How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas?

How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas?

Arctic warming over the Barents–Kara Seas and its impacts on the mid-latitude circulations have been widely discussed. However, the specific mechanism that brings the warming still remains unclear. In this study, a possible cause of the regional Arctic warming over the Barents–Kara Seas during early...

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Hlavní autoři: Ok Jung, Mi-Kyung Sung, Kazutoshi Sato, Young-Kwon Lim, Seong-Joong Kim, Eun-Hyuk Baek, Jee-Hoon Jeong, Baek-Min Kim
Médium: Článek
Jazyk:English
Vydáno: IOP Publishing 2017-01-01
Edice:Environmental Research Letters
Témata:
Arctic warming
Stationary Wave Model
transient eddy vorticity forcing
Western North Atlantic Ocean
On-line přístup:https://doi.org/10.1088/1748-9326/aa5f3b

Internet

https://doi.org/10.1088/1748-9326/aa5f3b

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