中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Modeling vertical heat transport in the wave affected surface layer of the ocean

文献类型:CNKI期刊论文

作者Wang JL(王金良); Song JB(宋金宝)
发表日期2009-05-15
出处Chinese Journal of Oceanology and Limnology
关键词wave effect heat diffusion air-sea flux sea surface temperature
英文摘要In considering the vertical heat transport problems in the upper ocean, the flat upper boundary approximation for the free surface and the horizontal homogenous hypothesis are usually applied. However, due to the existence of the wave motion, the application of this approximation may result in some errors to the solar irradiation since it decays quickly in respect to the actual thickness of the water layer below the surface; on the other hand, due to the fluctuation of the water layer depth, it is improper to neglect the effects of the horizontal advection and turbulent diffusion since they also contribute to the vertical heat transport. A new model is constructed in this study to reflect these effects. The corresponding numerical simulations show that the wave motion may remarkably accelerate the vertical heat transferring process and the variation of the temperature in the wave affected layer appears in an oscillating manner.
文献子类CNKI期刊论文
资助机构Supported by the National High Technology Research and Development Program of China (863 Program, No. 2006AA09A309) ; China Postdoctoral Science Foundation (No. 20070411111) ; the Fund of Shandong Province for the Excellent Post-Doctors (No. 200603056)
v.27期:02页:20-25
语种英文;
分类号P731.2
ISSN号0254-4059
源URL[http://ir.qdio.ac.cn/handle/337002/192586]  
专题中国科学院海洋研究所
作者单位1.InstituteofOceanology,ChineseAcademyofSciences
2.InstituteofAppliedMathematics,CollegeofScience,QingdaoTechnologicalUniversity
3.KeyLaboratoryofOceanCirculationandWaves(KLOCAW),ChineseAcademyofSciences
推荐引用方式
GB/T 7714
Wang JL,Song JB. Modeling vertical heat transport in the wave affected surface layer of the ocean. 2009.

入库方式: OAI收割

来源:海洋研究所

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