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投稿时间:2024-08-19 修订日期:2025-02-26
            投稿时间:2024-08-19 修订日期:2025-02-26
             中文摘要:  含有过冷水的积状云(简称过冷积状云)是飞机结冰试飞所需的条件。基于CloudSat-CALIPSO星载雷达云产品中的云相态、云分类、液态水顶高数据和ERA5再分析资料中的气温数据,聚焦年际连续性较好的当地太阳时下午数据,构建了2006—2019年中国过冷积状云历史数据集,并对过冷积状云的时空分布特征开展了统计分析。我国过冷积状云的出现频率平均高值区位于青藏高原东部,并经云贵川地区延伸到华中地区,年均出现频率可达0.4。相比于过冷层状云,过冷积状云的出现频率高值区位置偏西且频率更高。4类过冷积状云的出现频率由高到低依次为:云南、华中和华东地区的高积云;青藏高原东部、四川、我国东部洋面和我国北方界外的层积云;青藏高原地区的积云;我国东南部、云南西南部和我国东部洋面的深对流。过冷积状云的出现频率在冬季于四川盆地到贵州、我国东部洋面和日本海存在3个高值中心,而夏季的过冷积状云高值中心从青藏高原东部向高原其他位置和周边山地延伸。此外,1月过冷积状云的年际变化在华中地区、西北西部和高原西部呈现显著增多趋势。
            
            
            中文关键词: 过冷云,积状云,时空分布
            
            
            Abstract:A cumuliform cloud with supercooled water (shortened as supercooled cumuliform cloud) is the condition required for the icing test flight. 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 and focusing on the local solar afternoon data with good interannual continuity, we construct the historical supercooled cloud sample dataset over China during 2006-2019, and analyze the spatio-temporal distribution characteristics of supercooled cumuliform clouds. The supercooled cumuliform clouds in China mostly 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 the occurrence frequency 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 Yunnan, Central China and East China; stratocumulus over eastern Qinghai-Xizang Plateau, Sichuan,  the eastern sea surface of China and outside the northern boundary of China; cumulus over the Qinghai-Xizang Plateau; and deep convection over southwestern Yunnan,  Southeast China, and the eastern sea surface of China. In winter, there are three high-value centers of the occurrence frequency of supercooled cumuliform clouds from Sichuan Basin to Guizhou, the ocean over eastern China, and the Sea of Japan, while the high-value center of the occurrence frequency of supercooled cumuliform clouds 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 shows a significantly increasing trend in January in Central China, the west of Northwest China and the west of the Qinghai-Xizang Plateau.
            
            
            
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            基金项目:民用飞机专项科研项目(MJZ5-XXXX)、中国科学院战略性先导科技专项(XDB0760400)和国家自然科学基金项目(42105127)共同资助
            
			
				引用文本:
杨涛,孙跃,闫文辉,张月晴,吴俊辉,杨慧玲,肖辉,2025.中国过冷积状云的时空分布特征[J].气象,51(10):1193-1202.
YANG Tao,SUN Yue,YAN Wenhui,ZHANG Yueqing,WU Junhui,YANG Huiling,XIAO Hui,2025.Spatio-Temporal Distribution Characteristics of Supercooled Cumuliform Clouds in China[J].Meteor Mon,51(10):1193-1202.
            
			
			
			杨涛,孙跃,闫文辉,张月晴,吴俊辉,杨慧玲,肖辉,2025.中国过冷积状云的时空分布特征[J].气象,51(10):1193-1202.
YANG Tao,SUN Yue,YAN Wenhui,ZHANG Yueqing,WU Junhui,YANG Huiling,XIAO Hui,2025.Spatio-Temporal Distribution Characteristics of Supercooled Cumuliform Clouds in China[J].Meteor Mon,51(10):1193-1202.
 
			 
	    