Spatial distribution of pingos in northern Asia

Pingos are prominent periglacial landforms in vast regions of the Arctic and Subarctic. They are indicators of modern and past conditions of permafrost, surface geology, hydrology and climate. A first version of a detailed spatial geodatabase of 6059 pingo locations in a 3.5×106 km2 region of northe...

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Published in:The Cryosphere
Main Authors: G. Grosse, B. M. Jones
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
geo
Ice
Online Access:https://doi.org/10.5194/tc-5-13-2011
http://www.the-cryosphere.net/5/13/2011/tc-5-13-2011.pdf
https://doaj.org/article/d208202ea1854790903197207808906d
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:d208202ea1854790903197207808906d 2023-05-15T15:13:01+02:00 Spatial distribution of pingos in northern Asia G. Grosse B. M. Jones 2011-01-01 https://doi.org/10.5194/tc-5-13-2011 http://www.the-cryosphere.net/5/13/2011/tc-5-13-2011.pdf https://doaj.org/article/d208202ea1854790903197207808906d en eng Copernicus Publications doi:10.5194/tc-5-13-2011 1994-0416 1994-0424 http://www.the-cryosphere.net/5/13/2011/tc-5-13-2011.pdf https://doaj.org/article/d208202ea1854790903197207808906d undefined The Cryosphere, Vol 5, Iss 1, Pp 13-33 (2011) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.5194/tc-5-13-2011 2023-01-22T19:11:20Z Pingos are prominent periglacial landforms in vast regions of the Arctic and Subarctic. They are indicators of modern and past conditions of permafrost, surface geology, hydrology and climate. A first version of a detailed spatial geodatabase of 6059 pingo locations in a 3.5×106 km2 region of northern Asia was assembled from topographic maps. A first order analysis was carried out with respect to permafrost, landscape characteristics, surface geology, hydrology, climate, and elevation datasets using a Geographic Information System (GIS). Pingo heights in the dataset vary between 2 and 37 m, with a mean height of 4.8 m. About 64% of the pingos occur in continuous permafrost with high ice content and thick sediments; another 19% in continuous permafrost with moderate ice content and thick sediments. The majority of these pingos are likely hydrostatic pingos, which are typical of those located in drained thermokarst lake basins of northern lowlands with continuous permafrost. About 82% of the pingos are located in the tundra bioclimatic zone. Most pingos in the dataset are located in regions with mean annual ground temperatures between −3 and −11 °C and mean annual air temperatures between −7 and −18 °C. The dataset confirms that surface geology and hydrology are key factors for pingo formation and occurrence. Based on model predictions for near-future permafrost distribution, about 2073 pingos (34%) along the southern margins of permafrost will be located in regions with thawing permafrost by 2100, which ultimately may lead to increased occurrence of pingo collapse. Based on our dataset and previously published estimates of pingo numbers from other regions, we conclude that there are more than 11 000 pingos on Earth. Article in Journal/Newspaper Arctic Ice permafrost Subarctic The Cryosphere Thermokarst Tundra Unknown Arctic The Cryosphere 5 1 13 33
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
G. Grosse
B. M. Jones
Spatial distribution of pingos in northern Asia
topic_facet geo
envir
description Pingos are prominent periglacial landforms in vast regions of the Arctic and Subarctic. They are indicators of modern and past conditions of permafrost, surface geology, hydrology and climate. A first version of a detailed spatial geodatabase of 6059 pingo locations in a 3.5×106 km2 region of northern Asia was assembled from topographic maps. A first order analysis was carried out with respect to permafrost, landscape characteristics, surface geology, hydrology, climate, and elevation datasets using a Geographic Information System (GIS). Pingo heights in the dataset vary between 2 and 37 m, with a mean height of 4.8 m. About 64% of the pingos occur in continuous permafrost with high ice content and thick sediments; another 19% in continuous permafrost with moderate ice content and thick sediments. The majority of these pingos are likely hydrostatic pingos, which are typical of those located in drained thermokarst lake basins of northern lowlands with continuous permafrost. About 82% of the pingos are located in the tundra bioclimatic zone. Most pingos in the dataset are located in regions with mean annual ground temperatures between −3 and −11 °C and mean annual air temperatures between −7 and −18 °C. The dataset confirms that surface geology and hydrology are key factors for pingo formation and occurrence. Based on model predictions for near-future permafrost distribution, about 2073 pingos (34%) along the southern margins of permafrost will be located in regions with thawing permafrost by 2100, which ultimately may lead to increased occurrence of pingo collapse. Based on our dataset and previously published estimates of pingo numbers from other regions, we conclude that there are more than 11 000 pingos on Earth.
format Article in Journal/Newspaper
author G. Grosse
B. M. Jones
author_facet G. Grosse
B. M. Jones
author_sort G. Grosse
title Spatial distribution of pingos in northern Asia
title_short Spatial distribution of pingos in northern Asia
title_full Spatial distribution of pingos in northern Asia
title_fullStr Spatial distribution of pingos in northern Asia
title_full_unstemmed Spatial distribution of pingos in northern Asia
title_sort spatial distribution of pingos in northern asia
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/tc-5-13-2011
http://www.the-cryosphere.net/5/13/2011/tc-5-13-2011.pdf
https://doaj.org/article/d208202ea1854790903197207808906d
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Subarctic
The Cryosphere
Thermokarst
Tundra
genre_facet Arctic
Ice
permafrost
Subarctic
The Cryosphere
Thermokarst
Tundra
op_source The Cryosphere, Vol 5, Iss 1, Pp 13-33 (2011)
op_relation doi:10.5194/tc-5-13-2011
1994-0416
1994-0424
http://www.the-cryosphere.net/5/13/2011/tc-5-13-2011.pdf
https://doaj.org/article/d208202ea1854790903197207808906d
op_rights undefined
op_doi https://doi.org/10.5194/tc-5-13-2011
container_title The Cryosphere
container_volume 5
container_issue 1
container_start_page 13
op_container_end_page 33
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