Physical characteristics of Eurasian winter temperature variability

Despite the on-going global warming, recent winters in Eurasian mid-latitudes were much colder than average. In an attempt to better understand the physical characteristics for cold Eurasian winters, major sources of variability in surface air temperature (SAT) are investigated based on cyclostation...

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Main Authors: Kwang-Yul Kim, Seok-Woo Son
Format: Article
Language:English
Published: IOP Publishing 2016-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/11/4/044009
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author Kwang-Yul Kim
Seok-Woo Son
author_facet Kwang-Yul Kim
Seok-Woo Son
author_sort Kwang-Yul Kim
collection DOAJ
description Despite the on-going global warming, recent winters in Eurasian mid-latitudes were much colder than average. In an attempt to better understand the physical characteristics for cold Eurasian winters, major sources of variability in surface air temperature (SAT) are investigated based on cyclostationary EOF analysis. The two leading modes of SAT variability represent the effect of Arctic amplification (AA) and the Arctic oscillation (AO), respectively. These two modes are distinct in terms of the physical characteristics, including surface energy fluxes and tropospheric circulations, and result in significantly different winter SAT patterns over the Eurasian continent. The AA-related SAT anomalies are dipolar with warm Arctic, centered at the Barents–Kara Seas, and cold East Asia. In contrast, the negative AO-related SAT anomalies are characterized by widespread cold anomalies in Northern Eurasia. Relative importance of the AA and the negative AO contributions to cold Eurasian winters is sensitive to the region of interest.
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spelling doaj.art-52bc9bee8c454fe6abefef6209f2e64c2023-08-09T14:14:52ZengIOP PublishingEnvironmental Research Letters1748-93262016-01-0111404400910.1088/1748-9326/11/4/044009Physical characteristics of Eurasian winter temperature variabilityKwang-Yul Kim0Seok-Woo Son1School of Earth and Environmental Sciences, Seoul National University , 1 Gwanak-ro, Gwanak-gu, Seoul 08826, KoreaSchool of Earth and Environmental Sciences, Seoul National University , 1 Gwanak-ro, Gwanak-gu, Seoul 08826, KoreaDespite the on-going global warming, recent winters in Eurasian mid-latitudes were much colder than average. In an attempt to better understand the physical characteristics for cold Eurasian winters, major sources of variability in surface air temperature (SAT) are investigated based on cyclostationary EOF analysis. The two leading modes of SAT variability represent the effect of Arctic amplification (AA) and the Arctic oscillation (AO), respectively. These two modes are distinct in terms of the physical characteristics, including surface energy fluxes and tropospheric circulations, and result in significantly different winter SAT patterns over the Eurasian continent. The AA-related SAT anomalies are dipolar with warm Arctic, centered at the Barents–Kara Seas, and cold East Asia. In contrast, the negative AO-related SAT anomalies are characterized by widespread cold anomalies in Northern Eurasia. Relative importance of the AA and the negative AO contributions to cold Eurasian winters is sensitive to the region of interest.https://doi.org/10.1088/1748-9326/11/4/044009Eurasian winter coolingArctic sea ice lossArctic amplificationArctic oscillation
spellingShingle Kwang-Yul Kim
Seok-Woo Son
Physical characteristics of Eurasian winter temperature variability
Environmental Research Letters
Eurasian winter cooling
Arctic sea ice loss
Arctic amplification
Arctic oscillation
title Physical characteristics of Eurasian winter temperature variability
title_full Physical characteristics of Eurasian winter temperature variability
title_fullStr Physical characteristics of Eurasian winter temperature variability
title_full_unstemmed Physical characteristics of Eurasian winter temperature variability
title_short Physical characteristics of Eurasian winter temperature variability
title_sort physical characteristics of eurasian winter temperature variability
topic Eurasian winter cooling
Arctic sea ice loss
Arctic amplification
Arctic oscillation
url https://doi.org/10.1088/1748-9326/11/4/044009
work_keys_str_mv AT kwangyulkim physicalcharacteristicsofeurasianwintertemperaturevariability
AT seokwooson physicalcharacteristicsofeurasianwintertemperaturevariability