Introduction to Radar Imaging Margaret Cheney Outline Mathematical - PowerPoint PPT Presentation
Introduction to Radar Imaging Margaret Cheney Outline Mathematical model Image formation time domain viewpoint frequency domain viewpoint (for small scenes) Approximating targets by point clouds SAR interferometry
Introduction to Radar Imaging Margaret Cheney
Outline • Mathematical model • Image formation • time domain viewpoint • frequency domain viewpoint (for small scenes) • Approximating targets by point clouds • SAR interferometry
Mathematical Model Maxwell’s equations —-> scalar wave equation Green’s function + Born approximation ρ ( y ) f 00 [ t − τ ( y , x s ) − τ ( y , x r )] Z p ( t, x r ; x s ) ∝ d y | y − x s || y − x r | standard (monostatic) SAR: x r = x s = γ ( s ) τ ( y , x ) = | y − x | = | γ ( s ) − y | R s, y c 0 c 0 y ρ ( y ) f 00 ( t − 2 R s, y /c 0 ) Z p ( t, s ) ∝ d y R 2 s, y
figures from Brett Borden, Naval Postgraduate School
Image formation X I ( y ) = data( t = τ ( y , x s ) + τ ( y , x r ) , x r ; x s ) x r , x s array imaging X � � = data t = 2 R s, y /c 0 , γ ( s ) standard (monostatic) SAR s why does this work?
Imaging from a single viewing position
Example with 3 scatterers Imaging from a single view
Imaging from two views
Imaging from three views synthetic aperture
Frequency domain viewpoint ρ ( y ) f 00 ( t − 2 R s, y /c 0 ) Z p ( t, s ) ∝ d y time-domain model R 2 s, y Z . . . e − i ω t dt Fourier transform in t ρ ( y ) ω 2 F ( ω ) e − 2 i ω R s, y /c 0 Z P ( ω , s ) ∝ d y R 2 s, y far-field approximation R s, y = | γ ( s ) − y | ≈ | γ | − b γ · y + · · · | γ | � | y | γ = γ b | γ | Z ρ ( y ) e − 2 ik b γ ( s ) · y d y P ( ω , s ) ∝ k = ω to form image, invert Fourier transform! c 0
Approximating targets by point clouds Z ρ ( y ) e − 2 ik b P ( ω , s ) ∝ γ · y d y k large -> use geometrical optics main contributions are from corners, edges, and specular points
Interferometry ρ ( y ) f 00 ( t − 2 R s, y /c 0 ) Z p ( t, s ) ∝ d y R 2 s, y f ( t ) = a ( t ) e i ω 0 t narrowband slowly varying (complex) amplitude a = ρ ( y ) e i ω 0 ( t − 2 R s, y /c 0 ) a ( t − 2 R s, y /c 0 ) Z p ( t, s ) ∝ d y R 2 s, y scattering takes place on surface ρ ( y ) = ˜ ρ ( y 1 , y 2 ) δ ( y 3 − h ( y 1 , y 2 )) y = y T + h ( y T )ˆ y T = ( y 1 , y 2 , 0) e 3 e 3 · \ R s, y = | y T + h ˆ e 3 − γ | = | y T − γ | + h ( y T )ˆ y T − γ | {z } | {z } R s, y T d ( y T ) e i ω 0 ( t − R s, y T /c 0 ) a ( t − R s, y T /c 0 ) Z h ρ ( y T ) e 2 ik 0 d ( y T ) i p ( t, s ) ≈ ˜ d y T R 2 s, y T target phase encodes height information!
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