globalchange  > 气候变化与战略
CSCD记录号: CSCD:5383460
论文题名:
2012年7月内蒙古极端降水事件及成因
其他题名: Procession and Causes of the Extreme Rainstorm Event in Inner Mongolia in July 2012
作者: 宋桂英1; 李孝泽2; 江靖1; 荀学义1; 陈磊3; 马素艳1
刊名: 高原气象
ISSN: 1000-0534
出版年: 2015
卷: 34, 期:1, 页码:144-150
语种: 中文
中文关键词: 极端降水事件 ; 贝加尔湖低涡 ; 切变线 ; 中尺度系统
英文关键词: MCS ; Extreme rainstorm event ; Lake Baikal vortex ; Shear line ; Mesoscale system ; MCS
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 2012年7月下旬内蒙古中部出现罕见的极端降水事件(简称"7·27"暴雨)。利用NCEP再分析资料、 常规观测和精细化监测等资料分析了"7·27"暴雨成因。结果表明:(1)贝加尔湖低涡异于常年。巴尔喀什湖到鄂霍茨克海为阻塞高压, 其底部横槽加深生成贝加尔湖低涡。低涡内有冷空气活动, 在对流层低层及地面激发出低涡和气旋。(2)该过程的中尺度特征明显。地面中尺度切变线不断新生、 稳定维持, 形成多个中尺度雨带。高空beta中尺度对流云团不断新生、 合并加强, 形成对流复合体MCS。河套西北部、 河套南部、 锡林郭勒盟中西部三个暴雨区均是中尺度对流复合体MCS发展的结果。(3)垂直方向上, 暴雨发生前到暴雨期从地面至700 hPa的大气比湿达10~22 g·kg~(-1), 且850~700 hPa水汽垂直输送达到最强; 水平方向上, 南风风力辐合, 末端到达45°N以北, 河套南部地区为"水汽汇"。(4)对流层高层大气涡旋运动是该过程的直接诱因。大气涡旋运动由200 hPa向700 hPa传播, 正涡度平流在700 hPa到200 hPa随高度增加, 高层水平辐散、 低层补偿辐合, 大气强迫上升产生暴雨。(5)对流层中层持续"干侵入", 低层持续的暖湿输送, 大气不稳定能量不断重建, 这是极端暴雨过程的热力机制。(6)随着全球气候变暖, 亚洲夏季风加强, 来自孟加拉湾和南海的水汽向东亚副热带地区输送加强, 水汽输送进一步向北扩展到我国华北内陆地区, 是"7·27"暴雨过程的重要原因。
英文摘要: An extreme rainstorm named as '7·27' occurred in the middle of Inner Mongolia in China during late July 2012. Using data from NCEP reanalysis, conventional observations, and monitoring, the causes of the '7·27' extreme heavy rain were analyzed and discussed. The results showing: (1) Bell-Lake vortex happened in '7·27' rainstorm was quite different from that in perennial years. The area from Balkhash Lake to the Ochotsk Sea was controlled by blocking high, the bottom of the blocking high was occupied by Bell-Lake vortex.(2)'7·27' rainstorm has strongly the characteristics of the meso-scale. Many meso-scale rain belts were generated by surface shear lines formed constantly and swung north and south. The beta meso-scale convective clouds were produced constantly and enhanced by amalgamation and further formed the convective complexes (MCS or MCC). The rainstorms in the northwestern and southern Hetao area, and the western Xilin Gol League were all resulted from the meso-scale convective complex (MCC) or MCS and ground shear lines, (3) The distribution characteristics of the water-vapor were: the atmospheric specific humidity in vertical was up to 10~22 g·kg~(-1) from ground to 700 hPa. The water vapor transported strongest in the scope from 850 hPa to 700hPa. Horizontally, the south winds reached 45°N, which made the "moisture sink" of Southern Hetao. (4) Atmospheric vortex in Troposphere was the direct cause of the event. The atmosphere vortex spread from 200 hPa down to 700 hPa. Heavy rains were hence produced by the upper atmosphere divergence and the lower compensate convergence. (5) The thermodynamical mechanics of '7·27' rainstorm is: The instable energy of atmosphere was rebuilt constantly with the mid-level dry intrusion and the low-level humid transport. (6) With global warming, the Asian summer monsoon intensifying, from the bay of Bengal and the South China Sea to the East Asian subtropical region water vapor transport strengthening, water vapor transport further northward expansion into North China′s inland areas, is an important reason for '7·27' rainstorm process.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149403
Appears in Collections:气候变化与战略

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作者单位: 1.内蒙古气象台, 呼和浩特, 内蒙古 010051, 中国
2.中国科学院寒区旱区环境与工程研究所, 中国科学院沙漠与沙漠化重点实验室, 兰州, 甘肃 730000, 中国
3.民航温州空管站气象台, 温州, 浙江 325000, 中国

Recommended Citation:
宋桂英,李孝泽,江靖,等. 2012年7月内蒙古极端降水事件及成因[J]. 高原气象,2015-01-01,34(1):144-150
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