Affiliation:
1. Marine Physical Laboratory Scripps Institution of Oceanography, University of California San Diego , 9500 Gilman Drive, La Jolla, California 92093-0238, USA
Abstract
In their Comment, the authors conclude that acoustic glint is not present in the reflection coefficient of a two-layer sediment in which the top layer is an Airy medium. They conclude, not that the original, inverse-square analysis of the glint is incorrect, but rather that the presence of glint is very sensitive to the detailed shape of the sound speed profile in the top layer.
Publisher
Acoustical Society of America (ASA)