The mean annual temperature at the top of permafrost, the TTOP model, and the effect of unfrozen water

Permafrost and Periglacial Processes

Volumn 13, Issue 2, 2002, Pages 137-143

  Riseborough, D W ^a  

^a CARLETON UNIVERSITY   (Canada)

Author keywords

Modelling; Permafrost; Soil temperature; Soil thermal properties; Unfrozen water

Indexed keywords

MODELING; PERMAFROST; SOIL TEMPERATURE; THERMAL CONDUCTIVITY; WATER CONTENT;

EID: 0036306570     PISSN: 10456740     EISSN: None     Source Type: Journal    
DOI: 10.1002/ppp.418     Document Type: Article

References (22)

1. Predicting unfrozen water contents in frozen soils from surface area measurements
2. The influence of snow cover on the ground thermal regime
3. A model-based map of ground temperatures for the permafrost regions of Canada
4. The importance of water migration in the measurement of conductivity of unsaturated frozen soils
5. Theory of n-factors
6. Thermal conductivity of frozen soils
7. Soil latent heat as a filter of the climate signal in permafrost
8. Modelling permafrost response to climate change and climate variability
9. Exploring the limits of permafrost
10. Determination of the thermal properties of frozen soils
11. Interannual variations of the thermal regime of the active layer and near surface permafrost in Northern Alaska
12. Effects of unfrozen water on heat and mass transport processes in the active layer and permafrost
13. The sensitivity of thermal predictions to assumptions in thermal properties
14. Permafrost monitoring and detection of climate change
15. Climate and the limits of permafrost: A zonal analysis
16. The moving interface problem with finite elements
17. Ground thermal modeling in support of terrain evaluation and route selection in the Mackenzie River Valley