The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores
The permafrost organic carbon (OC) stock is of global significance because of its large pool size and the potential positive feedback to climate warming. However, due to the lack of systematic field observations and appropriate upscaling methodologies, substantial uncertainties exist in the permafro...
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GLOBAL CHANGE BIOLOGY
2016
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Online Access: | https://hdl.handle.net/20.500.11897/434757 https://doi.org/10.1111/gcb.13257 |
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ftpekinguniv:oai:localhost:20.500.11897/434757 2023-05-15T15:18:38+02:00 The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores Ding, Jinzhi Li, Fei Yang, Guibiao Chen, Leiyi Zhang, Beibei Liu, Li Fang, Kai Qin, Shuqi Chen, Yongliang Peng, Yunfeng Ji, Chengjun He, Honglin Smith, Pete Yang, Yuanhe Yang, YH (reprint author), Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China. Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China. Univ Chinese Acad Sci, Beijing 100049, Peoples R China. Inner Mongolia Univ Technol, Hohhot 010051, Inner Mongolia, Peoples R China. Peking Univ, Dept Ecol, Beijing 100871, Peoples R China. Peking Univ, Key Lab Earth Surface Proc, Minist Educ, Beijing 100871, Peoples R China. Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China. Univ Aberdeen, Inst Biol & Environm Sci, Aberdeen AB24 3UU, Scotland. 2016 https://hdl.handle.net/20.500.11897/434757 https://doi.org/10.1111/gcb.13257 en eng GLOBAL CHANGE BIOLOGY GLOBAL CHANGE BIOLOGY.2016,22(8),2688-2701. 1390637 1354-1013 http://hdl.handle.net/20.500.11897/434757 1365-2486 doi:10.1111/gcb.13257 26913840 WOS:000380016800005 PubMed SCI alpine permafrost carbon-climate feedback deep sediment soil organic carbon stock support vector machine SOIL ORGANIC-CARBON SUPPORT VECTOR MACHINES CLIMATE-CHANGE ARCTIC REGION VEGETATION CHINA STORAGE GRASSLANDS SIBERIA MATTER Journal 2016 ftpekinguniv https://doi.org/20.500.11897/434757 https://doi.org/10.1111/gcb.13257 2021-08-01T10:48:03Z The permafrost organic carbon (OC) stock is of global significance because of its large pool size and the potential positive feedback to climate warming. However, due to the lack of systematic field observations and appropriate upscaling methodologies, substantial uncertainties exist in the permafrost OC budget, which limits our understanding of the fate of frozen carbon in a warming world. In particular, the lack of comprehensive estimates of OC stocks across alpine permafrost means that current knowledge on this issue remains incomplete. Here, we evaluated the pool size and spatial variations of permafrost OC stock to 3m depth on the Tibetan Plateau by combining systematic measurements from a substantial number of pedons (i.e. 342 three-metre-deep cores and 177 50-cm-deep pits) with a machine learning technique (i.e. support vector machine, SVM). We also quantified uncertainties in permafrost carbon budget by conducting Monte Carlo simulations. Our results revealed that the combination of systematic measurements with the SVM model allowed spatially explicit estimates to be made. The OC density (OC amount per unit area, OCD) exhibited a decreasing trend from the south-eastern to the north-western plateau, with the exception that OCD in the swamp meadow was substantially higher than that in surrounding regions. Our results also demonstrated that Tibetan permafrost stored a large amount of OC in the top 3m, with the median OC pool size being 15.31 Pg C (interquartile range: 13.03-17.77Pg C). 44% of OC occurred in deep layers (i.e. 100-300cm), close to the proportion observed across the northern circumpolar permafrost region. The large carbon pool size together with significant permafrost thawing suggests a risk of carbon emissions and positive climate feedback across the Tibetan alpine permafrost region. National Basic Research Program of China on Global Change [2014CB954001, 2015CB954201]; National Natural Science Foundation of China [31322011, 41371213]; Chinese Acedemy of Sciences-Peking University Pioneer Collaboration Team; Thousand Young Talents Program SCI(E) PubMed ARTICLE yhyang@ibcas.ac.cn 8 2688-2701 22 Journal/Newspaper Arctic Climate change permafrost Siberia Peking University Institutional Repository (PKU IR) Arctic Global Change Biology 22 8 2688 2701 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
alpine permafrost carbon-climate feedback deep sediment soil organic carbon stock support vector machine SOIL ORGANIC-CARBON SUPPORT VECTOR MACHINES CLIMATE-CHANGE ARCTIC REGION VEGETATION CHINA STORAGE GRASSLANDS SIBERIA MATTER |
spellingShingle |
