1. 广西汛期大范围持续性强降水特征与天气学分型研究.
- Author
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李华实, 王东海, 陆虹, 陈思蓉, 曾智琳, and 张春燕
- Abstract
Based on the daily precipitation data from national meteorological stations, ERA5 reanalysis data and the CMA Tropical Cyclone Best Track Dataset during 1979-2019, this paper sets out to conduct statistical analysis and synoptic classification of 51 large-scale persistent severe rainfall (LPSR) events during the rainy season in Guangxi Autonomous Region, and study the key circulation characteristics and differences in frontogenetic structure. The main conclusions are as follows: There are six synoptic types of the LPSR events, namely North China Trough (NCT), South Branch Trough (SBT), Low Vortex&Shear (LVS), Subtropical High Edge (SHE), Tropical Cyclone (TC) and Monsoon Depression (MD), all of which are characterized by a background of stable synoptic circulation. The NCT has the highest frequency, and the SBT has the longest average duration and the widest average influence range. The precipitation intensity of NCT, SBT and LVS is almost the same, and their precipitation areas overlap in northeast Guangxi. The frontogenesis is caused by the special terrain of this area and its interaction with cold and warm air. The initial height of strong frontogenesis is higher and shallow. There are some intrusions of dry and cold air in the middle and low layers, especially in the NCT, and such intrusions increase atmospheric instability and induce frontogenesis development. Moreover, SBT is accompanied by warm rain belt along the coast. The precipitation intensity of SHE, TC and MD is more intense, and their main precipitation area is in southern Guangxi. In these cases, the frontogenesis is mostly caused by the warm air lifted by the terrain, the narrow tube effect, and the friction convergence, which triggers and maintains efficient warm cloud precipitation. The initial height of strong frontogenesis of the latter two are lower and deeper, and their efficiency of warm cloud precipitation is higher, while the strong frontogenesis of the SBT's coastal frontogenesis area and SHE are relatively shallower. [ABSTRACT FROM AUTHOR]
- Published
- 2023
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