Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia

Mongolia is one of the most sensitive regions to climate change, located in the transition of several natural and permafrost zones. Long-term trends in air freezing and thawing indices can therefore enhance our understanding of climate change. This study focuses on changes of the spatiotemporal patt...

Full description

Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Dashtseren, Avirmed, Temuujin, Khurelbaatar, Westermann, Sebastian, Batbold, Altangerel, Amarbayasgalan, Yondon, Battogtokh, Dorjgotov
Other Authors: Norges Forskningsråd
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2021
Subjects:
Online Access:http://dx.doi.org/10.3389/feart.2021.713498
https://www.frontiersin.org/articles/10.3389/feart.2021.713498/full
id crfrontiers:10.3389/feart.2021.713498
record_format openpolar
spelling crfrontiers:10.3389/feart.2021.713498 2024-09-15T18:29:58+00:00 Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia Dashtseren, Avirmed Temuujin, Khurelbaatar Westermann, Sebastian Batbold, Altangerel Amarbayasgalan, Yondon Battogtokh, Dorjgotov Norges Forskningsråd 2021 http://dx.doi.org/10.3389/feart.2021.713498 https://www.frontiersin.org/articles/10.3389/feart.2021.713498/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Earth Science volume 9 ISSN 2296-6463 journal-article 2021 crfrontiers https://doi.org/10.3389/feart.2021.713498 2024-08-20T04:04:24Z Mongolia is one of the most sensitive regions to climate change, located in the transition of several natural and permafrost zones. Long-term trends in air freezing and thawing indices can therefore enhance our understanding of climate change. This study focuses on changes of the spatiotemporal patterns in air freezing and thawing indices over Mongolia from 1960 to 2020, using observations at 30 meteorological stations. Our results shows that the freezing index ranges from −945.5 to −4,793.6°C day, while the thawing index ranges from 1,164.4 to 4,021.3°C day over Mongolia, and their spatial patterns clearly link to the latitude and altitude. During the study period, the trend in the thawing index (14.4°C-day per year) was larger than the trend in the freezing index (up to −10.1°C-day per year), which results in the net increase of air temperature by 2.4°C across Mongolia. Overall, the increase in the thawing index was larger in the low latitudes and altitudes (e.g., the Gobi-desert, steppes, the Great lake depression and major river valleys) than in high latitudes and altitudes (mountain regions), while it was the opposite for the freezing index. The highest values for both thawing index and freezing index (i.e. the least negative values) have occurred during the last 2 decades. As the trends in the freezing and thawing indices and mean annual air temperature confirm intensive climate warming, increased permafrost degradation and shallower seasonally frozen ground are expected throughout Mongolia. Article in Journal/Newspaper permafrost Frontiers (Publisher) Frontiers in Earth Science 9
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description Mongolia is one of the most sensitive regions to climate change, located in the transition of several natural and permafrost zones. Long-term trends in air freezing and thawing indices can therefore enhance our understanding of climate change. This study focuses on changes of the spatiotemporal patterns in air freezing and thawing indices over Mongolia from 1960 to 2020, using observations at 30 meteorological stations. Our results shows that the freezing index ranges from −945.5 to −4,793.6°C day, while the thawing index ranges from 1,164.4 to 4,021.3°C day over Mongolia, and their spatial patterns clearly link to the latitude and altitude. During the study period, the trend in the thawing index (14.4°C-day per year) was larger than the trend in the freezing index (up to −10.1°C-day per year), which results in the net increase of air temperature by 2.4°C across Mongolia. Overall, the increase in the thawing index was larger in the low latitudes and altitudes (e.g., the Gobi-desert, steppes, the Great lake depression and major river valleys) than in high latitudes and altitudes (mountain regions), while it was the opposite for the freezing index. The highest values for both thawing index and freezing index (i.e. the least negative values) have occurred during the last 2 decades. As the trends in the freezing and thawing indices and mean annual air temperature confirm intensive climate warming, increased permafrost degradation and shallower seasonally frozen ground are expected throughout Mongolia.
author2 Norges Forskningsråd
format Article in Journal/Newspaper
author Dashtseren, Avirmed
Temuujin, Khurelbaatar
Westermann, Sebastian
Batbold, Altangerel
Amarbayasgalan, Yondon
Battogtokh, Dorjgotov
spellingShingle Dashtseren, Avirmed
Temuujin, Khurelbaatar
Westermann, Sebastian
Batbold, Altangerel
Amarbayasgalan, Yondon
Battogtokh, Dorjgotov
Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
author_facet Dashtseren, Avirmed
Temuujin, Khurelbaatar
Westermann, Sebastian
Batbold, Altangerel
Amarbayasgalan, Yondon
Battogtokh, Dorjgotov
author_sort Dashtseren, Avirmed
title Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
title_short Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
title_full Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
title_fullStr Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
title_full_unstemmed Spatial and Temporal Variations of Freezing and Thawing Indices From 1960 to 2020 in Mongolia
title_sort spatial and temporal variations of freezing and thawing indices from 1960 to 2020 in mongolia
publisher Frontiers Media SA
publishDate 2021
url http://dx.doi.org/10.3389/feart.2021.713498
https://www.frontiersin.org/articles/10.3389/feart.2021.713498/full
genre permafrost
genre_facet permafrost
op_source Frontiers in Earth Science
volume 9
ISSN 2296-6463
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/feart.2021.713498
container_title Frontiers in Earth Science
container_volume 9
_version_ 1810471453726867456