Abstract
Acoustic reverberation data from SUS explosions collected during the CEAREX 89 Arctic experiment are analyzed to estimate both under-ice and bottom backscattering strengths at very low frequencies (below 50 Hz). Short range direct-path returns are analyzed to measure the backward scattering strengths of the under-ice surface for scattering angles between 2.5° and 40° grazing and frequencies between 24 Hz and 105 Hz. Medium range (5–20 km) ice and bottom reverberation returns received on a 1200-m vertical array are separated using the time-arrival angle relationship to measure ice and bottom backscattering strengths at 23 Hz for grazing angles of 15°–60°. Long range reverberation is modeled by combining a normal-mode based scattering description with grazing angle dependent scattering functions based on small-ka (low frequency) approximations. Reverberation data at 23 Hz are successfully modeled for four cases of different bottom bathymetry and source depth.
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