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 a Kamil LÁSKA

Základní údaje

Originální název

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

Autoři

HRBÁČEK, Filip (203 Česká republika, domácí), Daniel NÝVLT (203 Česká republika, domácí) a Kamil LÁSKA (203 Česká republika, domácí)

Vydání

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

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10508 Physical geography

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 3.256

Kód RIV

RIV/00216224:14310/17:00095860

Organizační jednotka

Přírodovědecká fakulta

DOI

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

UT WoS

000390733900009

Klíčová slova anglicky

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

Štítky

NZ, rivok

Změněno: 28. 3. 2018 09:31, Ing. Nicole Zrilić

Anotace

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.

Návaznosti

LM2015078, projekt VaV

Název: Česká polární výzkumná infrastruktura (Akronym: CzechPolar2)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Czech Polar Research Infrastructure

MUNI/A/1315/2015, interní kód MU

Název: Integrovaný výzkum environmentálních změn v krajinné sféře Země

Investor: Masarykova univerzita, Integrovaný výzkum environmentálních změn v krajinné sféře Země, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Citovat

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

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