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Space/time/frequency methods in adaptive radar - New Jersey ...

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10Figure 2.1 Side-Look<strong>in</strong>g SARFundamental characteristics of side-look<strong>in</strong>g SAR may be expla<strong>in</strong>ed <strong>in</strong> terms ofequirange and equi-Doppler l<strong>in</strong>es on the earth's surface to be mapped by the mov<strong>in</strong>g<strong>radar</strong> platform. Equirange l<strong>in</strong>es on the earth's surface are the <strong>in</strong>tersections withthe earth's surface of successive concentric spheres centers at the <strong>radar</strong> where po<strong>in</strong>tson these spheres are equidistant from the <strong>radar</strong>. Equi-Doppler l<strong>in</strong>es on the earth'ssurface are produced by <strong>in</strong>tersections with the earth's surface of coaxial cones, thatare concentric about the <strong>radar</strong>'s flight l<strong>in</strong>e as the axis and the <strong>radar</strong> position as theapex of the cones. Po<strong>in</strong>ts on the cones appear at constant velocity relative to the<strong>radar</strong>.The <strong>radar</strong> is able to view the portion of the range-Doppler coord<strong>in</strong>ate systemwhich is illum<strong>in</strong>ated by the real antenna beam. The echo power distribution as afunction of range delay and Doppler is the SAR image for that area.

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