2017
DOI: 10.1007/s40857-017-0082-y
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Sequential Inversion for Geoacoustic Parameters in the South China Sea Using Modal Dispersion Curves

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Cited by 7 publications
(3 citation statements)
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“…The state vector x k contains the geoacoustic parameters at frame k. In this paper, f (•) is simplified as the unit matrix I due to the lack of enough prior information about the change in geoacoustic parameters. The measurement vector y k contains the modal dispersion curves which are extracted from the time-frequency diagram of the received signal with warping transform and described as a set of travel time at different propagation modes and different frequencies [7]. The state noise vector w k and measurement noise vector v k can be modeled as covariance matrices Q k and R k , respectively.…”
Section: Sequential Estimation Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The state vector x k contains the geoacoustic parameters at frame k. In this paper, f (•) is simplified as the unit matrix I due to the lack of enough prior information about the change in geoacoustic parameters. The measurement vector y k contains the modal dispersion curves which are extracted from the time-frequency diagram of the received signal with warping transform and described as a set of travel time at different propagation modes and different frequencies [7]. The state noise vector w k and measurement noise vector v k can be modeled as covariance matrices Q k and R k , respectively.…”
Section: Sequential Estimation Methodsmentioning
confidence: 99%
“…In shallow ocean environments, the modal dispersion phenomenon can be observed, and its shape is strongly influenced by geoacoustic parameters. The fact that only one hydrophone is needed to observe this phenomenon reduces the experimental cost and the complexity of recording systems [6,7]. Compared with inversion methods that require high signal-to-noise ration (SNR) and complex signal processing techniques, modal dispersion curves can be extracted from the environment with unknown parameters and strong noise by using warping transform [8], making this method especially suitable for wide-band signals (air-gun or explosive charges) received by one hydrophone [9].…”
Section: Introductionmentioning
confidence: 99%
“…Numerous approaches have been developed to invert the sound speed in the water volume fast and accurate. To reduce the degrees of freedom, ocean parameters include the SSP are often represented in terms of EOFs [6,7]. The previous studies indicate that the inversion of SSP has a good agreement with the measured data, in both shallow [8] and deep ocean [9].…”
Section: Introductionmentioning
confidence: 99%