By C. Kramer and H.J. Gerhardt (Eds.)
Held below the auspices of the foreign organization for Wind Engineering, 226 delegates from twenty-three international locations took half within the convention. This 3 quantity paintings includes approximately ninety papers released in complete size, including summaries and discussions on different fascinating and useful papers provided on the convention
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Extra info for Advances in Wind Engineering
Turbulence of the The a b o v e p r o c e s s e s v component and v hold for the is power s p e c t r u m o f the w component. A s c a l e of turbulence, is a integral o b t a i n e d from a time i n t e g r a l g u s t y w i n d by T a y l o r ' s h y p o t h e s i s . component g i v e s the longitudinal scale of a s p a t i a l correlation s c a l e o f an a u t o c o r r e l a t i o n The a u t o c o r r e l a t i o n s c a l e of turbulence, L - X coefficient, coefficient Uc o e f f i c i e n t of of the u T h o s e o f the v and w 34 TABLE 1 Summary o f o b s e r v a t i o n u component Run No.
W. T e u n i s s e n , C h a r a c t e r i s t i c s o f t h e Mean Wind and T u r b u l e n c e Planetary 10 Characteristics E n g i n e e r i n g S c i e n c e s Data U n i t , i n the B o u n d a r y L a y e r , U T I A S Review No 3 2 , 1 9 7 0 . A. Panofsky, Scale A n a l y s i s o f Atmospheric Turbulence Roy. M e t . S o c , 8 8 , (1962) 57-69. a t 2 m, Q u a r t . J . , Amsterdam — Printed in The Netherlands 31 POWER SPECTRA OF LONGITUDINAL AND LATERAL WIND SPEED NEAR THE GROUND I N STRONG WINDS J.
8). (2) 1/a Fig. 2. Autocorrelation of wind speed in 8 m height in Meppen The integral scale varies with height according to the empirical formula. 3 z° This relation is valid only at a range of 8 to 80 m height and for the flat and open country in Meppen. 7) . l). the The scale, 43 VERTICAL The speed CROSSCORRELATION vertical crosscorrelation between two time series of in different heights gives information about the slope the eddyfront. The larger the distance between the two the weeker the peak of the crosscorrelation as is is wind of heights, shown in figure 3.