Active layer thermal dynamics at two lithologically different
sites on James Ross Island, Eastern Antarctic Peninsula

J 2017

Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula

HRBÁČEK, Filip, Daniel NÝVLT and Kamil LÁSKA

Basic information

Original name

Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula

Authors

HRBÁČEK, Filip (203 Czech Republic, belonging to the institution), Daniel NÝVLT (203 Czech Republic, belonging to the institution) and Kamil LÁSKA (203 Czech Republic, belonging to the institution)

Edition

Catena, AMSTERDAM, ELSEVIER SCIENCE BV, 2017, 0341-8162

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: 3.256

RIV identification code

RIV/00216224:14310/17:00095860

Organization unit

Faculty of Science

DOI

http://dx.doi.org/10.1016/j.catena.2016.06.020

UT WoS

000390733900009

Keywords in English

Active layer thermal regime; Ground temperature; Lithological properties; Active layer thickness; Air temperature; Antarctic peninsula

Abstract

V originále

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.

Links

LM2015078, research and development project

Name: Česká polární výzkumná infrastruktura (Acronym: CzechPolar2)

Investor: Ministry of Education, Youth and Sports of the CR

MUNI/A/1315/2015, interní kód MU

Name: Integrovaný výzkum environmentálních změn v krajinné sféře Země

Investor: Masaryk University, Category A

Citovat

HRBÁČEK, Filip, Daniel NÝVLT and Kamil LÁSKA. Active layer thermal dynamics at two lithologically different sites on James Ross Island, Eastern Antarctic Peninsula. Catena. AMSTERDAM: ELSEVIER SCIENCE BV, 2017, vol. 149, February, p. 592-602. ISSN 0341-8162. Available from: https://dx.doi.org/10.1016/j.catena.2016.06.020.

@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, 2017, vol.~149, February, p.~592-602. ISSN~0341-8162. Available from: https://dx.doi.org/10.1016/j.catena.2016.06.020.

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