Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming

Given the current confirmed permafrost degradation and its considerable impacts on ecosystems, water resources, infrastructure and climate, there is great interest in understanding the causes of permafrost degradation. Using the surface frost index (SFI) model and multimodel data from the fifth phas...

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Main Authors: Donglin Guo, Jianqi Sun, Huixin Li, Tingjun Zhang, Vladimir E Romanovsky
Format: Article
Language:English
Published: IOP Publishing 2020-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ab926f
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author Donglin Guo
Jianqi Sun
Huixin Li
Tingjun Zhang
Vladimir E Romanovsky
author_facet Donglin Guo
Jianqi Sun
Huixin Li
Tingjun Zhang
Vladimir E Romanovsky
author_sort Donglin Guo
collection DOAJ
description Given the current confirmed permafrost degradation and its considerable impacts on ecosystems, water resources, infrastructure and climate, there is great interest in understanding the causes of permafrost degradation. Using the surface frost index (SFI) model and multimodel data from the fifth phase of the Coupled Model Intercomparison Project (CMIP5), this study, for the first time, investigates external anthropogenic and natural forcing impacts on historical (1921–2005) near-surface permafrost change in the Northern Hemisphere. The results show that anthropogenic greenhouse gas (GHG) forcing produces a significant decrease in the area of near-surface permafrost distribution at a rate of 0.46 × 10 ^6 km ^2 decade ^−1 , similar to observations and the historical simulation (ALL). Anthropogenic aerosol (AA) forcing yields an increase in near-surface permafrost distribution area at a rate of 0.25 × 10 ^6 km ^2 decade ^−1 . Under natural (NAT) forcing, there is a weak trend and distinct decadal variability in near-surface permafrost area. The effects of ALL and GHG forcings are detectable in the observed change in historical near-surface permafrost area, but the effects of NAT and AA forcings are not detected using the optimal fingerprint methods. This indicates that the observed near-surface permafrost degradation can be largely attributed to GHG-induced warming, which has decreased the near-surface permafrost area in the Northern Hemisphere by approximately 0. 21 × 10 ^6 km ^2 decade ^−1 on average over the study period, according to the attribution analysis.
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spelling doaj.art-114712b82a774c84817d5fc862325faf2023-08-09T15:09:06ZengIOP PublishingEnvironmental Research Letters1748-93262020-01-0115808404010.1088/1748-9326/ab926fAttribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warmingDonglin Guo0https://orcid.org/0000-0002-3078-6556Jianqi Sun1Huixin Li2Tingjun Zhang3Vladimir E Romanovsky4Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; Key Laboratory of Meteorological Disaster, Ministry of Education/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology , Nanjing, People’s Republic of ChinaNansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of ChinaKey Laboratory of Meteorological Disaster, Ministry of Education/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology , Nanjing, People’s Republic of ChinaKey Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University , Lanzhou, People’s Republic of ChinaGeophysical Institute, University of Alaska Fairbanks , Fairbanks AK 99775 AK, United States of AmericaGiven the current confirmed permafrost degradation and its considerable impacts on ecosystems, water resources, infrastructure and climate, there is great interest in understanding the causes of permafrost degradation. Using the surface frost index (SFI) model and multimodel data from the fifth phase of the Coupled Model Intercomparison Project (CMIP5), this study, for the first time, investigates external anthropogenic and natural forcing impacts on historical (1921–2005) near-surface permafrost change in the Northern Hemisphere. The results show that anthropogenic greenhouse gas (GHG) forcing produces a significant decrease in the area of near-surface permafrost distribution at a rate of 0.46 × 10 ^6 km ^2 decade ^−1 , similar to observations and the historical simulation (ALL). Anthropogenic aerosol (AA) forcing yields an increase in near-surface permafrost distribution area at a rate of 0.25 × 10 ^6 km ^2 decade ^−1 . Under natural (NAT) forcing, there is a weak trend and distinct decadal variability in near-surface permafrost area. The effects of ALL and GHG forcings are detectable in the observed change in historical near-surface permafrost area, but the effects of NAT and AA forcings are not detected using the optimal fingerprint methods. This indicates that the observed near-surface permafrost degradation can be largely attributed to GHG-induced warming, which has decreased the near-surface permafrost area in the Northern Hemisphere by approximately 0. 21 × 10 ^6 km ^2 decade ^−1 on average over the study period, according to the attribution analysis.https://doi.org/10.1088/1748-9326/ab926fpermafrostanthropogenic forcingnatural forcingair temperature
spellingShingle Donglin Guo
Jianqi Sun
Huixin Li
Tingjun Zhang
Vladimir E Romanovsky
Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
Environmental Research Letters
permafrost
anthropogenic forcing
natural forcing
air temperature
title Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
title_full Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
title_fullStr Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
title_full_unstemmed Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
title_short Attribution of historical near-surface permafrost degradation to anthropogenic greenhouse gas warming
title_sort attribution of historical near surface permafrost degradation to anthropogenic greenhouse gas warming
topic permafrost
anthropogenic forcing
natural forcing
air temperature
url https://doi.org/10.1088/1748-9326/ab926f
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