Parallel coupling marine acoustic forecasting system and operation method
A forecasting system and marine technology, applied in ultrasonic/acoustic/infrasonic transmission systems, transmission systems, complex mathematical operations, etc., can solve the problem that there is no forecast system applicable to the global ocean acoustic field with a large time span, and there are few cross-researches on oceanography and acoustics. There are no problems such as underwater sound field prediction, and the effect of improving stability and calculation efficiency is achieved
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[0048] Example 1
[0049] A parallel coupled marine acoustic forecast system, including marine environment forecast modules, ocean-acoustic coupling modules, and marine acoustic transmission solution modules;
[0050] The role of the Marine Environmental Forecast Module throughout the system is to provide initialization environment input for the system;
[0051] Ocean-Acoustic Coupling Module, which is extracted for parameters initialization, terrain extraction, and marine environment parameters. By transforming the parameters of the ocean module including temperature, salinity, sea roughness output into an acoustic model, marine model and acoustics The model is combined.
[0052] The ocean acoustic transmission solution is the result of the calculation of the marine sound field, the result of the marine sound field and the active distance of the sonar. The model used is a sound field model. The sound field model is further improved to a three-dimensional model based on the prior ...
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[0080] Example 2
[0081] Selected two points A (124.1 ° E, 26.38 ° N) and B (124.8 ° E, 24.63 ° N), topographic map Figure 5 Calculate the propagation of vertical section from A to B. Image 6 It is given that the high abnormality of the sea surface in the Okinawa trench region can be seen that A, b is also affected by the black tide vortex, A point is located in the low temperature zone of the sea surface, and the B point is high temperature in the sea surface. District, sound velocity profile is horizontal. A vertical cross-sectional sound field forecast is performed for A and B, first, interpolation is performed between two points A and B, interposed interval, acquisition of the latitude and latitude of each interpolated point; secondly, read from the ocean mode hydrological forecasting results from A to The temperature and salinity of the rectangular region near the B wiring is read from the global seafood database (GEBCO), and the two-dimensional linear interpolation is perfo...
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[0082] Example 3
[0083] The sound field in the horizontal cross-azimuth horizontal cross section of a rotation of a rotation of A (124.1 ° E, 26.38 ° N) is calculated for the sound source point A (124.1 ° E, 26.38 ° N). For a sound field prediction around the horizontal profile around a, the aqueous deposition, temperature, salinity, sea surface roughness, and other predictions such as the circular region around A are first read. In the 360 ° square angle interval, each azimuth propagation path interval is 1km a water depth, temperature, salinity, etc., and data of each interpolated point is obtained by two-dimensional linear interpolation in the surrounding four latitude latitude points. The sound velocity is calculated from a water depth, temperature, salinity, and the like according to the empirical formula. The input sound field model such as data, sound source information, sea surface roughness, and sea floor parameters such as water depth, sound source information, sea s...
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