Thermal regime of permafrost active layer on James Ross Island, Maritime Antarctica in the years 2011-2012
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00079932" target="_blank" >RIV/00216224:14310/14:00079932 - isvavai.cz</a>
Result on the web
<a href="http://www.eucop4.org" target="_blank" >http://www.eucop4.org</a>
DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Thermal regime of permafrost active layer on James Ross Island, Maritime Antarctica in the years 2011-2012
Original language description
We present initial results of measurements of active layer thickness and its thermal regime on the Ulu Peninsula, the northern part of James Ross Island. Since 2011, data acquisition system records temperatures in the active layer at marine terrace on the northern shore of the Ulu Peninsula. Air temperature, snow depth, global and reflected radiation wre measured by an automatic weather station located several meters from the temperature borehole site (nearby the Czech Johann Gregor Mendel Station). Wedetermined the ground temperature regime and thickness of active layer in 2011-2012. The effect of air temperature on ground temperature variation was evaluated by means of regression analysis.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DE - Earth magnetism, geodesy, geography
OECD FORD branch
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Result continuities
Project
<a href="/en/project/LM2010009" target="_blank" >LM2010009: CzechPolar ? Czech Polar Stations: Construction and management</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach
Others
Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů