Articles | Volume 10, issue 1
The Cryosphere, 10, 433–444, 2016
https://doi.org/10.5194/tc-10-433-2016
The Cryosphere, 10, 433–444, 2016
https://doi.org/10.5194/tc-10-433-2016

Research article 29 Feb 2016

Research article | 29 Feb 2016

Bulk meltwater flow and liquid water content of snowpacks mapped using the electrical self-potential (SP) method

Sarah S. Thompson et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Svenja Lange on behalf of the Authors (15 Jan 2016)  Author's response
ED: Referee Nomination & Report Request started (20 Jan 2016) by Olaf Eisen
RR by Anonymous Referee #2 (25 Jan 2016)
RR by Anonymous Referee #1 (26 Jan 2016)
ED: Publish subject to minor revisions (Editor review) (27 Jan 2016) by Olaf Eisen
AR by Sarah Thompson on behalf of the Authors (05 Feb 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (15 Feb 2016) by Olaf Eisen
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Short summary
We show that strong electrical self-potential fields are generated in melting in in situ snowpacks at Rhone Glacier and Jungfraujoch Glacier, Switzerland. We conclude that the electrical self-potential method is a promising snow and firn hydrology sensor, owing to its suitability for sensing lateral and vertical liquid water flows directly and minimally invasively, complementing established observational programs and monitoring autonomously at a low cost.