A Parallel Coupled Ocean 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 sound field with a large time span, no underwater sound field forecast, and calculation scale Small problems, to achieve the effect of improving stability and computing efficiency
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Embodiment 1
[0049] A parallel coupled ocean acoustic forecasting system, the system includes an ocean environment forecast module, an ocean-acoustic coupling module, and an ocean acoustic propagation solution module;
[0050] The function of the marine environment forecasting module in the whole system is to provide the initial environment input for the system;
[0051] The ocean-acoustic coupling module is used for parameter initialization, terrain extraction, and marine environment parameter profile extraction. By converting the parameters of the ocean module, including temperature, salinity, and sea surface roughness output, into the input of the acoustic model, the ocean model and the acoustic Models are combined.
[0052] The role of the ocean acoustic propagation solution module is the calculation of the ocean acoustic field, the output of the results including the ocean acoustic field and the sonar range. The model adopted is a sound field model, and the sound field model is furth...
Embodiment 2
[0081] Two points A (124.1°E, 26.38°N) and B (124.8°E, 24.63°N) were selected, see the topographic map Figure 5 , to calculate the sound field propagation in the vertical section from A to B. Image 6 The sea surface height anomaly in the Okinawa trench area is given. It can be seen that the sound propagation at points A and B will also be affected by the Kuroshio frontal vortex. Point A is located in the low temperature area of the sea surface, and point B is located in the high temperature area of the sea surface. region, the sound velocity profile changes horizontally. To forecast the sound field of the vertical profile at two points A and B, firstly, interpolate between the two points A and B with an interpolation interval of 1km to obtain the latitude and longitude of each interpolation point; The temperature and salinity equivalent values of the rectangular area near the line B are read from the global ocean and land database (GEBCO), and two-dimensional linear i...
Embodiment 3
[0083] For the sound source point A (124.1°E, 26.38°N), calculate the sound field in the distance-azimuth horizontal profile for one revolution around A. For the sound field forecast of the horizontal section around point A, first read the forecast results of water depth, temperature, salinity, sea surface roughness, etc. in the circular area around A from the ocean model forecast results. The average value is taken at intervals within 360° azimuth angle, and the water depth, temperature, salinity, etc. are taken at intervals of 1km for each azimuth propagation path. The data of each interpolation point is obtained by two-dimensional linear interpolation of the data of the four surrounding latitude and longitude points. The speed of sound is calculated from water depth, temperature, salinity, etc. based on empirical formulas. Input the data such as water depth and sound velocity, sound source information, sea surface roughness and seabed parameters into the sound field model f...
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