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@article{1349007,
author = {Hrbáček, Filip and Nývlt, Daniel and Láska, Kamil},
article_location = {AMSTERDAM},
article_number = {February},
doi = {http://dx.doi.org/10.1016/j.catena.2016.06.020},
keywords = {Active layer thermal regime; Ground temperature; Lithological properties; Active layer thickness; Air temperature; Antarctic peninsula},
language = {eng},
issn = {0341-8162},
journal = {Catena},
title = {Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula},
volume = {149},
year = {2017}
}
TY - JOUR
ID - 1349007
AU - Hrbáček, Filip - Nývlt, Daniel - Láska, Kamil
PY - 2017
TI - Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula
JF - Catena
VL - 149
IS - February
SP - 592-602
EP - 592-602
PB - ELSEVIER SCIENCE BV
SN - 03418162
KW - Active layer thermal regime
KW - Ground temperature
KW - Lithological properties
KW - Active layer thickness
KW - Air temperature
KW - Antarctic peninsula
N2 - The active layer thermal regime was studied at two sites with different lithological properties located on James Ross Island, eastern Antarctic Peninsula, to assess the main driving factors. The Abernethy Flats site (41 m a.s.l.) is located in Cretaceous calcareous sandstones and siltstones of the Santa Marta Formation. In contrast, the Berry Hill slopes site (56 m) is composed of muddy to intermediate diamictites, tuffaceous siltstones to fine-grained sandstones of the Mendel Formation. The data of air temperature at 2 m and ground temperature at two 75 cm deep profiles were analysed for the period 1 January 2012, to 31 December 2014.
ER -
HRBÁČEK, Filip, Daniel NÝVLT and Kamil LÁSKA. Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula. \textit{Catena}. AMSTERDAM: ELSEVIER SCIENCE BV, vol.~149, February, p.~592-602. ISSN~0341-8162. doi:10.1016/j.catena.2016.06.020. 2017.
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