“…Thus, in arctic conditions sound can propagate with minimal bottom interaction, potentially reducing transmission loss. However, acoustic scattering by both ice cover and surface roughness increases attenuation beyond what is typically measured for temperate deep-water propagation and what would be expected from geometric spreading losses and volume attenuation alone (Marsh and Mellen, 1963;Buck and Greene, 1964;DiNapoli and Mellen, 1986). This attenuation is strongly frequency-dependent for ice-covered waters; empirical measurements of this excess transmission loss as a function of frequency indicate an f 3/2 or f 2 relationship up to the kilohertz range, and numerous theoretical studies have sought to derive this relationship from statistical properties of ice floes and various scattering theories (Lepage and Schmidt, 1994).…”