By C. Kramer and H.J. Gerhardt (Eds.)
Held less than 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 includes approximately ninety papers released in complete size, including summaries and discussions on different attention-grabbing and beneficial papers provided on the convention
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R e c e n t S p e c t r a o f A t m o s p h e r i c T u r b u l e n c e , Q . J . R o y . M e t . 94, 1968. S i n g e r , I . A . E. and F r i z z o l a , T . A . , The M i c r o m e t e o r o l o g y o f t h e T u r b u l e n t Flow F i e l d i n the A t m o s p h e r i c B o u n d a r y L a y e r , P r o c . I n t . R e s . S e m i n a r on Wind E f f e c t s on B u i l d i n g s and S t r u c t u r e s ( O t t a w a ) , Univ. of Toronto P r e s s , 1967. , Amsterdam — Printed in The Netherlands THE STRUCTURE OF TURBULENCE DURING STRONG WINDS H.
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 .
B u t when t h e v e r t i c a l i s v e r y l a r g e , the w e l l - k n o w n e x p r e s s i o n o f the c o r r e l a t i o n separation distance coefficient and t h e eddy c o h e r e n c e i s n o t a p p l i c a b l e . 15m, the v e r t i c a l recognized. tors for correlation o f t h e v e r t i c a l w i n d v e c t o r was s c a r c e l y F i g . 6 shows c o r r e l a t i o n t h e d u r a t i o n of coefficients, R^ of horizontal wind v e c D = 200 min and 20 min a g a i n s t t h e w i n d s p e e d , u 9 w h i c h i s g i v e n by t h e g e o m e t r i c a v e r a g e o f t h e w i n d s p e e d s a t two h e i g h t s .