORIZONTAL AND VERTICAL DISTRIBUTIONS OF CLOUD COVER OVER EASTERN CHINA AND THE EAST CHINA SEA  

作　　者：李昀英 隋兴斌 闫继平 

机构地区：[1]Institute of Meteorology,PLA University of Science and Technology

出　　处：《Journal of Tropical Meteorology》2012年第3期387-392,共6页热带气象学报（英文版）

基　　金：National Basic Research Program of China (973 Program) (2010CB951904);National Natural Science Foundation of China (41075034)

摘　　要：Based on data from satellite and surface observations,the horizontal and vertical distributions of clouds over eastern China and the East China Sea are examined.Three maximum centers of cloud cover are clearly visible in the horizontal distribution of total cloud cover.Two of these maxima occur over land.As the clouds mainly originate from the climbing airflows in the southern and eastern slopes of the Tibetan Plateau,they can be classified as dynamic clouds.The third center of cloud cover is over the sea.As the clouds mainly form from the evaporation of the warm Kuroshio Current,they can be categorized as thermodynamic clouds.Although the movement of the cloud centers reflect the seasonal variation of the Asian summer monsoon,cloud fractions of six cloud types that are distinct from the total cloud cover show individual horizontal patterns and seasonal variations.In their vertical distribution,cloud cover over the land and sea exhibits different patterns in winter but similar patterns in summer.In cold seasons,limited by divergent westerlies in the middle troposphere,mid-level clouds prevail over the leeside of the Tibetan Plateau.At the same time,suppressed by strong downdraft of the western Pacific subtropical high,low clouds dominate over the ocean.In warm seasons both continental and marine clouds can penetrate upward into the upper troposphere because they are subject to similar unstable stratification conditions.Based on data from satellite and surface observations, the horizontal and vertical distributions of clouds over eastern China and the East China Sea are examined. Three maximum centers of cloud cover are clearly visible in the horizontal distribution of total cloud cover. Two of these maxima occur over land. As the clouds mainly originate from the climbing airflows in the southern and eastern slopes of the Tibetan Plateau, they can be classified as dynamic clouds. The third center of cloud cover is over the sea. As the clouds mainly form from the evaporation of the warm Kuroshio Current, they can be categorized as thermodynamic clouds. Although the movement of the cloud centers reflect the seasonal variation of the Asian summer monsoon, cloud fractions of six cloud types that are distinct from the total cloud cover show individual horizontal patterns and seasonal variations. In their vertical distribution, cloud cover over the land and sea exhibits different patterns in winter but similar patterns in summer. In cold seasons, limited by divergent westerlies in the middle troposphere, mid-level clouds prevail over the leeside of the Tibetan Plateau. At the same time, suppressed by strong downdraft of the western Pacific subtropical high, low clouds dominate over the ocean. In warm seasons both continental and marine clouds can penetrate upward into the upper troposphere because they are subject to similar unstable stratification conditions.

关 键 词：CLOUDS DISTRIBUTION eastern China East China Sea 

分 类 号：P412.15[天文地球—大气科学及气象学]