Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia
Permafrost plays an important role in numerous environmental processes at high latitudes and in high mountain areas. The identification of mountain permafrost, particularly in the discontinuous permafrost regions, is challenging due to limited data availability and the high spatial variability of co...
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2020
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ftdoajarticles:oai:doaj.org/article:a9866b9c4e9c4efd956b6279e99baf01 2023-05-15T14:14:32+02:00 Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia Munkhdavaa Munkhjargal Gansukh Yadamsuren Jambaljav Yamkhin Lucas Menzel 2020-01-01T00:00:00Z https://doi.org/10.1080/15230430.2019.1704347 https://doaj.org/article/a9866b9c4e9c4efd956b6279e99baf01 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/15230430.2019.1704347 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 1523-0430 1938-4246 doi:10.1080/15230430.2019.1704347 https://doaj.org/article/a9866b9c4e9c4efd956b6279e99baf01 Arctic, Antarctic, and Alpine Research, Vol 52, Iss 1, Pp 13-26 (2020) mountain permafrost surface cover solar radiation temperature variability northern mongolia Environmental sciences GE1-350 Ecology QH540-549.5 article 2020 ftdoajarticles https://doi.org/10.1080/15230430.2019.1704347 2022-12-31T05:41:32Z Permafrost plays an important role in numerous environmental processes at high latitudes and in high mountain areas. The identification of mountain permafrost, particularly in the discontinuous permafrost regions, is challenging due to limited data availability and the high spatial variability of controlling factors. This study focuses on mountain permafrost in a data-scarce environment of northern Mongolia, at the interface between the boreal forest and the dry steppe mid-latitudes. In this region, the ground temperature has been increasing continuously since 2011 and has a high spatial variability due to the distribution of incoming solar radiation, as well as seasonal snow and vegetation cover. We analyzed the effect of these controlling factors to understand the climate–permafrost relationship based on in situ observations. Furthermore, mean ground surface temperature (MGST) was calculated at 30-m resolution to predict permafrost distribution. The calculated MGST, with a root mean square error of ±1.4°C, shows permafrost occurrence on north-facing slopes and at higher elevations and absence on south-facing slopes. Borehole temperature data indicate a serious wildfire-induced permafrost degradation in the region; therefore, special attention should be paid to further investigations on ecosystem resilience and climate change mitigation in this region. Article in Journal/Newspaper Antarctic and Alpine Research Arctic permafrost Directory of Open Access Journals: DOAJ Articles Arctic, Antarctic, and Alpine Research 52 1 13 26 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
mountain permafrost surface cover solar radiation temperature variability northern mongolia Environmental sciences GE1-350 Ecology QH540-549.5 |
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mountain permafrost surface cover solar radiation temperature variability northern mongolia Environmental sciences GE1-350 Ecology QH540-549.5 Munkhdavaa Munkhjargal Gansukh Yadamsuren Jambaljav Yamkhin Lucas Menzel Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
topic_facet |
mountain permafrost surface cover solar radiation temperature variability northern mongolia Environmental sciences GE1-350 Ecology QH540-549.5 |
description |
Permafrost plays an important role in numerous environmental processes at high latitudes and in high mountain areas. The identification of mountain permafrost, particularly in the discontinuous permafrost regions, is challenging due to limited data availability and the high spatial variability of controlling factors. This study focuses on mountain permafrost in a data-scarce environment of northern Mongolia, at the interface between the boreal forest and the dry steppe mid-latitudes. In this region, the ground temperature has been increasing continuously since 2011 and has a high spatial variability due to the distribution of incoming solar radiation, as well as seasonal snow and vegetation cover. We analyzed the effect of these controlling factors to understand the climate–permafrost relationship based on in situ observations. Furthermore, mean ground surface temperature (MGST) was calculated at 30-m resolution to predict permafrost distribution. The calculated MGST, with a root mean square error of ±1.4°C, shows permafrost occurrence on north-facing slopes and at higher elevations and absence on south-facing slopes. Borehole temperature data indicate a serious wildfire-induced permafrost degradation in the region; therefore, special attention should be paid to further investigations on ecosystem resilience and climate change mitigation in this region. |
format |
Article in Journal/Newspaper |
author |
Munkhdavaa Munkhjargal Gansukh Yadamsuren Jambaljav Yamkhin Lucas Menzel |
author_facet |
Munkhdavaa Munkhjargal Gansukh Yadamsuren Jambaljav Yamkhin Lucas Menzel |
author_sort |
Munkhdavaa Munkhjargal |
title |
Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
title_short |
Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
title_full |
Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
title_fullStr |
Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
title_full_unstemmed |
Ground surface temperature variability and permafrost distribution over mountainous terrain in northern Mongolia |
title_sort |
ground surface temperature variability and permafrost distribution over mountainous terrain in northern mongolia |
publisher |
Taylor & Francis Group |
publishDate |
2020 |
url |
https://doi.org/10.1080/15230430.2019.1704347 https://doaj.org/article/a9866b9c4e9c4efd956b6279e99baf01 |
genre |
Antarctic and Alpine Research Arctic permafrost |
genre_facet |
Antarctic and Alpine Research Arctic permafrost |
op_source |
Arctic, Antarctic, and Alpine Research, Vol 52, Iss 1, Pp 13-26 (2020) |
op_relation |
http://dx.doi.org/10.1080/15230430.2019.1704347 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 1523-0430 1938-4246 doi:10.1080/15230430.2019.1704347 https://doaj.org/article/a9866b9c4e9c4efd956b6279e99baf01 |
op_doi |
https://doi.org/10.1080/15230430.2019.1704347 |
container_title |
Arctic, Antarctic, and Alpine Research |
container_volume |
52 |
container_issue |
1 |
container_start_page |
13 |
op_container_end_page |
26 |
_version_ |
1766286948153950208 |