Articles | Volume 25, issue 9
Hydrol. Earth Syst. Sci., 25, 5047–5064, 2021
https://doi.org/10.5194/hess-25-5047-2021
Hydrol. Earth Syst. Sci., 25, 5047–5064, 2021
https://doi.org/10.5194/hess-25-5047-2021

Technical note 20 Sep 2021

Technical note | 20 Sep 2021

Technical note: Introduction of a superconducting gravimeter as novel hydrological sensor for the Alpine research catchment Zugspitze

Christian Voigt et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2021-78', Anonymous Referee #1, 16 Mar 2021
    • AC1: 'Reply on RC1', Christian Voigt, 17 Mar 2021
  • RC2: 'Comment on hess-2021-78', Anonymous Referee #2, 10 Apr 2021
    • AC2: 'Reply on RC2', Christian Voigt, 20 Apr 2021
  • CC1: 'Comment on hess-2021-78', David Crossley, 11 Apr 2021
    • AC3: 'Reply on CC1', Christian Voigt, 20 Apr 2021
  • AC4: 'Comment on hess-2021-78', Christian Voigt, 07 May 2021
  • EC1: 'Editor Comment on hess-2021-78', Bettina Schaefli, 26 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (26 May 2021) by Bettina Schaefli
AR by Christian Voigt on behalf of the Authors (15 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (23 Jun 2021) by Bettina Schaefli
RR by Anonymous Referee #1 (24 Jun 2021)
RR by Anonymous Referee #2 (28 Jul 2021)
ED: Publish subject to minor revisions (review by editor) (09 Aug 2021) by Bettina Schaefli
AR by Christian Voigt on behalf of the Authors (16 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (18 Aug 2021) by Bettina Schaefli
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Short summary
A continuously operating superconducting gravimeter at the Zugspitze summit is introduced to support hydrological studies of the Partnach spring catchment known as the Zugspitze research catchment. The observed gravity residuals reflect total water storage variations at the observation site. Hydro-gravimetric analysis show a high correlation between gravity and the snow water equivalent, with a gravimetric footprint of up to 4 km radius enabling integral insights into this high alpine catchment.