Simple analytical–statistical models (ASMs) for mean annual permafrost table temperature and active-layer thickness estimates

Abstract. A number of models have been developed for estimating the mean annual permafrost table temperature (MAPT) and active-layer thickness (ALT). These tools typically require at least a few ground physical properties as their input parameters in addition to air or ground temperatures. However, ground physical properties are frequently unavailable or unrepresentative and therefore need to be estimated, which introduces uncertainties into model outputs. Hence, we devised two simple analytical–statistical models (ASMs) for MAPT and ALT, which are driven solely by thawing and freezing indices from two depth levels within the active layer, while no ground physical properties are required. ASMs reproduced MAPT and ALT in the Earth's major permafrost regions with the total mean errors of less than 0.05 °C and 9 %, respectively. This is similar or better than other analytical or statistical models, which suggests that ASMs can be useful tools for estimating MAPT and ALT under a wide range of environmental conditions.

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Publication Details

Journal
˜The œcryosphere
Published
2026-01-07
DOI
https://doi.org/10.5194/tc-20-97-2026
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
0.00

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article

Simple analytical–statistical models (ASMs) for mean annual permafrost table temperature and active-layer thickness estimates

Michaela Kňažková, Tomáš Uxa, Filip Hrbáček
˜The œcryosphere
Climate change and permafrost
article

Simple analytical–statistical models (ASMs) for mean annual permafrost table temperature and active-layer thickness estimates

Michaela Kňažková, Tomáš Uxa, Filip Hrbáček
article en

Abstract

Abstract. A number of models have been developed for estimating the mean annual permafrost table temperature (MAPT) and active-layer thickness (ALT). These tools typically require at least a few ground physical properties as their input parameters in addition to air or ground temperatures. However, ground physical properties are frequently unavailable or unrepresentative and therefore need to be estimated, which introduces uncertainties into model outputs. Hence, we devised two simple analytical–statistical models (ASMs) for MAPT and ALT, which are driven solely by thawing and freezing indices from two depth levels within the active layer, while no ground physical properties are required. ASMs reproduced MAPT and ALT in the Earth's major permafrost regions with the total mean errors of less than 0.05 °C and 9 %, respectively. This is similar or better than other analytical or statistical models, which suggests that ASMs can be useful tools for estimating MAPT and ALT under a wide range of environmental conditions.

˜The œcryosphereVol. 20(1)
Czech Academy of Sciences (CZ), Masaryk University (CZ), Czech Academy of Sciences, Institute of Geophysics (CZ)
U.S. Department of Agriculture, Grantová Agentura České Republiky, Natural Resources Conservation Service
Openalex Percentile: Top 97%
Climate change and permafrost
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