Internal solitary waves (ISWs) are prevalent nonlinear hydrodynamic phenomena in topographically complex ocean regions. Automated identification of internal solitary waves mainly relies on surface-texture imagery, leaving the incremental value of sea-surface height information uncertain. We evaluated a framework using Surface Water and Ocean Topography (SWOT) observations for ISW segmentation in the East China Sea. It combines normalized radar cross section (σ 0 ), background-removed sea surface height anomaly (SSHA), and its gradient (∇SSHA). A TransUNet model was evaluated across five training runs on one fixed scene-level partition. Radar backscatter provided the dominant predictive information. With a prescribed σ 0 :SSHA:∇SSHA input-amplitude scaling of 95:4:1, W1 achieved a mean foreground-class intersection over union (IoU) of 0.790. The architecture-matched σ 0 reference (A1) achieved 0.766. The mean full-test-set gains in Precision, Recall, F1-score, and IoU were modest and not statistically significant (all p > 0.05). On 346 challenging-positive test patches, W1 increased mean Recall from 83.57% to 85.40% and foreground-class IoU from 69.06% to 71.00%. On 346 challenging-negative test patches, mean pixel-level false-positive rate decreased from 1.60% to 1.52%. These subset comparisons are descriptive. Shuffled, random-field, and σ 0 -gradient controls had lower mean performance than W1, suggesting that co-registered height-related inputs may provide incremental predictive value beyond generic channel-count or edge effects. The predicted masks also supported crest-line extraction and inter-crest spacing analysis. The framework extends texture-based ISW segmentation by incorporating height-related observations, with modest observed gains under the evaluated conditions.
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Xu et al. (2026) studied this question.
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