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Sensitivity of active-layer freezing process to snow cover in Arctic Alaska
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High nitrate variability on an Alaskan permafrost hillslope dominated by alder s...
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Numerical modeling of permafrost dynamics in Alaska using a high spatial resolut...
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Invited perspective: What lies beneath a changing Arctic?
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Assessing volumetric change distributions and scaling relations of retrogressive...
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Modelling and mapping climate change impacts on permafrost at high spatial resol...
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The effect of changing sea ice on the physical vulnerability of Arctic coasts
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Discovery and characterization of submarine groundwater discharge in the Siberia...
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Soil moisture and hydrology projections of the permafrost region – a model inter...
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Top-of-permafrost ground ice indicated by remotely sensed late-season subsidence
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Macromolecular composition of terrestrial and marine organic matter in sediments...
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Thermokarst lake inception and development in syngenetic ice-wedge polygon terra...
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Consequences of permafrost degradation for Arctic infrastructure – bridging the...
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Improved ELMv1-ECA simulations of zero-curtain periods and cold-season CH4 and C...
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Dissolved organic carbon (DOC) in Arctic ground ice
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An estimate of ice wedge volume for a High Arctic polar desert environment, Fosh...
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Automatic monitoring of the effective thermal conductivity of snow in a low-Arct...
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Soil moisture and hydrology projections of the permafrost region – a model inter...
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Permafrost thawing exhibits a greater influence on bacterial richness and commun...
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Surface temperatures and their influence on the permafrost thermal regime in hig...
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S. Westermann
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J. Boike
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M. Langer
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B. M. Jones
5
D. Fortier
5
G. Grosse
5
Ö. Gustafsson
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A. C. A. Rudy
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C. J. Wilson
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E. E. Jafarov
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F. Bouchard
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F. Domine
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G. Krinner
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I. Gouttevin
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I. P. Semiletov
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L. Cai
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L. Liu
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M. Fritz
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M. Paquette
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P. P. Overduin
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S. V. Kokelj
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geo
envir
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Herschel Island Territorial Park
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Hudson
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Hudson Bay
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Khaya
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English
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The Cryosphere
permafrost
Ice
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Alaska
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Active layer thickness
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wedge*
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Climate change
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laptev
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north slope
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lena river
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albedo
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