Acoustic Sensing Techniques for the Shallow Water Environment
Inversion Methods and Experiments
(Sprache: Englisch)
Thisvolume contains thecollection of papers from the second workshop on Expe- mental Acoustic Inversion Techniques for Exploration of theShallow Water Environment. Theworkshopthemefollowedtheoriginalconceptofthe rstworkshop, heldinCarvoeiro, Portugal, in...
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Thisvolume contains thecollection of papers from the second workshop on Expe- mental Acoustic Inversion Techniques for Exploration of theShallow Water Environment. Theworkshopthemefollowedtheoriginalconceptofthe rstworkshop, heldinCarvoeiro, Portugal, in 1999, i.e., to focus on experiments and experimental techniques for acoustic sensing in the shallow ocean. More than forty leading international scientists were invited to meet in the picturesque town of St. Angelo on the island of Ischia, in June 2004, to discuss progress in the application of new experimental techniques for exploration and assessment of shallowwater environments. Acoustic techniques provide the most effective means for remote sensing of ocean and sea oor processes, and for probing the structure beneath the sea oor. No other energy propagates as ef ciently in the ocean: radio waves and visible light are severely limited in range because the ocean is a highly conductive medium. However, sound from bre- ing waves and coastal shipping can be heard throughout the ocean, and marine mammals communicate acoustically over basin scale distances.
Inhaltsverzeichnis zu „Acoustic Sensing Techniques for the Shallow Water Environment “
- On the assessment of geoacoustic parameters in shallow water environments- Bayesian inversion of seabed reflection data
- Backpropagation techniques in ocean acoustic inversion: time reversal, retrogation and adjoint modelling - a review
- Acoustic inversion at low kHz frequencies using an active, vertical line array
- Dispersion of broadband acoustic normal modes in the context of long sediment tomography
- Characterization of local seabed properties using synthesized horizontal array data
- Characterization of a range-dependent environment from towed array data
- Accounting for bias in horizontal wavenumber estimates due to source motion
- Acoustic clutter from burried submarine mud volcanoes
- Nonlinear acoustical methods in the detection of gassy sediments
- Acoustic scattering from submerged and buried objects
- High-frequency bistatic scattering experiments using proud and buried targets
- A sediment probe for the rapid assessment of seabed characteristics
- Continuous acoustic monitoring of physiological and environmental processes in seagrass prairies with focus on photosynthesis
- Shallow water tomography in a highly variable scenario
- Inversion of reflection loss measurements of a smooth water/sand interface
- Estimation of transmissions loss and its uncertainty
- A forward model for geoacoustic inversion based on ray tracing and plane-wave reflection coefficients
- Inversion of the propeller harmonics from a light aircraft for the geoacoustic properties of marine sediments
- Inversion of shallow water ambient noise data by means of differential evolution as a global search method
- Reflection Loss and Sub-bottom Profiling with Ambient Noise
- Inversion of geoacoustic model parameters using ship radiated noise
- Matched-field processing of humpback whale song off eastern Australia
- Inversions of horizontal and vertical line array data for the estimation of geoacoustic model
... mehr
parameters
- Issues of environmental variability in inverse problems in ocean acoustics
- Issues of environmental variability in inverse problems in ocean acoustics
... weniger
Bibliographische Angaben
- 2006, 2006, 332 Seiten, mit Abbildungen, Maße: 16 x 24,1 cm, Gebunden, Englisch
- Herausgegeben:Caiti, Andrea; Chapman, N. Ross; Hermand, Jean-Pierre; Jesus, Sérgio M.
- Herausgegeben: Andrea Caiti, Sérgio M. Jesus, Jean-Pierre Hermand, N. Ross Chapman
- Verlag: Springer Netherlands
- ISBN-10: 1402043724
- ISBN-13: 9781402043727
- Erscheinungsdatum: 29.08.2006
Sprache:
Englisch
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