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 3.5×10 6 km 2 region of nort...

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Published in:The Cryosphere
Main Authors: Grosse, G., Jones, B. M.
Format: Text
Language:English
Published: 2018
Subjects:
Ice
Online Access:https://doi.org/10.5194/tc-5-13-2011
https://tc.copernicus.org/articles/5/13/2011/
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spelling ftcopernicus:oai:publications.copernicus.org:tc8836 2023-05-15T15:11:56+02:00 Spatial distribution of pingos in northern Asia Grosse, G. Jones, B. M. 2018-09-27 application/pdf https://doi.org/10.5194/tc-5-13-2011 https://tc.copernicus.org/articles/5/13/2011/ eng eng doi:10.5194/tc-5-13-2011 https://tc.copernicus.org/articles/5/13/2011/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-5-13-2011 2020-07-20T16:26:14Z 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 3.5×10 6 km 2 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. Text Arctic Ice permafrost Subarctic Thermokarst Tundra Copernicus Publications: E-Journals Arctic The Cryosphere 5 1 13 33
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
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 3.5×10 6 km 2 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 Text
author Grosse, G.
Jones, B. M.
spellingShingle Grosse, G.
Jones, B. M.
Spatial distribution of pingos in northern Asia
author_facet Grosse, G.
Jones, B. M.
author_sort Grosse, G.
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
publishDate 2018
url https://doi.org/10.5194/tc-5-13-2011
https://tc.copernicus.org/articles/5/13/2011/
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Subarctic
Thermokarst
Tundra
genre_facet Arctic
Ice
permafrost
Subarctic
Thermokarst
Tundra
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-5-13-2011
https://tc.copernicus.org/articles/5/13/2011/
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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