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| Atmospheric Boundary Layer Turbulence in the Presence of Swell: Turbulent Kinetic Energy Budget, Monin-Obukhov Similarity Theory, and Inertial Dissipation Method | |
| Zou, Zhongshui1,2; Li, Shuiqing3,4,5; Huang, Jian6; Li, Peiliang1; Song, Jinbao1; Zhang, Jun A.7,8; Wan, Zhanhong1 | |
| 2020-05-01 | |
| 发表期刊 | JOURNAL OF PHYSICAL OCEANOGRAPHY
 |
| ISSN | 0022-3670 |
| 卷号 | 50期号:5页码:1213-1225 |
| 通讯作者 | Huang, Jian([email protected]) |
| 摘要 | Turbulence over the mobile ocean surface has distinct properties compared to turbulence over land. Thus, findings that are based on the turbulent kinetic energy (TKE) budget and Monin-Obukhov similarity theory (MOST) over land may not be applicable to conditions over ocean partly because of the existence of a wave boundary layer (the lower part of atmospheric boundary layer including effects of surface waves; we used the term "WBL" in this article for convenience), where the total stress can be separated into turbulent stress and wave coherent stress. Here the turbulent stress is defined as the stress generated by wind shear and buoyancy, while the wave coherent stress accounts for the momentum transfer between ocean waves and atmosphere. In this study, applicability of the turbulent kinetic energy (TKE) budget and the inertial dissipation method (IDM) in the context of the MOST within the WBL are examined. It was found that turbulent transport terms in the TKE budget should not be neglected when calculating the total stress under swell conditions. This was confirmed by observations made on a fixed platform. The results also suggested that turbulent stress, rather than total stress, should be used when applying the MOST within the WBL. By combining the TKE budget and MOST, our study showed that the stress computed by the traditional IDM corresponds to the turbulent stress rather than the total stress. The swell wave coherent stress should be considered when applying the IDM to calculate the stress in the WBL. |
| 关键词 | Atmosphere-ocean interaction Boundary layer Microscale processes variability Air-sea interaction Atmosphere-ocean interaction |
| DOI | 10.1175/JPO-D-19-0136.1 |
| 收录类别 | SCI |
| 语种 | 英语 |
| 资助项目 | National Natural Science Foundation of China[41830533]; National Natural Science Foundation of China[41806028]; National Natural Science Foundation of China[41606024]; National Natural Science Foundation of China[41976010]; China Postdoctoral Science Foundation[2019 M65206]; National Basic Research Program of China, Monitoring and Forecasting of Finescale Structure and Impact Assessment of Landfalling Typhoons[2015CB452800] |
| WOS研究方向 | Oceanography |
| WOS类目 | Oceanography |
| WOS记录号 | WOS:000536602000006 |
| 出版者 | AMER METEOROLOGICAL SOC |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/167615 |
| 专题 | 海洋环流与波动重点实验室 |
| 通讯作者 | Huang, Jian |
| 作者单位 | 1.Zhejiang Univ, Ocean Coll, Zhoushan, Peoples R China 2.Zhejiang Univ, Ocean Res Ctr Zhou Shan, Zhoushan, Peoples R China 3.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Ocean & Climate Dynam, Qingdao, Peoples R China 5.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Peoples R China 6.CMA, Guangzhou Inst Trop & Marine Meteorol, Shenzhen, Guangdong, Peoples R China 7.Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA 8.NOAA, Hurricane Res Div, AOML, Miami, FL USA |
| 推荐引用方式 GB/T 7714 | Zou, Zhongshui,Li, Shuiqing,Huang, Jian,et al. Atmospheric Boundary Layer Turbulence in the Presence of Swell: Turbulent Kinetic Energy Budget, Monin-Obukhov Similarity Theory, and Inertial Dissipation Method[J]. JOURNAL OF PHYSICAL OCEANOGRAPHY,2020,50(5):1213-1225. |
| APA | Zou, Zhongshui.,Li, Shuiqing.,Huang, Jian.,Li, Peiliang.,Song, Jinbao.,...&Wan, Zhanhong.(2020).Atmospheric Boundary Layer Turbulence in the Presence of Swell: Turbulent Kinetic Energy Budget, Monin-Obukhov Similarity Theory, and Inertial Dissipation Method.JOURNAL OF PHYSICAL OCEANOGRAPHY,50(5),1213-1225. |
| MLA | Zou, Zhongshui,et al."Atmospheric Boundary Layer Turbulence in the Presence of Swell: Turbulent Kinetic Energy Budget, Monin-Obukhov Similarity Theory, and Inertial Dissipation Method".JOURNAL OF PHYSICAL OCEANOGRAPHY 50.5(2020):1213-1225. |
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