Machine Learning-Based Algorithm for One-Dimensional Wave Spectrum Retrieval from SAR Imagery as Passing Oceanic Eddy

The inversion of the one-dimensional wave spectrum from dual-polarized synthetic aperture radar (SAR) data is performed using machine learning methods, namely Random Forest (RF), eXtreme Gradient Boosting (XGBoost), Support Vector Regression (SVR) and Convolutional Neural Networks (CNNs). This proce...

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Vydáno v:IEEE transactions on geoscience and remote sensing s. 1
Hlavní autoři: Hu, Yuyi, Shao, Weizeng, Jiang, Xingwei, Migliaccio, Maurizio
Médium: Journal Article
Jazyk:angličtina
Vydáno: IEEE 26.11.2025
Témata:
Oceanic Eddy
Oceans
One-dimension Wave Spectrum
Radar polarimetry
Sea measurements
Sea state
Sea surface
Spaceborne radar
Spatial resolution
Surface waves
Synthetic aperture radar
Vectors
ISSN:0196-2892
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Shrnutí:The inversion of the one-dimensional wave spectrum from dual-polarized synthetic aperture radar (SAR) data is performed using machine learning methods, namely Random Forest (RF), eXtreme Gradient Boosting (XGBoost), Support Vector Regression (SVR) and Convolutional Neural Networks (CNNs). This process incorporates an improved hydrodynamic modulation transfer function (MTF), calibrated with more than 8000 Sentinel-1 (S-1) Ground Range Detected (GRD) images from 2021-2024, to account for shear currents induced by oceanic eddies. This study primarily aims to the differences between algorithm for one-dimension wave spectrum retrieval from S-1 SAR image as passing oceanic eddy and examine the characteristics of sea surface waves change observed by SAR passing through oceanic eddies. SAR retrievals are compared with significant wave heights (SWHs) from Haiyang-2 (HY-2) altimeter and wave spectrum from the Surface Wave Investigation and Monitoring (SWIM) and National Data Buoy Center (NDBC) buoys. The XGBoost model is established as superior for retrieving one-dimensional wave spectra and SWH, recording the lowest RMSE (0.33 m vs. SWIM, 0.30 m vs. HY-2, 0.68 m vs. Buoy) and highest correlation in validation. Applied to a North Atlantic case study, it effectively derives sea states from S-1 image. This high-resolution analysis reveals that oceanic eddies significantly amplify wave energy, resulting in elevated SWH inside their cores. While model accuracy declines in high kinetic energy eddies, the SAR-derived retrievals maintain reliability across eddy-affected regions.
ISSN:0196-2892
DOI:10.1109/TGRS.2025.3638164