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ZHAO Qian, TIAN Ji-wei, CAO Cong-hua, WANG Qiang. The numerical simulation and the assimilation technique of the current and the temperature field in the Bohai Sea, the Huanghai Sea and the East China Sea[J]. Haiyang Xuebao, 2005, 27(1): 1-6.
Citation: ZHAO Qian, TIAN Ji-wei, CAO Cong-hua, WANG Qiang. The numerical simulation and the assimilation technique of the current and the temperature field in the Bohai Sea, the Huanghai Sea and the East China Sea[J]. Haiyang Xuebao, 2005, 27(1): 1-6.

The numerical simulation and the assimilation technique of the current and the temperature field in the Bohai Sea, the Huanghai Sea and the East China Sea

  • Received Date: 2003-11-20
  • Rev Recd Date: 2004-07-20
  • The nudging assmiilation is used to smiulate the three dmiension temperature field of the Bohai Sea,the Huanghai Sea and the East China Sea to reduce the error of using heat flux as the upper boundary condition with the use of the high resolution satellite remote sensing data SST.The result shows that the smiulated current field can reflect the circulation characteristics of the Bohai Sea,the Huanghai Sea and the East China Sea satisfactorily.The temperature field after data assmi ilation is better than that without data assmi ilation.The RMS bewteen the assmi ilation data and the observed data of the three stations selected are 1.307,0.526,0.744 respectively,while the RMS between the temperature smiulated by heat flux and the observed data are 2.160,0.979,1.330 respectively.Data assmi ilation effects the three dmiensional temperature field a lthough we only assmiilate the sea surface temperature.
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  • WILLIAM R H,MALANOTTE-RIZZOLI Paola.Assimilation of altimeter data into an ocean circulation model:space versus time resolution studies[J].Journal of Physical Oceanography,1989,19(10):1 507-1 534.
    ROSATI A,GUDGEL R,MIYAKODA K.Decadal analysis produced from an ocean data assimilation system[J].Monthly Weather Review,1995,123(6):2 206-2 228.
    詹杰民,严晓海.基于大涡模拟和局部滤波同化方法的海洋环流模式[J].海洋学报,2004,26(3):8-15.
    海洋图集编委会.渤海、黄海、东海海洋图集(水文)[Z].北京:海洋出版社,1991.13-168.
    方国洪,魏泽勋,崔秉昊,等.中国近海域际水、热、盐输运:全球变网格模式结果[J].中国科学(D),2002,32(12):969-977.
    赵保仁,方国洪.东海主要水道的流量估算[J].海洋学报,1991,13(2):169-178.
    沈焕庭.长江河口物质通量[M].北京:海洋出版社,2001.32.
    管秉贤.黄、东海浅海水文学的主要特征[J].黄渤海海洋,1985,3(4):1-9.
    苏纪兰.中国近海的环流动力机制研究[J].海洋学报,2001,23(3):1-16.
    李徽翡,赵保仁.渤、黄、东海夏季环流的数值模拟[J].海洋科学,2001,25(1):28-32.
    方国洪.关于台湾-对马-津轻流系的结构及其与黑潮的关系[J].海洋科学,1995,19(4):43-48.
    汤明义,刘宇中,李洪海,等.渤、黄海及东海北部平均表面水温场季节变化特征及其成因的初步分析[J].海洋学报,1989,11(5):544-553.
    鲍献文,万修全,高郭平,等.渤黄东海AVHRR海表温度场的季节变化特征[J].海洋学报,2002,24(5):125-133.
    乐肯堂,毛汉礼.南黄海冬季温盐结构及其流系[J].海洋与湖沼,1990,21(6):505-515.
    鲍献文,万修全,吴德星,等.2000年夏末和翌年初冬渤海水文特征[J].海洋学报,2004,26(1):14-24.
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