Articles | Volume 16, issue 2
https://doi.org/10.5194/tc-16-719-2022
https://doi.org/10.5194/tc-16-719-2022
Research article
 | 
03 Mar 2022
Research article |  | 03 Mar 2022

A distributed temperature profiling system for vertically and laterally dense acquisition of soil and snow temperature

Baptiste Dafflon, Stijn Wielandt, John Lamb, Patrick McClure, Ian Shirley, Sebastian Uhlemann, Chen Wang, Sylvain Fiolleau, Carlotta Brunetti, Franklin H. Akins, John Fitzpatrick, Samuel Pullman, Robert Busey, Craig Ulrich, John Peterson, and Susan S. Hubbard

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Cited articles

Aguilar, O. F. S., Arredondo, J. A. A., Trujillo, B. A. E. and Fundora, A. J. B.: Determining the in situ apparent thermal diffusivity of a sandy soil, Rev. Bras. Ciênc. Solo, 42, e0180025, https://doi.org/10.1590/18069657rbcs20180025, 2018. 
Andújar Márquez, J. M., Martínez Bohórquez, M. Á., and Gómez Melgar, S.: Ground thermal diffusivity calculation by direct soil temperature measurement, Application to very low enthalpy geothermal energy systems, Sensors, 16, 306, https://doi.org/10.3390/s16030306, 2016. 
Barnett, T. P., Adam, J. C., and Lettenmaier, D. P.: Potential impacts of a warming climate on water availability in snow-dominated regions, Nature, 438, 303–309, 2005. 
Beardsmore, G., Egan, S., and Sandiford, M.: A Fourier Spectral Method to Measure the Thermal Diffusivity of Soil, Geotech. Test. J., 43, https://doi.org/10.1520/GTJ20180300, 2020. 
Biskaborn, B. K., Lanckman, J.-P., Lantuit, H., Elger, K., Streletskiy, D. A., Cable, W. L., and Romanovsky, V. E.: The new database of the Global Terrestrial Network for Permafrost (GTN-P), Earth Syst. Sci. Data, 7, 245–259, https://doi.org/10.5194/essd-7-245-2015, 2015. 
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Short summary
This study presents the development and validation of a novel acquisition system for measuring finely resolved depth profiles of soil and snow temperature at multiple locations. Results indicate that the system reliably captures the dynamics in snow thickness, as well as soil freezing and thawing depth, enabling advances in understanding the intensity and timing in surface processes and their impact on subsurface thermohydrological regimes.
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