Modal Mapping in Shallow Water Using Synthetic Aperture Horizontal Arrays

摘要

An experimental technique is described for mapping the wavenumber spectrum of the normal mode field as a function of position in a shallow water waveguide with three-dimensional variation in its acoustic properties. These modal maps provide a characterization of the modal properties of the waveguide, can be used as input data to inversion techniques for inferring the 3-D geoacoustic properties of the bottom, and improve our ability to localize and track source. The experimental configuration consists of a source radiating One or more pure tones to a field of freely drifting buoys, each containing a hydrophone, GPS navigation, and radio telemetry. A key component of the method In the establishment of a local differential CPS system between the source ship and each buoy, thereby enabling the determination of the positions of the buoys relative to the ship with submeter accuracy. In this manner, the drifting buoy create 2-D synthetic aperture horizontal array along which the modal evolution of the waveguide can be observed in the spatial domain, or after beam forming, in the horizontal wavenumber domain. Typical results from two modal mapping experiments (MOMAX) are presented in which flied aid moving source configurations were used to transmit pure tones in the band 50-300 Hz to several buoys at ranges up to 10 km. MOMAX I was conducted in about 70 m of water off the New Jersey coast in March, 1997, while MOMAX II was carried out in 50-150 m water depths in the Gulf of Mexico in February, 1999. A striking feature of these data is the remarkable stability and regularity of the phase, although the magnitude displays a complex multimodel interference pattern. A phase model is described which accurately predicts the source-receiver speed from these phase measurements. In addition, examples of modal maps are presented which illustrate the influence of lateral variations in the waveguide properties on the spatially evolving spectral content of the model field.