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Principles of Modern Radar - Volume 2 1891121537

Principles of Modern Radar - Volume 2 1891121537

Principles of Modern Radar - Volume 2 1891121537

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350 CHAPTER 8 Interferometric SAR and Coherent ExploitationAnother alternate form is obtained in terms <strong>of</strong> the angular baseline δψ B (see Figure 8-4),which satisfies B ⊥ ≈ R · δψ B so thatα IF =− λ cos ψ2π p · δψ B(8.18)Typical values <strong>of</strong> δψ B are quite small. For the earlier SRTM example, δψ B ≈ 177 μrador about 0.01 ◦ . For a typical airborne InSAR case with B ⊥ = 1 m and R = 7 km, δψ B ≈143 μrad or about 0.008 ◦ .Equation (8.16) states that a change in the elevation <strong>of</strong> the scatterer relative to thezero-elevation reference plane can be estimated by multiplying the measured change in theinterferometric phase difference relative to the zero-elevation IPD by the interferometricscale factor.To take advantage <strong>of</strong> this relationship, we first need the IPD map that results from azero-elevation scene. Recasting equation (8.12) in terms <strong>of</strong> elevation and ground range,the IPD for a scatterer at zero elevation and ground range y becomes2π pBφ ab (x,y) ≈− cos [ψ (y) + β]λ( [cos −12π pB=− cosλ2π pB=−λy√H2+ y 2 )+ β⎡ ⎛⎞ ⎤cos⎣cos −1 1⎝√1 + ( H / y ) ⎠ + β2](h(x,y) = 0)⎦ ≡ φab FE (x,y) (8.19)This ground plane IPD is called the flat earth IPD, here denoted as φab FE . If we considerδφ ab as the difference between the actual IPD and the flat earth IPD, then δh will be thedifference between zero elevation and the actual elevation <strong>of</strong> the scatterer (i.e., h). Theactual elevation <strong>of</strong> the scatterer producing the pixel at location (x,y) in the SAR imagescan therefore be estimated asĥ(x,y) ≈ α IF[φab (x,y) − φ FEab (x,y)] (8.20)In using this equation, it is important to realize that the interferometric scale factor is afunction <strong>of</strong> ψ and thus <strong>of</strong> ground range y. The value <strong>of</strong> α IF must be updated for eachground range bin.We now have a second InSAR DEM algorithm, defined by the following procedure.InSAR DEM Algorithm 21. Using the two SAR images, measure the IPD φ ab (x,y) at each ground plane pixellocation (x,y).2. Compute φab FE (x,y) using equation (8.19).3. For each ground plane image coordinate (x,y), compute the range R to a scatterer <strong>of</strong>elevation zero at that location using equation (8.1).4. Estimate the depression angle ψ <strong>of</strong> the scatterer imaged at each (x,y) ground coordinateusing equation (8.13).

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