Effect of Stokes drift on upper ocean mixing | |
Li Shuang1,2; Song Jinbao1; Sun Qun1 | |
刊名 | ACTA OCEANOLOGICA SINICA |
2008 | |
卷号 | 27期号:2页码:11-20 |
关键词 | Stokes Drift Langmuir Circulations Coriolis-stokes Forcing Upper Ocean Mixing Mellor-yamada 2.5 Turbulence Model Wave Breaking Surface Heating |
ISSN号 | 0253-505X |
文献子类 | Article |
英文摘要 | Stokes drift is the main source of vertical vorticity in the ocean mixed layer. In the ways of Coriolis - Stokes forcing and Langmuir circulations, Stokes drift can substantially affect the whole mixed layer. A modified Mellor-Yamada 2.5 level turbulence closure model is used to parameterize its effect on upper ocean mixing conventionally. Results show that comparing surface heating with wave breaking, Stokes drift plays the most important role in the entire ocean mixed layer, especially in the subsurface layer. As expected, Stokes drift elevates both the dissipation rate and the turbulence energy in the upper ocean mixing. Also, influence of the surface heating, wave breaking and wind speed on Stokes drift is investigated respectively. Research shows that it is significant and important to assessing the Stokes drift into ocean mixed layer studying. The laboratory observations are supporting numerical experiments quantitatively.; Stokes drift is the main source of vertical vorticity in the ocean mixed layer. In the ways of Coriolis - Stokes forcing and Langmuir circulations, Stokes drift can substantially affect the whole mixed layer. A modified Mellor-Yamada 2.5 level turbulence closure model is used to parameterize its effect on upper ocean mixing conventionally. Results show that comparing surface heating with wave breaking, Stokes drift plays the most important role in the entire ocean mixed layer, especially in the subsurface layer. As expected, Stokes drift elevates both the dissipation rate and the turbulence energy in the upper ocean mixing. Also, influence of the surface heating, wave breaking and wind speed on Stokes drift is investigated respectively. Research shows that it is significant and important to assessing the Stokes drift into ocean mixed layer studying. The laboratory observations are supporting numerical experiments quantitatively. |
学科主题 | Oceanography |
语种 | 英语 |
WOS记录号 | WOS:000256131900002 |
公开日期 | 2010-12-24 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/5219] |
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.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Li Shuang,Song Jinbao,Sun Qun. Effect of Stokes drift on upper ocean mixing[J]. ACTA OCEANOLOGICA SINICA,2008,27(2):11-20. |
APA | Li Shuang,Song Jinbao,&Sun Qun.(2008).Effect of Stokes drift on upper ocean mixing.ACTA OCEANOLOGICA SINICA,27(2),11-20. |
MLA | Li Shuang,et al."Effect of Stokes drift on upper ocean mixing".ACTA OCEANOLOGICA SINICA 27.2(2008):11-20. |
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