{"refrec":{"BRefID":215796,"RR":"<b>Carrière, O.; Hermand, J.-P.</b> (2012). Sequential Bayesian geoacoustic inversion for mobile and compact source-receiver configuration. <i>J. Acoust. Soc. Am. 131(4)</i>: 2668-2681. <a href=\"https://dx.doi.org/10.1121/1.3689552\" target=\"_blank\">https://dx.doi.org/10.1121/1.3689552</a>","BEntID":207552,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Acoust. Soc. Am. 131(4)</i>: 2668-2681. <a href=\"https://dx.doi.org/10.1121/1.3689552\" target=\"_blank\">https://dx.doi.org/10.1121/1.3689552</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Carrière, O.; Hermand, J.-P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Carrière, O.; Hermand, J.-P.","Englishabstract":"Geoacoustic characterization of wide areas through inversion requires easily deployable configurations including free-drifting platforms, underwater gliders and autonomous vehicles, typically performing repeated transmissions during their course. In this paper, the inverse problem is formulated as sequential Bayesian filtering to take advantage of repeated transmission measurements. Nonlinear Kalman filters implement a random-walk model for geometry and environment and an acoustic propagation code in the measurement model. Data from MREA/BP07 sea trials are tested consisting of multitone and frequency-modulated signals (bands: 0.25-0.8 and 0.8-1.6?kHz) received on a shallow vertical array of four hydrophones 5-m spaced drifting over 0.7-1.6?km range. Space- and time-coherent processing are applied to the respective signal types. Kalman filter outputs are compared to a sequence of global optimizations performed independently on each received signal. For both signal types, the sequential approach is more accurate but also more efficient. Due to frequency diversity, the processing of modulated signals produces a more stable tracking. Although an extended Kalman filter provides comparable estimates of the tracked parameters, the ensemble Kalman filter is necessary to properly assess uncertainty. In spite of mild range dependence and simplified bottom model, all tracked geoacoustic parameters are consistent with high-resolution seismic profiling, core logging P-wave velocity, and previous inversion results with fixed geometries.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Sequential Bayesian geoacoustic inversion for mobile and compact source-receiver configuration","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":2012,"MonPub":null,"DateUpdate":"2018-08-16","DateCreate":"2012-05-31","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000302854800024","VABBcode":null,"OpenAcc":0,"DOI":"10.1121/1.3689552"},"refs":null,"anarec":{"AnaID":215796,"PubliDate":2012,"Pagination":"2668-2681","XtraPublOfAnaID":null,"ISBN":null,"Volume":"131","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43301,"SerRR":"The Journal of the Acoustical Society of America. 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