Passive fathometer processing
Author(s) -
Peter Gerstoft,
William S. Hodgkiss,
Martin Siderius,
ChenFen Huang,
Chris H. Harrison
Publication year - 2008
Publication title -
the journal of the acoustical society of america
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.619
H-Index - 187
eISSN - 1520-8524
pISSN - 0001-4966
DOI - 10.1121/1.2831930
Subject(s) - seabed , acoustics , reflection (computer programming) , noise (video) , layering , ambient noise level , waveguide , geology , energy (signal processing) , sensor array , array processing , optics , signal processing , computer science , physics , sound (geography) , telecommunications , radar , oceanography , machine learning , image (mathematics) , biology , programming language , botany , quantum mechanics , artificial intelligence
Ocean acoustic noise can be processed efficiently to extract Green's function information between two receivers. By using noise array-processing techniques, it has been demonstrated that a passive array can be used as a fathometer [Siderius, et al., J. Acoust. Soc. Am. 120, 1315-1323 (2006)]. Here, this approach is derived in both frequency and time domains and the output corresponds to the reflection sequence. From this reflection sequence, it is possible to extract seabed layering. In the ocean waveguide, most of the energy is horizontally propagating, whereas the bottom information is contained in the vertically propagating noise. Extracting the seabed information requires a dense array, since the resolution of the bottom layer is about half the array spacing. If velocity sensors are used instead of pressure sensors, the array spacing requirement can be relaxed and simulations show that just one vertical velocity sensor is sufficient.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom