Permafrost Distribution Modeling in the Semi-arid Chilean Andes
International audience lMountain permafrost and rock glaciers in the Andes are of growing interest due to the increase in human activities in this remote area and new environmental regulations. Empirical models of mountain permafrost distribution based on the spatial analysis of intact and relict ro...
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fttriple:oai:gotriple.eu:m5CDwTk97RAMEingkm4JI 2023-05-15T16:36:56+02:00 Permafrost Distribution Modeling in the Semi-arid Chilean Andes Azócar, Guillermo Brenning, Alexander Bodin, Xavier Department of Geography and Environmental Management Waterloo University of Waterloo Waterloo Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) International Permafrost Association Potsdam, Germany 2016-06-20 https://doi.org/10.5194/tc-2016-100 https://hal-sde.archives-ouvertes.fr/hal-01887949 en eng HAL CCSD Copernicus hal-01887949 10670/1.36ymhv hal-01880553 doi:10.5194/tc-2016-100 10670/1.m59jjz https://hal-sde.archives-ouvertes.fr/hal-01887949 undefined Hyper Article en Ligne - Sciences de l'Homme et de la Société 11th International Conference on Permafrost. 11th International Conference on Permafrost., International Permafrost Association, Jun 2016, Potsdam, Germany geo envir Conference Output https://vocabularies.coar-repositories.org/resource_types/c_c94f/ Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2016 fttriple https://doi.org/10.5194/tc-2016-100 2023-01-22T17:52:42Z International audience lMountain permafrost and rock glaciers in the Andes are of growing interest due to the increase in human activities in this remote area and new environmental regulations. Empirical models of mountain permafrost distribution based on the spatial analysis of intact and relict rock glaciers and Mean Annual Air Temperature (MAAT) have been established as a tool for regional-scale assessments of permafrost favorability across entire mountain ranges. In this approach, bias adjustments are made to account for differences in permafrost presence within rock glaciers and in general debris-covered high-mountain terrain (Boeckli et al., 2012). This method allows for a rapid initial assessment of favorability for the presence of mountain permafrost in data-scarce vast mountain regions. In the present study, this methodology is applied to map a Permafrost Favorability Index (PFI) throughout the semi-arid Andes of central Chile (29° S-32°S), excluding areas of exposed bedrock. For this purpose, an inventory of relict and intact rock glaciers was compiled for the study region, MAAT was regionalized based on scarce meteorological data available in the study region, especially for high altitude area, and permafrost favorability was spatially modeled empirically based on MAAT and potential incoming solar radiation (PISR). The compiled inventory includes 3575 rock glaciers in the, Huasco, Elqui, Limarí and Choapa watersheds in Central Chile (total area: 38651 km 2 , including low elevation areas), 1664 of which were classified as relict and therefore as indicative of permafrost absence; 51 rock glaciers were removed before modeling due to their exceptional locations. Glaciers in the study region are limited to the highest parts of the Elqui and Huasco catchments. The estimated total ice volume of rock glaciers in the study region is about 2.5 times as large as the total glacier ice volume (Azócar and Brenning, 2010). MAAT for the 1981-2010 period was regionalized based on 116 station-years of annual air ... Article in Journal/Newspaper Ice permafrost Unknown |
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geo envir Azócar, Guillermo Brenning, Alexander Bodin, Xavier Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
topic_facet |
geo envir |
description |
International audience lMountain permafrost and rock glaciers in the Andes are of growing interest due to the increase in human activities in this remote area and new environmental regulations. Empirical models of mountain permafrost distribution based on the spatial analysis of intact and relict rock glaciers and Mean Annual Air Temperature (MAAT) have been established as a tool for regional-scale assessments of permafrost favorability across entire mountain ranges. In this approach, bias adjustments are made to account for differences in permafrost presence within rock glaciers and in general debris-covered high-mountain terrain (Boeckli et al., 2012). This method allows for a rapid initial assessment of favorability for the presence of mountain permafrost in data-scarce vast mountain regions. In the present study, this methodology is applied to map a Permafrost Favorability Index (PFI) throughout the semi-arid Andes of central Chile (29° S-32°S), excluding areas of exposed bedrock. For this purpose, an inventory of relict and intact rock glaciers was compiled for the study region, MAAT was regionalized based on scarce meteorological data available in the study region, especially for high altitude area, and permafrost favorability was spatially modeled empirically based on MAAT and potential incoming solar radiation (PISR). The compiled inventory includes 3575 rock glaciers in the, Huasco, Elqui, Limarí and Choapa watersheds in Central Chile (total area: 38651 km 2 , including low elevation areas), 1664 of which were classified as relict and therefore as indicative of permafrost absence; 51 rock glaciers were removed before modeling due to their exceptional locations. Glaciers in the study region are limited to the highest parts of the Elqui and Huasco catchments. The estimated total ice volume of rock glaciers in the study region is about 2.5 times as large as the total glacier ice volume (Azócar and Brenning, 2010). MAAT for the 1981-2010 period was regionalized based on 116 station-years of annual air ... |
author2 |
Department of Geography and Environmental Management Waterloo University of Waterloo Waterloo Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry ) International Permafrost Association |
format |
Article in Journal/Newspaper |
author |
Azócar, Guillermo Brenning, Alexander Bodin, Xavier |
author_facet |
Azócar, Guillermo Brenning, Alexander Bodin, Xavier |
author_sort |
Azócar, Guillermo |
title |
Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
title_short |
Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
title_full |
Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
title_fullStr |
Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
title_full_unstemmed |
Permafrost Distribution Modeling in the Semi-arid Chilean Andes |
title_sort |
permafrost distribution modeling in the semi-arid chilean andes |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://doi.org/10.5194/tc-2016-100 https://hal-sde.archives-ouvertes.fr/hal-01887949 |
op_coverage |
Potsdam, Germany |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Hyper Article en Ligne - Sciences de l'Homme et de la Société 11th International Conference on Permafrost. 11th International Conference on Permafrost., International Permafrost Association, Jun 2016, Potsdam, Germany |
op_relation |
hal-01887949 10670/1.36ymhv hal-01880553 doi:10.5194/tc-2016-100 10670/1.m59jjz https://hal-sde.archives-ouvertes.fr/hal-01887949 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-2016-100 |
_version_ |
1766027256677793792 |