Numeric simulation of permafrost degradation in the eastern Tibetan Plateau
Abstract Rates of permafrost degradation at both the permafrost table and the base of permafrost were simulated using a prescribed rate of increase in mean annual air temperatures of 0.04°C/a for a site in continuous permafrost near Changshitou Mountain, eastern Tibetan Plateau. The results indicate...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2008
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Subjects: | |
Online Access: | http://dx.doi.org/10.1002/ppp.611 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.611 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.611 |
Summary: | Abstract Rates of permafrost degradation at both the permafrost table and the base of permafrost were simulated using a prescribed rate of increase in mean annual air temperatures of 0.04°C/a for a site in continuous permafrost near Changshitou Mountain, eastern Tibetan Plateau. The results indicate that over 110 years, the permafrost table descends from a depth of 1.20 m to 1.48 m, and that the base of permafrost rises from the initial value of 55.0 m to 15.2 m. The predicted rate of basal permafrost degradation in low moisture content bedrock reaches a peak of 0.58 m/a after 60 years, assuming a constant thermal gradient at the base of 0.018°C/m. The permafrost is persistent due to the ice‐rich nature of the near‐surface soil layers. Copyright © 2008 John Wiley & Sons, Ltd. |
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