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渤黄东海40年温盐流模拟与初步分析
引用本文:黄必桂,谢波涛,程高磊,彭世球,李毅能,朱宇航.渤黄东海40年温盐流模拟与初步分析[J].应用海洋学学报,2023,42(1):110-117.
作者姓名:黄必桂  谢波涛  程高磊  彭世球  李毅能  朱宇航
作者单位:中海油研究总院有限责任公司,北京 100027;热带海洋环境国家重点实验室(中国科学院南海海洋研究所),广东 广州510301;南方海洋科学与工程广东省实验室(广州), 广东 广州 511458;北部湾大学,广西北部湾海洋灾害研究重点实验室,广西 钦州 535011
基金项目:南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项资助项目(GML2019ZD0303);广东省重点工程资助项目(2019BT2H594);深水浮式平台一体化在线监测与分析软件集成系统研制资助项目(LSZX 2020 HN 05 04);海上油气田精细化环境预报与参数区划关键技术资助项目(YXKY ZX 07 2020);南海北部内波区划及工程参数研究资助项目(YXKY ZX 10 2021);中国科学院空间科学战略性先导科技专项资助项目(XDA15020901);广西重点研发计划资助项目(桂科AB18294047)
摘    要:使用ROMS(regional oceanic modeling system)模式模拟了40年的渤黄东海温盐流,数据包括三维的温度、盐度、流速、流向和海表高度,同时包含了逐小时的潮汐信息。将模拟结果与观测资料和卫星反演数据进行对比,检验了模式准确性。整体上,模式模拟的水位与近岸观测值基本一致,能够准确再现风产生的增水;模式较为准确的再现了渤黄东海的温度分布,在深水区模拟的温盐剖面与观测值基本一致;模式模拟渤黄东海区域的海表高度和海表流与卫星反演结果相比偏小,但分布趋势相近。模式结果可以为研究气候变化对水位的影响和黄海暖舌的扩散过程等现象提供数据支持。

关 键 词:海洋水文学  温度  盐度  表层流  ROMS模式  渤黄东海

Modeling of temperature, salinity and current in Bohai Sea, the Yellow Sea and the East China Sea based on 40 year data
HUANG Bigui,XIE Botao,CHENG Gaolei,PENG Shiqiu,LI Yineng,ZHU Yuhang.Modeling of temperature, salinity and current in Bohai Sea, the Yellow Sea and the East China Sea based on 40 year data[J].Journal of Applied of Oceanography,2023,42(1):110-117.
Authors:HUANG Bigui  XIE Botao  CHENG Gaolei  PENG Shiqiu  LI Yineng  ZHU Yuhang
Institution:China National Offshore Oil Corporation General Research Institute, Beijing 100027, China;State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China;Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou 511458, China;Guangxi Key Laboratory of Marine Disaster in Beibu Gulf, Beibu Gulf University, Qinzhou 535011, China
Abstract:In this paper, ROMS(regional oceanic modeling system) is used to simulate the temperature, salinity and current variations in Bohai sea, the Yellow Sea and the East China Sea using 40 year data with hourly tidal information. The output includes three-dimensional temperatures, salinities, velocities and sea level heights as well. These results were verified by comparing the simulated results with the observation and remote sensing data. It shows that the simulated water level is in good agreement with the observatories, including an accurate reproducing of the water level variations influenced by winds. The model accurately reproduces the temperature distribution in Bohai Sea, the Yellow Sea and the East China Sea. Also, the simulated thermohaline profiles in the deepwater area are consistent with the observed values. Compared with remote sensing data, the sea surface heights and sea surface currents simulated by the model are smaller, but the distribution patterns are similar. These model results can provide data support for studying the influence of climate change on water level and the diffusion process of warm tongue in the Yellow Sea.
Keywords:marine hydrography  temperature  salinity  surface current  ROMS  Bohai Sea  Yellow Sea and East China Sea
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