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Titlebook: New Developments in Mode-Water Research; Dynamic and Climatic Atsushi Kubokawa,Shang-Ping Xie,Humio Mitsudera Book 2013 Springer Japan KK,

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書目名稱New Developments in Mode-Water Research
副標題Dynamic and Climatic
編輯Atsushi Kubokawa,Shang-Ping Xie,Humio Mitsudera
視頻videohttp://file.papertrans.cn/666/665024/665024.mp4
叢書名稱Springer Oceanography
圖書封面Titlebook: New Developments in Mode-Water Research; Dynamic and Climatic Atsushi Kubokawa,Shang-Ping Xie,Humio Mitsudera Book 2013 Springer Japan KK,
描述This book consists of the articles from the special issue of “New developments in mode-water research: Dynamic and climatic effects” in the .Journal of Oceanography., Vol. 68 No. 1, 2012, comprising 10 chapters that cover a wide spectrum of topics. Topics range from the formation, circulation, and variability of mode waters to their dynamic effect on surface current and climate impact, and point to new directions for mode-water research. How do mode waters vary on decadal and longer timescales, and how will they change in response to global warming? What causes mode-water variability, and how does it affect surface circulation and climate? What are the roles of mesoscale eddies in the formation and dissipation of mode waters and in their variability and change? This book serves as a signpost in our endeavor to answer these and other challenging questions..
出版日期Book 2013
關鍵詞Climate Change; Climate Variability; Mode Water; Ocean Circulation; Oceanic Nutrients; Subantarctic Mode
版次1
doihttps://doi.org/10.1007/978-4-431-54162-2
isbn_softcover978-4-431-56330-3
isbn_ebook978-4-431-54162-2Series ISSN 2365-7677 Series E-ISSN 2365-7685
issn_series 2365-7677
copyrightSpringer Japan KK, part of Springer Nature 2013
The information of publication is updating

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Mixed layer depth front and subduction of low potential vorticity water under seasonal forcings in with simple seasonal forcings. A sharp MLD front develops and subduction occurs at the front from late winter to early spring. The position of the MLD front agrees with the curve where . 0 is satisfied (. is time, .. is the upper-ocean geostrophic velocity, .. is the sea surface temperature (SST),
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Interannual variations in low potential vorticity water and the subtropical countercurrent in an edific Ocean are investigated on the basis of a 60-year-long hindcast integration of an eddy-resolving ocean general circulation model. Although vertically coherent variations are dominant shows that an intensified STCC vertical shear accompanies lower PV than usual to the north on 25.5- to 26.1-. iso
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Response of the North Pacific subtropical countercurrent and its variability to global warming,that is forced by increasing greenhouse gas concentrations. Compared with the present climate, the upper ocean is more stratified, and the mixed layer depth (MLD) shoals in warmer climate. The maximum change of winter MLD appears in the Kuroshio–Oyashio extension (KOE) region, where the mean MLD is
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