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 attention-grabbing and necessary papers offered on the convention
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Additional info for Advances in Wind Engineering
REFERENCES 1 J . W. T e u n i s s e n , S t r u c t u r e o f Mean Winds and T u r b u l e n c e B o u n d a r y - L a y e r Over R u r a l T e r r a i n , 3 M. S h i o t a n i and Y . J. J. Correlations in High Winds, J . Met. S o c , Japan, 5 6 , (1978) Flay, Structure (1982) 187-221. Velocity 59-67. of Vertical 35-42. o f a Rural Atmospheric Boundary L a y e r near the G r o u n d , F l a y e t a l . , Wind S t r u c t u r e New Z e a l a n d , ( T h e s i s : P h . D . ) , 1978. i n a Rural Atmospheric Boundary-Layer Near t h e G r o u n d , J .
106. (7) obtained as a s p e c t r a l in t h i s w frequency n L /U = n L /U x x peak f r e q u e n c y . work were t h e l o n g i t u d i n a l scale of t u r b u l e n c e o f the u c o m p o n e n t and the l a t e r a l o n e s o f the v and w c o m p o n e n t s since this observation was one position measurement by the ultra sonic anemometer. 4. RESULTS OF A N A L Y S I S An a u t o r e g r e s s i v e method i s used f o r of the data. 5. the v a r i a n c e , are summarized in Table 1.
The t h r e e c u r v e s w i t h s e p a r a t i o n s o f 7 . 5 , 15 and 2 2 . 5 m r e a c h e d maximum v a l u e s n e a r x = 0 and for |x| > 20 s e c o n d s a l l observed for run 6 . 9 for determined. correction r = (1 - r °° m is fluctuations, The for p to compute the zero for length scale curves p ' . This is ( A y , x ) were a l s o v v l a r g e x and s o the the measured c o r r e l a t i o n , r^ r^ following them i s the c o r r e l a t i o n i s the v a l u e o f t h e c o r r e l a t i o n correction v v F i g .