Assessment of SWOT Systematic Errors and Calibration Strategy

The SWOT KaRIN instrument provides wide-swath Sea Surface Height measurements affected by cross-swath systematic errors largely driven by thermo-elastic distortions and attitude knowledge errors. Using more than two years of science-orbit data, we evaluate a calibration procedure structured in two principal steps to estimate the systematic errors. The first step applies an empirical modeling approach—combining a solar–orbital model and a geographically fixed model. This empirical phase reduces the dominant linear swath-tilt variability from 17cm to 7cm. The second step implements a localized Optimal Interpolation framework that exploits the k-2 power-law behavior of the remaining attitude errors to isolate them from actual SLA signal to preserve. This combined approach reduces the final residual formal error of the linear term to ~1cm over open oceans and~3cm over continental regions, providing a calibration scheme for global oceanographic and hydrological applications.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-10-29
DOI
https://doi.org/10.5281/zenodo.23769309
Primary Topic
Ocean Waves and Remote Sensing
Type
preprint
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preprint

Assessment of SWOT Systematic Errors and Calibration Strategy

Clément Ubelmann, Matthias Raynal, Gérald Dibarboure, Antoine Delepoulle et al.
3 links
Zenodo (CERN European Organization for Nuclear Research)
Ocean Waves and Remote Sensing
preprint

Assessment of SWOT Systematic Errors and Calibration Strategy

Clément Ubelmann, Matthias Raynal, Gérald Dibarboure, Antoine Delepoulle, Cécile Anadon
preprint en

Abstract

The SWOT KaRIN instrument provides wide-swath Sea Surface Height measurements affected by cross-swath systematic errors largely driven by thermo-elastic distortions and attitude knowledge errors. Using more than two years of science-orbit data, we evaluate a calibration procedure structured in two principal steps to estimate the systematic errors. The first step applies an empirical modeling approach—combining a solar–orbital model and a geographically fixed model. This empirical phase reduces the dominant linear swath-tilt variability from 17cm to 7cm. The second step implements a localized Optimal Interpolation framework that exploits the k-2 power-law behavior of the remaining attitude errors to isolate them from actual SLA signal to preserve. This combined approach reduces the final residual formal error of the linear term to ~1cm over open oceans and~3cm over continental regions, providing a calibration scheme for global oceanographic and hydrological applications.

Zenodo (CERN European Organization for Nuclear Research)
Centre National d'Études Spatiales (FR)
Ocean Waves and Remote Sensing
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