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DOI10.1007/s00382-019-04816-y
Diagnosing the development of seasonal stratification using the potential energy anomaly in the North Pacific
Yamaguchi R.; Suga T.; Richards K.J.; Qiu B.
发表日期2019
ISSN0930-7575
起始页码4667
结束页码4681
卷号53期号:2020-07-08
英文摘要Upper-ocean seasonal stratification (seasonal pycnocline and/or transition layer) is a ubiquitous feature and its vertical structure has large spatial variability. The density stratification regulates the stability of the upper ocean and thus can affect the oceanic response to atmospheric forcing and biogeochemical processes by modulating vertical mixing. In this study, we described the development of the seasonal stratification in terms of the stability of the water column, using the potential energy anomaly (PEA) as a metric based on Argo profiles. PEA budget analysis reveals that over most of the North Pacific, seasonal stratification develops under a vertical one-dimensional energy balance between an increase in PEA (i.e., a strengthening of the stratification) driven by atmospheric buoyancy forcing and a decrease in PEA associated with vertical mixing within the water column. Horizontal advection of PEA plays a significant role in the seasonal development of the stratification only in the regions of the western boundary current and equatorial current system south of 10°N. We find that, in addition to the total magnitude of the oceanic buoyancy gain, the balance between compositions of the atmospheric forcing (non-penetrating surface buoyancy forcing and penetrating radiative heating) is also important in explaining regional differences in the development of the seasonal stratification. The vertical diffusivity in the seasonal stratification estimated from the residual of the PEA budget is in the range from 5 × 10−5 m2 s−1 to 5 × 10−4 m2 s−1 and shows spatial and seasonal variability associated with local wind forcing. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature.
语种英语
scopus关键词air-sea interaction; Argo; buoyancy forcing; energy balance; potential energy; seasonal variation; stratification; water column; Pacific Ocean; Pacific Ocean (North)
来源期刊Climate Dynamics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/145959
作者单位Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Japan; Research and Development Center for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan; International Pacific Research Center, University of Hawaii at Manoa, Honolulu, HI, United States; Department of Oceanography, University of Hawaii at Manoa, Honolulu, HI, United States
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Yamaguchi R.,Suga T.,Richards K.J.,et al. Diagnosing the development of seasonal stratification using the potential energy anomaly in the North Pacific[J],2019,53(2020-07-08).
APA Yamaguchi R.,Suga T.,Richards K.J.,&Qiu B..(2019).Diagnosing the development of seasonal stratification using the potential energy anomaly in the North Pacific.Climate Dynamics,53(2020-07-08).
MLA Yamaguchi R.,et al."Diagnosing the development of seasonal stratification using the potential energy anomaly in the North Pacific".Climate Dynamics 53.2020-07-08(2019).
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