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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Format: | Article in Journal/Newspaper |
Language: | English |
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Mongolian Academy of Sciences
2021
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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 |
record_format | openpolar |
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 |