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...
Published in: | International Journal of Climatology |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
John Wiley & Sons Ltd
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2727588 https://doi.org/10.1002/joc.6548 |
_version_ | 1821530397172826112 |
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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 |
id | ftunivbergen:oai:bora.uib.no:11250/2727588 |
institution | Open Polar |
language | English |
op_collection_id | ftunivbergen |
op_container_end_page | 5842 |
op_doi | https://doi.org/10.1002/joc.6548 |
op_relation | urn:issn:0899-8418 https://hdl.handle.net/11250/2727588 https://doi.org/10.1002/joc.6548 cristin:1811581 |
op_rights | Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © 2020 The Authors. |
op_source | International Journal of Climatology 40 14 |
publishDate | 2020 |
publisher | John Wiley & Sons Ltd |
record_format | openpolar |
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 |