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Using dynamical downscaling to close the gap between global change scenarios and local permafrost dynamics
Martin Stendel
*
, Vladimir E. Romanovsky,
Jens H. Christensen
, Tatiana Sazonova
*
Corresponding author af dette arbejde
LUKKET: Geografi
26
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Alfabetisk
Earth and Planetary Sciences
General Circulation Model
100%
Active Layer
100%
Global Change Scenario
100%
Downscaling
100%
Climate Modeling
66%
Regional Climate
66%
Soil Temperature
33%
Soil Property
33%
Frozen Soil
33%
Vegetation Cover
33%
Conductive Heat Transfer
33%
Soil Structure
33%
Global Climate Change
33%
Vegetation
33%
Zonation
33%
Keyphrases
Global Change Scenarios
100%
Mean Annual Ground Temperature
50%
Permafrost Temperature
25%
Permafrost Modelling
25%
IPCC SRES Scenarios
25%
Surface Climate
25%
Soil Freezing
25%
Atmosphere-ocean General Circulation Model
25%
Heterogeneous Soil
25%
Grid Box
25%