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基于海气耦合模型的渤海两种类型风暴潮数值模拟与对比分析
引用本文:李勇,陈鑫,姜兴钰,李建芬,田立柱.基于海气耦合模型的渤海两种类型风暴潮数值模拟与对比分析[J].海洋学报(英文版),2019,38(9):35-47.
作者姓名:李勇  陈鑫  姜兴钰  李建芬  田立柱
作者单位:天津地质调查中心, 中国地质调查局, 天津, 300170;泥质海岸带地质环境重点实验室, 中国地质调查局, 天津, 300170,北京安全节能技术工程研究中心, 中国农业大学, 北京, 100083,天津地质调查中心, 中国地质调查局, 天津, 300170;泥质海岸带地质环境重点实验室, 中国地质调查局, 天津, 300170,天津地质调查中心, 中国地质调查局, 天津, 300170;泥质海岸带地质环境重点实验室, 中国地质调查局, 天津, 300170,天津地质调查中心, 中国地质调查局, 天津, 300170;泥质海岸带地质环境重点实验室, 中国地质调查局, 天津, 300170
基金项目:The National Natural Science Foundation of China under contract Nos 41372173 and 51609244; the Geological Survey Projects of China Geological Survey under contract No. 121201006000182401.
摘    要:渤海一年四季都易受到由温带风暴和热带气旋所致风暴潮的影响。为了缓解风暴潮灾害对海岸地区人员生命财产的影响,十分有必要了解大型风暴潮的发生过程和机制。目前大部分研究主要局限于单一的温带风暴潮或台风风暴潮。本文利用所构建的海气耦合数值模型研究了发生于渤海的两种类型的风暴潮,对发生在渤海的2次典型强风暴潮过程进行了模拟。由WRF模型模拟得到的风场强度和最低海平面气压与实测数据吻合较好,由ROMS模型模拟得到的风暴潮期间水位变化过程与潮位站观测结果也吻合较好。对两种类型风暴潮期间的风场结钩、海面风应力、海洋表面平均流场以及水位分布进行了分析对比,并将耦合模型结果与非耦合模型结果进行了对比。研究表明,渤海两种类型风暴潮期间的风场结钩、海面风应力、海洋表面平均流场以及水位分布等均存在巨大差异。渤海风暴潮的强度主要由海洋表面的驱动力所决定,但同时也受海岸地形地貌的影响。

关 键 词:渤海  温带风暴潮  台风风暴潮  海气耦合模型  WRF  ROMS
收稿时间:2018/4/18 0:00:00

Numerical simulations and comparative analysis for two types of storm surges in the Bohai Sea using a coupled atmosphere-ocean model
LI Yong,CHEN Xin,JIANG Xingyu,LI Jianfen and TIAN Lizhu.Numerical simulations and comparative analysis for two types of storm surges in the Bohai Sea using a coupled atmosphere-ocean model[J].Acta Oceanologica Sinica,2019,38(9):35-47.
Authors:LI Yong  CHEN Xin  JIANG Xingyu  LI Jianfen and TIAN Lizhu
Institution:1.Tianjin Centre, China Geological Survey, Tianjin 300170, China;Key Laboratory of Coast Geo-environment, China Geological Survey, Tianjin 300170, China2.Beijing Engineering Research Center of Safety and Energy Saving Technology for Water Supply Network System, China Agricultural University, Beijing 100083, China
Abstract:The Bohai Sea is extremely susceptible to storm surges induced by extratropical storms and tropical cyclones in nearly every season. In order to relieve the impacts of storm surge disasters on structures and human lives in coastal regions, it is very important to understand the occurring of the severe storm surges. The previous research is mostly restricted to a single type of storm surge caused by extratropical storm or tropical cyclone. In present paper, a coupled atmosphere-ocean model is developed to study the storm surges induced by two types of extreme weather conditions. Two special cases happened in the Bohai Sea are simulated successively. The wind intensity and minimum sea-level pressure derived from the Weather Research and Forecasting(WRF) model agree well with the observed data. The computed time series of water level obtained from the Regional Ocean Modeling System(ROMS) also are in good agreement with the tide gauge observations. The structures of the wind fields and average currents for two types of storm surges are analyzed and compared. The results of coupled model are compared with those from the uncoupled model. The case studies indicate that the wind field and structure of the ocean surface current have great differences between extratropical storm surge and typhoon storm surge. The magnitude of storm surge in the Bohai Sea is shown mainly determined by the ocean surface driving force, but greatly affected by the coastal geometry and bathymetry.
Keywords:the Bohai Sea  extratropical storm surge  typhoon storm surge  coupled atmosphere-ocean model  WRF  ROMS
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