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What are the physical links between Arctic sea ice loss and Eurasian winter climate

Bibliographic Data

ID15550688
AuthorsIan Simmonds (0000-0002-4479-3255, The University of Melbourne, corresponding author), Pallavi Govekar (0000-0002-2857-2700, The University of Melbourne, corresponding author), Pallavi D Govekar
Year2014
Volume9
Issue10
Pages101003-101003
Publication date2014-10-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/9/10/101003
OpenAlexW2157214576
LanguageEN
Citations received9
References cited26

Rapid sea ice retreat and increases in temperature have characterised the Arctic basin in the last few decades. A number of studies have suggested that these changes have had a direct impact on extremes of weather and climate in the midlatitudes, while others have submitted that the evidence for this may not be robust. Sato et al (2014 Environ. Res. Lett. http://dx.doi.org/10.1088/1748-9326/9/8/084009 ) cast considerable light on this divergence of perspectives by revealing that apparent links between Barents Sea ice coverage and cold Eurasian winters form just a sector of a teleconnection pattern which originates remotely in the North Atlantic Gulf Stream region

Antarctic sea ice · Arctic · Arctic dipole anomaly · Arctic ice pack · Arctic sea ice decline · Climate change · Climatology · El Niño Southern Oscillation · Lead (geology · Middle latitudes · Sea ice · Teleconnection · Arctic and Antarctic ice dynamics · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Geology · Oceanography

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Unique citing works9
Citations per year0,69
Citation span2013 - 2022 (10)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 9

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