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2013, 08, v.43;No.220 8-14
内波混合方法与Mellor-Yamada混合方案在黄海和东海夏季温跃层模拟中的比较研究
基金项目(Foundation): 国家自然科学重点基金项目(41030855)资助
邮箱(Email):
DOI: 10.16441/j.cnki.hdxb.2013.08.002
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摘要:

观测显示夏季黄海和东海存在强温跃层,同时存在强内潮和内孤立波。考虑内潮和内孤立波的混合作用对于黄海和东海夏季温跃层以及环流的模拟工作是重要的,本文使用POM数值模式,设计了一组对照实验,在考虑风场和不考虑风场的强迫作用下,分别使用Mellor-Yamada混合方案和本文提出的内波混合参数化方法,对8月份的黄海和东海温度的垂直结构进行模拟。数值模拟结果表明,Mellor-Yamada二阶湍流混合方案主要反映风场对上层海洋的混合作用,对于内波引起的混合作用反映较差;内波混合参数化方法主要考虑内潮和内孤立波的混合作用,兼顾风场和底摩擦的混合作用,模拟结果较为理想。

Abstract:

Observations show that there exist strong thermocline,as well as internal tidal waves and internal solitary waves in the Yellow Sea and East China Sea in summer.It is important to consider the mixing effect of internal tidal wave and internal solitary wave when the thermocline and circulation in the East China Sea are studied.Based on the POM mode,two numerical experiments with wind forcing and without wind forcing are designed respectively.In both cases,Mellor-Yamada's second moment turbulence closure mixing scheme and internal wave mixing scheme are applied to simulate the thermocline in the Yellow Sea and East China Sea in august respectively,and the results of two mixing scheme are compared.The simulation results indicate that Mellor-Yamada second moment turbulence closure mixing scheme mainly reflects the influence of wind mixing in the upper ocean of continental shelf,but lacks in the reflection of internal wave mixing.Internal wave mixing scheme mainly considers internal tides and internal solitary waves,and partly considers wind and bottom friction mixing.The simulation result is in good agreement with the observation by using the internal wave mixing scheme.

参考文献

[1]范植松.海洋内部混合研究基础[M].北京:海洋出版社,2002:130.

[2]侍茂崇,鲍献文,高郭平.海洋调查方法导论[M].青岛:青岛海洋大学出版社,2000:343.

[3]海洋图集编委会.渤海、黄海、东海海洋图集,水文[M].北京:海洋出版社,1992:524.

[4]赵俊生.浅海内波研究[M].北京:海洋出版社,1992:102.

[5]Hsu M K,Liu A K,Liu C.A study of internal waves in the ChinaSeas and Yellow Sea using SAR[J].Continental Shelf Research,2000,20(4-5):389-410.

[6]Lee J H,Lozovatsky I,Jang S T,et al.Episodes of nonlinear in-ternal waves in the northern East China Sea[J].Geophysical Re-search Letters.2006,33(18):L18601.

[7]胡好国,袁业立,万振文.海浪混合参数化的渤海,黄海,东海水动力环境数值模拟[J].海洋学报.2004,26(4):19-32.

[8]乔方利,马建,夏长水,等.波浪和潮流混合对黄海,东海夏季温度垂直结构的影响研究[J].自然科学进展.2004,14(12):1434-1441.

[9]李明悝,侯一筠,乔方利.潮致垂直涡动粘性系数的参数化[J].自然科学进展.2006,16(001):55-60.

[10]SI Z S H,FAN Z S,DU L.Distribution of Vertical TurbulentMixing Parameter Caused by Internal Tidal Waves and SolitaryWaves in the South Yellow Sea[J].Journal of Ocean Universityof China,2012,11(3):279-289.

[11]于万春,范植松,司宗尚.南黄海非线性内波的数值模拟研究(1)——内潮的内Kelvin波模型[J].中国海洋大学学报:自然科学版,2011,41(4):28-32.

[12]司宗尚,范植松,于万春,等.南黄海非线性内波的数值模拟研究(2)——内潮的非线性演变[J].中国海洋大学学报:自然科学版,2011,41(5):15-22.

[13]Vlasenko V,Hutter K.Numerical experiments on the breakingof solitary internal wavesover a slope-shelf topography[J].Jour-nal of Physical Oceanography,2002,32(6):1779-1793.

[14]Pacanowski R C,Philander S.Parameterization of vertical mixingin numerical models of tropical oceans[J].Journal of Physical O-ceanography,1981,11(11):1443-1451.

[15]Shi X,Fan Z,Liu H.A numerical calculation method for eigen-value problems of nonlinear internal waves[J].Journal of Hydro-dynamics Ser B,2009,21(3):373-378.

[16]Mellor G L.Users guide for a three-dimensional,primitive equa-tion,numerical ocean model.[M].Princeton:Princeton Univer-sity,2004.

[17]Mellor G L,Yamada T.Development of a turbulence closuremodel for geophysical fluid problems[J].Reviews of Geophysicsand Space Physics,1982,20(4):851-875.

[18]刘海龙.LASG/IAP气候系统海洋模式(LICOM1.0)参考手册[M].北京:科学出版社,2004.

基本信息:

DOI:10.16441/j.cnki.hdxb.2013.08.002

中图分类号:P731.2

引用信息:

[1]王真,范植松,司宗尚,等.内波混合方法与Mellor-Yamada混合方案在黄海和东海夏季温跃层模拟中的比较研究[J],2013,43(08):8-14.DOI:10.16441/j.cnki.hdxb.2013.08.002.

基金信息:

国家自然科学重点基金项目(41030855)资助

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