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Bucchignani, Edoardo, Mansutti, Daniela, Navarro Valero, Francisco José ORCID: https://orcid.org/0000-0002-5147-0067, Otero García, Jaime
ORCID: https://orcid.org/0000-0002-3518-7763 and Glowacki, Piotr
(2013).
Plausibility of a subglacial lake under Amundsenisen Icefield (Svalbard): spatially variable water content and sensitivity to thermal effect of snow and firn layers.
In: "European Geosciences Union General Assembly 2013", 07/04/2013 - 12/04/2013, Vienna, Austria. p. 1.
Title: | Plausibility of a subglacial lake under Amundsenisen Icefield (Svalbard): spatially variable water content and sensitivity to thermal effect of snow and firn layers |
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Author/s: |
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Item Type: | Presentation at Congress or Conference (Other) |
Event Title: | European Geosciences Union General Assembly 2013 |
Event Dates: | 07/04/2013 - 12/04/2013 |
Event Location: | Vienna, Austria |
Title of Book: | Geophysical Research Abstracts |
Date: | 2013 |
Volume: | 15 |
Subjects: | |
Faculty: | E.T.S.I. Telecomunicación (UPM) |
Department: | Matemática Aplicada a las Tecnologías de la Información [hasta 2014] |
Creative Commons Licenses: | Recognition - No derivative works - Non commercial |
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Within our study of the plausibility of a subglacial lake under the Amundsenisen Icefield in Southern Spitzbergen, Svalbard achipelago (Glowacki et al., 2007), here we focus on the sensitivity of the system to the thermal effect of the firn and snow layers. Rough heat balance analysis shows that the firn layer plays an important role by driving the heat release to the atmosphere, so that its influence on the ice-water phase transition cannot be neglected (Bucchignani et al., 2012).
Item ID: | 29660 |
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DC Identifier: | https://oa.upm.es/29660/ |
OAI Identifier: | oai:oa.upm.es:29660 |
Deposited by: | Memoria Investigacion |
Deposited on: | 12 Jul 2014 08:53 |
Last Modified: | 13 Apr 2023 18:13 |