| HUANG Chuanjiang,QIAO Fangli,WEI Zexun.Effects of the surface wave-induced mixing on circulation in an isopycnal-coordinate oceanic circulation model[J].Acta Oceanologica Sinica,2013,32(5):7-14 |
| Effects of the surface wave-induced mixing on circulation in an isopycnal-coordinate oceanic circulation model |
| Effects of the surface wave-induced mixing on circulation in an isopycnal-coordinate oceanic circulation model |
| 投稿时间：2011-05-19 修订日期：2012-09-07 |
| DOI：10.1007/s13131-013-0308-2 |
| 中文关键词: wave-induced mixing oceanic interior seasonal thermocline oceanic circulation geostrophic adjustment |
| 英文关键词:wave-induced mixing oceanic interior seasonal thermocline oceanic circulation geostrophic adjustment |
| 基金项目:Basic Scientific Funds for National Public Research Institues of China under contract No. GY02-2009G24; Public Science and Technology Research Funds Projects of Ocean under contract No. 201105019; the Sino-US International Cooperation Project under contract No. S2011GR0348. |
| 作者 | 单位 | E-mail | | HUANG Chuanjiang | Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China | | | QIAO Fangli | Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China | qiaofl@fio.org.cn | | WEI Zexun | Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China | |
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| 中文摘要: |
| The influence of the nonbreaking surface wave-induced mixing under the mixed layer on the oceanic circulation was investigated using an isopycnal-coordinate oceanic circulation model. The effect of the waveinduced mixing within the mixed layer was eliminated via a bulk mixed layer model. The results show that the wave-induced mixing can penetrate through the mixed layer and into the oceanic interior. The waveinduced mixing under the mixed layer has an important effect on the distribution of temperature of the upper ocean at middle and high latitudes in summer, especially the structure of the seasonal thermocline. Moreover, the wave-induced mixing can affect the oceanic circulation, such as western boundary currents and the North Equatorial Currents through changes of sea surface height associated with the variation of the thermal structure of the upper ocean. |
| 英文摘要: |
| The influence of the nonbreaking surface wave-induced mixing under the mixed layer on the oceanic circulation was investigated using an isopycnal-coordinate oceanic circulation model. The effect of the waveinduced mixing within the mixed layer was eliminated via a bulk mixed layer model. The results show that the wave-induced mixing can penetrate through the mixed layer and into the oceanic interior. The waveinduced mixing under the mixed layer has an important effect on the distribution of temperature of the upper ocean at middle and high latitudes in summer, especially the structure of the seasonal thermocline. Moreover, the wave-induced mixing can affect the oceanic circulation, such as western boundary currents and the North Equatorial Currents through changes of sea surface height associated with the variation of the thermal structure of the upper ocean. |
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