A broadscale shift in antarctic temperature trends
During the second half of the twentieth century, the Antarctic Surface Air Temperature (SAT) trends are characterized by fast warming over West Antarctica but mild cooling over East Antarctica. However, after 2000, the warming over several stations in the Antarctic Peninsula slowed down, whereas the...
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ftnerc:oai:nora.nerc.ac.uk:534673 2023-12-10T09:42:03+01:00 A broadscale shift in antarctic temperature trends Xin, Meijiao Li, Xichen Stammerjohn, Sharon E. Cai, Wenju Zhu, Jiang Turner, John Clem, Kyle R. Song, Chentao Wang, Wenzhu Hou, Yurong 2023-11 http://nora.nerc.ac.uk/id/eprint/534673/ https://link.springer.com/article/10.1007/s00382-023-06825-4 unknown Springer Xin, Meijiao; Li, Xichen; Stammerjohn, Sharon E.; Cai, Wenju; Zhu, Jiang; Turner, John orcid:0000-0002-6111-5122 Clem, Kyle R.; Song, Chentao; Wang, Wenzhu; Hou, Yurong. 2023 A broadscale shift in antarctic temperature trends. Climate Dynamics, 61 (9-10). 4623-4641. https://doi.org/10.1007/s00382-023-06825-4 <https://doi.org/10.1007/s00382-023-06825-4> Publication - Article PeerReviewed 2023 ftnerc https://doi.org/10.1007/s00382-023-06825-4 2023-11-10T00:03:07Z During the second half of the twentieth century, the Antarctic Surface Air Temperature (SAT) trends are characterized by fast warming over West Antarctica but mild cooling over East Antarctica. However, after 2000, the warming over several stations in the Antarctic Peninsula slowed down, whereas the South Pole experienced fast warming. These reversed SAT trends show strong regionality and seasonality, together with large uncertainty and disagreement among different observational and reanalysis datasets, which makes it difficult to achieve a comprehensive understanding of the multi-decadal Antarctic SAT trend and its reversal. In this study, we use the Combined Maximum Covariance Analysis (CMCA) method to extract the most coherent modes of the Antarctic SAT trends among six reanalysis datasets and 26 station-based observations. Further analysis shows that the reversals of the SAT trends before and after 2000, especially for austral spring and summer, are mainly attributed to the reversed trends of the leading CMCA modes and their related atmospheric circulation and thermal advection patterns over Antarctica. For austral spring, the reversal of the west-warming-east-cooling pattern over Antarctica is closely related to the changes of thermal advection induced by the anomalous circulation center over the Antarctic Peninsula–Weddell Sea region. For summer, the post-2000 reversal of the Antarctic Peninsula-warming-East Antarctic-cooling is attributed to the stratospheric ozone recovery over the Antarctic, and the associated adjustment of the southern annular mode. The CMCA decomposition better combines the information from different measurements, clarifying the long-term SAT trend and its reversal for different seasons. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica South pole South pole Weddell Sea West Antarctica Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Weddell Sea East Antarctica Austral West Antarctica Weddell South Pole Climate Dynamics 61 9-10 4623 4641 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
During the second half of the twentieth century, the Antarctic Surface Air Temperature (SAT) trends are characterized by fast warming over West Antarctica but mild cooling over East Antarctica. However, after 2000, the warming over several stations in the Antarctic Peninsula slowed down, whereas the South Pole experienced fast warming. These reversed SAT trends show strong regionality and seasonality, together with large uncertainty and disagreement among different observational and reanalysis datasets, which makes it difficult to achieve a comprehensive understanding of the multi-decadal Antarctic SAT trend and its reversal. In this study, we use the Combined Maximum Covariance Analysis (CMCA) method to extract the most coherent modes of the Antarctic SAT trends among six reanalysis datasets and 26 station-based observations. Further analysis shows that the reversals of the SAT trends before and after 2000, especially for austral spring and summer, are mainly attributed to the reversed trends of the leading CMCA modes and their related atmospheric circulation and thermal advection patterns over Antarctica. For austral spring, the reversal of the west-warming-east-cooling pattern over Antarctica is closely related to the changes of thermal advection induced by the anomalous circulation center over the Antarctic Peninsula–Weddell Sea region. For summer, the post-2000 reversal of the Antarctic Peninsula-warming-East Antarctic-cooling is attributed to the stratospheric ozone recovery over the Antarctic, and the associated adjustment of the southern annular mode. The CMCA decomposition better combines the information from different measurements, clarifying the long-term SAT trend and its reversal for different seasons. |
format |
Article in Journal/Newspaper |
author |
Xin, Meijiao Li, Xichen Stammerjohn, Sharon E. Cai, Wenju Zhu, Jiang Turner, John Clem, Kyle R. Song, Chentao Wang, Wenzhu Hou, Yurong |
spellingShingle |
Xin, Meijiao Li, Xichen Stammerjohn, Sharon E. Cai, Wenju Zhu, Jiang Turner, John Clem, Kyle R. Song, Chentao Wang, Wenzhu Hou, Yurong A broadscale shift in antarctic temperature trends |
author_facet |
Xin, Meijiao Li, Xichen Stammerjohn, Sharon E. Cai, Wenju Zhu, Jiang Turner, John Clem, Kyle R. Song, Chentao Wang, Wenzhu Hou, Yurong |
author_sort |
Xin, Meijiao |
title |
A broadscale shift in antarctic temperature trends |
title_short |
A broadscale shift in antarctic temperature trends |
title_full |
A broadscale shift in antarctic temperature trends |
title_fullStr |
A broadscale shift in antarctic temperature trends |
title_full_unstemmed |
A broadscale shift in antarctic temperature trends |
title_sort |
broadscale shift in antarctic temperature trends |
publisher |
Springer |
publishDate |
2023 |
url |
http://nora.nerc.ac.uk/id/eprint/534673/ https://link.springer.com/article/10.1007/s00382-023-06825-4 |
geographic |
Antarctic The Antarctic Antarctic Peninsula Weddell Sea East Antarctica Austral West Antarctica Weddell South Pole |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Weddell Sea East Antarctica Austral West Antarctica Weddell South Pole |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica South pole South pole Weddell Sea West Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica South pole South pole Weddell Sea West Antarctica |
op_relation |
Xin, Meijiao; Li, Xichen; Stammerjohn, Sharon E.; Cai, Wenju; Zhu, Jiang; Turner, John orcid:0000-0002-6111-5122 Clem, Kyle R.; Song, Chentao; Wang, Wenzhu; Hou, Yurong. 2023 A broadscale shift in antarctic temperature trends. Climate Dynamics, 61 (9-10). 4623-4641. https://doi.org/10.1007/s00382-023-06825-4 <https://doi.org/10.1007/s00382-023-06825-4> |
op_doi |
https://doi.org/10.1007/s00382-023-06825-4 |
container_title |
Climate Dynamics |
container_volume |
61 |
container_issue |
9-10 |
container_start_page |
4623 |
op_container_end_page |
4641 |
_version_ |
1784884807059111936 |