The impact of monsoon on the landfalling tropical cyclone persistent precipitation in South China

IF 5.8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Environmental Research Letters Pub Date : 2024-07-09 DOI:10.1088/1748-9326/ad5c83
Lunkai He, Qinglan Li, Liguang Wu, Xuyang Ge, Chunxia Liu, Guangxin Li, Jiali Zhang
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Abstract

Interactions between landfalling tropical cyclones (TCs) and monsoons in South China significantly influence precipitation duration, leading to severe disasters. Previous studies have primarily been individual cases, lacking systematic large-scale statistical analysis of the monsoon and landfalling tropical cyclone persistent precipitation (LTCPP) relationship. This study quantitatively investigated the relationship between monsoonal wind intensity before TCs landfall and post-landfall persistent precipitation induced by TCs in South China, employing the ERA5 reanalysis data and the best track data of 147 TCs from 1979 to 2018. The LTCPP was characterized by the frequency of persistent precipitation events during 0–72 h after TC landfall within a 500 km radius from the TC center. TCs were subdivided into weak and strong LTCPP groups based on the category-specific median of Frequency of 24 h Landfalling Tropical Cyclone Persistent Precipitation (FLTCPP24): 2705 h for TS, 6007 h for STS, and 6419 h for TY. A South China Tropical Cyclone Precipitation Monsoon Index (SCTCPM) was proposed to quantify monsoonal wind intensity derived from zonal winds at 850 hPa over two regions located in the Indian Ocean and Northwestern Pacific Ocean, within 5 d before TC landfall. The results reveal that SCTCPM < 9 m s−1 yields a 72% probability of weak LTCPP occurrence, which increases to 77% when SCTCPM < 6 m s−1. Conversely, SCTCPM > 18 m s−1 corresponds to an 80% probability of strong LTCPP. SCTCPM is an effective indicator for monsoonal wind that impacts LTCPP. Enhanced monsoonal winds, quantified by higher SCTCPM, result in post-landfall changes in horizontal wind speed, moisture transport, convective activity and upward motion, ultimately increasing LTCPP. This study deepens our understanding of the monsoon-TC relationship, emphasizing the crucial role of monsoonal wind in LTCPP in South China and offering valuable insights for disaster preparedness and risk mitigation.
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季风对华南地区登陆热带气旋持续降水的影响
华南地区登陆热带气旋(TC)与季风之间的相互作用对降水持续时间有显著影响,从而导致严重灾害。以往的研究主要是个案研究,缺乏对季风与登陆热带气旋持续降水(LTCPP)关系的系统性大规模统计分析。本研究利用ERA5再分析资料和1979-2018年147个TC的最佳路径资料,定量研究了华南地区TC登陆前季风强度与登陆后TC诱发的持续降水之间的关系。LTCPP的特征是TC登陆后0-72 h内,以TC中心为半径500 km范围内的持续降水事件频次。根据24 h登陆热带气旋持续降水频率(FLTCPP24)的具体类别中值,将TC细分为弱LTCPP组和强LTCPP组:TS为2705小时,STS为6007小时,TY为6419小时。提出了华南热带气旋降水季风指数(SCTCPM),以量化热带气旋登陆前 5 d 内印度洋和西北太平洋两个区域 850 hPa 的带风推算出的季风强度。结果表明,SCTCPM < 9 m s-1 产生弱 LTCPP 的概率为 72%,当 SCTCPM < 6 m s-1 时,这一概率增加到 77%。相反,SCTCPM > 18 m s-1 相当于 80% 的强 LTCPP 发生概率。SCTCPM 是影响 LTCPP 的季风的有效指标。以较高的 SCTCPM 为量化指标的季风增强会导致降雨后水平风速、水汽输送、对流活动和上升运动的变化,最终增加 LTCPP。这项研究加深了我们对季风与对流关系的理解,强调了季风在华南 LTCPP 中的关键作用,并为防灾减灾提供了宝贵的见解。
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来源期刊
Environmental Research Letters
Environmental Research Letters 环境科学-环境科学
CiteScore
11.90
自引率
4.50%
发文量
763
审稿时长
4.3 months
期刊介绍: Environmental Research Letters (ERL) is a high-impact, open-access journal intended to be the meeting place of the research and policy communities concerned with environmental change and management. The journal''s coverage reflects the increasingly interdisciplinary nature of environmental science, recognizing the wide-ranging contributions to the development of methods, tools and evaluation strategies relevant to the field. Submissions from across all components of the Earth system, i.e. land, atmosphere, cryosphere, biosphere and hydrosphere, and exchanges between these components are welcome.
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