A new study by Moore et al. (2018, ) highlights a collapse of the anticyclonic Beaufort High atmospheric circulation over the western Arctic Ocean in the winter of 2017 and an associated reversal of the sea ice drift through the southern Beaufort Sea (eastward instead of the predominantly westward circulation). The authors linked this to the loss of sea ice in the Barents Sea, anomalous warming over the region, and the intrusion of low-pressure cyclones along the eastern Arctic. In this commentary we discuss the significance of this observation, the challenges associated with understanding these possible linkages, and some of the alternative hypotheses surrounding the impacts of winter Arctic sea ice loss.
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Univ Toronto, Dept Phys, Toronto, ON, Canada
Univ Washington, Jackson Sch Int Studies, Seattle, WA 98195 USAUniv Toronto, Dept Phys, Toronto, ON, Canada
Moore, G. W. K.
Schweiger, A.
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Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USAUniv Toronto, Dept Phys, Toronto, ON, Canada
Schweiger, A.
Zhang, J.
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Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USAUniv Toronto, Dept Phys, Toronto, ON, Canada
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City Univ Hong Kong, Sch Energy & Environm, Guy Carpenter Asia Pacific Climate Impact Ctr, Hong Kong, Hong Kong, Peoples R China
City Univ Hong Kong, Shenzhen Res Inst, Shenzhen 518057, Peoples R ChinaUniv Bergen, Inst Geophys, N-5007 Bergen, Norway
机构:
Chinese Acad Sci, Inst Oceanog, Qingdao, Peoples R ChinaChinese Acad Sci, Inst Oceanog, Qingdao, Peoples R China
Gong, Tingting
Luo, Dehai
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Chinese Acad Sci, CAS Key Lab Reg Climate Environm Temperate East A, Inst Atmospher Phys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Oceanog, Qingdao, Peoples R China