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影響因子(影響力)




書目名稱New Developments in Mode-Water Research影響因子(影響力)學(xué)科排名




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書目名稱New Developments in Mode-Water Research網(wǎng)絡(luò)公開度學(xué)科排名




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書目名稱New Developments in Mode-Water Research被引頻次學(xué)科排名




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書目名稱New Developments in Mode-Water Research年度引用學(xué)科排名




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書目名稱New Developments in Mode-Water Research讀者反饋學(xué)科排名

職業(yè)

Invigorate

有惡臭

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),

Cytokines

金絲雀

Lumbar-Stenosis

Fierce

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

Statins

Oafishness

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