Articles | Volume 18, issue 7
https://doi.org/10.5194/essd-18-5117-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
The Greenland GNSS Network (GNET): geodetic grade GNSS measurements of Greenland's 3D bedrock displacement from 1995–2025
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- Final revised paper (published on 20 Jul 2026)
- Preprint (discussion started on 08 Apr 2026)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
- RC1: 'Comment on essd-2026-198', Halfdan Pascal Kierulf, 06 May 2026
- RC2: 'Comment on essd-2026-198', Anonymous Referee #2, 26 May 2026
- AC1: 'Comment on essd-2026-198', Christian Solgaard, 18 Jun 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Christian Solgaard on behalf of the Authors (18 Jun 2026)
Author's response
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ED: Publish as is (24 Jun 2026) by Benjamin Männel
AR by Christian Solgaard on behalf of the Authors (26 Jun 2026)
The dataset presented in the paper “The Greenland GNSS Network (GNET): Geodetic‑grade GNSS measurements of Greenland’s 3D bedrock displacement from 1995–2025” is a very important and comprehensive compilation of GNSS records of Greenland’s crustal motion, covering everything from station construction and historical background to raw data, time series, and fundamental geodetic parameters.
I am impressed by the authors’ effort in bringing all of this together. I have only three minor comments.
Figure 12 compares similar parameters from different analyses on the two axes. The use of different scales on the axes is confusing and hampers interpretation.
The uncertainty estimates reported in Table A1 are at the 0.00x mm/yr level, which seems unrealistic. How are these uncertainties calculated?
The dataset is a valuable tool for studies of crustal deformation, in particular for investigating the elastic and visco‑elastic response to past and present ice‑mass changes. Separating these processes is challenging, and velocity estimates in glaciated regions such as Greenland strongly depend on the observation time span. I would like to see this discussed in more detail. For instance, the challenges associated with comparing time series with different time spans should be addressed.