Sea ice freeboard extrapolation from ICESat-2 to Sentinel-1

Abstract. The Ice, Cloud and Land Elevation Satellite (ICESat-2) laser altimeter can capture sea ice freeboard along-track at both high vertical and high spatial resolutions. The measurement occurs along three strong and three weak parallel beams. Thus, the across-track direction is only very sparsely covered, and capturing the two-dimensional spatial distribution of freeboard at a high resolution using this instrument alone is not possible. This work shows how, in the early Arctic winter months of October and November, Sentinel-1 synthetic aperture radar (SAR) acquisitions help bridge this gap. Freeboard measurements are shown to be meaningfully extrapolated to a full two-dimensional mapping. To achieve this, it is sufficient to use the cross-polarised (HV) SAR backscatter to sort the pixels by intensity and then map freeboards measured from altimetry in the area via the cumulative distribution functions. With the presented algorithm, the snow and ice freeboard derived from altimetry can be extrapolated to Sentinel-1 SAR scenes, unlocking an additional dimension of Arctic freeboard monitoring at a high spatial resolution, with ice freeboard errors between 6 and 10.5 cm for spatial resolutions between 100 and 400 m.

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Publication Details

Journal
˜The œcryosphere
Published
2025-10-21
DOI
https://doi.org/10.5194/tc-19-4701-2025
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Sea ice freeboard extrapolation from ICESat-2 to Sentinel-1

Gunnar Spreen, Suman Singha, Karl Kortum
˜The œcryosphere
Arctic and Antarctic ice dynamics
article

Sea ice freeboard extrapolation from ICESat-2 to Sentinel-1

Gunnar Spreen, Suman Singha, Karl Kortum
article en

Abstract

Abstract. The Ice, Cloud and Land Elevation Satellite (ICESat-2) laser altimeter can capture sea ice freeboard along-track at both high vertical and high spatial resolutions. The measurement occurs along three strong and three weak parallel beams. Thus, the across-track direction is only very sparsely covered, and capturing the two-dimensional spatial distribution of freeboard at a high resolution using this instrument alone is not possible. This work shows how, in the early Arctic winter months of October and November, Sentinel-1 synthetic aperture radar (SAR) acquisitions help bridge this gap. Freeboard measurements are shown to be meaningfully extrapolated to a full two-dimensional mapping. To achieve this, it is sufficient to use the cross-polarised (HV) SAR backscatter to sort the pixels by intensity and then map freeboards measured from altimetry in the area via the cumulative distribution functions. With the presented algorithm, the snow and ice freeboard derived from altimetry can be extrapolated to Sentinel-1 SAR scenes, unlocking an additional dimension of Arctic freeboard monitoring at a high spatial resolution, with ice freeboard errors between 6 and 10.5 cm for spatial resolutions between 100 and 400 m.

˜The œcryosphereVol. 19(10)
University of Calgary (CA), University of Bremen (DE), Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR) (DE), Danish Meteorological Institute (DK)
National Aeronautics and Space Administration, Deutsche Forschungsgemeinschaft, Deutsches Zentrum für Luft- und Raumfahrt
Openalex Percentile: Top 65%
Arctic and Antarctic ice dynamics
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Sea ice freeboard extrapolation from ICESat-2 to Sentinel-1 — Gunnar Spreen, Suman Singha, et al. · ˜The œcryosphere (2025) | TGRS Research Map | TGRS