Impacts of climate-induced permafrost degradation on vegetation: A review
Under a warming climate, degrading permafrost profoundly and extensively affects arctic and alpine ecology. However, most existing relevant studies are more focused on the hydrothermal impacts of vegetation on the underlying permafrost, or symbiosis between vegetation and permafrost, only very few o...
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Format: | Article |
Language: | English |
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KeAi Communications Co., Ltd.
2021-02-01
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Series: | Advances in Climate Change Research |
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Online Access: | http://www.sciencedirect.com/science/article/pii/S1674927820300605 |
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doaj-8bb120c6291b46f78222b44d76b826d5 |
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record_format |
Article |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xiao-Ying Jin Hui-Jun Jin Go Iwahana Sergey S. Marchenko Dong-Liang Luo Xiao-Ying Li Si-Hai Liang |
spellingShingle |
Xiao-Ying Jin Hui-Jun Jin Go Iwahana Sergey S. Marchenko Dong-Liang Luo Xiao-Ying Li Si-Hai Liang Impacts of climate-induced permafrost degradation on vegetation: A review Advances in Climate Change Research Degrading permafrost Vegetation Impact mechanisms Climate warming Ecological impacts |
author_facet |
Xiao-Ying Jin Hui-Jun Jin Go Iwahana Sergey S. Marchenko Dong-Liang Luo Xiao-Ying Li Si-Hai Liang |
author_sort |
Xiao-Ying Jin |
title |
Impacts of climate-induced permafrost degradation on vegetation: A review |
title_short |
Impacts of climate-induced permafrost degradation on vegetation: A review |
title_full |
Impacts of climate-induced permafrost degradation on vegetation: A review |
title_fullStr |
Impacts of climate-induced permafrost degradation on vegetation: A review |
title_full_unstemmed |
Impacts of climate-induced permafrost degradation on vegetation: A review |
title_sort |
impacts of climate-induced permafrost degradation on vegetation: a review |
publisher |
KeAi Communications Co., Ltd. |
series |
Advances in Climate Change Research |
issn |
1674-9278 |
publishDate |
2021-02-01 |
description |
Under a warming climate, degrading permafrost profoundly and extensively affects arctic and alpine ecology. However, most existing relevant studies are more focused on the hydrothermal impacts of vegetation on the underlying permafrost, or symbiosis between vegetation and permafrost, only very few on ecological impacts of permafrost degradation. Additionally, there are much more pertinent investigations in arctic and boreal regions than those in alpine and high-plateau regions at mid- and low latitudes. This study emphasizes on the impact mechanisms of permafrost degradation on vegetation both at high and mid-to low latitudes, addressing vegetation succession trajectories and associated changes in soil hydrology and soil nutrient above degrading permafrost. Permafrost degradation influences vegetation by altering soil hydrology, soil biogeochemical processes and microbial communities, which further improve soil nutrient availability. Furthermore, under a warming climate, vegetation may take two successional trajectories, towards a wetter or drier ecosystem within a certain time period, but to a drier ecosystem in the end upon the thaw of permafrost in case of permeable soils and good drainage. Thus, with rapidly developing remote-sensing and other space- and ground-based and air-borne observational networks and numerical predictive models, the impacting mechanisms of permafrost degradation on vegetation should be timely and better monitored, evaluated and modeled at desired spatiotemporal scales and resolutions by terrestrial or integrated ecosystem models. |
topic |
Degrading permafrost Vegetation Impact mechanisms Climate warming Ecological impacts |
url |
http://www.sciencedirect.com/science/article/pii/S1674927820300605 |
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doaj-8bb120c6291b46f78222b44d76b826d52021-03-17T04:13:51ZengKeAi Communications Co., Ltd.Advances in Climate Change Research1674-92782021-02-011212947Impacts of climate-induced permafrost degradation on vegetation: A reviewXiao-Ying Jin0Hui-Jun Jin1Go Iwahana2Sergey S. Marchenko3Dong-Liang Luo4Xiao-Ying Li5Si-Hai Liang6Northeast-China Observatory and Research Station of Permafrost Geological Environment (Ministry of Education), School of Civil Engineering, Institute of Cold Region Science and Technology, Northeast Forestry University, Harbin, 150040, China; State Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 100049, ChinaNortheast-China Observatory and Research Station of Permafrost Geological Environment (Ministry of Education), School of Civil Engineering, Institute of Cold Region Science and Technology, Northeast Forestry University, Harbin, 150040, China; State Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 100049, China; Corresponding author. Northeast-China Observatory and Research-Station of Permafrost Geo-Environment-Ministry of Education, Institute of ColdRegions Engineering and Environment and School of Civil Engineering, Northeast Forestry University, Harbin, 150040, China.International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, 99775, USAPermafrost Lab, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, 99775, USAState Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, ChinaNortheast-China Observatory and Research Station of Permafrost Geological Environment (Ministry of Education), School of Civil Engineering, Institute of Cold Region Science and Technology, Northeast Forestry University, Harbin, 150040, China; State Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 100049, ChinaSchool of Water Resources and Environment, China University of Geosciences, Beijing, 100083, ChinaUnder a warming climate, degrading permafrost profoundly and extensively affects arctic and alpine ecology. However, most existing relevant studies are more focused on the hydrothermal impacts of vegetation on the underlying permafrost, or symbiosis between vegetation and permafrost, only very few on ecological impacts of permafrost degradation. Additionally, there are much more pertinent investigations in arctic and boreal regions than those in alpine and high-plateau regions at mid- and low latitudes. This study emphasizes on the impact mechanisms of permafrost degradation on vegetation both at high and mid-to low latitudes, addressing vegetation succession trajectories and associated changes in soil hydrology and soil nutrient above degrading permafrost. Permafrost degradation influences vegetation by altering soil hydrology, soil biogeochemical processes and microbial communities, which further improve soil nutrient availability. Furthermore, under a warming climate, vegetation may take two successional trajectories, towards a wetter or drier ecosystem within a certain time period, but to a drier ecosystem in the end upon the thaw of permafrost in case of permeable soils and good drainage. Thus, with rapidly developing remote-sensing and other space- and ground-based and air-borne observational networks and numerical predictive models, the impacting mechanisms of permafrost degradation on vegetation should be timely and better monitored, evaluated and modeled at desired spatiotemporal scales and resolutions by terrestrial or integrated ecosystem models.http://www.sciencedirect.com/science/article/pii/S1674927820300605Degrading permafrostVegetationImpact mechanismsClimate warmingEcological impacts |