Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios

As an important parameter in permafrost research, the annual ground surface freezing/thawing index is widely used in the variation of permafrost. In addition, it is also an important indicator in climatology, providing a large amount of theoretical basis for the assessment of climate change. Based o...

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Published in:Sustainability
Main Authors: Xianglong Li, Ze Zhang, Andrey Melnikov, Mingyi Zhang, Doudou Jin, Jinbang Zhai
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
SSP
Online Access:https://doi.org/10.3390/su142114458
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spelling ftmdpi:oai:mdpi.com:/2071-1050/14/21/14458/ 2023-08-20T04:09:12+02:00 Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios Xianglong Li Ze Zhang Andrey Melnikov Mingyi Zhang Doudou Jin Jinbang Zhai agris 2022-11-03 application/pdf https://doi.org/10.3390/su142114458 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/su142114458 https://creativecommons.org/licenses/by/4.0/ Sustainability; Volume 14; Issue 21; Pages: 14458 China ground surface freezing/thawing index CMIP6 SSP warming scenarios Text 2022 ftmdpi https://doi.org/10.3390/su142114458 2023-08-01T07:11:04Z As an important parameter in permafrost research, the annual ground surface freezing/thawing index is widely used in the variation of permafrost. In addition, it is also an important indicator in climatology, providing a large amount of theoretical basis for the assessment of climate change. Based on the ground surface temperature data recorded at 707 meteorological stations from 1960 to 2020, the ground surface freezing/thawing index in China were calculated. The results showed that over the past six decades, the thawing index has shown an upward trend, whereas the freezing index has shown a downward trend, and the trend is stronger around 2000. The results of the R/S-based analysis indicate that the freezing/thawing index will remain on a decreasing/increasing trend for some time to come. Based on the five warming scenarios published by Coupled Model Intercomparison Project Phase 6 (CMIP6), the spatial–temporal variation characteristics of the ground surface freezing/thawing index in China during 2020–2100 was simulated. It was found that under SSP3-7.0 and SSP5-8.5 scenarios, the freezing/thawing index may be 0 °C-days in 2080 and 2070, respectively, which may imply that the ground surface freezing process in some regions of China may disappear. Text permafrost MDPI Open Access Publishing Sustainability 14 21 14458
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic China
ground surface freezing/thawing index
CMIP6
SSP
warming scenarios
spellingShingle China
ground surface freezing/thawing index
CMIP6
SSP
warming scenarios
Xianglong Li
Ze Zhang
Andrey Melnikov
Mingyi Zhang
Doudou Jin
Jinbang Zhai
Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
topic_facet China
ground surface freezing/thawing index
CMIP6
SSP
warming scenarios
description As an important parameter in permafrost research, the annual ground surface freezing/thawing index is widely used in the variation of permafrost. In addition, it is also an important indicator in climatology, providing a large amount of theoretical basis for the assessment of climate change. Based on the ground surface temperature data recorded at 707 meteorological stations from 1960 to 2020, the ground surface freezing/thawing index in China were calculated. The results showed that over the past six decades, the thawing index has shown an upward trend, whereas the freezing index has shown a downward trend, and the trend is stronger around 2000. The results of the R/S-based analysis indicate that the freezing/thawing index will remain on a decreasing/increasing trend for some time to come. Based on the five warming scenarios published by Coupled Model Intercomparison Project Phase 6 (CMIP6), the spatial–temporal variation characteristics of the ground surface freezing/thawing index in China during 2020–2100 was simulated. It was found that under SSP3-7.0 and SSP5-8.5 scenarios, the freezing/thawing index may be 0 °C-days in 2080 and 2070, respectively, which may imply that the ground surface freezing process in some regions of China may disappear.
format Text
author Xianglong Li
Ze Zhang
Andrey Melnikov
Mingyi Zhang
Doudou Jin
Jinbang Zhai
author_facet Xianglong Li
Ze Zhang
Andrey Melnikov
Mingyi Zhang
Doudou Jin
Jinbang Zhai
author_sort Xianglong Li
title Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
title_short Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
title_full Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
title_fullStr Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
title_full_unstemmed Variation of Ground Surface Freezing/Thawing Index in China under the CMIP6 Warming Scenarios
title_sort variation of ground surface freezing/thawing index in china under the cmip6 warming scenarios
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/su142114458
op_coverage agris
genre permafrost
genre_facet permafrost
op_source Sustainability; Volume 14; Issue 21; Pages: 14458
op_relation https://dx.doi.org/10.3390/su142114458
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/su142114458
container_title Sustainability
container_volume 14
container_issue 21
container_start_page 14458
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