Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia
Rapid climate warming at northern high latitudes is driving geomorphic changes across the permafrost zone. In the Yamal and Gydan peninsulas in western Siberia, subterranean accumulation of methane beneath or within ice-rich permafrost can create mounds at the land surface. Once over-pressurized by...
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ftdoajarticles:oai:doaj.org/article:d02549c26aba47f1a2b74e6377f1bc51 2023-05-15T16:37:21+02:00 Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia Scott Zolkos Greg Fiske Tiffany Windholz Gabriel Duran Zhiqiang Yang Vladimir Olenchenko Alexey Faguet Susan M. Natali 2021-01-01T00:00:00Z https://doi.org/10.3390/geosciences11010021 https://doaj.org/article/d02549c26aba47f1a2b74e6377f1bc51 EN eng MDPI AG https://www.mdpi.com/2076-3263/11/1/21 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11010021 2076-3263 https://doaj.org/article/d02549c26aba47f1a2b74e6377f1bc51 Geosciences, Vol 11, Iss 21, p 21 (2021) permafrost thermokarst landscape change remote sensing ArcticDEM Landsat Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.3390/geosciences11010021 2022-12-31T06:10:30Z Rapid climate warming at northern high latitudes is driving geomorphic changes across the permafrost zone. In the Yamal and Gydan peninsulas in western Siberia, subterranean accumulation of methane beneath or within ice-rich permafrost can create mounds at the land surface. Once over-pressurized by methane, these mounds can explode and eject frozen ground, forming a gas emission crater (GEC). While GECs pose a hazard to human populations and infrastructure, only a small number have been identified in the Yamal and Gydan peninsulas, where the regional distribution and frequency of GECs and other types of land surface change are relatively unconstrained. To understand the distribution of landscape change within 327,000 km 2 of the Yamal-Gydan region, we developed a semi-automated multivariate change detection algorithm using satellite-derived surface reflectance, elevation, and water extent in the Google Earth Engine cloud computing platform. We found that 5% of the landscape changed from 1984 to 2017. The algorithm detected all seven GECs reported in the scientific literature and three new GEC-like features, and further revealed that retrogressive thaw slumps were more abundant than GECs. Our methodology can be refined to detect and better understand diverse types of land surface change and potentially mitigate risks across the northern permafrost zone. Article in Journal/Newspaper Ice permafrost Thermokarst Siberia Directory of Open Access Journals: DOAJ Articles Geosciences 11 1 21 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
permafrost thermokarst landscape change remote sensing ArcticDEM Landsat Geology QE1-996.5 |
spellingShingle |
permafrost thermokarst landscape change remote sensing ArcticDEM Landsat Geology QE1-996.5 Scott Zolkos Greg Fiske Tiffany Windholz Gabriel Duran Zhiqiang Yang Vladimir Olenchenko Alexey Faguet Susan M. Natali Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
topic_facet |
permafrost thermokarst landscape change remote sensing ArcticDEM Landsat Geology QE1-996.5 |
description |
Rapid climate warming at northern high latitudes is driving geomorphic changes across the permafrost zone. In the Yamal and Gydan peninsulas in western Siberia, subterranean accumulation of methane beneath or within ice-rich permafrost can create mounds at the land surface. Once over-pressurized by methane, these mounds can explode and eject frozen ground, forming a gas emission crater (GEC). While GECs pose a hazard to human populations and infrastructure, only a small number have been identified in the Yamal and Gydan peninsulas, where the regional distribution and frequency of GECs and other types of land surface change are relatively unconstrained. To understand the distribution of landscape change within 327,000 km 2 of the Yamal-Gydan region, we developed a semi-automated multivariate change detection algorithm using satellite-derived surface reflectance, elevation, and water extent in the Google Earth Engine cloud computing platform. We found that 5% of the landscape changed from 1984 to 2017. The algorithm detected all seven GECs reported in the scientific literature and three new GEC-like features, and further revealed that retrogressive thaw slumps were more abundant than GECs. Our methodology can be refined to detect and better understand diverse types of land surface change and potentially mitigate risks across the northern permafrost zone. |
format |
Article in Journal/Newspaper |
author |
Scott Zolkos Greg Fiske Tiffany Windholz Gabriel Duran Zhiqiang Yang Vladimir Olenchenko Alexey Faguet Susan M. Natali |
author_facet |
Scott Zolkos Greg Fiske Tiffany Windholz Gabriel Duran Zhiqiang Yang Vladimir Olenchenko Alexey Faguet Susan M. Natali |
author_sort |
Scott Zolkos |
title |
Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
title_short |
Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
title_full |
Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
title_fullStr |
Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
title_full_unstemmed |
Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia |
title_sort |
detecting and mapping gas emission craters on the yamal and gydan peninsulas, western siberia |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doi.org/10.3390/geosciences11010021 https://doaj.org/article/d02549c26aba47f1a2b74e6377f1bc51 |
genre |
Ice permafrost Thermokarst Siberia |
genre_facet |
Ice permafrost Thermokarst Siberia |
op_source |
Geosciences, Vol 11, Iss 21, p 21 (2021) |
op_relation |
https://www.mdpi.com/2076-3263/11/1/21 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11010021 2076-3263 https://doaj.org/article/d02549c26aba47f1a2b74e6377f1bc51 |
op_doi |
https://doi.org/10.3390/geosciences11010021 |
container_title |
Geosciences |
container_volume |
11 |
container_issue |
1 |
container_start_page |
21 |
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1766027647956025344 |