PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions
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 envi...
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Copernicus Publications
2021
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Online Access: | https://doi.org/10.5194/gmd-14-1865-2021 https://doaj.org/article/8a0100da839a45779cb49ad06297900e |
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ftdoajarticles:oai:doaj.org/article:8a0100da839a45779cb49ad06297900e 2023-05-15T13:03:30+02:00 PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions T. Uxa M. Křížek F. Hrbáček 2021-04-01T00:00:00Z https://doi.org/10.5194/gmd-14-1865-2021 https://doaj.org/article/8a0100da839a45779cb49ad06297900e EN eng Copernicus Publications https://gmd.copernicus.org/articles/14/1865/2021/gmd-14-1865-2021.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 doi:10.5194/gmd-14-1865-2021 1991-959X 1991-9603 https://doaj.org/article/8a0100da839a45779cb49ad06297900e Geoscientific Model Development, Vol 14, Pp 1865-1884 (2021) Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/gmd-14-1865-2021 2022-12-31T10:45:19Z 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 ∘ C . The past mean annual air temperature modelled experimentally for two sites in the Czech Republic hosting relict cryoturbation structures was between <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">7.0</mn><mo>±</mo><mn mathvariant="normal">1.9</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="a73d94d6529884b0ef9c6e34a21b2cc9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-1865-2021-ie00001.svg" width="52pt" height="10pt" src="gmd-14-1865-2021-ie00001.png"/></svg:svg> and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">3.2</mn><mo>±</mo><mn mathvariant="normal">1.5</mn></mrow></math> <svg:svg ... Article in Journal/Newspaper Active layer thickness permafrost wedge* Directory of Open Access Journals: DOAJ Articles Geoscientific Model Development 14 4 1865 1884 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Geology QE1-996.5 |
spellingShingle |
Geology QE1-996.5 T. Uxa M. Křížek F. Hrbáček PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
topic_facet |
Geology QE1-996.5 |
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 ∘ C . The past mean annual air temperature modelled experimentally for two sites in the Czech Republic hosting relict cryoturbation structures was between <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">7.0</mn><mo>±</mo><mn mathvariant="normal">1.9</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="a73d94d6529884b0ef9c6e34a21b2cc9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-1865-2021-ie00001.svg" width="52pt" height="10pt" src="gmd-14-1865-2021-ie00001.png"/></svg:svg> and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">3.2</mn><mo>±</mo><mn mathvariant="normal">1.5</mn></mrow></math> <svg:svg ... |
format |
Article in Journal/Newspaper |
author |
T. Uxa M. Křížek F. Hrbáček |
author_facet |
T. Uxa M. Křížek F. Hrbáček |
author_sort |
T. Uxa |
title |
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
title_short |
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
title_full |
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
title_fullStr |
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
title_full_unstemmed |
PERICLIMv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
title_sort |
periclimv1.0: a model deriving palaeo-air temperatures from thaw depth in past permafrost regions |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/gmd-14-1865-2021 https://doaj.org/article/8a0100da839a45779cb49ad06297900e |
genre |
Active layer thickness permafrost wedge* |
genre_facet |
Active layer thickness permafrost wedge* |
op_source |
Geoscientific Model Development, Vol 14, Pp 1865-1884 (2021) |
op_relation |
https://gmd.copernicus.org/articles/14/1865/2021/gmd-14-1865-2021.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 doi:10.5194/gmd-14-1865-2021 1991-959X 1991-9603 https://doaj.org/article/8a0100da839a45779cb49ad06297900e |
op_doi |
https://doi.org/10.5194/gmd-14-1865-2021 |
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Geoscientific Model Development |
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4 |
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1865 |
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