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Role of Arctic Sea Ice in the 2014–2015 Eurasian Warm Winter
Author(s) -
Xie Jinbo,
Zhang Minghua,
Liu Hailong
Publication year - 2019
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2018gl080793
Subject(s) - climatology , anomaly (physics) , sea ice , arctic ice pack , skewness , arctic , arctic oscillation , geology , forcing (mathematics) , north atlantic oscillation , environmental science , arctic sea ice decline , atmospheric sciences , oceanography , drift ice , northern hemisphere , physics , statistics , mathematics , condensed matter physics
Because of large internal variabilities, the role of Arctic sea ice concentration (SIC) on regional climate cannot be easily separated. This study uses two groups of large ensemble atmospheric model simulations under climatological and observed SIC boundary conditions to investigate the role of SIC in the 2014–2015 December to February Eurasian warm winter (DJF15). It is shown that the SIC has large impact on the probability distribution function of the DJF15 temperature and pressure fields. The anomalous high Barents Sea ice during the 2014–2015 autumn and winter leads to significant shift in the probability distribution function skewness of the DJF15 surface temperature (from −0.13 to −0.48) and the related sea level pressure (from −0.18 to 0.32) that favor more occurrences of warm temperature anomaly and positive North Atlantic Oscillation‐like pattern. This asymmetry is consistent with anomalous forcing in phase with the anomalies of the sea level pressure field.