A method for inversion of internal wave amplitude based on multi-dimensional sea surface information
A wave amplitude and inversion technology, which is applied in the field of internal wave amplitude inversion based on multi-dimensional sea surface information, can solve the problem of inability to obtain the fluctuation of sea surface height caused by internal waves and other problems, and achieve the effect of high-precision inversion.
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Embodiment 3
[0031] Example 3: Influence of Internal Waves on Sea Surface Height
[0032] Such as Figure 5 As shown, both the measured and simulated internal wave experiments have shown that internal waves can cause fluctuations in sea surface height.
[0033] During the actual measurement in the Andaman Sea, it was found that the passage of internal waves would cause the sea surface to bulge, and the empirical formula for the change of sea surface height was given as ~(ρ 2 -ρ 1 )·η 0 , where ρ 1 is the upper water depth density, ρ 2 Lower water depth density, η 0 is the amplitude of the internal wave, indicating that the height of the sea surface fluctuation caused by the internal wave is also closely related to the amplitude of the internal wave.
[0034] Using quasi-synchronous observations of altimeter and SAR images to detect internal waves in the South China Sea, the results show that the sea surface height anomaly caused by internal waves can reach 0.5m. Such as Image 6 As...
Embodiment 2
[0036] Example 2: The influence of internal waves on the sea surface current field
[0037] By analyzing the large-scale internal waves in Dongsha Island, such as Figure 7 As shown, the left picture shows the SAR image of the internal wave, and the right picture shows the information map of the flow velocity caused by the internal wave. The comparison between the two shows that the propagation will cause a strong wave-induced flow. big. The relationship between the amplitude of the internal wave and the wave-induced flow can be expressed as where U x Indicates radial flow velocity caused by internal waves, c 0 Indicates the internal wave linear velocity, h 1 Indicates the upper water depth, η 0 Indicates the amplitude of the internal wave, l represents the characteristic wavelength of the internal wave, and x, t represent the temporal and spatial changes of the internal wave.
[0038] This embodiment shows that the internal wave will have a significant impact on the se...
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