Temperature variation and apparent thermal diffusivity in the refreezing active layer, Toolik Lake, Alaska
Abstract Temperatures were sampled at eight‐hour intervals over a five‐month period within the refreezing active layer at Toolik Lake, Alaska. The variance spectra of the temperature series, calculated as a function of wavelength, reveal relatively high‐frequency (sub‐diurnal) temperature fluctuatio...
| Published in: | Permafrost and Periglacial Processes |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1990
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1002/ppp.3430010306 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010306 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010306 |
| Summary: | Abstract Temperatures were sampled at eight‐hour intervals over a five‐month period within the refreezing active layer at Toolik Lake, Alaska. The variance spectra of the temperature series, calculated as a function of wavelength, reveal relatively high‐frequency (sub‐diurnal) temperature fluctuations near the base of the active layer during refreezing, behaviour that is not consistent with a purely conductive system. The thermal records were also used in a numerical scheme to calculate apparent thermal diffusivity at regularly spaced depths in the substrate. Widely fluctuating positive and negative diffusivity values suggest that non‐conductive processes play an important role in heat transport during and after freezeback. Phase transformations, vapour diffusion and water advection all can enhance or oppose the conductive tendency. Models based exclusively on conductive principles are inadequate to explain thermal evolution in the dynamic near‐surface layer of permafrost regions. |
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