Increased precipitation drives mega slump development and destabilization of ice-rich permafrost terrain, northwestern Canada

Author:

Kokelj S.V.,Tunnicliffe J.,Lacelle D.,Lantz T.C.,Chin K.S.,Fraser R.

Funder

NWT Cumulative Impact Monitoring Program

Aurora Research Institute

NWT Geoscience Office

Government of the Northwest Territories

Natural Sciences and Engineering Research

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference48 articles.

1. Depositional history of North Taymyr ice-marginal zone, Siberia – a landsystem approach;Alexanderson;J. Quat. Sci.,2002

2. Pleistocene permafrost of West Siberia as a deformable glacier bed;Astakhov;Permafr. Periglac.,1996

3. Les glissements retrogressifs de fonte de la riviere Willow, Territoires du Nord-Ouest, Canada: caractéristiques sedimentologiques, distribution spatiale et temporelle;Bjornson,2003

4. Mapping the activity and evolution of retrogressive thaw slumps by Tasseled Cap trend analysis of a Landsat satellite image stack;Brooker;Permafr. Periglac.,2014

5. The permafrost and environment of the Mackenzie Delta area;Burn;Permafr. Periglac.,2009

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