Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation
The West Antarctic climate has witnessed large changes during the second half of the twentieth century including a strong and widespread continental warming, important regional changes in sea-ice extent and snow accumulation, as well as a major mass loss from the melting of some ice shelves. However...
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ftnerc:oai:nora.nerc.ac.uk:530400 2023-05-15T13:23:52+02:00 Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation Dalaiden, Quentin Goosse, Hugues Rezsöhazy, Jeanne Thomas, Elizabeth R. 2021-12 http://nora.nerc.ac.uk/id/eprint/530400/ https://link.springer.com/article/10.1007/s00382-021-05879-6 unknown Springer Dalaiden, Quentin; Goosse, Hugues; Rezsöhazy, Jeanne; Thomas, Elizabeth R. orcid:0000-0002-3010-6493 . 2021 Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation. Climate Dynamics, 57. 3479-3503. https://doi.org/10.1007/s00382-021-05879-6 <https://doi.org/10.1007/s00382-021-05879-6> Publication - Article PeerReviewed 2021 ftnerc https://doi.org/10.1007/s00382-021-05879-6 2023-02-04T19:52:08Z The West Antarctic climate has witnessed large changes during the second half of the twentieth century including a strong and widespread continental warming, important regional changes in sea-ice extent and snow accumulation, as well as a major mass loss from the melting of some ice shelves. However, the potential links between those observed changes are still unclear and instrumental data do not allow determination of whether they are part of a long-term evolution or specific to the recent decades. In this study, we analyze the climate variability of the past two centuries in the West Antarctic sector by reconstructing the key atmospheric variables (atmospheric circulation, near-surface air temperature and snow accumulation) as well as the sea-ice extent at the annual timescale using a data assimilation approach. To this end, information from Antarctic ice core records (snow accumulation and δ18O) and tree-ring width records situated in the mid-latitudes of the Southern Hemisphere are combined with the physics of climate models using a data assimilation method. This ultimately provides a complete spatial reconstruction over the West Antarctic region. Our reconstruction reproduces well the main characteristics of the observed changes over the instrumental period. We show that the observed sea-ice reduction in the Bellingshausen-Amundsen Sea sector over the satellite era is part of a long-term trend, starting at around 1850 CE, while the sea-ice expansion in the Ross Sea sector has only started around 1950 CE. Furthermore, according to our reconstruction, the Amundsen Sea Low pressure (ASL) displays no significant linear trend in its strength or position over 1850–1950 CE but becomes stronger and shifts eastward afterwards. The year-to-year sea-ice variations in the Ross Sea sector are strongly related to the ASL variability over the past two centuries, including the recent trends. By contrast, the link between ASL and sea-ice in the Bellingshausen-Amundsen Sea sector changes with time, being stronger in recent ... Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic ice core Ice Shelves Ross Sea Sea ice Natural Environment Research Council: NERC Open Research Archive Amundsen Sea Antarctic Ross Sea Climate Dynamics 57 11-12 3479 3503 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
description |
The West Antarctic climate has witnessed large changes during the second half of the twentieth century including a strong and widespread continental warming, important regional changes in sea-ice extent and snow accumulation, as well as a major mass loss from the melting of some ice shelves. However, the potential links between those observed changes are still unclear and instrumental data do not allow determination of whether they are part of a long-term evolution or specific to the recent decades. In this study, we analyze the climate variability of the past two centuries in the West Antarctic sector by reconstructing the key atmospheric variables (atmospheric circulation, near-surface air temperature and snow accumulation) as well as the sea-ice extent at the annual timescale using a data assimilation approach. To this end, information from Antarctic ice core records (snow accumulation and δ18O) and tree-ring width records situated in the mid-latitudes of the Southern Hemisphere are combined with the physics of climate models using a data assimilation method. This ultimately provides a complete spatial reconstruction over the West Antarctic region. Our reconstruction reproduces well the main characteristics of the observed changes over the instrumental period. We show that the observed sea-ice reduction in the Bellingshausen-Amundsen Sea sector over the satellite era is part of a long-term trend, starting at around 1850 CE, while the sea-ice expansion in the Ross Sea sector has only started around 1950 CE. Furthermore, according to our reconstruction, the Amundsen Sea Low pressure (ASL) displays no significant linear trend in its strength or position over 1850–1950 CE but becomes stronger and shifts eastward afterwards. The year-to-year sea-ice variations in the Ross Sea sector are strongly related to the ASL variability over the past two centuries, including the recent trends. By contrast, the link between ASL and sea-ice in the Bellingshausen-Amundsen Sea sector changes with time, being stronger in recent ... |
format |
Article in Journal/Newspaper |
author |
Dalaiden, Quentin Goosse, Hugues Rezsöhazy, Jeanne Thomas, Elizabeth R. |
spellingShingle |
Dalaiden, Quentin Goosse, Hugues Rezsöhazy, Jeanne Thomas, Elizabeth R. Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
author_facet |
Dalaiden, Quentin Goosse, Hugues Rezsöhazy, Jeanne Thomas, Elizabeth R. |
author_sort |
Dalaiden, Quentin |
title |
Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
title_short |
Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
title_full |
Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
title_fullStr |
Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
title_full_unstemmed |
Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation |
title_sort |
reconstructing atmospheric circulation and sea-ice extent in the west antarctic over the past 200 years using data assimilation |
publisher |
Springer |
publishDate |
2021 |
url |
http://nora.nerc.ac.uk/id/eprint/530400/ https://link.springer.com/article/10.1007/s00382-021-05879-6 |
geographic |
Amundsen Sea Antarctic Ross Sea |
geographic_facet |
Amundsen Sea Antarctic Ross Sea |
genre |
Amundsen Sea Antarc* Antarctic ice core Ice Shelves Ross Sea Sea ice |
genre_facet |
Amundsen Sea Antarc* Antarctic ice core Ice Shelves Ross Sea Sea ice |
op_relation |
Dalaiden, Quentin; Goosse, Hugues; Rezsöhazy, Jeanne; Thomas, Elizabeth R. orcid:0000-0002-3010-6493 . 2021 Reconstructing atmospheric circulation and sea-ice extent in the West Antarctic over the past 200 years using data assimilation. Climate Dynamics, 57. 3479-3503. https://doi.org/10.1007/s00382-021-05879-6 <https://doi.org/10.1007/s00382-021-05879-6> |
op_doi |
https://doi.org/10.1007/s00382-021-05879-6 |
container_title |
Climate Dynamics |
container_volume |
57 |
container_issue |
11-12 |
container_start_page |
3479 |
op_container_end_page |
3503 |
_version_ |
1766375968844283904 |