Microwave over-the-horizon radar echo chart calculating method
A technology of over-the-horizon radar and graph computing, applied in radio wave measurement systems, instruments, etc., can solve the problems of over-the-horizon sea clutter interference, sea surface reflection, radar blind spots, etc., and achieve the effect of evaluating sea surface echo power
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Embodiment 1
[0059] Embodiment 1, in the development process of the microwave over-the-horizon radar, parameters such as the height and strength of the ocean-atmosphere waveguide or the atmospheric refractive index profile are set in the laboratory. The expression of the atmospheric modified refractive index profile of the evaporation waveguide is:
[0060]
[0061] In the formula, M(0) and M(z) are the atmospheric corrected refractivity at sea surface and height z respectively, h 1 =h t =z EDH is the height of the evaporation waveguide, the roughness length z 0 =1.5×10 -4 .
[0062] Compute the sea surface grazing angle for atmospheric duct conditions, such as Figure 5 shown. Further, the sea surface scattering coefficient is obtained by using the clutter model, and the RCS of the corresponding resolution unit is obtained from the radar parameters.
[0063] Calculate the basic propagation loss considering the influence of the environment, and extract the propagation factor F: ...
Embodiment 2
[0068] Embodiment 2, during the use of microwave over-the-horizon radar, based on the monitoring equipment of marine hydrometeorological parameters, the oceanic atmospheric temperature, humidity, pressure, wind speed and direction, and sea surface temperature are obtained, and the evaporation waveguide prediction model such as the P-J model is selected to calculate the evaporation waveguide height , intensity and atmospheric refractivity profiles. The P-J model is the most widely used prediction model for evaporation waveguide. Jeske uses the potential refractive index instead of the atmospheric refractive index, the potential temperature instead of the ordinary temperature, and the potential water vapor pressure instead of the usual water vapor pressure. The atmospheric stability and Monin are determined by the overall empirical Richardson number. -Obukhov similar length, based on the assumption that the bit refractive index is conserved and is a similar variable, the evaporat...
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