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A comparison of empirical and physically based glacier surface melt models for long-term simulations of glacier response

Author
GABBI, Jeannette1 ; CARENZO, Marco2 ; PELLLCCIOTTI, Francesca2 ; BAUDER, Andreas1 ; FUNK, Martin1
[1] Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zürich, Switzerland
[2] Institute of Environmental Engineering, ETH Zürich, Zürich, Switzerland
Source

Journal of Glaciology. 2014, Vol 60, Num 224, pp 1140-1154, 15 p ; ref : 1 p.1/4

CODEN
JOGLAO
ISSN
0022-1430
Scientific domain
Glaciology; Geology; Geophysics; Climatology, meteorology
Publisher
International Glaciological Society, Cambridge
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Bilan glaciaire Bilan masse Bilan énergie Etude comparative Evaluation performance Fusion surface Glacier vallée Long terme Modélisation Alpes Centrales Suisse Valais Alpes Suisses Alpes Europe Centrale Europe Suisse
Keyword (en)
Glacier balance mass balance energy balance Comparative study Performance evaluation Surface melting Valley glaciar Long term Modeling Central Swiss Alps Valais Switzerland Swiss Alps Alps Central Europe Europe Switzerland
Keyword (es)
Balance glaciar Balance masa Estudio comparativo Evaluación prestación Fusión superficie Glaciar valle Largo plazo Modelización Alpes Centrales Suizos Alpes Suizos Alpes Europa central Europa Suiza
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02C Snow. Ice. Glaciers

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
29109281

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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