Modeling vertical heat transport in the wave affected surface layer of the ocean

doi:10.1007/s00343-009-9133-z

IOCAS-IR > 海洋环流与波动重点实验室

	Modeling vertical heat transport in the wave affected surface layer of the ocean
	Wang Jinliang 1,2; Song Jinbao 1,3
	2009-06-01
发表期刊	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN	0254-4059
卷号	27 期号:2 页码:202-207
文章类型	Article
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.; 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.
关键词	Wave Effect Heat Diffusion Air-sea Flux Sea Surface Temperature
学科领域	Limnology ; Oceanography
DOI	10.1007/s00343-009-9133-z
URL	查看原文
收录类别	SCI
语种	英语
WOS记录号	WOS:000267970300003
引用统计
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/2400
专题	海洋环流与波动重点实验室
作者单位	1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Qingdao Technol Univ, Coll Sci, Inst Appl Math, Qingdao 266033, Peoples R China 3.Chinese Acad Sci, Key Lab Ocean Circulat & Waves KLOCAW, Qingdao 266071, Peoples R China
第一作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Wang Jinliang,Song Jinbao. Modeling vertical heat transport in the wave affected surface layer of the ocean[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2009,27(2):202-207.
APA	Wang Jinliang,&Song Jinbao.(2009).Modeling vertical heat transport in the wave affected surface layer of the ocean.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,27(2),202-207.
MLA	Wang Jinliang,et al."Modeling vertical heat transport in the wave affected surface layer of the ocean".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 27.2(2009):202-207.

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