Articles | Volume 20, issue 12
https://doi.org/10.5194/bg-20-2301-2023
https://doi.org/10.5194/bg-20-2301-2023
Research article
 | 
21 Jun 2023
Research article |  | 21 Jun 2023

Glacier loss and vegetation expansion alter organic and inorganic carbon dynamics in high-mountain streams

Andrew L. Robison, Nicola Deluigi, Camille Rolland, Nicolas Manetti, and Tom Battin

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This preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).
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Cited articles

Anderson, S. P., Drever, J. I., and Humphrey, N. F.: Chemical weathering in glacial environments, Geology, 25, 399–402, https://doi.org/10.1130/0091-7613(1997)025<0399:CWIGE>2.3.CO, 1997. 
Begum, M. S., Park, J. H., Yang, L., Shin, K. H., and Hur, J.: Optical and molecular indices of dissolved organic matter for estimating biodegradability and resulting carbon dioxide production in inland waters: A review, Water Res., 228, 119362, https://doi.org/10.1016/j.watres.2022.119362, 2023. 
Bergstrom, A., Koch, J. C., O'Nee, S., and Baker, E.: Seasonality of solute flux and water source chemistry in a coastal glacierized watershed undergoing rapid change: Wolverine Glacier watershed, Alaska, Water Resour. Res., 57, e2020WR028725, https://doi.org/10.1029/2020WR028725, 2021. 
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Climate change is affecting mountain ecosystems intensely, including the loss of glaciers and the uphill migration of plants. How these changes will affect the streams draining these landscapes is unclear. We sampled streams across a gradient of glacier and vegetation cover in Switzerland and found glacier loss reduced the carbon dioxide sink from weathering, while vegetation cover increased dissolved organic carbon in the stream. These changes are important to consider for mountains globally.
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