Preprints
https://doi.org/10.5194/egusphere-2025-2683
https://doi.org/10.5194/egusphere-2025-2683
04 Jul 2025
 | 04 Jul 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

ICESat-2 surface elevation assessment with kinematic GPS and static GNSS near the ice divide in Greenland

Derek J. Pickell, Robert L. Hawley, Denis Felikson, and Jamie C. Good

Abstract. Since 2007, researchers have conducted monthly or bi-monthly kinematic GPS surveys along a 15-km transect near Summit Station, Greenland, providing ice surface elevation data with high relative accuracy (±0.8 cm) and high precision (±0.8 cm). We use these surveys to assess the long-term stability of ICESat-2 surface height measurements, revealing a sub-1.0 cm bias and sub-6.0 cm precision relative to ICESat-2 data, with no significant temporal trend in performance. While reliable, these surveys are resource-intensive. We introduce an alternative, novel validation method using autonomous GNSS stations with interferometric reflectometry (GNSS-IR) to measure surface elevation concurrent with ICESat-2 overflights. This method agrees well with kinematic GPS (-0.2 ± 5.0 cm) and is sensitive to active accumulation and surface roughness, offering additional environmental context. The ICESat-2 measurements are biased by -0.9 ± 3.8 cm compared to these autonomous stations. Together, these results demonstrate the importance of sustained, high-accuracy GNSS for building a long-term elevation benchmark record in Greenland, while also establishing GNSS-IR as a scalable alternative in support of current and future altimetry missions.

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Derek J. Pickell, Robert L. Hawley, Denis Felikson, and Jamie C. Good

Status: open (until 22 Aug 2025)

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Derek J. Pickell, Robert L. Hawley, Denis Felikson, and Jamie C. Good
Derek J. Pickell, Robert L. Hawley, Denis Felikson, and Jamie C. Good

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Short summary
We compared satellite measurements of ice surface height in Greenland with ground-based observations, revealing sub-centimeter accuracy of the satellite instrument. We also demonstrated a new autonomous method using reflected radio signals to measure the surface without human traverses. This method produces comparable results, and we find no long-term changes in satellite performance to date.
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