Method for estimating uncertainty of wind speed fluctuation based on effective turbulence intensity instantaneous model
A technology of turbulence intensity and uncertainty, applied in computing, special data processing applications, instruments, etc., can solve problems such as unusable power grid dispatching plan, excessive forecast error, and excessive forecast error estimation, so as to avoid redundancy Effects of rotating hot spares, avoiding security settings, and improving accuracy
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specific Embodiment approach 1
[0029] Specific embodiment 1: The method for estimating the uncertainty of wind speed fluctuations based on the instantaneous model of effective turbulence intensity in this embodiment, the specific steps are as follows:
[0030] Step 1: Determine the decomposition scale according to the spectral gap of the low-level atmospheric motion power spectrum;
[0031] Step 2: Use Mallat wavelet decomposition and reconstruction algorithm as a tool to decompose and reconstruct the wind speed time series of the measured wind speed data to obtain the hourly average wind speed and the corresponding turbulence residual;
[0032] Step 3. Use Mallat wavelet decomposition algorithm to decompose the squared turbulence residual and then reconstruct to obtain the filtered and smoothed variance. The square root of the filtered and smoothed variance is the instantaneous standard deviation of the turbulence residual;
[0033] Step 4. Find the effective turbulence intensity I corresponding to the hourly avera...
specific Embodiment approach 2
[0038] Specific implementation manner 2: The difference between the uncertainty estimation method of wind speed fluctuation in this implementation manner and the specific implementation manner is that the wavelet base of wavelet decomposition in step two is db10. The rest is the same as the first embodiment.
specific Embodiment approach 3
[0039] Embodiment 3: The difference between the uncertainty estimation method of wind speed fluctuations in this embodiment and the second embodiment is that in step 2, the average wind speed at the hourly level is obtained by combining the Shannon sampling theorem during wavelet reconstruction. The rest is the same as the second embodiment.
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