{"title":"Radial Rainfall Pattern Changes of Intense Over-Ocean Tropical Cyclones Under Global Warming: Insights From an MRI HighRes CMIP6 Simulation","authors":"Jianan Chen, Ralf Toumi, Lujia Zhang, Mengqian Lu, Dazhi Xi, Xiaoming Shi","doi":"10.1029/2025GL116146","DOIUrl":null,"url":null,"abstract":"<p>Tropical cyclone (TC) rainfall is an important hazard. Radial rainfall patterns of intense over-ocean TCs under global warming are investigated using the MRI HighRes Coupled Model Intercomparison Project Phase 6 simulation with the SSP5-8.5 high-emission scenario. These patterns are characterized by four parameters: rainfall at the cyclone center <span></span><math>\n <semantics>\n <mrow>\n <mfenced>\n <msub>\n <mi>T</mi>\n <mi>o</mi>\n </msub>\n </mfenced>\n </mrow>\n <annotation> $\\left({T}_{o}\\right)$</annotation>\n </semantics></math>, maximum rainfall <span></span><math>\n <semantics>\n <mrow>\n <mfenced>\n <msub>\n <mi>T</mi>\n <mi>m</mi>\n </msub>\n </mfenced>\n </mrow>\n <annotation> $\\left({T}_{m}\\right)$</annotation>\n </semantics></math>, radius of maximum rainfall <span></span><math>\n <semantics>\n <mrow>\n <mfenced>\n <msub>\n <mi>R</mi>\n <mi>m</mi>\n </msub>\n </mfenced>\n </mrow>\n <annotation> $\\left({R}_{m}\\right)$</annotation>\n </semantics></math>, and e-folding radius <span></span><math>\n <semantics>\n <mrow>\n <mfenced>\n <msub>\n <mi>R</mi>\n <mi>e</mi>\n </msub>\n </mfenced>\n </mrow>\n <annotation> $\\left({R}_{e}\\right)$</annotation>\n </semantics></math>. We find <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>T</mi>\n <mi>m</mi>\n </msub>\n </mrow>\n <annotation> ${T}_{m}$</annotation>\n </semantics></math> strongly correlates <span></span><math>\n <semantics>\n <mrow>\n <mo>(</mo>\n <mrow>\n <mi>r</mi>\n <mo>=</mo>\n <mn>0.8</mn>\n </mrow>\n <mo>)</mo>\n </mrow>\n <annotation> $(r=0.8)$</annotation>\n </semantics></math> with a moisture convergence proxy—boundary-layer maximum wind times column moisture divided by the radius of maximum wind—across different intensities and under climate change. Under warming, mean <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>T</mi>\n <mi>m</mi>\n </msub>\n </mrow>\n <annotation> ${T}_{m}$</annotation>\n </semantics></math> and <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>T</mi>\n <mi>o</mi>\n </msub>\n </mrow>\n <annotation> ${T}_{o}$</annotation>\n </semantics></math> increase by 8.65%/K and 8.86%/K, while <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>R</mi>\n <mi>m</mi>\n </msub>\n </mrow>\n <annotation> ${R}_{m}$</annotation>\n </semantics></math> and <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>R</mi>\n <mi>e</mi>\n </msub>\n </mrow>\n <annotation> ${R}_{e}$</annotation>\n </semantics></math> shrink by 1.03%/K and 1.79%/K, respectively. Notably, under warming, <span></span><math>\n <semantics>\n <mrow>\n <msub>\n <mi>T</mi>\n <mi>m</mi>\n </msub>\n </mrow>\n <annotation> ${T}_{m}$</annotation>\n </semantics></math> exhibits greater sensitivity to TC intensity, and its increases are mainly attributed to column moisture increase.</p>","PeriodicalId":12523,"journal":{"name":"Geophysical Research Letters","volume":"52 9","pages":""},"PeriodicalIF":4.6000,"publicationDate":"2025-05-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2025GL116146","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geophysical Research Letters","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2025GL116146","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Tropical cyclone (TC) rainfall is an important hazard. Radial rainfall patterns of intense over-ocean TCs under global warming are investigated using the MRI HighRes Coupled Model Intercomparison Project Phase 6 simulation with the SSP5-8.5 high-emission scenario. These patterns are characterized by four parameters: rainfall at the cyclone center , maximum rainfall , radius of maximum rainfall , and e-folding radius . We find strongly correlates with a moisture convergence proxy—boundary-layer maximum wind times column moisture divided by the radius of maximum wind—across different intensities and under climate change. Under warming, mean and increase by 8.65%/K and 8.86%/K, while and shrink by 1.03%/K and 1.79%/K, respectively. Notably, under warming, exhibits greater sensitivity to TC intensity, and its increases are mainly attributed to column moisture increase.
热带气旋(TC)降雨是一种重要的灾害。利用MRI高分辨率耦合模式比对项目第6阶段与SSP5-8.5高排放情景的模拟,研究了全球变暖背景下强烈海洋上空tc的径向降雨模式。这些模式的特征有四个参数:气旋中心雨量T $\左({T}_{o}\右)$,最大雨量T m $\左({T}_{m}\右)$,最大降雨量半径R m $\left({R}_{m}\right)$,和e折叠半径R e $\left({R}_{e}\right)$。我们发现T m ${T}_{m}$与水汽辐合强相关(r=0.8)$ (r=0.8)$在不同强度和气候变化条件下,代理边界层最大风次柱湿度除以最大风半径。变暖条件下,平均T m ${T}_{m}$和T o ${T}_{o}$分别增加8.65%/K和8.86%/K;R m ${R}_{m}$和R e ${R}_{e}$分别下降了1.03%/K和1.79%/K。值得注意的是,在增温条件下,T m ${T}_{m}$对TC强度表现出更大的敏感性,其增加主要归因于塔柱湿度的增加。
期刊介绍:
Geophysical Research Letters (GRL) publishes high-impact, innovative, and timely research on major scientific advances in all the major geoscience disciplines. Papers are communications-length articles and should have broad and immediate implications in their discipline or across the geosciences. GRLmaintains the fastest turn-around of all high-impact publications in the geosciences and works closely with authors to ensure broad visibility of top papers.