{"title":"A shallow-water ocean acoustics inverse problem","authors":"D. Stickler","doi":"10.1121/1.2127116","DOIUrl":null,"url":null,"abstract":"A shallow-water ocean acoustics experiment is proposed from which it is possible to determine in principle the scattering data necessary to recover the sound-speed profile in the ocean bottom. These data are a “reflection coefficient,” which is not the usual one. The reflection coefficient is amplitude of the outgoing wave at infinite depth due to a unit amplitude plane wave incident from infinite depth. The unusual fact is that this reflection coefficient can be recovered from a measurement in the ocean. The essential assumptions are that the sound-speed profile is known in the ocean but unknown in the bottom, and that the measurements are made in the ocean layer.","PeriodicalId":87384,"journal":{"name":"Acoustics research letters online : ARLO","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2005-11-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acoustics research letters online : ARLO","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1121/1.2127116","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
Abstract
A shallow-water ocean acoustics experiment is proposed from which it is possible to determine in principle the scattering data necessary to recover the sound-speed profile in the ocean bottom. These data are a “reflection coefficient,” which is not the usual one. The reflection coefficient is amplitude of the outgoing wave at infinite depth due to a unit amplitude plane wave incident from infinite depth. The unusual fact is that this reflection coefficient can be recovered from a measurement in the ocean. The essential assumptions are that the sound-speed profile is known in the ocean but unknown in the bottom, and that the measurements are made in the ocean layer.