alpine permafrost carbon-climate feedback deep sediment soil organic carbon stock support vector machine SOIL ORGANIC-CARBON SUPPORT VECTOR MACHINES CLIMATE-CHANGE ARCTIC REGION VEGETATION CHINA STORAGE GRASSLANDS SIBERIA MATTER Ding, Jinzhi Li, Fei Yang, Guibiao Chen, Leiyi Zhang, Beibei Liu, Li Fang, Kai Qin, Shuqi Chen, Yongliang Peng, Yunfeng Ji, Chengjun He, Honglin Smith, Pete Yang, Yuanhe The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
topic_facet |
alpine permafrost carbon-climate feedback deep sediment soil organic carbon stock support vector machine SOIL ORGANIC-CARBON SUPPORT VECTOR MACHINES CLIMATE-CHANGE ARCTIC REGION VEGETATION CHINA STORAGE GRASSLANDS SIBERIA MATTER |
description |
The permafrost organic carbon (OC) stock is of global significance because of its large pool size and the potential positive feedback to climate warming. However, due to the lack of systematic field observations and appropriate upscaling methodologies, substantial uncertainties exist in the permafrost OC budget, which limits our understanding of the fate of frozen carbon in a warming world. In particular, the lack of comprehensive estimates of OC stocks across alpine permafrost means that current knowledge on this issue remains incomplete. Here, we evaluated the pool size and spatial variations of permafrost OC stock to 3m depth on the Tibetan Plateau by combining systematic measurements from a substantial number of pedons (i.e. 342 three-metre-deep cores and 177 50-cm-deep pits) with a machine learning technique (i.e. support vector machine, SVM). We also quantified uncertainties in permafrost carbon budget by conducting Monte Carlo simulations. Our results revealed that the combination of systematic measurements with the SVM model allowed spatially explicit estimates to be made. The OC density (OC amount per unit area, OCD) exhibited a decreasing trend from the south-eastern to the north-western plateau, with the exception that OCD in the swamp meadow was substantially higher than that in surrounding regions. Our results also demonstrated that Tibetan permafrost stored a large amount of OC in the top 3m, with the median OC pool size being 15.31 Pg C (interquartile range: 13.03-17.77Pg C). 44% of OC occurred in deep layers (i.e. 100-300cm), close to the proportion observed across the northern circumpolar permafrost region. The large carbon pool size together with significant permafrost thawing suggests a risk of carbon emissions and positive climate feedback across the Tibetan alpine permafrost region. National Basic Research Program of China on Global Change [2014CB954001, 2015CB954201]; National Natural Science Foundation of China [31322011, 41371213]; Chinese Acedemy of Sciences-Peking University Pioneer Collaboration Team; Thousand Young Talents Program SCI(E) PubMed ARTICLE yhyang@ibcas.ac.cn 8 2688-2701 22 |
author2 |
Yang, YH (reprint author), Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China. Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China. Univ Chinese Acad Sci, Beijing 100049, Peoples R China. Inner Mongolia Univ Technol, Hohhot 010051, Inner Mongolia, Peoples R China. Peking Univ, Dept Ecol, Beijing 100871, Peoples R China. Peking Univ, Key Lab Earth Surface Proc, Minist Educ, Beijing 100871, Peoples R China. Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China. Univ Aberdeen, Inst Biol & Environm Sci, Aberdeen AB24 3UU, Scotland. |
format |
Journal/Newspaper |
author |
Ding, Jinzhi Li, Fei Yang, Guibiao Chen, Leiyi Zhang, Beibei Liu, Li Fang, Kai Qin, Shuqi Chen, Yongliang Peng, Yunfeng Ji, Chengjun He, Honglin Smith, Pete Yang, Yuanhe |
author_facet |
Ding, Jinzhi Li, Fei Yang, Guibiao Chen, Leiyi Zhang, Beibei Liu, Li Fang, Kai Qin, Shuqi Chen, Yongliang Peng, Yunfeng Ji, Chengjun He, Honglin Smith, Pete Yang, Yuanhe |
author_sort |
Ding, Jinzhi |
title |
The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
title_short |
The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
title_full |
The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
title_fullStr |
The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
title_full_unstemmed |
The permafrost carbon inventory on the Tibetan Plateau: a new evaluation using deep sediment cores |
title_sort |
permafrost carbon inventory on the tibetan plateau: a new evaluation using deep sediment cores |
publisher |
GLOBAL CHANGE BIOLOGY |
publishDate |
2016 |
url |
https://hdl.handle.net/20.500.11897/434757 https://doi.org/10.1111/gcb.13257 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change permafrost Siberia |
genre_facet |
Arctic Climate change permafrost Siberia |
op_source |
PubMed SCI |
op_relation |
GLOBAL CHANGE BIOLOGY.2016,22(8),2688-2701. 1390637 1354-1013 http://hdl.handle.net/20.500.11897/434757 1365-2486 doi:10.1111/gcb.13257 26913840 WOS:000380016800005 |
op_doi |
https://doi.org/20.500.11897/434757 https://doi.org/10.1111/gcb.13257 |
container_title |
Global Change Biology |
container_volume |
22 |
container_issue |
8 |
container_start_page |
2688 |
op_container_end_page |
2701 |
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1766348828658630656 |