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Plausibility of a subglacial lake under Amundsenisen Icefield (Svalbard): spatially variable water content and sensitivity to thermal effect of snow and firn layers
Cita
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.
En: "European Geosciences Union General Assembly 2013", 07/04/2013 - 12/04/2013, Vienna, Austria. p. 1.
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.
En: "European Geosciences Union General Assembly 2013", 07/04/2013 - 12/04/2013, Vienna, Austria. p. 1.
Descripción
| Título: | 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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| Autor/es: |
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| Tipo de Documento: | Ponencia en Congreso o Jornada (Otro) |
| Título del Evento: | European Geosciences Union General Assembly 2013 |
| Fechas del Evento: | 07/04/2013 - 12/04/2013 |
| Lugar del Evento: | Vienna, Austria |
| Título del Libro: | Geophysical Research Abstracts |
| Fecha: | 2013 |
| Volumen: | 15 |
| Materias: | |
| ODS: | |
| Escuela: | E.T.S.I. Telecomunicación (UPM) |
| Departamento: | Matemática Aplicada a las Tecnologías de la Información [hasta 2014] |
| Licencias Creative Commons: | Reconocimiento - Sin obra derivada - No comercial |
Resumen
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).
Más información
| ID de Registro: | 29660 |
|---|---|
| Identificador DC: | https://oa.upm.es/29660/ |
| Identificador OAI: | oai:oa.upm.es:29660 |
| Depositado por: | Memoria Investigacion |
| Depositado el: | 12 Jul 2014 08:53 |
| Ultima Modificación: | 13 Abr 2023 18:13 |
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