Extensive retreat of Greenland tidewater glaciers, 2000-2010
Overall mass loss from the Greenland ice sheet nearly doubled during the early 2000sresulting in an increased contribution to sea-level rise, with this step-change being mainlyattributed to the widespread frontal retreat and accompanying dynamic thinning of tidewaterglaciers. Changes in glacier calv...
Published in: | Arctic, Antarctic, and Alpine Research |
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Online Access: | https://doi.org/10.1657/AAAR0014-049 http://ecite.utas.edu.au/102760 |
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ftunivtasecite:oai:ecite.utas.edu.au:102760 2023-05-15T14:14:41+02:00 Extensive retreat of Greenland tidewater glaciers, 2000-2010 Murray, T Scharrer, K Selmes, N Booth, AD James, TD Bevan, SL Bradley, J Cook, S Cordero Llana, L Drocourt, Y Dyke, L Goldsack, A Hughes, AL Luckman, AJ McGovern, J 2015 https://doi.org/10.1657/AAAR0014-049 http://ecite.utas.edu.au/102760 en eng Inst Arctic Alpine Res http://dx.doi.org/10.1657/AAAR0014-049 Murray, T and Scharrer, K and Selmes, N and Booth, AD and James, TD and Bevan, SL and Bradley, J and Cook, S and Cordero Llana, L and Drocourt, Y and Dyke, L and Goldsack, A and Hughes, AL and Luckman, AJ and McGovern, J, Extensive retreat of Greenland tidewater glaciers, 2000-2010, Arctic, Antarctic and Alpine Research, 47, (3) pp. 427-447. ISSN 1523-0430 (2015) [Refereed Article] http://ecite.utas.edu.au/102760 Earth Sciences Physical Geography and Environmental Geoscience Glaciology Refereed Article PeerReviewed 2015 ftunivtasecite https://doi.org/10.1657/AAAR0014-049 2019-12-13T22:04:17Z Overall mass loss from the Greenland ice sheet nearly doubled during the early 2000sresulting in an increased contribution to sea-level rise, with this step-change being mainlyattributed to the widespread frontal retreat and accompanying dynamic thinning of tidewaterglaciers. Changes in glacier calving-front positions are easily derived from remotelysensed imagery and provide a record of dynamic change. However, ice-sheet-wide studiesof calving fronts have been either spatially or temporally limited. In this study multiplecalving-front positions were derived for 199 Greenland marine-terminating outlet glacierswith width greater than 1 km using Landsat imagery for the 11-year period 20002010 inorder to identify regional seasonal and inter-annual variations. During this period, outletglaciers were characterized by sustained and substantial retreat summing to more than 267km, with only 11 glaciers showing overall advance. In general, the pattern of mass loss detectedby GRACE (Gravity Recovery and Climate Experiment) and other measurementsis reflected in the calving record of Greenland glaciers. Our results suggest several regionsin the south and east of the ice sheet likely share controls on their dynamic changes, butno simple single control is apparent. Article in Journal/Newspaper Antarctic and Alpine Research Arctic glacier Greenland Ice Sheet Tidewater eCite UTAS (University of Tasmania) Greenland Arctic, Antarctic, and Alpine Research 47 3 427 447 |
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Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology Murray, T Scharrer, K Selmes, N Booth, AD James, TD Bevan, SL Bradley, J Cook, S Cordero Llana, L Drocourt, Y Dyke, L Goldsack, A Hughes, AL Luckman, AJ McGovern, J Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
description |
Overall mass loss from the Greenland ice sheet nearly doubled during the early 2000sresulting in an increased contribution to sea-level rise, with this step-change being mainlyattributed to the widespread frontal retreat and accompanying dynamic thinning of tidewaterglaciers. Changes in glacier calving-front positions are easily derived from remotelysensed imagery and provide a record of dynamic change. However, ice-sheet-wide studiesof calving fronts have been either spatially or temporally limited. In this study multiplecalving-front positions were derived for 199 Greenland marine-terminating outlet glacierswith width greater than 1 km using Landsat imagery for the 11-year period 20002010 inorder to identify regional seasonal and inter-annual variations. During this period, outletglaciers were characterized by sustained and substantial retreat summing to more than 267km, with only 11 glaciers showing overall advance. In general, the pattern of mass loss detectedby GRACE (Gravity Recovery and Climate Experiment) and other measurementsis reflected in the calving record of Greenland glaciers. Our results suggest several regionsin the south and east of the ice sheet likely share controls on their dynamic changes, butno simple single control is apparent. |
format |
Article in Journal/Newspaper |
author |
Murray, T Scharrer, K Selmes, N Booth, AD James, TD Bevan, SL Bradley, J Cook, S Cordero Llana, L Drocourt, Y Dyke, L Goldsack, A Hughes, AL Luckman, AJ McGovern, J |
author_facet |
Murray, T Scharrer, K Selmes, N Booth, AD James, TD Bevan, SL Bradley, J Cook, S Cordero Llana, L Drocourt, Y Dyke, L Goldsack, A Hughes, AL Luckman, AJ McGovern, J |
author_sort |
Murray, T |
title |
Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
title_short |
Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
title_full |
Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
title_fullStr |
Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
title_full_unstemmed |
Extensive retreat of Greenland tidewater glaciers, 2000-2010 |
title_sort |
extensive retreat of greenland tidewater glaciers, 2000-2010 |
publisher |
Inst Arctic Alpine Res |
publishDate |
2015 |
url |
https://doi.org/10.1657/AAAR0014-049 http://ecite.utas.edu.au/102760 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarctic and Alpine Research Arctic glacier Greenland Ice Sheet Tidewater |
genre_facet |
Antarctic and Alpine Research Arctic glacier Greenland Ice Sheet Tidewater |
op_relation |
http://dx.doi.org/10.1657/AAAR0014-049 Murray, T and Scharrer, K and Selmes, N and Booth, AD and James, TD and Bevan, SL and Bradley, J and Cook, S and Cordero Llana, L and Drocourt, Y and Dyke, L and Goldsack, A and Hughes, AL and Luckman, AJ and McGovern, J, Extensive retreat of Greenland tidewater glaciers, 2000-2010, Arctic, Antarctic and Alpine Research, 47, (3) pp. 427-447. ISSN 1523-0430 (2015) [Refereed Article] http://ecite.utas.edu.au/102760 |
op_doi |
https://doi.org/10.1657/AAAR0014-049 |
container_title |
Arctic, Antarctic, and Alpine Research |
container_volume |
47 |
container_issue |
3 |
container_start_page |
427 |
op_container_end_page |
447 |
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1766287018169466880 |