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海平面上升背景下北部湾台风风暴潮的数值研究OA

Numerical study of typhoon-induced storm surges in the Beibu Gulf under sea-level rise

中文摘要英文摘要

全球气候变暖导致海平面加速上升,进而加剧北部湾沿岸风暴潮灾害.本文基于 ADCIRC 模型对北部湾台风风暴潮进行数值模拟,以占比 60.1%的雷州半岛进入北部湾和占比 29.2%的海南岛进入北部湾两类路径的台风分析了北部湾的增水情况,并进一步探究未来海平面上升0.77 m和1.02 m情景下北部湾风暴潮的变化.结果表明:当前情景下,第一类台风最大增减水在广西沿海的高值分别达到 1~2.5 m 和0.8~4 m,第二类台风最大增减水在广西沿海的高值分别达到 1~1.7 m 和 0.7~1.8 m.未来海平面上升情景下,北部湾大部分区域的最大增减水呈现减小趋势,广西沿海的减小量分别达到 0~18 cm和 0~45 cm,广西沿海典型站位的极值水位在大多数台风的作用下呈现增加趋势,增加量 0~6 cm 不等.研究结果可以为未来广西沿海风暴潮的防灾减灾提供理论依据.

Global warming has led to accelerated sea-level rise,thereby exacerbating storm surge disasters along the coast of the Beibu Gulf.Based on the ADCIRC model,this study conducts numerical simulations of ty-phoon-induced storm surges in the Beibu Gulf.It analyzes the storm surge elevations under two typhoon tracks:entry via the Leizhou Peninsula(60.1%)and via Hainan(29.2%).Furthermore,it examines changes in storm surges under future sea-level rise scenarios of 0.77 and 1.02 m.The results show that,under the current scenario,the maximum storm surge elevations(rise and fall)caused by Type-1 typhoons along the Guangxi coast reach 1-2.5 and 0.8-4 m,respectively,whereas those caused by Type-2 typhoons reach 1-1.7 and 0.7-1.8 m,respectively.Under future sea-level rise scenarios,the maximum storm surge increments and decrements in most areas of the Beibu Gulf show a decreasing trend,with reductions ranging from 0 to 18 cm and 0 to 45 cm,respectively,along the Guangxi coast.Under the influence of most typhoons,the extreme water level at representative stations along the Guangxi coast increases by up to 6 cm.The research results provide a theoretical basis for future storm surge dis-aster prevention and mitigation along the Guangxi coast.

谭富元;杨波;孙建

中国海洋大学海洋与大气学院,山东 青岛 266100中国海洋大学海洋与大气学院,山东 青岛 266100中国海洋大学海洋与大气学院,山东 青岛 266100||中国海洋大学物理海洋教育部重点实验室,山东 青岛 266100

海洋科学

海平面上升北部湾ADCIRC风暴潮数值模拟

sea-level riseBeibu GulfADCIRCstorm surgenumerical simulation

《海洋科学》 2026 (3)

27-42,16

国家自然科学基金联合基金重点支持项目(U20A2099)Key Supported Project of the Joint Funds of the National Natural Science Foundation of China,No.U20A2099

10.11759/hykx20250402001

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