The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures
Since the mid-1960s, rapid regional summer warming has occurred on the east coast of the northern Antarctic Peninsula, with near-surface temperatures increasing by more than 2°C. This warming has contributed significantly to the collapse of the northern sections of the Larsen Ice Shelf. Coincident w...
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Language: | English |
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ftvliz:oai:oma.vliz.be:252651 2023-05-15T13:54:11+02:00 The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures Marshall, G.J. Orr, A. van Lipzig, N. King, J.C. 2006 application/pdf https://www.vliz.be/imisdocs/publications/283801.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000241755900020 info:eu-repo/semantics/altIdentifier/doi/oi.org/10.1175/JCLI3844.1 https://www.vliz.be/imisdocs/publications/283801.pdf info:eu-repo/semantics/openAccess %3Ci%3EJ.+Clim.+19%2820%29%3C%2Fi%3E%3A+5388-5404.+%3Ca+href%3D%22http%3A%2F%2Fdx.doi.org%2F10.1175%2FJCLI3844.1%22+target%3D%22_blank%22%3Ehttp%3A%2F%2Fdx.doi.org%2F10.1175%2FJCLI3844.1%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2006 ftvliz https://doi.org/10.1175/JCLI3844.1 2022-05-01T10:34:12Z Since the mid-1960s, rapid regional summer warming has occurred on the east coast of the northern Antarctic Peninsula, with near-surface temperatures increasing by more than 2°C. This warming has contributed significantly to the collapse of the northern sections of the Larsen Ice Shelf. Coincident with this warming, the summer Southern Hemisphere Annular Mode (SAM) has exhibited a marked trend, suggested by modeling studies to be predominantly a response to anthropogenic forcing, resulting in increased westerlies across the northern peninsula.Observations and reanalysis data are utilized to demonstrate that the changing SAM has played a key role in driving this local summer warming. It is proposed that the stronger summer westerly winds reduce the blocking effect of the Antarctic Peninsula and lead to a higher frequency of air masses being advected eastward over the orographic barrier of the northern Antarctic Peninsula. When this occurs, a combination of a climatological temperature gradient across the barrier and the formation of a föhn wind on the lee side typically results in a summer near-surface temperature sensitivity to the SAM that is 3 times greater on the eastern side of the peninsula than on the west. SAM variability is also shown to play a less important role in determining summer temperatures at stations west of the barrier in the northern peninsula (~62°S), both at the surface and throughout the troposphere. This is in contrast to a station farther south (~65°S) where the SAM exerts little influence. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf Larsen Ice Shelf Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) Antarctic Antarctic Peninsula Larsen Ice Shelf ENVELOPE(-62.500,-62.500,-67.500,-67.500) The Antarctic Journal of Climate 19 20 5388 5404 |
institution |
Open Polar |
collection |
Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) |
op_collection_id |
ftvliz |
language |
English |
description |
Since the mid-1960s, rapid regional summer warming has occurred on the east coast of the northern Antarctic Peninsula, with near-surface temperatures increasing by more than 2°C. This warming has contributed significantly to the collapse of the northern sections of the Larsen Ice Shelf. Coincident with this warming, the summer Southern Hemisphere Annular Mode (SAM) has exhibited a marked trend, suggested by modeling studies to be predominantly a response to anthropogenic forcing, resulting in increased westerlies across the northern peninsula.Observations and reanalysis data are utilized to demonstrate that the changing SAM has played a key role in driving this local summer warming. It is proposed that the stronger summer westerly winds reduce the blocking effect of the Antarctic Peninsula and lead to a higher frequency of air masses being advected eastward over the orographic barrier of the northern Antarctic Peninsula. When this occurs, a combination of a climatological temperature gradient across the barrier and the formation of a föhn wind on the lee side typically results in a summer near-surface temperature sensitivity to the SAM that is 3 times greater on the eastern side of the peninsula than on the west. SAM variability is also shown to play a less important role in determining summer temperatures at stations west of the barrier in the northern peninsula (~62°S), both at the surface and throughout the troposphere. This is in contrast to a station farther south (~65°S) where the SAM exerts little influence. |
format |
Article in Journal/Newspaper |
author |
Marshall, G.J. Orr, A. van Lipzig, N. King, J.C. |
spellingShingle |
Marshall, G.J. Orr, A. van Lipzig, N. King, J.C. The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
author_facet |
Marshall, G.J. Orr, A. van Lipzig, N. King, J.C. |
author_sort |
Marshall, G.J. |
title |
The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
title_short |
The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
title_full |
The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
title_fullStr |
The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
title_full_unstemmed |
The impact of a changing southern hemisphere annular mode on Antarctic Peninsula summer temperatures |
title_sort |
impact of a changing southern hemisphere annular mode on antarctic peninsula summer temperatures |
publishDate |
2006 |
url |
https://www.vliz.be/imisdocs/publications/283801.pdf |
long_lat |
ENVELOPE(-62.500,-62.500,-67.500,-67.500) |
geographic |
Antarctic Antarctic Peninsula Larsen Ice Shelf The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula Larsen Ice Shelf The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Larsen Ice Shelf |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Larsen Ice Shelf |
op_source |
%3Ci%3EJ.+Clim.+19%2820%29%3C%2Fi%3E%3A+5388-5404.+%3Ca+href%3D%22http%3A%2F%2Fdx.doi.org%2F10.1175%2FJCLI3844.1%22+target%3D%22_blank%22%3Ehttp%3A%2F%2Fdx.doi.org%2F10.1175%2FJCLI3844.1%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000241755900020 info:eu-repo/semantics/altIdentifier/doi/oi.org/10.1175/JCLI3844.1 https://www.vliz.be/imisdocs/publications/283801.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1175/JCLI3844.1 |
container_title |
Journal of Climate |
container_volume |
19 |
container_issue |
20 |
container_start_page |
5388 |
op_container_end_page |
5404 |
_version_ |
1766259838185111552 |