PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F21%3A00541618" target="_blank" >RIV/67985530:_____/21:00541618 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/21:10433410 RIV/00216224:14310/21:00122894
Result on the web
<a href="https://gmd.copernicus.org/articles/14/1865/2021/" target="_blank" >https://gmd.copernicus.org/articles/14/1865/2021/</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/gmd-14-1865-2021" target="_blank" >10.5194/gmd-14-1865-2021</a>
Alternative languages
Result language
angličtina
Original language name
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions
Original language description
Periglacial features, such as various kinds of patterned ground, cryoturbations, frost wedges, solifluction structures, and blockfields, are among the most common relics of cold climate periods, which repetitively occurred throughout the Quaternary. As such, they are widespread archives of past environmental conditions. Climate controls on the development of most periglacial features, however, remain poorly known, and thus empirical palaeo-climate reconstructions based on them have limited validity. This study presents and evaluates a simple new inverse modelling scheme called PERICLIMv1.0 (PERIglacial CLIMate) that derives palaeo-air temperature characteristics related to the palaeo-active-layer thickness, which can be recognized using many relict periglacial features found in past permafrost regions. The evaluation against modern temperature records showed that the model reproduces air temperature characteristics with average errors <= 1.3 degrees C. The past mean annual air temperature modelled experimentally for two sites in the Czech Republic hosting relict cryoturbation structures was between -7.0 +/- 1.9 and -3.2 +/- 1.5 degrees C, which is well in line with earlier reconstructions utilizing various palaeo-archives. These initial results are promising and suggest that the model could become a useful tool for reconstructing Quaternary palaeo-environments across vast areas of mid-latitudes and low latitudes where relict periglacial assemblages frequently occur, but their full potential remains to be exploited.
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
<a href="/en/project/GA17-21612S" target="_blank" >GA17-21612S: Patterned ground development and its implications for the Quaternary environment in central Europe</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geoscientific Model Development
ISSN
1991-959X
e-ISSN
1991-9603
Volume of the periodical
14
Issue of the periodical within the volume
4
Country of publishing house
DE - GERMANY
Number of pages
20
Pages from-to
1865-1884
UT code for WoS article
000638995900001
EID of the result in the Scopus database
2-s2.0-85103770270