Inverse problem for a stratified ocean and bottom

D. C. Stickler, P. A. Deift

Research output: Contribution to journalArticlepeer-review

Abstract

In this paper it is shown how to use the methods of one-dimensional inverse scattering theory, in particular the new approach of Deift and Trubowitz [Comm. Pure Appl. Math. 32, 121–251 (1979)], to recover the sound speed for the case of a stratified ocean with a pressure release surface driven by a harmonic point source at a finite depth from a measurement of the normal derivative at the pressure release surface. The method is not a perturbation technique. For comparison, this same problem is examined when the sound speed is slightly perturbed from unity using a technique of Cohen and Bleistein [SIAM J. Appl. Math. 32, 784–799 (1977) and Geophysics 44, 1077–1087 (1979)].

Original languageEnglish (US)
Pages (from-to)1723-1727
Number of pages5
JournalJournal of the Acoustical Society of America
Volume70
Issue number6
DOIs
StatePublished - Dec 1981

ASJC Scopus subject areas

  • Arts and Humanities (miscellaneous)
  • Acoustics and Ultrasonics

Fingerprint Dive into the research topics of 'Inverse problem for a stratified ocean and bottom'. Together they form a unique fingerprint.

Cite this