KŇAŽKOVÁ, Michaela and Filip HRBÁČEK. Interannual variability of soil thermal conductivity and moisture on the Abernethy Flats (James Ross Island) during thawing seasons 2015-2023. Catena. Elsevier Science, 2024, vol. 234, January 2024, p. 1-12. ISSN 0341-8162. Available from: https://dx.doi.org/10.1016/j.catena.2023.107640.
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Basic information
Original name Interannual variability of soil thermal conductivity and moisture on the Abernethy Flats (James Ross Island) during thawing seasons 2015-2023
Authors KŇAŽKOVÁ, Michaela (703 Slovakia, guarantor, belonging to the institution) and Filip HRBÁČEK (203 Czech Republic, belonging to the institution).
Edition Catena, Elsevier Science, 2024, 0341-8162.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10510 Climatic research
Country of publisher Netherlands
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 6.200 in 2022
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.catena.2023.107640
UT WoS 001156721700001
Keywords in English Soil thermal properties; Soil thermal properties; Soil thermal regime; Soil thermal regime; Active layer thickness; Active layer thickness; Antarctic Peninsula; Antarctic Peninsula; Climate change; Climate change
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 28/2/2024 14:35.
Abstract
The knowledge of soil thermal properties is important for determining how a soil will behave under changing climate conditions, especially in the sensitive environment of permafrost affected soils. This paper represents the first complex study of the interplay between the different parameters affecting soil thermal conductivity of soils in Antarctica. Antarctic Peninsula is currently the most rapidly warming region of the whole Antarctica, with predictions of this warming to continue in the upcoming decades. This study focuses on James Ross Island, where the Abernethy Flats automatic weather station is located in a lowland area with semi-arid climate. Air and ground temperature, soil heat flux and soil moisture during the thawing season were monitored on this site from 2015 to 2023. Moreover, two approaches to determining soil thermal conductivity were compared – laboratory measurements and calculation from field data. During this period, mean annual temperatures have increased dramatically for both air (from −6.9 °C in 2015/2016 to −3.8 °C in 2022/2023) and ground (from −6.5 °C to −3.2 °C), same as active layer thickness (from 68 cm to 95 cm). Average soil thermal conductivity for the thawing period reached values between 0.49 and 0.74 W/m.K−1 based on field data. Statistically significant relationships were found between the seasonal means of volumetric water content and several other parameters – soil thermal conductivity (r = 0.91), thawing degree days (r = −0.87) and active layer thickness (r = −0.88). Although wetter soils generally have a higher conductivity, the increase in temperature exhibits a much stronger control over the active layer thickening, also contributing to the overall drying of the upper part of the soil profile.
Links
GM22-28659M, research and development projectName: Vliv změny klimatu na dynamiku periglaciálního prostředí v oblasti Antarktického poloostrova
Investor: Czech Science Foundation
VAN 2022, interní kód MUName: Český antarktický výzkumný program 2022 (Acronym: CARP 2022)
Investor: Ministry of Education, Youth and Sports of the CR, Czech Antarctic Research Programme 2022, Antarctic research
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