A Sea Surface Wind Velocity Retrieval Method Based on Imaging Altimeter Remote Sensing Data
A sea surface wind speed and inversion technology, applied in speed/acceleration/shock measurement, radio wave reflection/re-radiation, fluid velocity measurement, etc., can solve the problem of not applicable sea surface wind speed inversion model function, etc., to achieve data processing process Ease of use, high inversion accuracy and simple principle
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Embodiment 1
[0037] Example 1: Building a function model
[0038] S1: Matching data preparation:
[0039] S1-1: Simulation Dataset
[0040] S1-1-1: When the measured data cannot be obtained before the launch of the imaging altimeter satellite, the simulation data set can be used to construct the model function. The simulation data is obtained based on the theoretical formula of the sea surface backscatter coefficient combined with the observation conditions of the imaging altimeter, and the observation band, incident angle and sea surface wind speed are the input parameters.
[0041] S1-1-2: Assuming that the imaging altimeter observation conditions are: the observation band is the Ku band, the satellite orbit height is 850km, the sea surface observation swath is 160km, and the sub-satellite observation blank length is 10km, then the angle of incidence θ ranges from 0.67° to 11.3° ( See Figure 4 ).
[0042] S1-1-3: The formula for calculating the sea surface backscatter coefficient is ...
Embodiment 2
[0079] Example 2: Inversion of sea surface wind speed
[0080] S4-1: Perform quality control and grid processing on the imaging altimeter remote sensing data to provide basic data support for the inversion of sea surface wind speed;
[0081] S4-2: when the angle of incidence is less than 7°, the sea surface wind speed inversion selects the model function of the radar altimeter; within the angle of incidence of 7° to 11.3°, utilizes the newly established double-exponential wind speed model function to invert the wind speed;
[0082] S4-3: By setting the wind speed initial guess value and iteration method, utilize the maximum likelihood method criterion to invert the sea surface wind speed;
[0083] S4-4: The maximum likelihood method for sea surface wind field inversion, which determines the sea surface wind speed by comparing the difference between the backscatter coefficient calculated by the model function and the backscatter coefficient obtained by measurement.
[0084] Th...
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