Calculating method for limited area of wind-driven rain amount
A limited area and calculation method technology, applied in the field of wind engineering, can solve the problems of huge raindrop trajectory calculation amount, single raindrop trajectory calculation amount, etc., and achieve the effect of reducing the number of raindrop trajectory, reducing the calculation amount, and accurate collection rate distribution
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Embodiment 1
[0041] Example 1: Calculation of three-dimensional accessibility index wind field collection rate.
[0042] The calculation domain is a three-dimensional barrier-free index wind field, which is 300m long, 50m wide, and 200m high, and corresponds to the x-y-z three-axis directions. Such as figure 2 As shown, the inlet boundary 4 of the calculation domain is given the incoming flow velocity type, and the expression is as follows:
[0043]
[0044] In the formula, u represents the local wind speed; u 0 Represents the reference speed, take 10m / s; h represents the local height; h 0 It represents the reference height, which is 10m; α is the index, which is 0.176.
[0045] The plane 6 to be calculated for the collection rate is located at the exit boundary 5, and the width and height of the plane 6 to be calculated are 10m. Divide the plane 6 to be calculated into 8×8 finite areas, image 3 The limited area division is given. The chosen reconstruction function has the follo...
Embodiment 2
[0049] Example 2: Calculation of collection rate on the windward side of a three-dimensional square building. The length, width and height of the building are all 10m. Such as Figure 7 In the calculation area of the three-dimensional square building shown, the incoming flow velocity type is given at the entrance boundary 7 of the calculation area, the expression is the same as formula (2), and the reference velocity u 0 =10m / s, reference height h 0 = 10m, exponent α = 0.15. Divide the windward side 8 of the three-dimensional square building into 20×20 limited areas, and the form of the selected reconstruction function is as follows:
[0050]
[0051] In the formula,
[0052]
[0053] Among them, L is the Lagrangian interpolation function; (y p ,z q ), (y l ,z k ) are the sample point coordinates respectively.
[0054] Figure 9 and Figure 10 References [1] are given respectively (References [1]: B. Blocken, J. Carmeliet, On the validity of the cosine proje...
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