Planet surface irregular grid three-dimensional geometric modeling method
A modeling method and 3D geometric technology, applied in 3D modeling, image enhancement, instrumentation, etc., to solve problems such as the inability to directly apply scattering and imaging characteristic analysis, the limited radar resolution of elevation data models, and the neglect of surface microstructures. , to achieve the effect of improved scattering calculation efficiency, simple and easy operation, and smooth boundary area
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Embodiment 1
[0055] Embodiment 1: Mars local topography;
[0056] Such as Figure 5 As shown, the coordinate system is added to the original regular elevation grid model, and Monte Carlo is used to superimpose the random roughness with root mean square height δ=0.65cm and correlation length l=10cm, according to the grid number-threshold curve and image similarity-threshold Curve, the optimal threshold is 0.5, to generate the local optimal irregular grid model of Mars. Scattering simulations were performed on the regular rough grid model and the irregularly subdivided grid model in the figure, and the RCS-angle change curve was calculated. The results are as follows Figure 6 Shown, among them, frequency f=3GHz, dielectric parameter ε=3.8+i0.1140. Detailed results regarding the number of grids, calculation time and coherence coefficient of the curves are listed in the following table:
[0057] Table 1 Comparison of calculation results between the irregular grid model and the regular mode...
Embodiment 2
[0060] Embodiment 2: volcano topography;
[0061] Figure 7 A 6m*6m*0.06m rough (root mean square height δ=0.65cm, correlation length l=10cm) regular grid model of volcanic peaks and a schematic diagram after irregular subdivision are shown, and a diagram suitable for traditional PO calculation (subdivision according to 1 / 8λ) regular grid model. Under the conditions of frequency f=3GHz and dielectric parameter ε=2.9+i 0.0812, use our algorithm to calculate the RCS curve of the grid model after irregular subdivision and import the regular grid model suitable for traditional PO calculation into The results calculated by the commercial software FEKO are compared, and the comparison results are as follows Figure 8 shown. The detailed data are shown in the table below:
[0062] Table 2 Comparison of Calculation Results Between Irregular Grid Model and Regular Model of Volcanic Topography
[0063]
[0064] Under the condition of 3GHz incident frequency, the traditional PO i...
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