High-resolution 4D electrical resistivity tomography and below-ground point sensor monitoring of High Arctic deglaciated sediments capture zero-curtain effects, freeze–thaw transitions, and mid-winter thawing

High-resolution 4D electrical resistivity tomography and below-ground point sensor monitoring of High Arctic deglaciated sediments capture zero-curtain effects, freeze–thaw transitions, and mid-winter thawing

<p>Arctic regions are under immense pressure from a continuously warming climate. During the winter and shoulder seasons, recently deglaciated sediments are particularly sensitive to human-induced warming. Understanding the physical mechanisms and processes that determine soil liquid moisture...

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Main Authors: M. O. Cimpoiasu, O. Kuras, H. Harrison, P. B. Wilkinson, P. Meldrum, J. E. Chambers, D. Liljestrand, C. Oroza, S. K. Schmidt, P. Sommers, L. Vimercati, T. P. Irons, Z. Lyu, A. Solon, J. A. Bradley
Format: Article
Language:English
Published: Copernicus Publications 2025-01-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/19/401/2025/tc-19-401-2025.pdf
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