Articles | Volume 25, issue 1
https://doi.org/10.5194/hess-25-217-2021
https://doi.org/10.5194/hess-25-217-2021
Research article
 | 
14 Jan 2021
Research article |  | 14 Jan 2021

Hydrological signals in tilt and gravity residuals at Conrad Observatory (Austria)

Bruno Meurers, Gábor Papp, Hannu Ruotsalainen, Judit Benedek, and Roman Leonhardt

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
  • RC1: 'Review', Anonymous Referee #1, 13 Jul 2020 Printer-friendly Version
    • AC1: 'AC1', Bruno Meurers, 07 Oct 2020 Printer-friendly Version
  • RC2: 'Review', Anonymous Referee #2, 07 Sep 2020 Printer-friendly Version
    • AC2: 'AC2', Bruno Meurers, 07 Oct 2020 Printer-friendly Version
  • EC1: 'HESS-2020-316', Marnik Vanclooster, 09 Sep 2020 Printer-friendly Version

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (12 Oct 2020) by Marnik Vanclooster
AR by Bruno Meurers on behalf of the Authors (22 Oct 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (28 Oct 2020) by Marnik Vanclooster
RR by Anonymous Referee #1 (28 Oct 2020)
ED: Publish subject to minor revisions (review by editor) (29 Oct 2020) by Marnik Vanclooster
AR by Bruno Meurers on behalf of the Authors (05 Nov 2020)  Author's response   Manuscript 
ED: Publish as is (23 Nov 2020) by Marnik Vanclooster
AR by Bruno Meurers on behalf of the Authors (25 Nov 2020)
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Short summary
Gravity and tilt time series acquired at Conrad Observatory (Austria) reflect gravity and deformation associated with short- and long-term environmental processes, revealing a complex water transport process after heavy rain and rapid snowmelt. Gravity residuals are sensitive to the Newtonian effect of water mass transport. Tilt residual anomalies capture strain–tilt coupling effects due to surface or subsurface deformation from precipitation or pressure changes in the adjacent fracture system.