An ice-core proxy for northerly air mass incursions into West Antarctica
A 200-year proxy for northerly air mass incursions (NAMI) into central and western West Antarctica is developed from the examination of 19 shallow (21–150 m deep) Antarctic ice-core non-sea-salt (nss) Ca2+ concentration records. The NAMI proxy reveals a significant rise in recent decades. This ris...
Published in: | International Journal of Climatology |
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ftmaineuniv:oai:digitalcommons.library.umaine.edu:ers_facpub-1175 2024-09-15T17:40:06+00:00 An ice-core proxy for northerly air mass incursions into West Antarctica Dixon, Daniel D. Mayewski, Paul Andrew Goodwin, Ian D. Marshall, Gareth J. Freeman, Rhaelene Maasch, Kirk A. Sneed, Sharon B. 2011-07-04T07:00:00Z application/pdf https://digitalcommons.library.umaine.edu/ers_facpub/176 https://doi.org/10.1002/joc.2371 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1175/viewcontent/Dixon_Icecoreproxy.pdf unknown DigitalCommons@UMaine https://digitalcommons.library.umaine.edu/ers_facpub/176 doi:10.1002/joc.2371 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1175/viewcontent/Dixon_Icecoreproxy.pdf This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). Earth Science Faculty Scholarship Antarctic glaciochemistry Southern Hemisphere westerlies climate change International Trans Antarctic Scientific Expedition atmospheric circulation Earth Sciences Geochemistry Glaciology text 2011 ftmaineuniv https://doi.org/10.1002/joc.2371 2024-07-24T05:38:40Z A 200-year proxy for northerly air mass incursions (NAMI) into central and western West Antarctica is developed from the examination of 19 shallow (21–150 m deep) Antarctic ice-core non-sea-salt (nss) Ca2+ concentration records. The NAMI proxy reveals a significant rise in recent decades. This rise is unprecedented for at least the past 200 years and is coincident with anthropogenically driven changes in other large-scale Southern Hemisphere (SH) environmental phenomena such as greenhouse gas (GHG) induced warming, ozone depletion, and the associated intensification of the SH westerlies. The Hysplit trajectory model is used to examine air mass transport pathways into West Antarctica. Empirical orthogonal function analysis, in combination with trajectory results, suggests that atmospheric circulation is the dominant factor affecting nssCa2+ concentrations throughout central and western West Antarctica. Ozone recovery will likely weaken the spring-summer SH westerlies in the future. Consequently, Antarctica could lose one of its best defences against SH GHG warming. Copyright 2011 Royal Meteorological Society Text Antarc* Antarctic Antarctica ice core West Antarctica The University of Maine: DigitalCommons@UMaine International Journal of Climatology 32 10 1455 1465 |
institution |
Open Polar |
collection |
The University of Maine: DigitalCommons@UMaine |
op_collection_id |
ftmaineuniv |
language |
unknown |
topic |
Antarctic glaciochemistry Southern Hemisphere westerlies climate change International Trans Antarctic Scientific Expedition atmospheric circulation Earth Sciences Geochemistry Glaciology |
spellingShingle |
Antarctic glaciochemistry Southern Hemisphere westerlies climate change International Trans Antarctic Scientific Expedition atmospheric circulation Earth Sciences Geochemistry Glaciology Dixon, Daniel D. Mayewski, Paul Andrew Goodwin, Ian D. Marshall, Gareth J. Freeman, Rhaelene Maasch, Kirk A. Sneed, Sharon B. An ice-core proxy for northerly air mass incursions into West Antarctica |
topic_facet |
Antarctic glaciochemistry Southern Hemisphere westerlies climate change International Trans Antarctic Scientific Expedition atmospheric circulation Earth Sciences Geochemistry Glaciology |
description |
A 200-year proxy for northerly air mass incursions (NAMI) into central and western West Antarctica is developed from the examination of 19 shallow (21–150 m deep) Antarctic ice-core non-sea-salt (nss) Ca2+ concentration records. The NAMI proxy reveals a significant rise in recent decades. This rise is unprecedented for at least the past 200 years and is coincident with anthropogenically driven changes in other large-scale Southern Hemisphere (SH) environmental phenomena such as greenhouse gas (GHG) induced warming, ozone depletion, and the associated intensification of the SH westerlies. The Hysplit trajectory model is used to examine air mass transport pathways into West Antarctica. Empirical orthogonal function analysis, in combination with trajectory results, suggests that atmospheric circulation is the dominant factor affecting nssCa2+ concentrations throughout central and western West Antarctica. Ozone recovery will likely weaken the spring-summer SH westerlies in the future. Consequently, Antarctica could lose one of its best defences against SH GHG warming. Copyright 2011 Royal Meteorological Society |
format |
Text |
author |
Dixon, Daniel D. Mayewski, Paul Andrew Goodwin, Ian D. Marshall, Gareth J. Freeman, Rhaelene Maasch, Kirk A. Sneed, Sharon B. |
author_facet |
Dixon, Daniel D. Mayewski, Paul Andrew Goodwin, Ian D. Marshall, Gareth J. Freeman, Rhaelene Maasch, Kirk A. Sneed, Sharon B. |
author_sort |
Dixon, Daniel D. |
title |
An ice-core proxy for northerly air mass incursions into West Antarctica |
title_short |
An ice-core proxy for northerly air mass incursions into West Antarctica |
title_full |
An ice-core proxy for northerly air mass incursions into West Antarctica |
title_fullStr |
An ice-core proxy for northerly air mass incursions into West Antarctica |
title_full_unstemmed |
An ice-core proxy for northerly air mass incursions into West Antarctica |
title_sort |
ice-core proxy for northerly air mass incursions into west antarctica |
publisher |
DigitalCommons@UMaine |
publishDate |
2011 |
url |
https://digitalcommons.library.umaine.edu/ers_facpub/176 https://doi.org/10.1002/joc.2371 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1175/viewcontent/Dixon_Icecoreproxy.pdf |
genre |
Antarc* Antarctic Antarctica ice core West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica ice core West Antarctica |
op_source |
Earth Science Faculty Scholarship |
op_relation |
https://digitalcommons.library.umaine.edu/ers_facpub/176 doi:10.1002/joc.2371 https://digitalcommons.library.umaine.edu/context/ers_facpub/article/1175/viewcontent/Dixon_Icecoreproxy.pdf |
op_rights |
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). |
op_doi |
https://doi.org/10.1002/joc.2371 |
container_title |
International Journal of Climatology |
container_volume |
32 |
container_issue |
10 |
container_start_page |
1455 |
op_container_end_page |
1465 |
_version_ |
1810484727852826624 |