• Acta Optica Sinica
  • Vol. 42, Issue 2, 0226001 (2022)
Dezhi Su1, Liang Liu2、*, Shiyong Wu1, and Lingshun Liu1
Author Affiliations
  • 1College of Basic Sciences for Aviation, Naval Aviation University, Yantai, Shandong 264001, China
  • 2Coast Guard College, Naval Aviation University, Yantai, Shandong 264001, China
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    DOI: 10.3788/AOS202242.0226001 Cite this Article Set citation alerts
    Dezhi Su, Liang Liu, Shiyong Wu, Lingshun Liu. Sea Surface Modeling Based on Ocean Wave Spectrum Correction Method[J]. Acta Optica Sinica, 2022, 42(2): 0226001 Copy Citation Text show less
    Three wave spectrum curves
    Fig. 1. Three wave spectrum curves
    Microfacet slope variance and ESTD of wave spectra varying with wind speed. (a) Microfacet slope variance; (b) ESTD
    Fig. 2. Microfacet slope variance and ESTD of wave spectra varying with wind speed. (a) Microfacet slope variance; (b) ESTD
    Microfacet slope variance varying with number of sampling points under different wind speeds
    Fig. 3. Microfacet slope variance varying with number of sampling points under different wind speeds
    Sea surface height variance varying with number of sampling points under different wind speeds
    Fig. 4. Sea surface height variance varying with number of sampling points under different wind speeds
    Comparison of sea surface height before and after correction
    Fig. 5. Comparison of sea surface height before and after correction
    Microfacet slope variance varying with number of sampling points after correction
    Fig. 6. Microfacet slope variance varying with number of sampling points after correction
    Sea surface height variance varying with number of sampling points after correction
    Fig. 7. Sea surface height variance varying with number of sampling points after correction
    Microfacet slope variance varying with wind speed under different r
    Fig. 8. Microfacet slope variance varying with wind speed under different r
    Sea surface height variance varying with wind speed
    Fig. 9. Sea surface height variance varying with wind speed
    Model of sea surface infrared radiation
    Fig. 10. Model of sea surface infrared radiation
    Simulation flow chart
    Fig. 11. Simulation flow chart
    Polarization degree varying with detection angle under different wind speeds. (a) Mean polarization degree; (b) variance of polarization degree; (c) maximum polarization degree; (d) minimum polarization degree
    Fig. 12. Polarization degree varying with detection angle under different wind speeds. (a) Mean polarization degree; (b) variance of polarization degree; (c) maximum polarization degree; (d) minimum polarization degree
    Dezhi Su, Liang Liu, Shiyong Wu, Lingshun Liu. Sea Surface Modeling Based on Ocean Wave Spectrum Correction Method[J]. Acta Optica Sinica, 2022, 42(2): 0226001
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