Mitigating errors in marine gravity recovery induced by sea level variability in SWOT observations

• Sea level variations in SWOT observations can bias gravity modeling. • Sea level variability correction reduces RMSE by ∼40 % (DOV), ∼9% (gravity anomaly) • Regions with sea level variability >15 cm should be corrected to ensure accuracy. The Surface Water and Ocean Topography (SWOT) mission has significantly advanced marine gravity recovery, yet its wide-swath measurements reveal the effects of strong sea level variability, emphasizing the need for effective correction methods. This study reveals that traditional correction strategies, such as stacking method, are insufficient for SWOT gravity recovery in high-variability environments, and quantifies the conditions under which more targeted correction approaches are necessary. Experimental results in the Kuroshio indicate that strong sea level variability directly affects SWOT observations, leading to gravity anomaly disturbances of approximately 2 mGal. To mitigate these disturbances, two strategies are implemented: stacking and sea level anomaly (SLA) model correction. Using SLA model correction, deflection of the vertical (DOV) accuracy improves by ∼40 % in regions of strong sea level variations, while gravity anomaly accuracy is enhanced by 0.25 mGal (∼9%). To determine the conditions under which correction becomes necessary, this study evaluates gravity anomaly accuracy across varying sea level variability levels, quantified by the standard deviation of sea level anomaly (STD-SLA). Results show that when STD-SLA is below 15 cm, gravity recovery remains largely unaffected. However, above this threshold, SLA-induced disturbances become non-negligible, and applying correction improves gravity anomaly accuracy by more than 0.1 mGal on average. Global analysis reveals these regions exceeding this threshold, where correction is essential, are predominantly located along major Western Boundary Currents and the Antarctic Circumpolar Current. These findings underscore the need to reassess standard correction approaches in SWOT-era gravity recovery, and provide quantitative guidance on where SLA-based correction should be applied.

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Publication Details

Journal
International Journal of Applied Earth Observation and Geoinformation
Published
2025-12-13
DOI
https://doi.org/10.1016/j.jag.2025.105027
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
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article

Mitigating errors in marine gravity recovery induced by sea level variability in SWOT observations

Taoyong Jin, Sun Heyuan, Jiasheng Shi, Jiancheng Li et al.
International Journal of Applied Earth Observation and Geoinformation
Geophysics and Gravity Measurements
article

Mitigating errors in marine gravity recovery induced by sea level variability in SWOT observations

Taoyong Jin, Sun Heyuan, Jiasheng Shi, Jiancheng Li, Huiyi Xian
article en

Abstract

• Sea level variations in SWOT observations can bias gravity modeling. • Sea level variability correction reduces RMSE by ∼40 % (DOV), ∼9% (gravity anomaly) • Regions with sea level variability >15 cm should be corrected to ensure accuracy. The Surface Water and Ocean Topography (SWOT) mission has significantly advanced marine gravity recovery, yet its wide-swath measurements reveal the effects of strong sea level variability, emphasizing the need for effective correction methods. This study reveals that traditional correction strategies, such as stacking method, are insufficient for SWOT gravity recovery in high-variability environments, and quantifies the conditions under which more targeted correction approaches are necessary. Experimental results in the Kuroshio indicate that strong sea level variability directly affects SWOT observations, leading to gravity anomaly disturbances of approximately 2 mGal. To mitigate these disturbances, two strategies are implemented: stacking and sea level anomaly (SLA) model correction. Using SLA model correction, deflection of the vertical (DOV) accuracy improves by ∼40 % in regions of strong sea level variations, while gravity anomaly accuracy is enhanced by 0.25 mGal (∼9%). To determine the conditions under which correction becomes necessary, this study evaluates gravity anomaly accuracy across varying sea level variability levels, quantified by the standard deviation of sea level anomaly (STD-SLA). Results show that when STD-SLA is below 15 cm, gravity recovery remains largely unaffected. However, above this threshold, SLA-induced disturbances become non-negligible, and applying correction improves gravity anomaly accuracy by more than 0.1 mGal on average. Global analysis reveals these regions exceeding this threshold, where correction is essential, are predominantly located along major Western Boundary Currents and the Antarctic Circumpolar Current. These findings underscore the need to reassess standard correction approaches in SWOT-era gravity recovery, and provide quantitative guidance on where SLA-based correction should be applied.

International Journal of Applied Earth Observation and GeoinformationVol. 146
Openalex Percentile: Top 61%
Geophysics and Gravity Measurements
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