Journal of Electronic Science and Technology, Volume. 23, Issue 1, 100292(2025)

Compensation for topographic effect on P-band PolSAR data with a polarimetric decomposition technique

Yin Zhang1 and Ding-Feng Duan2、*
Author Affiliations
  • 1Department of State-owned Assets and Laboratory Management, University of Electronic Science and Technology of China, Chengdu, 611731, China
  • 2School of Resources and Environment, University of Electronic Science and Technology of China, Chengdu, 611731, China
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    Figures & Tables(12)
    Mt. Shasta area, California: (a) SHH intensity image of the NASA/JPL AIRSAR P-band PolSAR data, (b) azimuth orientation angle (θ0) image derived from the P-band PolSAR data, and (c) azimuth slope angle θ (°), image derived from DEM. The pixel size of DEM is 10 m by 10 m. Each image covers an area of about 3.8 km (width) by 5.3 km (height).
    Relationships of the radar look angle (θl), local incidence angle (θi), and range slope angle (θs): (a) θl ≥ θs and (b) θl θs. The slope (or inclined surface) faces the radar look direction. (c) slope faces away from the radar look direction, and θl + θs ≤ 90°.
    Howland forest, Maine: (a) SHH intensity image of the NASA/JPL UAVSAR P-band PolSAR data. θ0 images, (b) topographic compensation, before, and (c) topographic compensation, after. The image is 570 columns by 570 rows, covering an area of about 8.8 km by 8.8 km.
    Mt. Shasta area, California. The θ0 image after the topographic compensation.
    Mt. Shasta area, California. Scatterplots of backscatter of (a) |SHH|2, (b) |SVV|2, and (c) |SHV|2 before (x-axis) and after (y-axis) the topographic compensation algorithm.
    Eno river state park, North Carolina: (a) SHH intensity images of DukeFr_225 and (b) DukeFr_045. The azimuth slope images calculated from the DEM data with the aspect angles of (c) 225°, (d) 45°, (e) local radar incidence angle images of DukeFr_225, and (f) DukeFr_045.
    Eno river state park, North Carolina: θ0 images of (a) DukeFr_225 and (b) DukeFr_045 before the topographic compensation; (c) DukeFr_225, and (d) DukeFr_045 after the compensation.
    Altamaha wildlife management area, Georgia: (a) SHH intensity image of the NASA/JPL AIRSAR P-band PolSAR data. One sample site at near range with a radar local incidence angle of about 36.25° and one at far range with an incidence angle of ~54.14°. Each square has a size of 50×50. θ0 images (b) the topographic compensation, before, and (c) the topographic compensation, after. Each image covers an area of about 10.5 km by 4.8 km.
    • Table 1. Statistical results of θ0 including the value range and the proportion of pixels with values > 5°.

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      Table 1. Statistical results of θ0 including the value range and the proportion of pixels with values > 5°.

      Main range of θ0Percentage of θ0 > 5° (%)
      ShastaBefore[–20°, 20°]45.2
      After[–10°, 10°]4.2
    • Table 2. Mean(μ) and standard deviation (σ) of backscatter components before and after the topographic compensation algorithm. The relative change rate (%) is Δ.

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      Table 2. Mean(μ) and standard deviation (σ) of backscatter components before and after the topographic compensation algorithm. The relative change rate (%) is Δ.

      ${\left| {{S_{{\text{HH}}}}} \right|^2}$${\left| {{S_{{\text{VV}}}}} \right|^2}$$\left| {{S_{{\text{HH}}}}S_{{\text{VV}}}^*} \right|$|2SHV|2|$\sqrt 2 {S_{{\text{HH}}}}S_{{\text{HV}}}^*$|$\sqrt 2 {S_{{\text{VV}}}}S_{{\text{HV}}}^*$
      Beforeμ0.4010.2070.1250.1690.0890.061
      σ0.3910.2940.2620.1290.0830.061
      Afterμ0.4230.2170.1320.1370.0710.055
      σ0.4000.3020.2630.1110.0690.056
      Δ5.2014.6085.303–23.358–25.352–10.909
    • Table 3. Mean value (μ) and standard deviation (σ) of the θ0 values. The θ0 < 0° andθ0 ≥ 0° categories were created using DukeFr_225_mask for DukeFr_225 and DukeFr_0455_mask for DukeFr_045, respectively.

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      Table 3. Mean value (μ) and standard deviation (σ) of the θ0 values. The θ0 < 0° andθ0 ≥ 0° categories were created using DukeFr_225_mask for DukeFr_225 and DukeFr_0455_mask for DukeFr_045, respectively.

      θ0 < 0° categoryθ0 ≥ 0° category
      BeforeAfterBeforeAfter
      DukeFr_225μ–2.390.473.44–0.70
      σ2.111.222.401.21
      DukeFr_045μ–1.670.203.35–0.69
      σ1.511.232.341.18
    • Table 4. Mean value (μ) and one standard deviation (σ) of the absolute θ0 values at a sample size at the near range and the other site at the far range.

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      Table 4. Mean value (μ) and one standard deviation (σ) of the absolute θ0 values at a sample size at the near range and the other site at the far range.

      Near rangeFar range
      1Ratio = (mean before the compensation) / (mean after the compensation).
      Beforeμ0.881.02
      σ0.640.76
      Afterμ0.140.20
      σ0.110.18
      1Ratio6.295.10
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    Yin Zhang, Ding-Feng Duan. Compensation for topographic effect on P-band PolSAR data with a polarimetric decomposition technique[J]. Journal of Electronic Science and Technology, 2025, 23(1): 100292

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    Paper Information

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    Received: Mar. 1, 2024

    Accepted: Nov. 14, 2024

    Published Online: Apr. 7, 2025

    The Author Email: Ding-Feng Duan (dingfengduan@uestc.edu.cn)

    DOI:10.1016/j.jnlest.2024.100292

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