these relations are: 



F I=^ 



(x D + 6iy/i.s , if x D < - 3Rh 



| X D |/1.5 , if -3^ < X D < 



X D |/7 , if X D > 



(H-12) 



and 



D f = 0.2 , 



S f = 0.5 , 



1.0 



(H-13) 

 (H-14) 



(H-15) 



The Hurricane Gracie wind fields were not deformed because the 

 winds are presented in digital form. Any deformation obtained would 

 be dependent upon a subjective analysis which requires additional 

 developmental work. Moreover, the selection of Gracie was made on 

 the knowledge that the results would possibly be compared with those 

 obtained by other investigators using symmetric wind fields. 



162 



