Uncertainty Estimation Method of Wind Speed Fluctuation Based on Instantaneous Model of Effective Turbulence Intensity
A technology of turbulence intensity and uncertainty, applied in the direction of calculation, special data processing applications, instruments, etc., can solve problems such as excessive forecast error, excessive forecast error estimation, and inability to use power grid dispatching plans to improve accuracy , avoid security settings, avoid the effect of redundant rotating hot standby
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specific Embodiment approach 1
[0033] Specific implementation mode one: In this implementation mode, the uncertainty estimation method of wind speed fluctuation based on the instantaneous model of effective turbulence intensity, its specific steps are as follows:
[0034] Step 1, determining the decomposition scale according to the spectral gap of the low-level atmospheric motion power spectrum;
[0035] Step 2. Using the Mallat wavelet decomposition and reconstruction algorithm as a tool to decompose and reconstruct the wind speed time series of the measured wind speed data, obtain the hourly average wind speed and the corresponding turbulence residual;
[0036] Step 3, using the Mallat wavelet decomposition algorithm to decompose the squared turbulent residual and then reconstruct it to obtain the smoothed variance, the arithmetic square root of the smoothed variance is the instantaneous standard deviation of the turbulent residual;
[0037] Step 4. Calculate the effective instantaneous turbulence intensi...
specific Embodiment approach 2
[0046] Embodiment 2: The uncertainty estimation method of wind speed fluctuation in this embodiment is different from Embodiment 1 in that the wavelet base of the wavelet decomposition in step 2 is db10. The rest are the same as in the first embodiment.
specific Embodiment approach 3
[0047] Embodiment 3: The uncertainty estimation method of wind speed fluctuation in this embodiment is different from Embodiment 2 in that: in step 2, the wavelet reconstruction is combined with Shannon sampling theorem to obtain the hour-level average wind speed. The rest are the same as in the second embodiment.
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