By C. Kramer and H.J. Gerhardt (Eds.)
Held below the auspices of the overseas organization for Wind Engineering, 226 delegates from twenty-three international locations took half within the convention. This 3 quantity paintings comprises approximately ninety papers released in complete size, including summaries and discussions on different attention-grabbing and invaluable papers awarded on the convention
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Extra info for Advances in Wind Engineering
Aerodynamics, 1 0 , 63-78. A . J . Bowen e t a l . , V e r t i c a l C o h e r e n c e and Phase D e l a y Between Wind Components i n S t r o n g Winds Below 2 0 m, B o u n d a r y - L a y e r M e t e o r o l o g y , 2 6 , ( 1 9 8 3 ) 3 1 3 - 3 2 4 . , o f Atmospheric Turbulence Near t h e G r o u n d , Nos 74030 a n d 7 4 0 3 1 , 1 9 7 4 . 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 .
Al A 2 ' Line = Al combining Al A2 A2' the Figure sin a is always perpendicular to (4) the winddirection. maximum of the correlation with the virtual distance, ted. * 9 By corresponding a horizontal crosscorrelation can be construc shows correlation versus width of the eddy at a 45 height of 8 m. 0 _ with is the needed tower A 2 ' . 6. 7. Horizontal lation with a tower 200 400 r in m crosscorre distance of 60 m and an angle of 44° of 60 m and an angle of 4° Similar to the autocorrelation, an exponential function is fitted and an integral scale calculated.
0 the s t r o n g g u s t , t h e maximum i n s t a n t a n e o u s wind speed s u d d e n l y i n c r e a s e d from about 20m/s to Fig. to s y s t e m . Wind v e c t o r s m e a s u r e d were s a m p l e d e v e r y 0 . 0 6 s e c , and a n a l i z e d by s t a t i s t i c a l 10 m i n , 30 min o r 4 0 0 min i n of respectively. two heights. 30 54 the well-known e m p i r i c a l ordinally e x p r e s s i o n s . The l o w e r p o i n t s were o b t a i n e d f o r We f i n d h e r e t h a t t h e g u s t f a c t o r s turbulence.