{"refrec":{"BRefID":254156,"RR":"<b>Ainslie, M.A.</b> (2010). Introduction, <b><i>in</i></b>: Ainslie, M. <i>Principles of sonar performance modelling.</i> pp. 3-26. <a href=\"https://dx.doi.org/10.1007/978-3-540-87662-5_1\" target=\"_blank\">https://dx.doi.org/10.1007/978-3-540-87662-5_1</a>","BEntID":245969,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Ainslie, M. <i>Principles of sonar performance modelling.</i> pp. 3-26. <a href=\"https://dx.doi.org/10.1007/978-3-540-87662-5_1\" target=\"_blank\">https://dx.doi.org/10.1007/978-3-540-87662-5_1</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ainslie, M.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ainslie, M.A.","Englishabstract":"Sonar can be thought of as a kind of underwater radar, using sound instead of radio waves to interrogate its surroundings. But what is special about sound in the sea? 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In water, the opposite is the case: low absorption and the presence of natural oceanic waveguides combine to permit propagation of sound over thousands of kilometers, whereas the sea is opaque to most of the electromagnetic spectrum.","AbstractOtherLang":null,"BibLvlCode":"AM","StandardTitle":"Introduction","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2010,"MonPub":null,"DateUpdate":"2017-05-30","DateCreate":"2016-03-17","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1007/978-3-540-87662-5_1"},"refs":null,"anarec":{"AnaID":254156,"PubliDate":2010,"Pagination":"3-26","XtraPublOfAnaID":null,"ISBN":"978-3-540-87661-8","Volume":null,"Issue":null,"BRefMon":254155,"BRefMonRR":"<b>Ainslie, M.</b> (2010). 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