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, Ulf; Navarro Valero, Francisco Jose; Bañón, Manolo; Lapazaran Izargain, Javier Jesús y Otero García, Jaime (2012). Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica. "The Cryosphere", v. 6 (n. 3); pp. 539-552. ISSN 1994-0416. https://doi.org/10.5194/tc-6-539-2012.

Descripción

Título: Sensitivity of a distributed temperature-radiation index melt model based on AWS observations and surface energy balance fluxes, Hurd Peninsula glaciers, Livingston Island, Antarctica
Autor/es:
  • Jonsell, Ulf
  • Navarro Valero, Francisco Jose
  • Bañón, Manolo
  • Lapazaran Izargain, Javier Jesús
  • Otero García, Jaime
Tipo de Documento: Artículo
Título de Revista/Publicación: The Cryosphere
Fecha: 2012
Volumen: 6
Materias:
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

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Resumen

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.

Más información

ID de Registro: 14171
Identificador DC: http://oa.upm.es/14171/
Identificador OAI: oai:oa.upm.es:14171
Identificador DOI: 10.5194/tc-6-539-2012
URL Oficial: http://www.the-cryosphere.net/6/issue3.html
Depositado por: Memoria Investigacion
Depositado el: 19 Dic 2012 08:40
Ultima Modificación: 21 Abr 2016 13:41
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