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Par Collection Par Auteur- NELSON, F.E., (Editeur scientifique) (3)
- CHESTNYKH, O. (1)
- KUTNY, L. (1)
- MALKOVA, G. (1)
- NIXON, F.M. (1)
- ZAMOLODCHIKOV, D. (1)
- ZHANG, T. (1)
- MAZHITOVA, G. (1)
- OELKE, C. (1)
- TARNOCAI, C. (1)
- 2004 (3)
- Active layer ; Air temperature ; Arctic Region ; Cold area ; Modelling ; Permafrost ; Soil temperature ; Temperature ; Time series ; Years 1980-89 ; Years 1990-99 (1)
- Active layer ; Arctic Region ; Canada ; Cold area ; Ground survey ; Microclimate ; Northwest Territories ; Permafrost ; Soil properties ; Soil temperature ; Thawing ; Vegetation (1)
- Active layer ; Arctic Region ; Cold area ; Model ; Permafrost ; Seasonal variability ; Spatial variation ; Thawing (1)
- Années 1980 ; Années 1990 ; Arctique ; Modélisation ; Mollisol ; Pergélisol ; Série chronologique ; Température ; Température de l'air ; Température du sol ; Zone froide (1)
- Arctique ; Canada ; Dégel ; Mesure de terrain ; Microclimat ; Mollisol ; Northwest Territories ; Pergélisol ; Propriétés du sol ; Température du sol ; Végétation ; Zone froide (1)
- Arctique ; Dégel ; Modèle ; Mollisol ; Pergélisol ; Variabilité saisonnière ; Variation spatiale ; Zone froide (1)
- Circumpolar-Active-Layer-Monitoring (CALM) Workshop : special issue (3)
- A model study of Circum-Arctic soil temperatures (1)
- Active-layer spatial and temporal variability at European Russian Circum-Active-Layer-Monitoring (CALM) sites (1)
- Circumpolar-Active-Layer-Monitoring (CALM) sites in the Mackenzie Valley, Northwestern Canada (1)
- Thirteen sites have been selected. In this paper the data on active-layer depth and surface subsidence will be evaluated and changes within broad ecoclimatic zones will be discussed.
- 2004
- This paper analyses data from those European Russian CALM sites, primarily with regard to the interannual and spatial variability of the active layer. The effects of organic-layer thickness on thaw depth are shown to change during the warm season.
- 2004
- A one-dimensional heat transfer model with phase change is applied to the entire Arctic terrestrial drainage area. The main forcing parameters are reanalysed surface air temperature that was topography-enhanced, and snow depth, derived from passive
- 2004