Permafrost response to climate change: Linking field observation with numerical simulation

International audience The Scotty Creek basin (152 km 2) is located in the Northwest Territories, Canada, within the peat-covered discontinuous permafrost zone with a high density of wetlands. The extensive peat layer (up to 3-4 m thick) is underlain by generally clay-rich glacial sediments. The lan...

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Bibliographic Details
Main Authors: Hayashi, Masaki, Rivière, Agnès, Quinton, William, Mckenzie, Jeffrey, Voss, Clifford
Other Authors: University of Calgary, Centre de Géosciences (GEOSCIENCES), MINES ParisTech - École nationale supérieure des mines de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), McGill University = Université McGill Montréal, Canada, Wilfrid Laurier University (WLU), Department of Earth and Planetary Sciences Montréal (EPS), United States Geological Survey Reston (USGS), American Geophysical Union, AGU
Format: Conference Object
Language:English
Published: HAL CCSD 2013
Subjects:
Ice
Online Access:https://hal.archives-ouvertes.fr/hal-01396677
https://hal.archives-ouvertes.fr/hal-01396677/document
https://hal.archives-ouvertes.fr/hal-01396677/file/AGU2013_Riviere_etal.pdf