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DOI | 10.1029/2019JC015529 |
Vertical Turbulent Cooling of the Mixed Layer in the Atlantic ITCZ and Trade Wind Regions | |
Foltz G.R.; Hummels R.; Dengler M.; Perez R.C.; Araujo M. | |
发表日期 | 2020 |
ISSN | 21699275 |
卷号 | 125期号:2 |
英文摘要 | The causes of the seasonal cycle of vertical turbulent cooling at the base of the mixed layer are assessed using observations from moored buoys in the tropical Atlantic Intertropical Convergence Zone (ITCZ) (4°N, 23°W) and trade wind (15°N, 38°W) regions together with mixing parameterizations and a one-dimensional model. At 4°N the parameterized turbulent cooling rates during 2017–2018 and 2019 agree with indirect estimates from the climatological mooring heat budget residual: both show mean cooling of 25–30 W m (Formula presented.) during November–July, when winds are weakest and the mixed layer is thinnest, and 0–10 W m (Formula presented.) during August–October. Mixing during November–July is driven by variability on multiple time scales, including subdiurnal, near-inertial, and intraseasonal. Shear associated with tropical instability waves (TIWs) is found to generate mixing and monthly mean cooling of 15–30 W m (Formula presented.) during May–July in 2017 and 2019. At 15°N the seasonal cycle of turbulent cooling is out of phase compared to 4°N, with largest cooling of up to 60 W m (Formula presented.) during boreal fall. However, the relationships between wind speed, mixed layer depth, and turbulent mixing are similar: weaker mean winds and a thinner mixed layer in the fall are associated with stronger mixing and turbulent cooling of SST. These results emphasize the importance of seasonal modulations of mixed layer depth at both locations and shear from TIWs at 4°N. ©2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | mixing; near-inertial waves; sea surface temperature; tropical Atlantic; tropical instability waves |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Oceans
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/186985 |
作者单位 | NOAA/Atlantic Oceanographic and Meteorological Laboratory, Miami, FL, United States; GEOMAR Helmholz Centre for Ocean Research, Kiel, Germany; Department of Oceanography, DOCEAN, UFPE, University Federal Pernambuco, Recife, Brazil; Brazilian Research Network on Global Climate Change, São José Dos Campos, Brazil |
推荐引用方式 GB/T 7714 | Foltz G.R.,Hummels R.,Dengler M.,et al. Vertical Turbulent Cooling of the Mixed Layer in the Atlantic ITCZ and Trade Wind Regions[J],2020,125(2). |
APA | Foltz G.R.,Hummels R.,Dengler M.,Perez R.C.,&Araujo M..(2020).Vertical Turbulent Cooling of the Mixed Layer in the Atlantic ITCZ and Trade Wind Regions.Journal of Geophysical Research: Oceans,125(2). |
MLA | Foltz G.R.,et al."Vertical Turbulent Cooling of the Mixed Layer in the Atlantic ITCZ and Trade Wind Regions".Journal of Geophysical Research: Oceans 125.2(2020). |
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