Modeling vertical heat transport in the wave affected surface layer of the ocean
文献类型：期刊论文
| 作者 | Wang Jinliang1,2; Song Jinbao1,3 |
| 刊名 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
 |
| 出版日期 | 2009-06-01 |
| 卷号 | 27期号:2页码:202-207 |
| 关键词 | Wave Effect Heat Diffusion Air-sea Flux Sea Surface Temperature |
| ISSN号 | 0254-4059 |
| DOI | 10.1007/s00343-009-9133-z |
| 文献子类 | Article |
| 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.; 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. |
| 学科主题 | Limnology ; Oceanography |
| URL标识 | 查看原文 |
| 语种 | 英语 |
| WOS记录号 | WOS:000267970300003 |
| 公开日期 | 2010-12-22 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/2401]  |
| 专题 | 海洋研究所_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 |
| 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. |
入库方式： OAI收割
来源：海洋研究所
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