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Influence of the Gulf Stream on the Barents Sea ice retreat and Eurasian coldness during early winter

Bibliographic Data

ID15544451
AuthorsKazutoshi Sato (0000-0003-0216-8942, Japan Agency for Marine-Earth Science and Technology, corresponding author), Jun Inoue (0000-0002-7409-2556, National Institute of Polar Research), Masahiro Watanabe (0000-0003-3483-0240)
Year2014
Volume9
Issue8
Pages084009-084009
Publication date2014-08-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/9/8/084009
OpenAlexW1967045843
LanguageEN
Citations received23
References cited42

Abnormal sea-ice retreat over the Barents Sea during early winter has been considered a leading driver of recent midlatitude severe winters over Eurasia. However, causal relationships between such retreat and the atmospheric circulation anomalies remains uncertain. Using a reanalysis dataset, we found that poleward shift of a sea surface temperature front over the Gulf Stream likely induces warm southerly advection and consequent sea-ice decline over the Barents Sea sector, and a cold anomaly over Eurasia via planetary waves triggered over the Gulf Stream region. The above mechanism is supported by the steady atmospheric response to the diabatic heating anomalies over the Gulf Stream region obtained with a linear baroclinic model. The remote atmospheric response from the Gulf Stream would be amplified over the Barents Sea region via interacting with sea-ice anomaly, promoting the warm Arctic and cold Eurasian pattern

Advection · Anomaly (physics · Arctic · Arctic ice pack · Baroclinity · Climatology · Gulf Stream · Sea ice · Arctic and Antarctic ice dynamics · Climate change and permafrost · Climate variability and models · Geology · Oceanography

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Unique citing works23
Citations per year1,92
Citation span2014 - 2026 (13)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 23

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