Globally elevated chemical weathering rates beneath glaciers

Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemp...

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Published inNature communications Vol. 13; no. 1; pp. 407 - 13
Main Authors Li, Xiangying, Wang, Ninglian, Ding, Yongjian, Hawkings, Jon R., Yde, Jacob C., Raiswell, Robert, Liu, Jintao, Zhang, Shiqiang, Kang, Shichang, Wang, Rongjun, Liu, Qiao, Liu, Shiyin, Bol, Roland, You, Xiaoni, Li, Guoyu
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 20.01.2022
Nature Publishing Group
Nature Portfolio
Subjects
704/106/125
704/106/242
Air temperature
Biogeochemical cycles
Catchments
Cations
Climate change
Denudation
Erosion rates
Glaciers
Global warming
Humanities and Social Sciences
Ice sheets
Meltwater
multidisciplinary
Nutrient loading
Science
Science (multidisciplinary)
Weathering
Online AccessGet full text

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Abstract Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq + m − 2 year − 1 ) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq + m − 2 year − 1 ), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq + m − 2 year − 1 ) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq + m −2 year − 1 ). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles. 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.
AbstractList Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq + m − 2 year − 1 ) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq + m − 2 year − 1 ), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq + m − 2 year − 1 ) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq + m −2 year − 1 ). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles. 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.
Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq+ m−2 year−1) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq+ m−2 year−1), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq+ m−2 year−1) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq+ m−2 year−1). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles.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.
Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq+ m-2 year-1) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq+ m-2 year-1), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq+ m-2 year-1) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq+ m-2 year-1). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles.Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq+ m-2 year-1) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq+ m-2 year-1), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq+ m-2 year-1) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq+ m-2 year-1). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles.
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.
Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq + m − 2 year − 1 ) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq + m − 2 year − 1 ), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq + m − 2 year − 1 ) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq + m −2 year − 1 ). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles.
Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained. We present a global dataset of cations in meltwaters of 77 glaciers, including new data from 19 Asian glaciers. Our study shows that contemporary cation denudation rates (CDRs) beneath glaciers (2174 ± 977 Σ*meq m year ) are ~3 times higher than two decades ago, up to 10 times higher than ice sheet catchments (~150-2000 Σ*meq m year ), up to 50 times higher than whole ice sheet means (~30-45 Σ*meq m year ) and ~4 times higher than major non-glacial riverine means (~500 Σ*meq m year ). Glacial CDRs are positively correlated with air temperature, suggesting glacial chemical weathering yields are likely to increase in future. Our findings highlight that chemical weathering beneath glaciers is more intense than many other terrestrial systems and may become increasingly important for regional biogeochemical cycles.
ArticleNumber 407
Author Kang, Shichang
Liu, Shiyin
Hawkings, Jon R.
Zhang, Shiqiang
Wang, Rongjun
Ding, Yongjian
Li, Guoyu
Raiswell, Robert
Liu, Qiao
You, Xiaoni
Li, Xiangying
Liu, Jintao
Yde, Jacob C.
Wang, Ninglian
Bol, Roland
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  organization: State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, University of Chinese Academy of Sciences
BackLink https://www.ncbi.nlm.nih.gov/pubmed/35058445$$D View this record in MEDLINE/PubMed
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Snippet Physical erosion and chemical weathering rates beneath glaciers are expected to increase in a warming climate with enhanced melting but are poorly constrained....
Global glacial chemical denudation is one of the largest contributors to global elemental cycles and, amplified by climate warming, will significantly impact...
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SubjectTerms 704/106/125
704/106/242
Air temperature
Biogeochemical cycles
Catchments
Cations
Climate change
Denudation
Erosion rates
Glaciers
Global warming
Humanities and Social Sciences
Ice sheets
Meltwater
multidisciplinary
Nutrient loading
Science
Science (multidisciplinary)
Weathering
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Title Globally elevated chemical weathering rates beneath glaciers
URI https://link.springer.com/article/10.1038/s41467-022-28032-1
https://www.ncbi.nlm.nih.gov/pubmed/35058445
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Volume 13
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