2021
Active layer monitoring in Antarctica: an overview of results from 2006 to 2015
HRBÁČEK, Filip, Goncalo VIEIRA, Marc OLIVA, Megan BALKS, Mauro GUGLIELMIN et. al.Základní údaje
Originální název
Active layer monitoring in Antarctica: an overview of results from 2006 to 2015
Autoři
HRBÁČEK, Filip (203 Česká republika, garant, domácí), Goncalo VIEIRA, Marc OLIVA, Megan BALKS, Mauro GUGLIELMIN, Miguel Ángel DE PABLO, Antonio MOLINA, Miguel RAMOS, Gabriel GOYANES, Ian MEIKLEJOHN, Andrey ABRAMOV, Nikita DEMIDOV, Dmitry FEDOROV-DAVYDOV, Alexey LUPACHEV, Elizaveta RIVKINA, Kamil LÁSKA (203 Česká republika, domácí), Michaela KŇAŽKOVÁ (703 Slovensko, domácí), Daniel NÝVLT (203 Česká republika, domácí), Rossana RAFFI, Jorge STRELIN, Toshio SONE, Kotaro FUKUI, Andrey DOLGIKH, Elya ZAZOVSKAYA, Nikita MERGELOV, Nikolay OSOKIN a Vladislav MIAMIN
Vydání
Polar Geography, Taylor & Francis Ltd, 2021, 1088-937X
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10508 Physical geography
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Kód RIV
RIV/00216224:14310/21:00120403
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000727056000001
Klíčová slova anglicky
CALM-S; active layer thickness; ground temperature; Antarctica; active layer monitoring; climate
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 20. 12. 2021 13:46, Mgr. Marie Šípková, DiS.
Anotace
V originále
Monitoring of active layer thawing depth and active layer thickness (ALT), using mechanical pronging and continuous temperature data logging, has been undertaken under the Circumpolar Active Layer Monitoring – South (CALM-S) program at a range of sites across Antarctica. The objective of this study was to summarize key data from sites in different Antarctic regions from 2006 to 2015 to review the state of the active layer in Antarctica and the effectiveness of the CALM-S program. The data from 16 sites involving 8 CALM-S and another 8 boreholes across the Antarctic have been used in the study. Probing for thaw depth, while giving information on local spatial variability, often underestimates the maximum ALT of Antarctic soils compared to that determined using continuous temperature monitoring. The differences are likely to be caused by stones limiting probe penetration and the timing of probing not coinciding with the timing of maximum thaw, which varies between seasons. The information on the active layer depth is still sparse in many regions and the monitoring needs to be extended and continued to provide a better understanding of both spatial and temporal variability in Antarctic soil thermal properties.
Návaznosti
LM2015078, projekt VaV |
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MUNI/A/1251/2017, interní kód MU |
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MUNI/A/1315/2015, interní kód MU |
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