The evolution of a near‐surface ground thermal regime and modeled active‐layer thickness on James Ross Island, Eastern Antarctic Peninsula, in 2006–2016
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F20%3A00508265" target="_blank" >RIV/67985530:_____/20:00508265 - isvavai.cz</a>
Alternative codes found
RIV/00216224:14310/20:00115563 RIV/00216208:11310/20:10397085
Result on the web
<a href="https://onlinelibrary.wiley.com/doi/abs/10.1002/ppp.2018" target="_blank" >https://onlinelibrary.wiley.com/doi/abs/10.1002/ppp.2018</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/ppp.2018" target="_blank" >10.1002/ppp.2018</a>
Alternative languages
Result language
angličtina
Original language name
The evolution of a near‐surface ground thermal regime and modeled active‐layer thickness on James Ross Island, Eastern Antarctic Peninsula, in 2006–2016
Original language description
Thermal regime and thickness of the active layer respond rapidly to climate variations, and thus they are important measures of cryosphere changes in polar environments. We monitored air temperature and ground temperature at a depth of 5 cm and modeled active-layer thickness using the Stefan and Kudryavtsev models at the Abernethy Flats site, James Ross Island, Eastern Antarctic Peninsula, in the period March 2006 to February 2016. The decadal average of air and ground temperature was -7.3 and -6.1 degrees C, respectively, and the average modeled active-layer thickness reached 60 cm. Mean annual air temperature increased by 0.10 degrees C y(-1) over the study period, while mean annual ground temperature showed the opposite tendency of -0.05 degrees C y(-1). The cooling took place mainly in summer and caused thawing season shortening and active-layer thinning of 1.6 cm y(-1). However, these trends need to be taken carefully because all were non-significant at p < 0.05. The Stefan and Kudryavtsev models reproduced the active-layer thickness with mean absolute errors of 2.6 cm (5.0%) and 3.4 cm (5.9%), respectively, which is better than in most previous studies, making them promising tools for active-layer modeling over Antarctica.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10508 - Physical geography
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Permafrost and Periglacial Processes
ISSN
1045-6740
e-ISSN
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Volume of the periodical
31
Issue of the periodical within the volume
1
Country of publishing house
CA - CANADA
Number of pages
15
Pages from-to
141-155
UT code for WoS article
000482869100001
EID of the result in the Scopus database
2-s2.0-85071234155