The effect of the environmental factors on permafrost has been studied. Three main factors, namely: the air temperature, the accumulated amounts of solid precipitation, and the vegetation dynamics, which govern the state of the frozen ground at time scales from few years to decades, are identified. The quantitative evaluation of their effect on the soil temperature variations and the construction of the conceptual model for predicting permafrost dynamics under the current and expected for the future climatic conditions, which accounts for the cumulative effect of major governing factors, have been carried out
The heat exchange between the ground and the atmosphere in the North is extremely important in the f...
Permafrost in the subarctic exists in close and complex interrelation with many climatic and terrain...
A realistic simulation of snow cover and its thermal properties are important for accurate modelling...
This translation is the seventh arranged by the Permafrost Subcommittee of the Associate Committee o...
The current climate change in Russia is characterized as continuing warming. There is an increase of...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1996This thesis represents a collection of pape...
The permafrost regions occupy about 25 % of the Northern Hemisphere’s terrestrial surface, and more ...
This translation is the ninth arranged by the Permafrost Subcommittee of the Associate Committee on ...
In the framework of the study, we investigate spatiotemporal variability of the main climatic variab...
Boreal forests exert a strong influence on the permafrost dynamics protecting the landscapes under c...
Climate warming in the Russian Arctic over the past 40 years shows a variety of patterns at differen...
One terrain feature of great significance to the extent, thickness and thermal regime of permafrost ...
Permafrost is the ground that remains at or below 0. °C for 2 years or more, and is therefore a geol...
This paper presents the results of long-term temperature monitoring at the Yakutsk and Zeleny Lug st...
Soil temperature variation is one of the governing factors of mechanical properties of frozen soils ...
The heat exchange between the ground and the atmosphere in the North is extremely important in the f...
Permafrost in the subarctic exists in close and complex interrelation with many climatic and terrain...
A realistic simulation of snow cover and its thermal properties are important for accurate modelling...
This translation is the seventh arranged by the Permafrost Subcommittee of the Associate Committee o...
The current climate change in Russia is characterized as continuing warming. There is an increase of...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1996This thesis represents a collection of pape...
The permafrost regions occupy about 25 % of the Northern Hemisphere’s terrestrial surface, and more ...
This translation is the ninth arranged by the Permafrost Subcommittee of the Associate Committee on ...
In the framework of the study, we investigate spatiotemporal variability of the main climatic variab...
Boreal forests exert a strong influence on the permafrost dynamics protecting the landscapes under c...
Climate warming in the Russian Arctic over the past 40 years shows a variety of patterns at differen...
One terrain feature of great significance to the extent, thickness and thermal regime of permafrost ...
Permafrost is the ground that remains at or below 0. °C for 2 years or more, and is therefore a geol...
This paper presents the results of long-term temperature monitoring at the Yakutsk and Zeleny Lug st...
Soil temperature variation is one of the governing factors of mechanical properties of frozen soils ...
The heat exchange between the ground and the atmosphere in the North is extremely important in the f...
Permafrost in the subarctic exists in close and complex interrelation with many climatic and terrain...
A realistic simulation of snow cover and its thermal properties are important for accurate modelling...