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Abstract Glacial meltwater has been increasingly recognised as a potential source of atmospheric methane, yet its origin and variability in the High Arctic remain poorly constrained. In this study, we present measurements of methane concentration and carbon‑isotope composition in meltwater draining the northern Greenland Ice Sheet.
Commentary J. G. Ernakovich Corresponding Author jessica.ernakovich@unh.edu orcid.org/0000-0002-4493-2489 Department of Natural Resources and the Environment, University of New Hampshire, Durham, New Hampshire, USA Correspondence J. G. Ernakovich, jessica.ernakovich@unh.edu Search for more papers by this author R. K.
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