Articles | Volume 19, issue 7
https://doi.org/10.5194/tc-19-2715-2025
https://doi.org/10.5194/tc-19-2715-2025
Research article
 | 
31 Jul 2025
Research article |  | 31 Jul 2025

Numerical study of the error sources in the experimental estimation of thermal diffusivity: an application to debris-covered glaciers

Calvin Beck and Lindsey Nicholson

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Cited articles

Adhikary, S., Seko, K., Nakawo, M., Ageta, Y., and Miyazaki, N.: Effect of surface dust on snow melt, Bulletin of Glacier Research, 15, 85–92, 1997. a
Anderson, R. S., Anderson, L. S., Armstrong, W. H., Rossi, M. W., and Crump, S. E.: Glaciation of alpine valleys: The glacier–debris-covered glacier–rock glacier continuum, Geomorphology, 311, 127–142, https://doi.org/10.1016/j.geomorph.2018.03.015, 2018. a, b
Beck, C. and Nicholson, L.: TC-DTD (v1.0.1), Zenodo [data set], https://doi.org/10.5281/zenodo.15829843, 2025. a
Benn, D., Bolch, T., Hands, K., Gulley, J., Luckman, A., Nicholson, L., Quincey, D., Thompson, S., Toumi, R., and Wiseman, S.: Response of debris-covered glaciers in the Mount Everest region to recent warming, and implications for outburst flood hazards, Earth-Sci. Rev., 114, 156–174, https://doi.org/10.1016/j.earscirev.2012.03.008, 2012. a
Bhambri, R., Bolch, T., Chaujar, R. K., and Kulshreshtha, S. C.: Glacier changes in the Garhwal Himalaya, India, from 1968 to 2006 based on remote sensing, J. Glaciol., 57, 543–556, https://doi.org/10.3189/002214311796905604, 2011. a
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A glacier's debris cover strongly modifies its mass balance in contrast to a clean-ice glacier. A key parameter for calculating sub-debris melt is the thermal diffusivity of the debris layer. Conway and Rasmussen (2000) present a method to estimate this value based on simple heat diffusion principles. Our analysis shows that the selected temporal and spatial sampling intervals affect the estimated value of thermal diffusivity, resulting in glacier melt being systematically underestimated.
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