Abstract
In this section we shall study the capability of a sounder system mounted in an aircraft flying at a certain height above the ice surface. We shall assume an idealized situation comprising a flat, homogeneous ice sheet resting on a horizontal rock bed; the interfaces are smooth planes so that no scattering takes place. We may therefore consider the measurement situation by the mirror principle (Section 3.7).
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Bogorodsky, V.V., Bentley, C.R., Gudmandsen, P.E. (1985). Equipment for Radar Sounding of Glaciers. In: Radioglaciology. Glaciology and Quaternary Geology, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5275-1_4
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DOI: https://doi.org/10.1007/978-94-009-5275-1_4
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