the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief Communication – InSAR Svalbard Ground Motion Service: Observing Surface Displacements in the High Arctic
Abstract. The InSAR Svalbard Ground Motion Service (GMS) provides open-access surface displacement maps and time series in the Svalbard archipelago, derived from Sentinel-1 Interferometric Synthetic Aperture Radar (InSAR). The service provides seasonal products capturing short-term 2016–2024 displacements and interannual products documenting long-term 2018–2024 velocity trends. InSAR Svalbard covers five areas on Spitsbergen Island (Longyearbyen, Ny-Ålesund, Svea, Hornsund and Kapp Linné). The service consists in a web-based visualisation tool at https://svalbard.insar.no. The products are also distributed at https://doi.org/10.5281/zenodo.18442696. InSAR Svalbard establishes a foundation for geohazard assessment in Arctic regions and interdisciplinary research on permafrost dynamics, ground stability, and environmental changes.
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Status: open (until 02 Jul 2026)
- RC1: 'Comment on egusphere-2026-2189', Anonymous Referee #1, 26 May 2026 reply
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RC2: 'Comment on egusphere-2026-2189', Anonymous Referee #2, 08 Jun 2026
reply
See the supplement file.
Data sets
InSAR Svalbard WebGIS Marie Bredal et al. https://svalbard.insar.no
InSAR Svalbard Zenodo Dataset Marie Bredal et al. https://doi.org/10.5281/zenodo.18442696
InSAR Svalbard Product Description and User Manual Marie Bredal et al. https://svalbard.insar.no/docs/User-manual-InSAR-Svalbard.pdf
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The InSAR Svalbard initiative represents a significant milestone for Arctic research. The manuscript presents its background and relevance in a clear and functional manner. Overall, I believe the paper is suitable for publication, pending minor revisions.
I would suggest that the handling editor consider elevating the manuscript to a Research Article, given the uniqueness and potential impact of the service proposed to users. In its current form, the paper gives the impression that additional technical detail could have been included, and that the reliance on external documentation is driven more by space constraints than by a deliberate stylistic choice.
For instance, a more detailed discussion of InSAR limitations in Chapter 3 would be valuable for technical readers, particularly in relation to the motion characteristics of the Svalbard archipelago. Similarly, the solutions adopted for the data viewer, currently only briefly described in Chapter 4, would likely be of interest to InSAR service providers and practitioners, and could be expanded.
Specific comments: