The work upon which this report is based was made possible by a cooperative aid agreement between the U.S. Forest Service, Institute of Northern Forestry, Fairbanks, Alaska, and the Institute of Water Resources, University of Alaska. Contributions to this study were also made by the University of California at Davis and Ohio State University. The collection of winter data on pore pressures was made possible by a separate grant by the Office of Water Research and Technology (project A-053 ALAS)
Dissertation (Ph.D.) University of Alaska Fairbanks, 1990The heat and mass transfer processes which ...
[1] The impact to the permafrost during and after wildfire was studied using 11 boreal forest fire s...
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. How...
Completion Report for U. S. Forest Service Institute of Northern Forestry Cooperative Agreement ...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1985Hydrologic research of processes related to...
The movement of soil moisture through cold regions soils is an active process that continues throug...
A physical model of the soil thermal regime in a permafrost terrain has been developed and validated...
Soil temperature and moisture are important factors that control many ecosystem processes. However, ...
Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of Am...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
<p><b>Table 1.</b> Thermal properties used in ground temperature simulations for the...
The pathways of soil water in cold climates are influenced, in addition to the normal forces, by the...
Dissertation (Ph.D.) University of Alaska Fairbanks, 2001A Soil Thermal Model (STM) with the capabil...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The thermal conductivity of the thin seasonally freezing and thawing soil layer in permafrost landsc...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1990The heat and mass transfer processes which ...
[1] The impact to the permafrost during and after wildfire was studied using 11 boreal forest fire s...
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. How...
Completion Report for U. S. Forest Service Institute of Northern Forestry Cooperative Agreement ...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1985Hydrologic research of processes related to...
The movement of soil moisture through cold regions soils is an active process that continues throug...
A physical model of the soil thermal regime in a permafrost terrain has been developed and validated...
Soil temperature and moisture are important factors that control many ecosystem processes. However, ...
Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of Am...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
<p><b>Table 1.</b> Thermal properties used in ground temperature simulations for the...
The pathways of soil water in cold climates are influenced, in addition to the normal forces, by the...
Dissertation (Ph.D.) University of Alaska Fairbanks, 2001A Soil Thermal Model (STM) with the capabil...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The thermal conductivity of the thin seasonally freezing and thawing soil layer in permafrost landsc...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1990The heat and mass transfer processes which ...
[1] The impact to the permafrost during and after wildfire was studied using 11 boreal forest fire s...
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. How...