Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012

The early 21st century was marked by several severe winters over Central Eurasia linked to a blocking anti-cyclone centered south of the Barents Sea. Severe winters in Central Eurasia were frequent in the 1960s when Arctic sea ice cover was anomalously large, and rare in the 1990s featuring consider...

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Main Authors: V A Semenov, M Latif
Format: Article
Language:English
Published: IOP Publishing 2015-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/10/5/054020
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author V A Semenov
M Latif
author_facet V A Semenov
M Latif
author_sort V A Semenov
collection DOAJ
description The early 21st century was marked by several severe winters over Central Eurasia linked to a blocking anti-cyclone centered south of the Barents Sea. Severe winters in Central Eurasia were frequent in the 1960s when Arctic sea ice cover was anomalously large, and rare in the 1990s featuring considerably less sea ice cover; the 1960s being characterized by a low, the 1990s by a high phase of the North Atlantic Oscillation, the major driver of surface climate variability in Central Eurasia. We performed ensemble simulations with an atmospheric general circulation model using a set of multi-year Arctic sea ice climatologies corresponding to different periods during 1966–2012. The atmospheric response to the strongly reduced sea ice cover of 2005–2012 exhibits a statistically significant anti-cyclonic surface pressure anomaly which is similar to that observed. A similar response is found when the strongly positive sea ice cover anomaly of 1966–1969 drives the model. Basically no significant atmospheric circulation response was simulated when the model was forced by the sea ice cover anomaly of 1990–1995. The results suggest that sea ice cover reduction, through a changed atmospheric circulation, considerably contributed to the recent anomalously cold winters in Central Eurasia. Further, a nonlinear atmospheric circulation response to shrinking sea ice cover is suggested that depends on the background sea ice cover.
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spelling doaj.art-99268eb1b58b4ccc9a429327a77e5b772023-08-09T14:11:27ZengIOP PublishingEnvironmental Research Letters1748-93262015-01-0110505402010.1088/1748-9326/10/5/054020Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012V A Semenov0M Latif1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany; A M Obukhov Institute of Atmospheric Physics RAS, Moscow, Russia; Institute of Geography RAS, Moscow, Russia; P P Shirshov Institute of Oceanology RAS, Moscow, RussiaGEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany; Kiel University , Kiel, GermanyThe early 21st century was marked by several severe winters over Central Eurasia linked to a blocking anti-cyclone centered south of the Barents Sea. Severe winters in Central Eurasia were frequent in the 1960s when Arctic sea ice cover was anomalously large, and rare in the 1990s featuring considerably less sea ice cover; the 1960s being characterized by a low, the 1990s by a high phase of the North Atlantic Oscillation, the major driver of surface climate variability in Central Eurasia. We performed ensemble simulations with an atmospheric general circulation model using a set of multi-year Arctic sea ice climatologies corresponding to different periods during 1966–2012. The atmospheric response to the strongly reduced sea ice cover of 2005–2012 exhibits a statistically significant anti-cyclonic surface pressure anomaly which is similar to that observed. A similar response is found when the strongly positive sea ice cover anomaly of 1966–1969 drives the model. Basically no significant atmospheric circulation response was simulated when the model was forced by the sea ice cover anomaly of 1990–1995. The results suggest that sea ice cover reduction, through a changed atmospheric circulation, considerably contributed to the recent anomalously cold winters in Central Eurasia. Further, a nonlinear atmospheric circulation response to shrinking sea ice cover is suggested that depends on the background sea ice cover.https://doi.org/10.1088/1748-9326/10/5/054020Arctic sea iceanomalously cold wintersAGCMEurasian climate change
spellingShingle V A Semenov
M Latif
Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
Environmental Research Letters
Arctic sea ice
anomalously cold winters
AGCM
Eurasian climate change
title Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
title_full Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
title_fullStr Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
title_full_unstemmed Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
title_short Nonlinear winter atmospheric circulation response to Arctic sea ice concentration anomalies for different periods during 1966–2012
title_sort nonlinear winter atmospheric circulation response to arctic sea ice concentration anomalies for different periods during 1966 2012
topic Arctic sea ice
anomalously cold winters
AGCM
Eurasian climate change
url https://doi.org/10.1088/1748-9326/10/5/054020
work_keys_str_mv AT vasemenov nonlinearwinteratmosphericcirculationresponsetoarcticseaiceconcentrationanomaliesfordifferentperiodsduring19662012
AT mlatif nonlinearwinteratmosphericcirculationresponsetoarcticseaiceconcentrationanomaliesfordifferentperiodsduring19662012