Articles | Volume 13, issue 7
Earth Syst. Sci. Data, 13, 3491–3512, 2021
https://doi.org/10.5194/essd-13-3491-2021

Special issue: Extreme environment datasets for the three poles

Earth Syst. Sci. Data, 13, 3491–3512, 2021
https://doi.org/10.5194/essd-13-3491-2021
Data description paper
19 Jul 2021
Data description paper | 19 Jul 2021

Greenland ice velocity maps from the PROMICE project

Anne Solgaard et al.

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Cited articles

Ahlstrøm, A. P., Andersen, S. B., Andersen, M. L., Machguth, H., Nick, F. M., Joughin, I., Reijmer, C. H., van de Wal, R. S. W., Merryman Boncori, J. P., Box, J. E., Citterio, M., van As, D., Fausto, R. S., and Hubbard, A.: Seasonal velocities of eight major marine-terminating outlet glaciers of the Greenland ice sheet from continuous in situ GPS instruments, Earth Syst. Sci. Data, 5, 277–287, https://doi.org/10.5194/essd-5-277-2013, 2013. a, b
Bartholomew, I., Nienow, P., Sole, A., Mair, D., Cowton, T., and King, M. A.: Short-term variability in Greenland Ice Sheet motion forced by time-varying meltwater drainage: Implications for the relationship between subglacial drainage system behavior and ice velocity, J. Geophys. Res.-Earth, 117, F03002, https://doi.org/10.1029/2011JF002220, 2012. a
Davison, B. J., Sole, A. J., Cowton, T. R., Lea, J. M., Slater, D. A., Fahrner, D., and Nienow, P. W.: Subglacial Drainage Evolution Modulates Seasonal Ice Flow Variability of Three Tidewater Glaciers in Southwest Greenland, J. Geophys. Res.-Earth, 125, e2019JF005492, https://doi.org/10.1029/2019JF005492, 2020. a
de Lange, R., Luckman, A., and Murray, T.: Improvement of Satellite Radar Feature Tracking for Ice Velocity Derivation by Spatial Frequency Filtering, IEEE T. Geosci. Remote, 45, 2309–2318, https://doi.org/10.1109/TGRS.2007.896615, 2007. a
De Zan, F.: Accuracy of Incoherent Speckle Tracking for Circular Gaussian Signals, IEEE Geosci. Remote S., 11, 264–267, https://doi.org/10.1109/LGRS.2013.2255259, 2014. a
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Short summary
The PROMICE Ice Velocity product is a time series of Greenland Ice Sheet ice velocity mosaics spanning September 2016 to present. It is derived from Sentinel-1 SAR data and has a spatial resolution of 500 m. Each mosaic spans 24 d (two Sentinel-1 cycles), and a new one is posted every 12 d (every Sentinel-1A cycle). The spatial comprehensiveness and temporal consistency make the product ideal for monitoring and studying ice-sheet-wide ice discharge and dynamics of glaciers.