Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú

International audience Sublimation plays a decisive role in the surface energy and mass balance of tropical glaciers. During the dry season (May-September) low specific humidity and high surface roughness favour the direct transition from ice to vapour and drastically reduce the energy available for...

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Published in:The Cryosphere
Main Authors: Winkler, M., Juen, I., Mölg, T., Wagnon, Patrick, Gómez, J., Kaser, G.
Other Authors: Tropical Glaciology Group, Faculty of Geo- and Atmospheric Sciences, University of Innsbruck, Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Unidad de Glaciología y Recursos Hídricos, Austrian Science Foundation (FWF) grants number P16113-N06 and P20089-N10.
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-00421261
https://hal-insu.archives-ouvertes.fr/insu-00421261/document
https://hal-insu.archives-ouvertes.fr/insu-00421261/file/tc-3-21-2009.pdf
https://doi.org/10.5194/tc-3-21-2009
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record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Winkler, M.
Juen, I.
Mölg, T.
Wagnon, Patrick
Gómez, J.
Kaser, G.
Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
topic_facet [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience Sublimation plays a decisive role in the surface energy and mass balance of tropical glaciers. During the dry season (May-September) low specific humidity and high surface roughness favour the direct transition from ice to vapour and drastically reduce the energy available for melting. However, field measurements are scarce and little is known about the performance of sublimation parameterisations in glacier mass balance and runoff models. During 15 days in August 2005 sublimation was measured on the tongue of Glaciar Artesonraju (8°58' S, 77°38' W) in the Cordillera Blanca, Perú, using simple lysimeters. Indicating a strong dependence on surface roughness, daily totals of sublimation range from 1-3 kg m−2 for smooth to 2-5 kg m−2 for rough conditions. (The 15-day means at that time of wind speed and specific humidity were 4.3 m s−1 and 3.8 g kg−1, respectively.) Measured sublimation was related to characteristic surface roughness lengths for momentum (zm) and for the scalar quantities of temperature and water vapour (zs), using a process-based mass balance model. Input data were provided by automatic weather stations, situated on the glacier tongue at 4750 m a.s.l. and 4810 m a.s.l., respectively. Under smooth conditions the combination zm=2.0 mm and zs=1.0 mm appeared to be most appropriate, for rough conditions zm=20.0 mm and zs=10.0 mm fitted best. Extending the sublimation record from April 2004 to December 2005 with the process-based model confirms, that sublimation shows a clear seasonality. 60-90% of the energy available for ablation is consumed by sublimation in the dry season, but only 10-15% in the wet season (October-April). The findings are finally used to evaluate the parameterisation of sublimation in the lower-complexity mass balance model ITGG, which has the advantage of requiring precipitation and air temperature as only input data. It turns out that the implementation of mean wind speed is a possible improvement for the representation of sublimation in the ITGG model.
author2 Tropical Glaciology Group, Faculty of Geo- and Atmospheric Sciences
University of Innsbruck
Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
Unidad de Glaciología y Recursos Hídricos
Austrian Science Foundation (FWF) grants number P16113-N06 and P20089-N10.
format Article in Journal/Newspaper
author Winkler, M.
Juen, I.
Mölg, T.
Wagnon, Patrick
Gómez, J.
Kaser, G.
author_facet Winkler, M.
Juen, I.
Mölg, T.
Wagnon, Patrick
Gómez, J.
Kaser, G.
author_sort Winkler, M.
title Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
title_short Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
title_full Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
title_fullStr Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
title_full_unstemmed Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú
title_sort measured and modelled sublimation on the tropical glaciar artesonraju, perú
publisher HAL CCSD
publishDate 2009
url https://hal-insu.archives-ouvertes.fr/insu-00421261
https://hal-insu.archives-ouvertes.fr/insu-00421261/document
https://hal-insu.archives-ouvertes.fr/insu-00421261/file/tc-3-21-2009.pdf
https://doi.org/10.5194/tc-3-21-2009
genre The Cryosphere
genre_facet The Cryosphere
op_source ISSN: 1994-0424
EISSN: 1994-0416
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https://hal-insu.archives-ouvertes.fr/insu-00421261
The Cryosphere, Copernicus 2009, 3 (1), pp.21-30. ⟨10.5194/tc-3-21-2009⟩
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spelling ftccsdartic:oai:HAL:insu-00421261v1 2023-05-15T18:32:16+02:00 Measured and modelled sublimation on the tropical Glaciar Artesonraju, Perú Winkler, M. Juen, I. Mölg, T. Wagnon, Patrick Gómez, J. Kaser, G. Tropical Glaciology Group, Faculty of Geo- and Atmospheric Sciences University of Innsbruck Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Unidad de Glaciología y Recursos Hídricos Austrian Science Foundation (FWF) grants number P16113-N06 and P20089-N10. 2009-02-09 https://hal-insu.archives-ouvertes.fr/insu-00421261 https://hal-insu.archives-ouvertes.fr/insu-00421261/document https://hal-insu.archives-ouvertes.fr/insu-00421261/file/tc-3-21-2009.pdf https://doi.org/10.5194/tc-3-21-2009 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-3-21-2009 insu-00421261 https://hal-insu.archives-ouvertes.fr/insu-00421261 https://hal-insu.archives-ouvertes.fr/insu-00421261/document https://hal-insu.archives-ouvertes.fr/insu-00421261/file/tc-3-21-2009.pdf doi:10.5194/tc-3-21-2009 info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal-insu.archives-ouvertes.fr/insu-00421261 The Cryosphere, Copernicus 2009, 3 (1), pp.21-30. ⟨10.5194/tc-3-21-2009⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2009 ftccsdartic https://doi.org/10.5194/tc-3-21-2009 2021-10-24T19:33:18Z International audience Sublimation plays a decisive role in the surface energy and mass balance of tropical glaciers. During the dry season (May-September) low specific humidity and high surface roughness favour the direct transition from ice to vapour and drastically reduce the energy available for melting. However, field measurements are scarce and little is known about the performance of sublimation parameterisations in glacier mass balance and runoff models. During 15 days in August 2005 sublimation was measured on the tongue of Glaciar Artesonraju (8°58' S, 77°38' W) in the Cordillera Blanca, Perú, using simple lysimeters. Indicating a strong dependence on surface roughness, daily totals of sublimation range from 1-3 kg m−2 for smooth to 2-5 kg m−2 for rough conditions. (The 15-day means at that time of wind speed and specific humidity were 4.3 m s−1 and 3.8 g kg−1, respectively.) Measured sublimation was related to characteristic surface roughness lengths for momentum (zm) and for the scalar quantities of temperature and water vapour (zs), using a process-based mass balance model. Input data were provided by automatic weather stations, situated on the glacier tongue at 4750 m a.s.l. and 4810 m a.s.l., respectively. Under smooth conditions the combination zm=2.0 mm and zs=1.0 mm appeared to be most appropriate, for rough conditions zm=20.0 mm and zs=10.0 mm fitted best. Extending the sublimation record from April 2004 to December 2005 with the process-based model confirms, that sublimation shows a clear seasonality. 60-90% of the energy available for ablation is consumed by sublimation in the dry season, but only 10-15% in the wet season (October-April). The findings are finally used to evaluate the parameterisation of sublimation in the lower-complexity mass balance model ITGG, which has the advantage of requiring precipitation and air temperature as only input data. It turns out that the implementation of mean wind speed is a possible improvement for the representation of sublimation in the ITGG model. Article in Journal/Newspaper The Cryosphere Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) The Cryosphere 3 1 21 30