Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica
We use an automatic weather station and surface mass balance dataset spanning four melt seasons collected on Hurd Peninsula Glaciers, South Shetland Islands, to investigate the point surface energy balance, to determine the absolute and relative contribution of the various energy fluxes acting on th...
Published in: | The Cryosphere |
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Language: | English |
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European Geosciences Union
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Online Access: | https://hdl.handle.net/20.500.11765/1508 |
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ftaemet:oai:repositorio.aemet.es:20.500.11765/1508 2024-06-23T07:47:48+00:00 Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica Jonsell, U. Y. Navarro, Francisco J. Bañón García, Manuel Lapazaran, Javier Jesús Otero, Jaime 2012 application/pdf https://hdl.handle.net/20.500.11765/1508 eng eng European Geosciences Union https://dx.doi.org/10.5194/tc-6-539-2012 Cryosphere. 2012, 6(3), p. 539-552 1994-0416 1994-0424 http://hdl.handle.net/20.500.11765/1508 info:eu-repo/semantics/openAccess Temperature-radiation index Automatic weather station Energy fluxes Glaciers info:eu-repo/semantics/article 2012 ftaemet https://doi.org/20.500.11765/150810.5194/tc-6-539-2012 2024-06-03T14:17:56Z We use an automatic weather station and surface mass balance dataset spanning four melt seasons collected on Hurd Peninsula Glaciers, South Shetland Islands, to investigate the point surface energy balance, to determine the absolute and relative contribution of the various energy fluxes acting on the glacier surface and to estimate the sensitivity of melt to ambient temperature changes. Long-wave incoming radiation is the main energy source for melt, while short-wave radiation is the most important flux controlling the variation of both seasonal and daily mean surface energy balance. Short-wave and long-wave radiation fluxes do, in general, balance each other, resulting in a high correspondence between daily mean net radiation flux and available melt energy flux. We calibrate a distributed melt model driven by air temperature and an expression for the incoming short-wave radiation. The model is calibrated with the data from one of the melt seasons and validated with the data of the three remaining seasons. The model results deviate at most 140 mm w.e. from the corresponding observations using the glaciological method. The model is very sensitive to changes in ambient temperature: a 0.5 °C increase results in 56 % higher melt rates. This research was funded by projects CGL2005-05483 and CTM2008-05878/ANT from the Spanish Ministry of Science and Innovation. Article in Journal/Newspaper Antarc* Antarctica Livingston Island South Shetland Islands ARCIMÍS (Archivo Climatológico y Meteorológico Institucional - AEMET, Agencia Estatal de Meteorología) South Shetland Islands Livingston Island ENVELOPE(-60.500,-60.500,-62.600,-62.600) Hurd ENVELOPE(-60.366,-60.366,-62.682,-62.682) Hurd peninsula ENVELOPE(-60.366,-60.366,-62.676,-62.676) The Cryosphere 6 3 539 552 |
institution |
Open Polar |
collection |
ARCIMÍS (Archivo Climatológico y Meteorológico Institucional - AEMET, Agencia Estatal de Meteorología) |
op_collection_id |
ftaemet |
language |
English |
topic |
Temperature-radiation index Automatic weather station Energy fluxes Glaciers |
spellingShingle |
Temperature-radiation index Automatic weather station Energy fluxes Glaciers Jonsell, U. Y. Navarro, Francisco J. Bañón García, Manuel Lapazaran, Javier Jesús Otero, Jaime Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
topic_facet |
Temperature-radiation index Automatic weather station Energy fluxes Glaciers |
description |
We use an automatic weather station and surface mass balance dataset spanning four melt seasons collected on Hurd Peninsula Glaciers, South Shetland Islands, to investigate the point surface energy balance, to determine the absolute and relative contribution of the various energy fluxes acting on the glacier surface and to estimate the sensitivity of melt to ambient temperature changes. Long-wave incoming radiation is the main energy source for melt, while short-wave radiation is the most important flux controlling the variation of both seasonal and daily mean surface energy balance. Short-wave and long-wave radiation fluxes do, in general, balance each other, resulting in a high correspondence between daily mean net radiation flux and available melt energy flux. We calibrate a distributed melt model driven by air temperature and an expression for the incoming short-wave radiation. The model is calibrated with the data from one of the melt seasons and validated with the data of the three remaining seasons. The model results deviate at most 140 mm w.e. from the corresponding observations using the glaciological method. The model is very sensitive to changes in ambient temperature: a 0.5 °C increase results in 56 % higher melt rates. This research was funded by projects CGL2005-05483 and CTM2008-05878/ANT from the Spanish Ministry of Science and Innovation. |
format |
Article in Journal/Newspaper |
author |
Jonsell, U. Y. Navarro, Francisco J. Bañón García, Manuel Lapazaran, Javier Jesús Otero, Jaime |
author_facet |
Jonsell, U. Y. Navarro, Francisco J. Bañón García, Manuel Lapazaran, Javier Jesús Otero, Jaime |
author_sort |
Jonsell, U. Y. |
title |
Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
title_short |
Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
title_full |
Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
title_fullStr |
Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
title_full_unstemmed |
Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica |
title_sort |
sensitivity of a distributed temperature-radiation index melt model based on aws observations and surface energy balance fluxes, hurd peninsula glaciers, livingston island, antarctica |
publisher |
European Geosciences Union |
publishDate |
2012 |
url |
https://hdl.handle.net/20.500.11765/1508 |
long_lat |
ENVELOPE(-60.500,-60.500,-62.600,-62.600) ENVELOPE(-60.366,-60.366,-62.682,-62.682) ENVELOPE(-60.366,-60.366,-62.676,-62.676) |
geographic |
South Shetland Islands Livingston Island Hurd Hurd peninsula |
geographic_facet |
South Shetland Islands Livingston Island Hurd Hurd peninsula |
genre |
Antarc* Antarctica Livingston Island South Shetland Islands |
genre_facet |
Antarc* Antarctica Livingston Island South Shetland Islands |
op_relation |
https://dx.doi.org/10.5194/tc-6-539-2012 Cryosphere. 2012, 6(3), p. 539-552 1994-0416 1994-0424 http://hdl.handle.net/20.500.11765/1508 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/20.500.11765/150810.5194/tc-6-539-2012 |
container_title |
The Cryosphere |
container_volume |
6 |
container_issue |
3 |
container_start_page |
539 |
op_container_end_page |
552 |
_version_ |
1802637958800474112 |