Urban Impact on Landfalling Tropical Cyclone Precipitation:A Numerical Study of Typhoon Rumbia(2018)

作     者：Xinguan DU Haishan CHEN Qingqing LI Xuyang GE Xinguan DU;Haishan CHEN;Qingqing LI;Xuyang GE

作者机构：KLME/ILCEC/CIC-FEMDNanjing University of Information Science and TechnologyNanjing 210044China School of Atmospheric SciencesNanjing University of Information Science and TechnologyNanjing 210044China 

出 版 物：《Advances in Atmospheric Sciences》 (大气科学进展（英文版）)

年 卷 期：2023年第40卷第6期

页      面：988-1004页

核心收录：

学科分类：07[理学] 0706[理学-大气科学] 

基　　金：supported by the National Science Foundation of China (Grant Nos. 42088101 and 42175005) by the Postgraduate Research and Practice Innovation Program of Jiangsu Province (KYCX22_1137)。 

主　　题：landfalling tropical cyclone urban agglomeration quantitative diagnosis rainfall physical mechanisms surface friction 

摘      要：Coastal urban areas are prone to serious disasters caused by landfalling tropical cyclones(TCs). Despite the crucial role of urban forcing in precipitation, how fine-scale urban features impact landfalling TC precipitation remains poorly understood. In this study, high-resolution ensemble simulations of Typhoon Rumbia(2018), which crossed the Yangtze River Delta urban agglomeration, were conducted to analyze the potential urban impact on TC precipitation. Results show that the inner-core rainfall of Rumbia is strengthened by approximately 10% due to the urban impact near the landfall,whereas minor differences in outer-core rainfall are found when the urban impact is excluded. Further diagnostic analyses indicate that low-level upward motion is crucial for precipitation evolution, as both co-vary during landfall. Moreover, the frictionally induced upward motion plays a decisive role in enhancing the rainfall when the urban impacts are included.Urban surface friction can decelerate the tangential wind and therefore destroy the gradient balance and strengthen the radial wind within the boundary layer and thus can enhance upward motion. This study demonstrates that urban surface friction and related physical processes make the most significant contribution to landfalling TC rainfall enhancement.