Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments

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Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments. / Yang, Shuting; Christensen, Jens H.

I: Geophysical Research Letters, Bind 39, Nr. 20, L20707, 28.10.2012.

Publikation: Bidrag til tidsskriftTidsskriftartikelfagfællebedømt

Harvard

Yang, S & Christensen, JH 2012, 'Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments', Geophysical Research Letters, bind 39, nr. 20, L20707. https://doi.org/10.1029/2012GL053338

APA

Yang, S., & Christensen, J. H. (2012). Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments. Geophysical Research Letters, 39(20), [L20707]. https://doi.org/10.1029/2012GL053338

Vancouver

Yang S, Christensen JH. Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments. Geophysical Research Letters. 2012 okt. 28;39(20). L20707. https://doi.org/10.1029/2012GL053338

Author

Yang, Shuting ; Christensen, Jens H. / Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments. I: Geophysical Research Letters. 2012 ; Bind 39, Nr. 20.

Bibtex

@article{81602652bdcb46728d71d0922aeda5e9,
title = "Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments",
abstract = "European winter climate and its possible relationship with the Arctic sea ice reduction in the recent past and future as simulated by the models of the Climate Model Intercomparison Project phase 5 (CMIP5) is investigated, with focus on the cold winters. While Europe will warm overall in the future, we find that episodes of cold months will continue to occur and there remains substantial probability for the occurrence of cold winters in Europe linked with sea ice reduction in the Barents and Kara Sea sector. A pattern of cold-European warm-Arctic anomaly is typical for the cold events in the future, which is associated with the negative phase of the Arctic Oscillation. These patterns, however, differ from the corresponding patterns in the historical period, and underline the connection between European cold winter events and Arctic sea ice reduction.",
author = "Shuting Yang and Christensen, {Jens H.}",
year = "2012",
month = oct,
day = "28",
doi = "10.1029/2012GL053338",
language = "English",
volume = "39",
journal = "Geophysical Research Letters (Online)",
issn = "1944-8007",
publisher = "Wiley-Blackwell",
number = "20",

}

RIS

TY - JOUR

T1 - Arctic sea ice reduction and European cold winters in CMIP5 climate change experiments

AU - Yang, Shuting

AU - Christensen, Jens H.

PY - 2012/10/28

Y1 - 2012/10/28

N2 - European winter climate and its possible relationship with the Arctic sea ice reduction in the recent past and future as simulated by the models of the Climate Model Intercomparison Project phase 5 (CMIP5) is investigated, with focus on the cold winters. While Europe will warm overall in the future, we find that episodes of cold months will continue to occur and there remains substantial probability for the occurrence of cold winters in Europe linked with sea ice reduction in the Barents and Kara Sea sector. A pattern of cold-European warm-Arctic anomaly is typical for the cold events in the future, which is associated with the negative phase of the Arctic Oscillation. These patterns, however, differ from the corresponding patterns in the historical period, and underline the connection between European cold winter events and Arctic sea ice reduction.

AB - European winter climate and its possible relationship with the Arctic sea ice reduction in the recent past and future as simulated by the models of the Climate Model Intercomparison Project phase 5 (CMIP5) is investigated, with focus on the cold winters. While Europe will warm overall in the future, we find that episodes of cold months will continue to occur and there remains substantial probability for the occurrence of cold winters in Europe linked with sea ice reduction in the Barents and Kara Sea sector. A pattern of cold-European warm-Arctic anomaly is typical for the cold events in the future, which is associated with the negative phase of the Arctic Oscillation. These patterns, however, differ from the corresponding patterns in the historical period, and underline the connection between European cold winter events and Arctic sea ice reduction.

UR - http://www.scopus.com/inward/record.url?scp=84868009398&partnerID=8YFLogxK

U2 - 10.1029/2012GL053338

DO - 10.1029/2012GL053338

M3 - Journal article

AN - SCOPUS:84868009398

VL - 39

JO - Geophysical Research Letters (Online)

JF - Geophysical Research Letters (Online)

SN - 1944-8007

IS - 20

M1 - L20707

ER -

ID: 186940180