The Spatiotemporal Distribution Characteristics of Supercooled Cumuliform Clouds in China
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Abstract:
A cumuliform cloud with supercooled water is the condition required for the icing test flight, which is referred to as supercooled cumuliform cloud in this paper. On the basis of the cloud phase state, cloud classification and liquid water top height data from CloudSat-CALIPSO cloud products and the air temperature from ERA5 reanalysis data, focusing on the local solar afternoon data with good interannual continuity, the historical supercooled cloud sample data over China from 2006-2019 were derived, and the spatiotemporal distribution characteristics of supercooled cumuliform clouds were analyzed. The supercooled cumuliform clouds in China most occur in the eastern part of the Qinghai?Xizang Plateau and extend to central China via the Yunnan–Guizhou–Sichuan region, with an annual average occurrence frequency of 0.4. The high value areas of supercooled cumuliform clouds are more westward than that of supercooled stratiform cloud and the occurrence frequency is higher. The occurrence frequencies of the four types of supercooled cumuliform clouds in descending order were as follows: altocumulus over Southwest China, Central China, and East China; stratocumulus over the plateau and the eastern sea surface; cumulus over the southern side of the plateau; and deep convection over Yunnan, Central China, and the southeast land and sea. In winter, there are three high-value centers over Sichuan, Guizhou, the ocean over eastern China, and the Sea of Japan, while the high-value center in summer extends from the eastern part of the Qinghai–Xizang Plateau to other locations on the plateau and the surrounding mountainous areas. In addition, the interannual variation of supercooled cumuliform clouds showed significant increasing trends in January in central China, the west of Northwest China and the west of the Qinghai-Xizang Plateau.
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Project Supported:
Civil Aircraft Special Scientific Research Project (MJZ5-XXXX), Strategic Priority Research Program of the Chinese Academy of Sciences (XDB0760400), Natural Science Foundation of China (42105127)