A new method detects Arctic sea fog effectively, enhancing navigation safety in marine environments.
Arctic sea ice melting enhances surface evaporation over open waters, thereby intensifying sea fog occurrence and posing serious risks to navigation safety. However, accurate satellite-based detection of Arctic sea fog remains a persistent challenge due to weak spectral contrasts among fog, low cloud, sea ice, and snow, especially under low solar elevation in high-latitude regions. To address these issues, we propose the Surface-Adaptive Multispectral Threshold Segmentation (SA-MSTS) method tailored to the Medium-Resolution Spectral Imager-II (MERSI-II) aboard the FY-3D satellite. SA-MSTS dynamically adjusts spectral thresholds based on the underlying surface type (sea ice or open water), enabling robust fog discrimination under diverse backgrounds. High-quality ground-truth labels are derived from the Aerosol and Carbon Detection Lidar (ACDL) onboard the atmospheric environment monitoring satellite, DQ-1. Through systematic spectral analysis across all MERSI-II channels, nine critical bands (bands 1, 3, 5, 6, 7, 16, 20, 24, 25) and four optimized spectral indices for sea fog detection are identified. The method is validated using in-situ shipborne meteorological observations collected by the research vessel Xuelong 2 during Arctic expeditions. Validation shows that SA-MSTS achieves a probability of detection (POD) of 87.5% over open water and 88.6% over sea ice, with corresponding false alarm ratios (FAR) of 23.7% and 29.5%, and critical success indices (CSI) of 68.8% and 64.7%, respectively. These results demonstrate that SA-MSTS can achieve high accuracy in Arctic sea fog detection across heterogeneous Arctic surface conditions and highlight the potential of MERSI-II data for polar atmospheric applications.
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Dai et al. (2026) studied this question.
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