The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet

We present the seasonal cycle and interannual variability of the surface energy balance (SEB) in the ablation zone of the west Greenland ice sheet, using seven years (September 2003–August 2010) of hourly observations from three automatic weather stations (AWS). The AWS are situated along the 67° N...

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Published in:The Cryosphere
Main Authors: M. R. van den Broeke, C. J. P. P. Smeets, R. S. W. van de Wal
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-5-377-2011
http://www.the-cryosphere.net/5/377/2011/tc-5-377-2011.pdf
https://doaj.org/article/d83bbb3ebb3d492ca1b1b2df7f56b825
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:d83bbb3ebb3d492ca1b1b2df7f56b825 2023-05-15T16:28:21+02:00 The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet M. R. van den Broeke C. J. P. P. Smeets R. S. W. van de Wal 2011-05-01 https://doi.org/10.5194/tc-5-377-2011 http://www.the-cryosphere.net/5/377/2011/tc-5-377-2011.pdf https://doaj.org/article/d83bbb3ebb3d492ca1b1b2df7f56b825 en eng Copernicus Publications doi:10.5194/tc-5-377-2011 1994-0416 1994-0424 http://www.the-cryosphere.net/5/377/2011/tc-5-377-2011.pdf https://doaj.org/article/d83bbb3ebb3d492ca1b1b2df7f56b825 undefined The Cryosphere, Vol 5, Iss 2, Pp 377-390 (2011) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.5194/tc-5-377-2011 2023-01-22T17:57:10Z We present the seasonal cycle and interannual variability of the surface energy balance (SEB) in the ablation zone of the west Greenland ice sheet, using seven years (September 2003–August 2010) of hourly observations from three automatic weather stations (AWS). The AWS are situated along the 67° N latitude circle at elevations of 490 m a.s.l. (S5), 1020 m a.s.l. (S6) and 1520 m a.s.l. (S9) at distances of 6, 38 and 88 km from the ice sheet margin. The hourly AWS data are fed into a model that calculates all SEB components and melt rate; the model allows for shortwave radiation penetration in ice and time-varying surface momentum roughness. Snow depth is prescribed from albedo and sonic height ranger observations. Modelled and observed surface temperatures for non-melting conditions agree very well, with RMSE's of 0.97–1.26 K. Modelled and observed ice melt rates at the two lowest sites also show very good agreement, both for total cumulative and 10-day cumulated amounts. Melt frequencies and melt rates at the AWS sites are discussed. Although absorbed shortwave radiation is the most important energy source for melt at all three sites, interannual melt variability at the lowest site is driven mainly by variability in the turbulent flux of sensible heat. This is explained by the quasi-constant summer albedo in the lower ablation zone, limiting the influence of the melt-albedo feedback, and the proximity of the snow free tundra, which heats up considerably in summer. Article in Journal/Newspaper Greenland Ice Sheet The Cryosphere Tundra Unknown Greenland The Cryosphere 5 2 377 390
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
M. R. van den Broeke
C. J. P. P. Smeets
R. S. W. van de Wal
The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
topic_facet geo
envir
description We present the seasonal cycle and interannual variability of the surface energy balance (SEB) in the ablation zone of the west Greenland ice sheet, using seven years (September 2003–August 2010) of hourly observations from three automatic weather stations (AWS). The AWS are situated along the 67° N latitude circle at elevations of 490 m a.s.l. (S5), 1020 m a.s.l. (S6) and 1520 m a.s.l. (S9) at distances of 6, 38 and 88 km from the ice sheet margin. The hourly AWS data are fed into a model that calculates all SEB components and melt rate; the model allows for shortwave radiation penetration in ice and time-varying surface momentum roughness. Snow depth is prescribed from albedo and sonic height ranger observations. Modelled and observed surface temperatures for non-melting conditions agree very well, with RMSE's of 0.97–1.26 K. Modelled and observed ice melt rates at the two lowest sites also show very good agreement, both for total cumulative and 10-day cumulated amounts. Melt frequencies and melt rates at the AWS sites are discussed. Although absorbed shortwave radiation is the most important energy source for melt at all three sites, interannual melt variability at the lowest site is driven mainly by variability in the turbulent flux of sensible heat. This is explained by the quasi-constant summer albedo in the lower ablation zone, limiting the influence of the melt-albedo feedback, and the proximity of the snow free tundra, which heats up considerably in summer.
format Article in Journal/Newspaper
author M. R. van den Broeke
C. J. P. P. Smeets
R. S. W. van de Wal
author_facet M. R. van den Broeke
C. J. P. P. Smeets
R. S. W. van de Wal
author_sort M. R. van den Broeke
title The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
title_short The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
title_full The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
title_fullStr The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
title_full_unstemmed The seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west Greenland ice sheet
title_sort seasonal cycle and interannual variability of surface energy balance and melt in the ablation zone of the west greenland ice sheet
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/tc-5-377-2011
http://www.the-cryosphere.net/5/377/2011/tc-5-377-2011.pdf
https://doaj.org/article/d83bbb3ebb3d492ca1b1b2df7f56b825
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
The Cryosphere
Tundra
genre_facet Greenland
Ice Sheet
The Cryosphere
Tundra
op_source The Cryosphere, Vol 5, Iss 2, Pp 377-390 (2011)
op_relation doi:10.5194/tc-5-377-2011
1994-0416
1994-0424
http://www.the-cryosphere.net/5/377/2011/tc-5-377-2011.pdf
https://doaj.org/article/d83bbb3ebb3d492ca1b1b2df7f56b825
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op_doi https://doi.org/10.5194/tc-5-377-2011
container_title The Cryosphere
container_volume 5
container_issue 2
container_start_page 377
op_container_end_page 390
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