Greenland Ice Sheet - Arctic Report Card: Update for 2011
A persistent and strong negative North Atlantic Oscillation (NAO) index was responsible for southerly air flow along the west of Greenland, which caused anomalously warm weather in winter 2010-11 and summer 2011. The area and duration of melting at the surface of the ice sheet in summer 2011 were th...
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ftorbi:oai:orbi.ulg.ac.be:2268/107836 2024-04-21T07:44:16+00:00 Greenland Ice Sheet - Arctic Report Card: Update for 2011 Box, J. Cappelen, J. Chen, C. Decker, D. Fettweis, Xavier Hall, D. Hanna, E. Jorgensen, B. Lipscomb, W. Mernild, S. Mote, T. Steiner, N. Tedesco, M. van de Wal, R. Wahr, J. 2011-12 https://orbi.uliege.be/handle/2268/107836 https://orbi.uliege.be/bitstream/2268/107836/1/ArcticReportCard_Greenland.pdf en eng http://www.arctic.noaa.gov/reportcard/greenland_ice_sheet.html https://orbi.uliege.be/handle/2268/107836 info:hdl:2268/107836 https://orbi.uliege.be/bitstream/2268/107836/1/ArcticReportCard_Greenland.pdf open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique report http://purl.org/coar/resource_type/c_93fc info:eu-repo/semantics/report 2011 ftorbi 2024-03-27T14:44:09Z A persistent and strong negative North Atlantic Oscillation (NAO) index was responsible for southerly air flow along the west of Greenland, which caused anomalously warm weather in winter 2010-11 and summer 2011. The area and duration of melting at the surface of the ice sheet in summer 2011 were the third highest since 1979. The lowest surface albedo observed in 12 years of satellite observations (2000-2011) was a consequence of enhanced surface melting and below normal summer snowfall. The area of marine-terminating glaciers continued to decrease, though at less than half the rate of the previous 10 years. In situ measurements revealed near record-setting mass losses concentrated at higher elevations on the western slope of the ice sheet, and at an isolated glacier in southeastern Greenland. Total ice sheet mass loss in 2011 was 70% larger than the 2003-09 average annual loss rate of -250 Gt y-1. According to satellite gravity data obtained since 2002, ice sheet mass loss is accelerating. Report albedo glacier Greenland Ice Sheet North Atlantic North Atlantic oscillation University of Liège: ORBi (Open Repository and Bibliography) |
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Open Polar |
collection |
University of Liège: ORBi (Open Repository and Bibliography) |
op_collection_id |
ftorbi |
language |
English |
topic |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
spellingShingle |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique Box, J. Cappelen, J. Chen, C. Decker, D. Fettweis, Xavier Hall, D. Hanna, E. Jorgensen, B. Lipscomb, W. Mernild, S. Mote, T. Steiner, N. Tedesco, M. van de Wal, R. Wahr, J. Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
topic_facet |
Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
description |
A persistent and strong negative North Atlantic Oscillation (NAO) index was responsible for southerly air flow along the west of Greenland, which caused anomalously warm weather in winter 2010-11 and summer 2011. The area and duration of melting at the surface of the ice sheet in summer 2011 were the third highest since 1979. The lowest surface albedo observed in 12 years of satellite observations (2000-2011) was a consequence of enhanced surface melting and below normal summer snowfall. The area of marine-terminating glaciers continued to decrease, though at less than half the rate of the previous 10 years. In situ measurements revealed near record-setting mass losses concentrated at higher elevations on the western slope of the ice sheet, and at an isolated glacier in southeastern Greenland. Total ice sheet mass loss in 2011 was 70% larger than the 2003-09 average annual loss rate of -250 Gt y-1. According to satellite gravity data obtained since 2002, ice sheet mass loss is accelerating. |
format |
Report |
author |
Box, J. Cappelen, J. Chen, C. Decker, D. Fettweis, Xavier Hall, D. Hanna, E. Jorgensen, B. Lipscomb, W. Mernild, S. Mote, T. Steiner, N. Tedesco, M. van de Wal, R. Wahr, J. |
author_facet |
Box, J. Cappelen, J. Chen, C. Decker, D. Fettweis, Xavier Hall, D. Hanna, E. Jorgensen, B. Lipscomb, W. Mernild, S. Mote, T. Steiner, N. Tedesco, M. van de Wal, R. Wahr, J. |
author_sort |
Box, J. |
title |
Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
title_short |
Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
title_full |
Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
title_fullStr |
Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
title_full_unstemmed |
Greenland Ice Sheet - Arctic Report Card: Update for 2011 |
title_sort |
greenland ice sheet - arctic report card: update for 2011 |
publishDate |
2011 |
url |
https://orbi.uliege.be/handle/2268/107836 https://orbi.uliege.be/bitstream/2268/107836/1/ArcticReportCard_Greenland.pdf |
genre |
albedo glacier Greenland Ice Sheet North Atlantic North Atlantic oscillation |
genre_facet |
albedo glacier Greenland Ice Sheet North Atlantic North Atlantic oscillation |
op_relation |
http://www.arctic.noaa.gov/reportcard/greenland_ice_sheet.html https://orbi.uliege.be/handle/2268/107836 info:hdl:2268/107836 https://orbi.uliege.be/bitstream/2268/107836/1/ArcticReportCard_Greenland.pdf |
op_rights |
open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess |
_version_ |
1796935130266206208 |