Sea surface wind direction extraction method based on ship-borne high-frequency ground wave beyond visual range radar
A technology of over-the-horizon radar and sea surface wind direction, which is applied in the reflection/re-radiation of radio waves, radio wave measurement systems, and the use of re-radiation. High resolution, simple system, easy to achieve
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specific Embodiment approach 1
[0024] Specific implementation mode one: the following combination figure 1 Describe this embodiment, the sea surface wind direction extraction method based on ship-borne high-frequency ground wave over-the-horizon radar described in this embodiment, the specific process of this method is:
[0025] Step 1. Select a range gate, and use a single receiving array element to obtain the first-order sea clutter spread spectrum in a range gate;
[0026] Step 2, establishing the space-time correspondence relationship of the first-order sea clutter broadened spectrum, and obtaining the space-time distribution characteristics of the first-order sea clutter broadened spectrum;
[0027] Step 3. According to the space-time distribution characteristics of the first-order sea clutter, determine the positive Bragg peak B corresponding to the incident azimuth of the sea clutter + , negative Bragg peak B - and spatial resolution;
[0028] Step 4. Obtain the relative intensity R of the positiv...
specific Embodiment approach 2
[0041] Specific implementation mode two: the following combination figure 1 This embodiment is described. This embodiment further describes Embodiment 1. The first-order sea clutter spread spectrum described in Step 1 is obtained by using a single receiving array element set on a mobile ship-borne platform.
specific Embodiment approach 3
[0042] Specific implementation mode three: the following combination figure 2 with image 3 Describe this embodiment, this embodiment will further explain Embodiment 2, the space-time distribution characteristic of the first-order sea clutter broadening spectrum described in step 2 is:
[0043]
[0044] where f d is the Doppler frequency, is the Bragg frequency, v is the velocity of the ship-borne platform, λ is the working wavelength of the radar, and g is the acceleration of gravity.
[0045] In this embodiment, through the space-time distribution characteristics of the first-order sea clutter broadening spectrum, according to the incident azimuth of the sea clutter The position and peak size of the corresponding positive and negative first-order Bragg peaks can be determined B + ,B - .
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