Climate Conditions of the Permafrost Active Layer Development
in Petuniabukta, Billefjorden, Spitsbergen.

a 2010

Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen.

LÁSKA, Kamil, Denisa WITOSZOVÁ a Pavel PROŠEK

Základní údaje

Originální název

Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen.

Autoři

LÁSKA, Kamil (203 Česká republika, garant, domácí), Denisa WITOSZOVÁ (203 Česká republika, domácí) a Pavel PROŠEK (203 Česká republika, domácí)

Vydání

Mertes, J.R., Christiansen, H.H., Etzelmüller, B. (eds.): Thermal State of Frozen Ground in a Changing Climate During the IPY. Proceedings of the Third European Conference on Permafrost. Longyearbyen, June 13-17, 2010. Svalbard, pp. 128-128. 2010

Další údaje

Jazyk

angličtina

Typ výsledku

Konferenční abstrakt

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Norsko

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/10:00047874

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-82-481-0010-2

Klíčová slova anglicky

microclimate;permafrost;soil temperature;Arctic;Spitsbergen

Změněno: 29. 4. 2011 16:01, doc. Mgr. Kamil Láska, Ph.D.

Anotace

V originále

The investigated area is located in the coastal zone of Petuniabukta, north-western branch of Billefjorden, Spitsbergen. The most part of Petuniabukta is covered with cement type of the permafrost. During summer season, the permafrost table is located in the depth of 40-120 cm depending on the altitude, slope and relief exposition. Since 2008, fourth automatic weather stations have been operated along the northern coast of Petuniabukta at different altitudes ranging from seashore level to the mountain ridge up to 500 m a.s.l. Seasonal variation of microclimate parameters and other environmental factors were analyzed and discussed with respect to the permafrost active layer development and constituents of terrestrial polar ecosystems.

Návaznosti

B/CZ0046/3/0013, interní kód MU

Název: Effects of climate change on tundra ecosystem: Interaction of vegetation with extreme environments (Akronym: Norské fondy 2010)

Investor: Evropský hospodářský prostor, Effects of climate change on tundra ecosystem: Interaction of vegetation with extreme environments

Citovat

LÁSKA, Kamil, Denisa WITOSZOVÁ a Pavel PROŠEK. Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen. In Mertes, J.R., Christiansen, H.H., Etzelmüller, B. (eds.): Thermal State of Frozen Ground in a Changing Climate During the IPY. Proceedings of the Third European Conference on Permafrost. Longyearbyen, June 13-17, 2010. Svalbard, pp. 128-128. 2010. ISBN 978-82-481-0010-2.

@proceedings{935774,
   author = {Láska, Kamil and Witoszová, Denisa and Prošek, Pavel},
   booktitle = {Mertes, J.R., Christiansen, H.H., Etzelmüller, B. (eds.): Thermal State of Frozen Ground in a Changing Climate During the IPY. Proceedings of the Third European Conference on Permafrost. Longyearbyen, June 13-17, 2010. Svalbard, pp. 128-128.},
   keywords = {microclimate;permafrost;soil temperature;Arctic;Spitsbergen},
   language = {eng},
   isbn = {978-82-481-0010-2},
   title = {Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen.},
   year = {2010}
}

TY  - CONF
ID  - 935774
AU  - Láska, Kamil - Witoszová, Denisa - Prošek, Pavel
PY  - 2010
TI  - Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen.
SN  - 9788248100102
KW  - microclimate;permafrost;soil temperature;Arctic;Spitsbergen
N2  - The investigated area is located in the coastal zone of Petuniabukta, north-western branch of Billefjorden, Spitsbergen. The most part of Petuniabukta is covered with cement type of the permafrost. During summer season, the permafrost table is located in the depth of 40-120 cm depending on the altitude, slope and relief exposition. Since 2008, fourth automatic weather stations have been operated along the northern coast of Petuniabukta at different altitudes ranging from seashore level to the mountain ridge up to 500 m a.s.l. Seasonal variation of microclimate parameters and other environmental factors were analyzed and discussed with respect to the permafrost active layer development and constituents of terrestrial polar ecosystems.
ER  -

LÁSKA, Kamil, Denisa WITOSZOVÁ a Pavel PROŠEK. Climate Conditions of the Permafrost Active Layer Development in Petuniabukta, Billefjorden, Spitsbergen. In \textit{Mertes, J.R., Christiansen, H.H., Etzelmüller, B. (eds.): Thermal State of Frozen Ground in a Changing Climate During the IPY. Proceedings of the Third European Conference on Permafrost. Longyearbyen, June 13-17, 2010. Svalbard, pp. 128-128.}. 2010. ISBN~978-82-481-0010-2.

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