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...

Full description

Bibliographic Details
Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Munkhdavaa Munkhjargal, Gansukh Yadamsuren, Jambaljav Yamkhin, Lucas Menzel
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2020
Subjects:
Online Access:https://doi.org/10.1080/15230430.2019.1704347
https://doaj.org/article/a9866b9c4e9c4efd956b6279e99baf01
id ftdoajarticles:oai:doaj.org/article:a9866b9c4e9c4efd956b6279e99baf01
record_format openpolar
spelling 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
spellingShingle 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