Oceanic forcing of the global warming slowdown in multi-model simulations

Abstract Concurrent with the slowdown of global warming during 2002–2013, the wintertime land surface air temperatures over Eurasia, North America, Africa, Australia, South America, and Greenland experienced notable cooling trends. The oceanic effects on the continental cooling trends are here inves...

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Published in:International Journal of Climatology
Main Authors: Xu, Xinping, He, Shengping, Furevik, Tore, Gao, Yongqi, Wang, Huijun, Li, Fei, Ogawa, Fumiaki
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Ltd 2020
Subjects:
Online Access:https://hdl.handle.net/11250/2727588
https://doi.org/10.1002/joc.6548
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author Xu, Xinping
He, Shengping
Furevik, Tore
Gao, Yongqi
Wang, Huijun
Li, Fei
Ogawa, Fumiaki
author_facet Xu, Xinping
He, Shengping
Furevik, Tore
Gao, Yongqi
Wang, Huijun
Li, Fei
Ogawa, Fumiaki
author_sort Xu, Xinping
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
container_issue 14
container_start_page 5829
container_title International Journal of Climatology
container_volume 40
description Abstract Concurrent with the slowdown of global warming during 2002–2013, the wintertime land surface air temperatures over Eurasia, North America, Africa, Australia, South America, and Greenland experienced notable cooling trends. The oceanic effects on the continental cooling trends are here investigated using two sets of uncoupled experiments with six different climate models. Daily and annually varying sea ice is prescribed for both sets of experiments, while daily and annually varying SST is used in the first set (EXP1) and daily and annually repeating climatological mean SST in the second set (EXP2). All six models capture the slowdown of global-mean land surface air temperature during 2002–2013 winters in EXP1 only. The slowdown concurs with a negative phase of the Pacific Decadal Oscillation (PDO), indicating that PDO plays an important role in modulating the global warming signal. Not all ensemble members capture the cooling trends over the continents, suggesting additional contribution from internal atmospheric variability. KEYWORDS continental cooling, global warming, multi-model simulations, Pacific Decadal Oscillation published version
format Article in Journal/Newspaper
genre Greenland
Sea ice
genre_facet Greenland
Sea ice
geographic Greenland
Pacific
geographic_facet Greenland
Pacific
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op_doi https://doi.org/10.1002/joc.6548
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op_rights Navngivelse 4.0 Internasjonal
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spelling ftunivbergen:oai:bora.uib.no:11250/2727588 2025-01-16T22:12:04+00:00 Oceanic forcing of the global warming slowdown in multi-model simulations Xu, Xinping He, Shengping Furevik, Tore Gao, Yongqi Wang, Huijun Li, Fei Ogawa, Fumiaki 2020 application/pdf https://hdl.handle.net/11250/2727588 https://doi.org/10.1002/joc.6548 eng eng John Wiley & Sons Ltd urn:issn:0899-8418 https://hdl.handle.net/11250/2727588 https://doi.org/10.1002/joc.6548 cristin:1811581 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © 2020 The Authors. International Journal of Climatology 40 14 Journal article Peer reviewed 2020 ftunivbergen https://doi.org/10.1002/joc.6548 2023-03-14T17:41:09Z Abstract Concurrent with the slowdown of global warming during 2002–2013, the wintertime land surface air temperatures over Eurasia, North America, Africa, Australia, South America, and Greenland experienced notable cooling trends. The oceanic effects on the continental cooling trends are here investigated using two sets of uncoupled experiments with six different climate models. Daily and annually varying sea ice is prescribed for both sets of experiments, while daily and annually varying SST is used in the first set (EXP1) and daily and annually repeating climatological mean SST in the second set (EXP2). All six models capture the slowdown of global-mean land surface air temperature during 2002–2013 winters in EXP1 only. The slowdown concurs with a negative phase of the Pacific Decadal Oscillation (PDO), indicating that PDO plays an important role in modulating the global warming signal. Not all ensemble members capture the cooling trends over the continents, suggesting additional contribution from internal atmospheric variability. KEYWORDS continental cooling, global warming, multi-model simulations, Pacific Decadal Oscillation published version Article in Journal/Newspaper Greenland Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Greenland Pacific International Journal of Climatology 40 14 5829 5842
spellingShingle Xu, Xinping
He, Shengping
Furevik, Tore
Gao, Yongqi
Wang, Huijun
Li, Fei
Ogawa, Fumiaki
Oceanic forcing of the global warming slowdown in multi-model simulations
title Oceanic forcing of the global warming slowdown in multi-model simulations
title_full Oceanic forcing of the global warming slowdown in multi-model simulations
title_fullStr Oceanic forcing of the global warming slowdown in multi-model simulations
title_full_unstemmed Oceanic forcing of the global warming slowdown in multi-model simulations
title_short Oceanic forcing of the global warming slowdown in multi-model simulations
title_sort oceanic forcing of the global warming slowdown in multi-model simulations
url https://hdl.handle.net/11250/2727588
https://doi.org/10.1002/joc.6548