Sources of black carbon to the Himalayan–Tibetan Plateau glaciers

Black carbon accelerates melting of glaciers in the Himalayas and Tibet, yet the source of these aerosols remains enigmatic. Here, the authors use isotope fingerprinting techniques to determine the origin of black carbon preserved in glacier ice cores recovered from the Himalayas and Tibetan Plateau...

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Main Authors: Chaoliu Li, Carme Bosch, Shichang Kang, August Andersson, Pengfei Chen, Qianggong Zhang, Zhiyuan Cong, Bing Chen, Dahe Qin, Örjan Gustafsson
Format: Article
Language:English
Published: Nature Publishing Group 2016-08-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/ncomms12574
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spelling doaj-ae54dfae814f4aab876cdb09961e60c82021-05-11T11:04:55ZengNature Publishing GroupNature Communications2041-17232016-08-01711710.1038/ncomms12574Sources of black carbon to the Himalayan–Tibetan Plateau glaciersChaoliu Li0Carme Bosch1Shichang Kang2August Andersson3Pengfei Chen4Qianggong Zhang5Zhiyuan Cong6Bing Chen7Dahe Qin8Örjan Gustafsson9Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS)Department of Environmental Science and Analytical Chemistry; The Bolin Centre for Climate Research, Stockholm UniversityCAS Center for Excellence in Tibetan Plateau Earth SciencesDepartment of Environmental Science and Analytical Chemistry; The Bolin Centre for Climate Research, Stockholm UniversityKey Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS)Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS)Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS)Environmental Research Institute, School of Environmental Science and Engineering, Shandong UniversityState Key Laboratory of Cryosphere Science, Cold and Arid Regions Environmental and Engineering Research Institute, CASDepartment of Environmental Science and Analytical Chemistry; The Bolin Centre for Climate Research, Stockholm UniversityBlack carbon accelerates melting of glaciers in the Himalayas and Tibet, yet the source of these aerosols remains enigmatic. Here, the authors use isotope fingerprinting techniques to determine the origin of black carbon preserved in glacier ice cores recovered from the Himalayas and Tibetan Plateau.https://doi.org/10.1038/ncomms12574
collection DOAJ
language English
format Article
sources DOAJ
author Chaoliu Li
Carme Bosch
Shichang Kang
August Andersson
Pengfei Chen
Qianggong Zhang
Zhiyuan Cong
Bing Chen
Dahe Qin
Örjan Gustafsson
spellingShingle Chaoliu Li
Carme Bosch
Shichang Kang
August Andersson
Pengfei Chen
Qianggong Zhang
Zhiyuan Cong
Bing Chen
Dahe Qin
Örjan Gustafsson
Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
Nature Communications
author_facet Chaoliu Li
Carme Bosch
Shichang Kang
August Andersson
Pengfei Chen
Qianggong Zhang
Zhiyuan Cong
Bing Chen
Dahe Qin
Örjan Gustafsson
author_sort Chaoliu Li
title Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
title_short Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
title_full Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
title_fullStr Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
title_full_unstemmed Sources of black carbon to the Himalayan–Tibetan Plateau glaciers
title_sort sources of black carbon to the himalayan–tibetan plateau glaciers
publisher Nature Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2016-08-01
description Black carbon accelerates melting of glaciers in the Himalayas and Tibet, yet the source of these aerosols remains enigmatic. Here, the authors use isotope fingerprinting techniques to determine the origin of black carbon preserved in glacier ice cores recovered from the Himalayas and Tibetan Plateau.
url https://doi.org/10.1038/ncomms12574
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