Abstract
L. M. Brekovskikh’s book Waves in Layered Media has provided decades of graduate students and researchers alike with a comprehensive and enormously useful reference. One topic from that work, reflection from a point source above a plane-layered medium (the seabed), is discussed here. Both theoretical underpinnings and observations of reflection from a homogeneous halfspace, a transition layer with smoothly varying density and velocity profiles, and discrete layered media are considered for various shallow water sediment fabrics. [Work supported by the Office of Naval Research and NATO Undersea Research Centre.]
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