| 华维,邓浩,夏昌基,张永莉,朱丽华,赖欣,范广洲.青藏高原水循环中高原低涡及多季风交汇的研究进展[J].沙漠与绿洲气象,2024,18(2):1~11 |
| 青藏高原水循环中高原低涡及多季风交汇的研究进展 |
| Advance of Research on Plateau Vortex and Multi-monsoon Interaction in Water Cycle of Tibetan Plateau |
| 投稿时间：2022-11-07 修订日期：2023-08-04 |
| DOI： |
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| 英文关键词: |
| 基金项目:国家自然科学(42075019,42275022)；第二次青藏高原综合科学考察研究项目(2019QZKK010203)；国家重点研发计划项目(2018YFC1505702)。 |
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| 中文摘要: |
| 由于青藏高原特殊而强大的动力和热力效应，东亚季风、印度季风和高原季风多季风交汇于此。受多季风交汇影响，青藏高原低涡影响水循环的过程极为复杂，而高原水循环的异常往往造成高原及周边乃至我国中东部地区频发灾害性天气过程，因此一直是国内外学者关注的热点和难点问题。本文系统回顾了国内外关于高原低涡活动特征、结构特征、生成发展机制等方面研究进展，并从低涡的水汽输送、降水和云-降水物理等角度概括了高原低涡参与水循环过程研究成果，特别在总结东亚季风、印度季风和高原季风相互作用研究的基础上分析了多季风交汇对高原水循环的影响。最后对当前高原低涡在多季风作用下影响水循环过程方面存在的问题进行了讨论，并展望了未来研究方向。 |
| 英文摘要: |
| Due to the special and powerful dynamic and thermal effects of Tibetan Plateau, the East Asian monsoon, Indian monsoon and Tibetan Plateau monsoon interact with each other over Tibetan Plateau. Under the influence of multi-monsoon interactions, the water cycle of Tibetan Plateau influenced by the Tibetan Plateau vortex is extremely complex. The abnormal water cycle of Tibetan Plateau will cause frequent occurrence of catastrophic weather processes over Tibetan Plateau and surrounding areas and even in the middle and lower reaches of the Yangtze River, so it has been a hot issue of concern for atmospheric science at home and abroad. We systematically review the research progress on the activity characteristics, structural characteristics, generation and development mechanisms of Tibetan Plateau vortex. And the research results on how the Tibetan Plateau vortex affects the water cycle are outlined from the perspectives of water vapor transport, precipitation and cloud-precipitation physics. In particular, the impact of the multi-monsoon interaction on the water cycle of Tibetan Plateau is analyzed based on the summary of interaction between East Asian monsoon, Indian monsoon and Tibetan Plateau monsoon. Finally, the shortcomings of the current study were pointed out, and the future research directions were prospected. |
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