Mountain area plane gust coefficient calculation method
A technology of coefficient calculation and gust, applied in calculation, computer-aided design, data processing application, etc., can solve problems such as early warning of difficult and strong gust events, reduced reliability of power system operation, and increased risk of power grid operation, so as to achieve management and control of operational risks, The effect of improving the level of operational reliability
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Embodiment 1
[0036] This embodiment provides the specific structure of the method for calculating the plane gust coefficient in mountainous areas, such as figure 1 As shown, the steps include:
[0037] Create a planar grid;
[0038] Based on the planar grid, calculate the average terrain elevation;
[0039] Calculate the height of the canyon surface based on the planar grid;
[0040] Calculate the height of the mountain surface based on the planar grid;
[0041] Calculate the grid gust coefficient based on the average terrain elevation, canyon face height, and mountain face height.
[0042] Further, the planarized grid is established by using the Lambert conformal conic projection to project the area of interest onto a 1km×1km grid.
[0043] Further, the calculation of the average terrain elevation is to use the refined terrain elevation data to obtain the average terrain elevation data of each grid point, and the terrain elevation of the i-th grid point is represented by Z i expres...
Embodiment 2
[0066] Such as figure 2 and image 3 As shown, the calculation method of the plane gust coefficient in mountainous areas includes:
[0067] Option 1: Utilize the technical method of the present invention to calculate such as figure 2 The distribution of gust coefficients in the Beijing area shown;
[0068] Scheme 2: Based on the data of 150 ground observation stations in the Beijing area, select the period of time when the wind speed is relatively high and calculate as follows image 3 The gust coefficient plane distribution shown.
[0069] By comparing the results of the two schemes, the following conclusions can be drawn:
[0070] The gust coefficient distribution maps obtained by the two schemes are relatively similar in terms of distribution shape and magnitude. This method simulates the large-value area of the gust coefficient in the valley in the northern mountainous area of western Beijing, which is consistent with most of the ground observation stations in ...
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