21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia

Permafrost in Mongolia is at the southern edge of the Siberian permafrost, which is most vulnerable to climate change. In this study, we used ERA5-Land data to determine the distribution of permafrost in Mongolia, and used MIROC5 data for future projection of the soil temperature. The future change...

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Main Authors: Adiya, Saruulzaya, Erdenebat, Enkhbat
Format: Article in Journal/Newspaper
Language:English
Published: Mongolian Academy of Sciences 2021
Subjects:
Online Access:https://www.mongoliajol.info/index.php/PMAS/article/view/1927
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author Adiya, Saruulzaya
Erdenebat, Enkhbat
author_facet Adiya, Saruulzaya
Erdenebat, Enkhbat
author_sort Adiya, Saruulzaya
collection Mongolia Journals Online
description Permafrost in Mongolia is at the southern edge of the Siberian permafrost, which is most vulnerable to climate change. In this study, we used ERA5-Land data to determine the distribution of permafrost in Mongolia, and used MIROC5 data for future projection of the soil temperature. The future change of soil temperature obtained during 2020–2100 under Representative Concentration Pathways (RCP) scenarios was RCP 2.6 and RCP 8.5 respectively. This is a first attempt to identify the distribution of permafrost using ERA5-Land data in Mongolia. We examined the projection of permafrost distribution using RCP 2.6 and RCP 8.5 scenarios in Mongolia. The rapid increase of near-surface temperature was obtained in RCP8.5 scenario during 2020-2100. Soil temperature also has a high increasing trend similar to the near-surface temperature in the RCP 8.5 scenario. Future projection suggests that permafrost will completely thaw in Mongolia when area-averaged soil temperature in Mongolia exceeds 1.8°C in comparison with the current climate.
format Article in Journal/Newspaper
genre permafrost
genre_facet permafrost
id ftmongoliajo:oai:mongoliajol:article/1927
institution Open Polar
language English
op_collection_id ftmongoliajo
op_relation https://www.mongoliajol.info/index.php/PMAS/article/view/1927/2125
https://www.mongoliajol.info/index.php/PMAS/article/view/1927
op_rights Copyright (c) 2021 Saruulzaya Adiya, Enkhbat Erdenebat
http://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_source Proceedings of the Mongolian Academy of Sciences; Vol. 61 No 04 (240) 2021; 9-14
2312-2994
2310-4716
publishDate 2021
publisher Mongolian Academy of Sciences
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spelling ftmongoliajo:oai:mongoliajol:article/1927 2025-01-17T00:12:36+00:00 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia Adiya, Saruulzaya Erdenebat, Enkhbat 2021-12-22 application/pdf https://www.mongoliajol.info/index.php/PMAS/article/view/1927 eng eng Mongolian Academy of Sciences https://www.mongoliajol.info/index.php/PMAS/article/view/1927/2125 https://www.mongoliajol.info/index.php/PMAS/article/view/1927 Copyright (c) 2021 Saruulzaya Adiya, Enkhbat Erdenebat http://creativecommons.org/licenses/by/4.0 CC-BY Proceedings of the Mongolian Academy of Sciences; Vol. 61 No 04 (240) 2021; 9-14 2312-2994 2310-4716 permafrost RCP2.6 RCP8.5 Mongolia info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-Reviewed Article 2021 ftmongoliajo 2022-12-11T16:12:37Z Permafrost in Mongolia is at the southern edge of the Siberian permafrost, which is most vulnerable to climate change. In this study, we used ERA5-Land data to determine the distribution of permafrost in Mongolia, and used MIROC5 data for future projection of the soil temperature. The future change of soil temperature obtained during 2020–2100 under Representative Concentration Pathways (RCP) scenarios was RCP 2.6 and RCP 8.5 respectively. This is a first attempt to identify the distribution of permafrost using ERA5-Land data in Mongolia. We examined the projection of permafrost distribution using RCP 2.6 and RCP 8.5 scenarios in Mongolia. The rapid increase of near-surface temperature was obtained in RCP8.5 scenario during 2020-2100. Soil temperature also has a high increasing trend similar to the near-surface temperature in the RCP 8.5 scenario. Future projection suggests that permafrost will completely thaw in Mongolia when area-averaged soil temperature in Mongolia exceeds 1.8°C in comparison with the current climate. Article in Journal/Newspaper permafrost Mongolia Journals Online
spellingShingle permafrost
RCP2.6
RCP8.5
Mongolia
Adiya, Saruulzaya
Erdenebat, Enkhbat
21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title_full 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title_fullStr 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title_full_unstemmed 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title_short 21st century permafrost distribution under the scenario of RCP2.6 and RCP8.5 in Mongolia
title_sort 21st century permafrost distribution under the scenario of rcp2.6 and rcp8.5 in mongolia
topic permafrost
RCP2.6
RCP8.5
Mongolia
topic_facet permafrost
RCP2.6
RCP8.5
Mongolia
url https://www.mongoliajol.info/index.php/PMAS/article/view/1927