THE FORMATION AND DIURNAL CHANGES OF STRATIFORM CLOUDS IN SOUTHERN CHINA
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Abstract
Strati form clouds have thicker optical depths,which affect the local climate seriously.Southern China(20-35°N,103-120°E) is the unique region where stratif ormcloud amount is veryhigh in the mid and low latitude,but little attention has been focused on stratif ormclouds in this region.Based on the monthly and hourly data from surface observations and radiosonde,the circulation condition and diurnal changes of stratiform clouds in southern China are illust rated and interpreted.The main conclusions are as follows:
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