West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate
In September-October 2005, the juxtaposition of low-and high-pressure anomalies at 130 degrees W and 60 degrees W, respectively, created strong and persistent northerly airflow across the West Antarctic Peninsula (WAP). This had a major impact on regional sea ice conditions, with extreme ice compact...
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Online Access: | http://hdl.handle.net/2078.1/36795 https://doi.org/10.1029/2007JC004239 |
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ftunivlouvain:oai:dial.uclouvain.be:boreal:36795 2024-05-19T07:28:46+00:00 West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate Massom, Robert A. Stammerjohn, Sharon E. Lefebvre, Wouter Harangozo, Stephen A. Adams, Neil Scambos, Theodore A. Pook, Michael J. Fowler, Charles UCL 2008 http://hdl.handle.net/2078.1/36795 https://doi.org/10.1029/2007JC004239 eng eng Amer Geophysical Union boreal:36795 http://hdl.handle.net/2078.1/36795 doi:10.1029/2007JC004239 urn:ISSN:0148-0227 Journal of Geophysical Research, Vol. 113, no. C2 (2008) info:eu-repo/semantics/article 2008 ftunivlouvain https://doi.org/10.1029/2007JC004239 2024-04-24T01:49:53Z In September-October 2005, the juxtaposition of low-and high-pressure anomalies at 130 degrees W and 60 degrees W, respectively, created strong and persistent northerly airflow across the West Antarctic Peninsula (WAP). This had a major impact on regional sea ice conditions, with extreme ice compaction in the Bellingshausen and East Amundsen seas (60 degrees W-130 degrees W) but divergence in the West Amundsen and East Ross seas. This resulted in the former in a highly compact marginal ice zone and ice cover, mean modeled ice thicknesses of >5 m, and an earlier-than-average maximum extent (mid-August). While rapid ice retreat in late winter-spring created a major negative ice extent anomaly, compact ice persisted in the subsequent summer. Other effects were anomalies in air temperature (of +1 degrees C to +5 degrees C) and precipitation rates (to >2.5 mm/d). The patterns in late 2005 are consistent with the occurrence of a weak La Nina and a near-neutral Southern Annular Mode, with a quasi-stationary zonal wave three pattern dominating hemispheric atmospheric circulation. Once a compact ice edge was created, it took only one additional week of strong winds to "solidify'' the pack in place. Conditions in 2005 are analyzed in the context of 1979-2005 and compared with the springs of 1993, 1997, 1999, 2001, and 2004. A statistically significant increase of the northerly 10-m wind component between 110 degrees W and 125 degrees W occurred in the Septembers of 1979-2005. No clear trends occur in other spring months. This work underlines the key importance of ice dynamics in recent changes in the WAP sea ice regime. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Sea ice DIAL@UCLouvain (Université catholique de Louvain) Journal of Geophysical Research 113 C2 |
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DIAL@UCLouvain (Université catholique de Louvain) |
op_collection_id |
ftunivlouvain |
language |
English |
description |
In September-October 2005, the juxtaposition of low-and high-pressure anomalies at 130 degrees W and 60 degrees W, respectively, created strong and persistent northerly airflow across the West Antarctic Peninsula (WAP). This had a major impact on regional sea ice conditions, with extreme ice compaction in the Bellingshausen and East Amundsen seas (60 degrees W-130 degrees W) but divergence in the West Amundsen and East Ross seas. This resulted in the former in a highly compact marginal ice zone and ice cover, mean modeled ice thicknesses of >5 m, and an earlier-than-average maximum extent (mid-August). While rapid ice retreat in late winter-spring created a major negative ice extent anomaly, compact ice persisted in the subsequent summer. Other effects were anomalies in air temperature (of +1 degrees C to +5 degrees C) and precipitation rates (to >2.5 mm/d). The patterns in late 2005 are consistent with the occurrence of a weak La Nina and a near-neutral Southern Annular Mode, with a quasi-stationary zonal wave three pattern dominating hemispheric atmospheric circulation. Once a compact ice edge was created, it took only one additional week of strong winds to "solidify'' the pack in place. Conditions in 2005 are analyzed in the context of 1979-2005 and compared with the springs of 1993, 1997, 1999, 2001, and 2004. A statistically significant increase of the northerly 10-m wind component between 110 degrees W and 125 degrees W occurred in the Septembers of 1979-2005. No clear trends occur in other spring months. This work underlines the key importance of ice dynamics in recent changes in the WAP sea ice regime. |
author2 |
UCL |
format |
Article in Journal/Newspaper |
author |
Massom, Robert A. Stammerjohn, Sharon E. Lefebvre, Wouter Harangozo, Stephen A. Adams, Neil Scambos, Theodore A. Pook, Michael J. Fowler, Charles |
spellingShingle |
Massom, Robert A. Stammerjohn, Sharon E. Lefebvre, Wouter Harangozo, Stephen A. Adams, Neil Scambos, Theodore A. Pook, Michael J. Fowler, Charles West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
author_facet |
Massom, Robert A. Stammerjohn, Sharon E. Lefebvre, Wouter Harangozo, Stephen A. Adams, Neil Scambos, Theodore A. Pook, Michael J. Fowler, Charles |
author_sort |
Massom, Robert A. |
title |
West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
title_short |
West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
title_full |
West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
title_fullStr |
West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
title_full_unstemmed |
West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
title_sort |
west antarctic peninsula sea ice in 2005: extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate |
publisher |
Amer Geophysical Union |
publishDate |
2008 |
url |
http://hdl.handle.net/2078.1/36795 https://doi.org/10.1029/2007JC004239 |
genre |
Antarc* Antarctic Antarctic Peninsula Sea ice |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Sea ice |
op_source |
Journal of Geophysical Research, Vol. 113, no. C2 (2008) |
op_relation |
boreal:36795 http://hdl.handle.net/2078.1/36795 doi:10.1029/2007JC004239 urn:ISSN:0148-0227 |
op_doi |
https://doi.org/10.1029/2007JC004239 |
container_title |
Journal of Geophysical Research |
container_volume |
113 |
container_issue |
C2 |
_version_ |
1799475798581706752 |