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Interdecadal variability of the warm Arctic-cold Eurasia pattern linked to the Barents oscillation

Cai, Z. Y. (author)
Fudan University
You, Q. L. (author)
China Meteorological Administration,Fudan University
Chen, Hans W. (author)
Lund University,Lunds universitet,MERGE: ModElling the Regional and Global Earth system,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,Institutionen för naturgeografi och ekosystemvetenskap,Centre for Environmental and Climate Science (CEC),Faculty of Science,Dept of Physical Geography and Ecosystem Science
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Zhang, R. N. (author)
Fudan University
Zuo, Z. Y. (author)
Dai, G. K. (author)
Fudan University
Chen, Deliang, 1961 (author)
University of Gothenburg,Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
Cohen, J. (author)
Massachusetts Institute of Technology,Massachusetts Institute of Technology (MIT)
Zolina, O. (author)
Shirshov Institute of Oceanology, RAS,Russian Academy of Sciences
Gulev, S. K. (author)
Shirshov Institute of Oceanology, RAS,Russian Academy of Sciences
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 (creator_code:org_t)
Elsevier BV, 2023
2023
English.
In: Atmospheric Research. - : Elsevier BV. - 0169-8095. ; 287
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Observed winter near-surface air temperature anomalies in the Northern Hemisphere have exhibited a warm Arctic-cold Eurasia (WACE) pattern with interdecadal variation in recent decades, but the exact mechanism behind WACE is still under debate. This study used reanalysis data and climate model simulations to investigate the interdecadal variability of the WACE pattern on a centennial scale, as well as the role of atmospheric circulations. It is found that the second mode of atmospheric variability over the North Atlantic-Arctic region, known as the Barents oscillation (BO), played a dominant role in regulating the interdecadal variability of WACE. The atmospheric circulation associated with the positive phase of the BO corresponds to an anomalous enhancement of the quasi-barotropic anticyclone near the southern Barents-Kara Seas (BKS) and the North Atlantic, as well as a weakening of the mid-latitude westerly jet. This atmospheric circulation anomaly favors the northward transport of atmospheric heat and moisture to the BKS from the mid-latitudes, resulting in an increased air temperature through downward longwave radiation. Concurrently cold air is transported from the polar region to Central Eurasia (CE), decreasing air temperature over CE. The amplified temperature anomaly dipole results in the decadal enhancement of the WACE pattern. The atmospheric circulation anomalies related to the negative phase of the BO are the opposite, which in turn leads to the decadal weakening of the WACE pattern. Our results further support the important role of internal atmospheric variability in the formation of WACE and emphasize that the atmospheric circulation associated with the BO is the main driver of WACE decadal variability over the past century.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
HUMANIORA  -- Historia och arkeologi -- Historia (hsv//swe)
HUMANITIES  -- History and Archaeology -- History (hsv//eng)

Keyword

Warm Arctic-cold Eurasia
Interdecadal variability
Atmospheric
circulation changes
Barents Oscillation
sea-ice loss
midlatitude weather
north-america
ural blocking
temperature
impacts
winters
amplification
anomalies
events
Meteorology & Atmospheric Sciences
Atmospheric circulation changes

Publication and Content Type

ref (subject category)
art (subject category)

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