Descripción
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It is known that the Amundsenisen Icefield in Southern Spitzbergen (Svalbard achipelago) is temperate with an upper layer of snow and firn. It is an accumulation area and, though ice/water mass balance is clearly subject to time evolution, observation data on the long-term elevation changes over the past 40 years (Nuth et al., 2010) allow to assume constant icefield surface. Within our study of the plausibility of a subglacial lake (Glowacki et al., 2007), here, we focus on the sensitivity of the system to the thermal effect of the firn and snow layers. | |
Internacional
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Si |
Nombre congreso
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International Arctic Science Committee - Network on Arctic Glaciology, 2013 Annual Meeting |
Tipo de participación
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960 |
Lugar del congreso
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Obergurgl, Austria |
Revisores
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Si |
ISBN o ISSN
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978-90-393-6003-3 |
DOI
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Fecha inicio congreso
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26/02/2013 |
Fecha fin congreso
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28/02/2013 |
Desde la página
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27 |
Hasta la página
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27 |
Título de las actas
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IASC Workshop on the dynamics and mass budget of Arctic glaciers - Abstracts and program. IASC Network on Arctic Glaciology |