Detailed Information on Publication Record
2017
Active layer monitoring at CALM-S site near J.G.Mendel Station, James Ross Island, eastern Antarctic Peninsula
HRBÁČEK, Filip, Michaela KŇAŽKOVÁ, Daniel NÝVLT, Kamil LÁSKA, Carsten W MUELLER et. al.Basic information
Original name
Active layer monitoring at CALM-S site near J.G.Mendel Station, James Ross Island, eastern Antarctic Peninsula
Authors
HRBÁČEK, Filip (203 Czech Republic, belonging to the institution), Michaela KŇAŽKOVÁ (703 Slovakia, belonging to the institution), Daniel NÝVLT (203 Czech Republic, belonging to the institution), Kamil LÁSKA (203 Czech Republic, belonging to the institution), Carsten W MUELLER (276 Germany) and Jakub ONDRUCH (203 Czech Republic, belonging to the institution)
Edition
Science of the Total Environment, Amsterdam, ELSEVIER SCIENCE BV, 2017, 0048-9697
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10508 Physical geography
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 4.610
RIV identification code
RIV/00216224:14310/17:00097070
Organization unit
Faculty of Science
UT WoS
000406294900097
Keywords in English
Active layer thickness; Ground thermal regime; Permafrost; CALM-S; Antarctic Peninsula; Climate
Tags
International impact, Reviewed
Změněno: 20/2/2019 17:48, Mgr. Filip Hrbáček, Ph.D.
Abstract
V originále
Circumpolar Active Layer Monitoring – South (CALM-S) site was established in February 2014 on James Ross Island as the first CALM-S site in the eastern Antarctic Peninsula region. The site located near the Johann Gregor Mendel Station is labelled CALM-S JGM. The grid area is gently sloped ¬< 3° and elevated between 8 to 11 m a.s.l. Lithology of the site is formed by more muddy sediments of Holocene marine terrace and clayey sandy Cretaceous sedimentary rocks, which significantly affect texture, moisture content and physical parameters of the ground on the grid. Our objective was to study seasonal and interannual variability of active layer depth and thermal regime on CALM-S site and at two ground temperature measurement profiles AWS-JGM and AWS-CALM located in the grid. Average air temperature in the period March 2013 to February 2016 reached -6.8 °C. Average ground temperature decreased with depth from -5.1 °C to -5.3 °C at 5 cm to -5.5 °C to -5.9 °C at 200 cm. Active layer thickness defined as the depth of 0 °C isotherm was significantly higher at AWS-CALM between 86 cm (2014/15) and 87 cm (2015/16), while at AWS-JGM reached only 51 cm (2013/14) to 65 cm (2015/16). Mean probed active layer depth increased from 66.4 cm in 2013/14 to 78.0 cm in 2014/15. High differences were observed when compared minimum (51 cm to 59 cm) and maximum (100 cm to 113 cm) probed depth. The distribution of active layer depth at CALM-S JGM clearly shows the effect of different lithological properties between the two lithologically distinct parts of the grid.
Links
LM2015078, research and development project |
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MUNI/A/1419/2016, interní kód MU |
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