Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90

Abstract Annual ice ablation has been measured at three locations at the margin of the Greenland ice sheet: Nordbogletscher (for 6 years: 1977–78 to 1982– 83), Qamanârssûp sermia (8 years: 1979–80 to 1986–87) and at Paakitsup Akuliarusersua (7 years: 1982–83 to the present). As the data sets cover d...

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Published in:Journal of Glaciology
Main Authors: Braithwaite, Roger J., Olesen, Ole Β., HøJmark Thomsen, Henrik
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000003671
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003671
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spelling crcambridgeupr:10.1017/s0022143000003671 2024-03-03T08:44:56+00:00 Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90 Braithwaite, Roger J. Olesen, Ole Β. HøJmark Thomsen, Henrik 1992 http://dx.doi.org/10.1017/s0022143000003671 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003671 en eng Cambridge University Press (CUP) Journal of Glaciology volume 38, issue 129, page 266-272 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0022143000003671 2024-02-08T08:42:50Z Abstract Annual ice ablation has been measured at three locations at the margin of the Greenland ice sheet: Nordbogletscher (for 6 years: 1977–78 to 1982– 83), Qamanârssûp sermia (8 years: 1979–80 to 1986–87) and at Paakitsup Akuliarusersua (7 years: 1982–83 to the present). As the data sets cover different periods, it is difficult to compare ablation directly between the three sites. However, measured series at each site can be extended over the last 30 years (1961–90) by simulations using climatic data, and the extended data series can be compared. The pattern of calculated ablation variations at the three locations is remarkably similar with no sign of any trend towards increased ablation in recent years. There was generally low ablation from the mid-1970s to the mid-1980s that may explain the recent thickening of the ablation area which has been detected by satellite radar altimetry. Ablation varies substantially from year to year, e.g. with a standard deviation of the order of ±0.5 m water a −1 , and any future monitoring programme must detect trends of increasing ablation against this background of natural variations. Article in Journal/Newspaper Greenland Ice Sheet Journal of Glaciology Cambridge University Press Greenland Qamanârssûp Sermia ENVELOPE(-49.500,-49.500,64.483,64.483) Journal of Glaciology 38 129 266 272
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Braithwaite, Roger J.
Olesen, Ole Β.
HøJmark Thomsen, Henrik
Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
topic_facet Earth-Surface Processes
description Abstract Annual ice ablation has been measured at three locations at the margin of the Greenland ice sheet: Nordbogletscher (for 6 years: 1977–78 to 1982– 83), Qamanârssûp sermia (8 years: 1979–80 to 1986–87) and at Paakitsup Akuliarusersua (7 years: 1982–83 to the present). As the data sets cover different periods, it is difficult to compare ablation directly between the three sites. However, measured series at each site can be extended over the last 30 years (1961–90) by simulations using climatic data, and the extended data series can be compared. The pattern of calculated ablation variations at the three locations is remarkably similar with no sign of any trend towards increased ablation in recent years. There was generally low ablation from the mid-1970s to the mid-1980s that may explain the recent thickening of the ablation area which has been detected by satellite radar altimetry. Ablation varies substantially from year to year, e.g. with a standard deviation of the order of ±0.5 m water a −1 , and any future monitoring programme must detect trends of increasing ablation against this background of natural variations.
format Article in Journal/Newspaper
author Braithwaite, Roger J.
Olesen, Ole Β.
HøJmark Thomsen, Henrik
author_facet Braithwaite, Roger J.
Olesen, Ole Β.
HøJmark Thomsen, Henrik
author_sort Braithwaite, Roger J.
title Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
title_short Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
title_full Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
title_fullStr Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
title_full_unstemmed Calculated variations of annual ice ablation at the margin of the Greenland ice sheet, West Greenland, 1961–90
title_sort calculated variations of annual ice ablation at the margin of the greenland ice sheet, west greenland, 1961–90
publisher Cambridge University Press (CUP)
publishDate 1992
url http://dx.doi.org/10.1017/s0022143000003671
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003671
long_lat ENVELOPE(-49.500,-49.500,64.483,64.483)
geographic Greenland
Qamanârssûp Sermia
geographic_facet Greenland
Qamanârssûp Sermia
genre Greenland
Ice Sheet
Journal of Glaciology
genre_facet Greenland
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 38, issue 129, page 266-272
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000003671
container_title Journal of Glaciology
container_volume 38
container_issue 129
container_start_page 266
op_container_end_page 272
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