Globally elevated chemical weathering rates beneath glaciers

Global glacial chemical denudation is one of the largest contributors to global elemental cycles and, amplified by climate warming, will significantly impact nutrient loads in downstream ecosystems.

Bibliographic Details
Main Authors: Xiangying Li, Ninglian Wang, Yongjian Ding, Jon R. Hawkings, Jacob C. Yde, Robert Raiswell, Jintao Liu, Shiqiang Zhang, Shichang Kang, Rongjun Wang, Qiao Liu, Shiyin Liu, Roland Bol, Xiaoni You, Guoyu Li
Format: Article
Language:English
Published: Nature Portfolio 2022-01-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-022-28032-1
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author Xiangying Li
Ninglian Wang
Yongjian Ding
Jon R. Hawkings
Jacob C. Yde
Robert Raiswell
Jintao Liu
Shiqiang Zhang
Shichang Kang
Rongjun Wang
Qiao Liu
Shiyin Liu
Roland Bol
Xiaoni You
Guoyu Li
author_facet Xiangying Li
Ninglian Wang
Yongjian Ding
Jon R. Hawkings
Jacob C. Yde
Robert Raiswell
Jintao Liu
Shiqiang Zhang
Shichang Kang
Rongjun Wang
Qiao Liu
Shiyin Liu
Roland Bol
Xiaoni You
Guoyu Li
author_sort Xiangying Li
collection DOAJ
description Global glacial chemical denudation is one of the largest contributors to global elemental cycles and, amplified by climate warming, will significantly impact nutrient loads in downstream ecosystems.
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spelling doaj.art-2cb19bf506a74798b88659a3791a4edd2022-12-21T23:43:16ZengNature PortfolioNature Communications2041-17232022-01-0113111310.1038/s41467-022-28032-1Globally elevated chemical weathering rates beneath glaciersXiangying Li0Ninglian Wang1Yongjian Ding2Jon R. Hawkings3Jacob C. Yde4Robert Raiswell5Jintao Liu6Shiqiang Zhang7Shichang Kang8Rongjun Wang9Qiao Liu10Shiyin Liu11Roland Bol12Xiaoni You13Guoyu Li14Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest UniversityShaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest UniversityState Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesDepartment of Earth and Environmental Science, University of PennsylvaniaDepartment of Environmental Sciences, Western Norway University of Applied SciencesCohen Biogeochemistry Laboratory, School of Earth and Environment, University of LeedsCollege of Hydrology and Water Resources, Hohai UniversityShaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest UniversityState Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesState Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of International Rivers and Eco-security, Yunnan UniversityForschungszentrum Jülich IBG-3, Wilhelm-Johnen-StraßeCollege of Resources and Environmental Engineering, Tianshui Normal UniversityState Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesGlobal glacial chemical denudation is one of the largest contributors to global elemental cycles and, amplified by climate warming, will significantly impact nutrient loads in downstream ecosystems.https://doi.org/10.1038/s41467-022-28032-1
spellingShingle Xiangying Li
Ninglian Wang
Yongjian Ding
Jon R. Hawkings
Jacob C. Yde
Robert Raiswell
Jintao Liu
Shiqiang Zhang
Shichang Kang
Rongjun Wang
Qiao Liu
Shiyin Liu
Roland Bol
Xiaoni You
Guoyu Li
Globally elevated chemical weathering rates beneath glaciers
Nature Communications
title Globally elevated chemical weathering rates beneath glaciers
title_full Globally elevated chemical weathering rates beneath glaciers
title_fullStr Globally elevated chemical weathering rates beneath glaciers
title_full_unstemmed Globally elevated chemical weathering rates beneath glaciers
title_short Globally elevated chemical weathering rates beneath glaciers
title_sort globally elevated chemical weathering rates beneath glaciers
url https://doi.org/10.1038/s41467-022-28032-1
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