ESSDD Earth System Science Data Discussions ESSDD Earth Syst. Sci. Data Discuss. 1866-3591 Göttingen, Germany 10.5194/essd-2026-221 PROMICE: Greenland ice velocity maps v2026 Solgaard Anne https://orcid.org/0000-0002-8693-620X 1 Kusk Anders https://orcid.org/0000-0001-7822-4758 2 Merryman Boncori John Peter 2 Dall Jørgen https://orcid.org/0000-0002-3873-1074 2 Ahlstrøm Andreas P. https://orcid.org/0000-0001-8235-8070 1 Andersen Signe B. https://orcid.org/0000-0002-8216-0141 1 Citterio Michele 1 How Penelope 1 Karlsson Nanna B. https://orcid.org/0000-0003-0423-8705 1 Kjeldsen Kristian K. https://orcid.org/0000-0002-8557-5131 1 Larsen Signe H. https://orcid.org/0000-0002-3656-3521 1 Lund Mads C. 1 Løkkegaard Anja https://orcid.org/0000-0002-1947-5773 1 Lüthi Martin P. https://orcid.org/0000-0003-4419-8496 3 Mejia Jessica https://orcid.org/0000-0002-5489-4711 4 Mankoff Kenneth D. https://orcid.org/0000-0001-5453-2019 5 6 van As Dirk https://orcid.org/0000-0002-6553-8982 1 7 Sugiyama Shin https://orcid.org/0000-0001-5323-9558 8 Fausto Robert S. https://orcid.org/0000-0003-1317-8185 1 The Geological Survey of Denmark and Greenland, Østervoldgade 10, 1350 København K, Denmark Technical University of Denmark - National Space Institute, Ørsteds Plads 348, 2800 Kongens Lyngby, Denmark University of Zürich, Winterthurerstrasse 190, CH-8057 Zürich, Switzerland Department of Earth and Environmental Sciences, Syracuse University, Syracuse, NY, USA NASA Goddard Institute for Space Studies, New York, NY, 10025 USA Autonomic Integra LLC, New York, NY, 10025 USA Ice and Climate Research Organization (ICRO), Kangerlussuaq, Greenland Institute of Low Temperature Science / Arctic Research Center, Hokkaido University, Nishi 8, Kita 19, Sapporo, Japan 13 05 2026 2026 1 33 Copyright: © 2026 Anne Solgaard et al. 2026 This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/4.0/ This article is available from https://essd.copernicus.org/preprints/essd-2026-221/ The full text article is available as a PDF file from https://essd.copernicus.org/preprints/essd-2026-221/essd-2026-221.pdf

We present an updated version of the Programme for Monitoring of the Greenland Ice Sheet (PROMICE) ice velocity product (<a href="https://doi.org/10.22008/FK2/K70OPK" target="_blank" rel="noopener">https://doi.org/10.22008/FK2/K70OPK</a>; Solgaard and Kusk (2026)), providing a continuous time series of Greenland Ice Sheet velocity mosaics from January 2016 to the present. The product is derived from Sentinel-1 synthetic aperture radar (SAR) data, gridded at 200 m spatial resolution and updated every 12 days using data spanning two consecutive Sentinel-1 repeat cycles (24 days). Data are typically released within 10 days of the final acquisition and include all valid 6- and 12-day image pairs within the 24-day window.</p> <p>This update includes several important improvements to the processing chain. The spatial resolution has been refined from 500 m to 200 m, justified by the implementation of an adaptive correlation template size approach for offset tracking, improving velocity retrievals and enhancing delineation of narrow outlet glaciers. We further implement a new mosaicking strategy, which reduces noise associated with ionospheric disturbances. Additional improvements include enhanced error handling and outlier rejection. The full processing workflow is described, including data selection, mosaicking, uncertainty estimation, and filtering procedures.</p> <p>Validation against in-situ GNSS measurements over the full time series shows that the standard deviation of the differences between satellite- and GNSS-derived velocities (with corresponding bias) is 22 m/yr (-0.3 m/yr) and 38 m/yr (-0.4 m/yr) for the easting and northing components, respectively. These values fall within expected ranges, although a substantial fraction of the discrepancy likely reflects uncertainty in the GNSS measurements. This interpretation is supported by validation over stable terrain, where substantially lower values are obtained: 9 m/yr (0.1 m/yr) and 15 m/yr (-0.1 m/yr) for the easting and northing components, respectively. Compared to the previous product version, uncertainties are higher due to a prolonged period when only one Sentinel-1 satellite was operational, resulting in increased noise and reduced temporal sampling. We quantify the impact of these conditions on spatial coverage.</p> <p>Overall, coverage is highest during winter, when radar coherence is strong and acquisitions are most comprehensive, whereas summer coverage is reduced due to surface melt. Despite these seasonal and mission-related constraints, the PROMICE ice velocity product provides consistent temporal sampling and broad spatial coverage, supporting investigations of ice-sheet-wide and glacier-specific dynamics and ice discharge on seasonal to multi-year timescales.