摘要Following the closure relation of normal mode theory, the source depth can be estimated approximately provided that the eigenfunction and the excited amplitude with correct polarity of each effective mode are given. Both the eigenfunction and the excited amplitude of each effective mode can be extracted using the data-derived method, which does not require a priori knowledge about ocean environment and source range but the sound pressure data observed by vertical line array. The polarities, undetermined by data-derived method, can be estimated using a cost function. Then, the source depth is determined by locating the peak of the object function defined by the closure relation with the correct polarities. Numerical simulation and experiment are carried out to illustrate the performance of this method.
Abstract：Following the closure relation of normal mode theory, the source depth can be estimated approximately provided that the eigenfunction and the excited amplitude with correct polarity of each effective mode are given. Both the eigenfunction and the excited amplitude of each effective mode can be extracted using the data-derived method, which does not require a priori knowledge about ocean environment and source range but the sound pressure data observed by vertical line array. The polarities, undetermined by data-derived method, can be estimated using a cost function. Then, the source depth is determined by locating the peak of the object function defined by the closure relation with the correct polarities. Numerical simulation and experiment are carried out to illustrate the performance of this method.
(Space-time signal processing, other than matched field processing)
引用本文:
WANG Hao-Zhong;WANG Ning;GAO Da-Zhi
. Data-Derived Estimation of Source Depth Using Vertical Line Array Data in Shallow Water[J]. 中国物理快报, 2011, 28(11): 114302-114302.
WANG Hao-Zhong, WANG Ning, GAO Da-Zhi
. Data-Derived Estimation of Source Depth Using Vertical Line Array Data in Shallow Water. Chin. Phys. Lett., 2011, 28(11): 114302-114302.
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