title: Effects of upper ocean sound-speed structure on deep acoustic shadow-zone arrivals at 500- and 1000-km range.
abstract: Deep acoustic shadow-zone arrivals observed in the late 1990s in the North Pacific Ocean reveal significant acoustic energy penetrating the geometric shadow. Comparisons of acoustic data obtained from vertical line arrays deployed in conjunction with 250-Hz acoustic sources at ranges of 500 and 1000 km from June to November 2004 in the North Pacific, with simulations incorporating scattering consistent with the Garrett-Munk internal-wave spectrum, are able to describe both the energy contained in and vertical extent of deep shadow-zone arrivals. Incoherent monthly averages of acoustic timefronts indicate that lower cusps associated with acoustic rays with shallow upper turning points (UTPs), where sound-speed structure is most variable and seasonally dependent, deepen from June to October as the summer thermocline develops. Surface-reflected rays, or those with near-surface UTPs, exhibit less scattering due to internal waves than in later months when the UTP deepens. Data collected in November exhibit dramatically more vertical extension than previous months. The depth to which timefronts extend is a complex combination of deterministic changes in the depths of the lower cusps as the range-average profiles evolve with seasonal change and of the amount of scattering, which depends on the mean vertical gradients at the depths of the UTPs.
authors.affiliation: Scripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093, USA. lvanuffe@ucsd.edu
authors.forename: Lora J
authors.initials: LJ
authors.lastname: Van Uffelen
authors.forename: Peter F
authors.initials: PF
authors.lastname: Worcester
authors.forename: Matthew A
authors.initials: MA
authors.lastname: Dzieciuch
authors.forename: Daniel L
authors.initials: DL
authors.lastname: Rudnick
authors.forename: John A
authors.initials: JA
authors.lastname: Colosi
mesh_terms: D000162:Acoustics / Q000295:instrumentation; D003198:Computer Simulation; D008962:Models, Theoretical; D009038:Motion; D009716:Numerical Analysis, Computer-Assisted; D010140:Pacific Ocean; D054712:Salinity; D012621:Seasons; D012623:Seawater; D012815:Signal Processing, Computer-Assisted; D013016:Sound; D013018:Sound Spectrography; D013696:Temperature; D013997:Time Factors; D014159:Transducers