Nature Communications (Jan 2022)
Globally elevated chemical weathering rates beneath glaciers
- 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
Affiliations
- Xiangying Li
- Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest University
- Ninglian Wang
- Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest University
- Yongjian Ding
- State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Jon R. Hawkings
- Department of Earth and Environmental Science, University of Pennsylvania
- Jacob C. Yde
- Department of Environmental Sciences, Western Norway University of Applied Sciences
- Robert Raiswell
- Cohen Biogeochemistry Laboratory, School of Earth and Environment, University of Leeds
- Jintao Liu
- College of Hydrology and Water Resources, Hohai University
- Shiqiang Zhang
- Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest University
- Shichang Kang
- State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Rongjun Wang
- State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Qiao Liu
- Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
- Shiyin Liu
- Institute of International Rivers and Eco-security, Yunnan University
- Roland Bol
- Forschungszentrum Jülich IBG-3, Wilhelm-Johnen-Straße
- Xiaoni You
- College of Resources and Environmental Engineering, Tianshui Normal University
- Guoyu Li
- State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- DOI
- https://doi.org/10.1038/s41467-022-28032-1
- Journal volume & issue
-
Vol. 13,
no. 1
pp. 1 – 13
Abstract
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.
