IOCAS-IR  > 海洋环流与波动重点实验室
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
Source PublicationJOURNAL OF PHYSICAL OCEANOGRAPHY
ISSN0022-3670
Volume50Issue:5Pages:1213-1225
Corresponding AuthorHuang, Jian(hj@gd121.cn)
AbstractTurbulence 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.
KeywordAtmosphere-ocean interaction Boundary layer Microscale processes variability Air-sea interaction Atmosphere-ocean interaction
DOI10.1175/JPO-D-19-0136.1
Indexed BySCI
Language英语
Funding ProjectNational 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 Research AreaOceanography
WOS SubjectOceanography
WOS IDWOS:000536602000006
PublisherAMER METEOROLOGICAL SOC
Citation statistics
Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/167615
Collection海洋环流与波动重点实验室
Corresponding AuthorHuang, Jian
Affiliation1.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
Recommended Citation
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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