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A Fourteen-Year Climatology of the Southwest Vortex in Summer |
FU Shen-Ming1,2, ZHANG Jing-Ping3, SUN Jian-Hua4,5, SHEN Xin-Yong3 |
1Chengdu Institute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, China
2International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
3Department of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
4Laboratory of Cloud-Precipitation Physics and Severe Storms, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
5Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing 210044, China |
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Abstract Statistical studies were conducted on the southwest vortex (SWV) during the summers of 2000–13 using high-resolution reanalysis data with a horizontal resolution of 0.5° × 0.5°. A total of 578 SWVs were detected, with a maximum interannual frequency of 55. The variation of the interannual frequency featured a period of around six years. The most active period of SWVs was early July and the maximum occurrence of SWVs appeared in early morning (0200–0800 Beijing Standard Time (BST)). Most of the SWVs were short-lived, with only 66 cases (11.4%) lasting for more than 24 h. In addition, the moving tracks and three-dimensional shape of long-lived (≥ 36 h) SWVs are also presented. For those SWVs that lasted for more than 12 h, four types of SWVs (Types I–IV) were identified using a new method, and the results indicated that the dynamical and thermodynamical conditions before the formation of SWVs are effective indicators of the subsequent evolution of the vortex and associated severe weathers. Moreover, a further level of classification was also constructed for Type II SWVs, which accounted for the largest proportion out of Types I–IV, and the results indicated that the lifespan, radius and maximum 6-h precipitation were all closely related to the intensity of precipitation before the formation of SWVs.
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Received: 12 May 2014
Revised: 04 June 2014
Accepted: 05 June 2014
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Corresponding Author:
FU Shen-Ming
E-mail: fusm@mail.iap.ac.cn
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