(A) SMC 



1000 



500 - 



n 1 1 1 i 1 1 1 1 1 1 1 1 r 



j! L 



\^ 



1[ 



1 1 \ i 1 r 



•.**»^ — H- 



(B) East Wind Component 



20 



■g 



-20 



20 



^ 



-20 



T 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 r 



v^/V-Nv-^ 



J I I I I I I L 





(C) North Wind Component 



—I 1 1 1 1 1 1 1 1 1 1 1 1 1 1 \ 1 1 1 T" 



_i I I I I I I I I I I I i_ 



J I I L. 



(D) East Current Component 



n I I I I I I I I I I I I I I I I ( I I * I 



(E) N«th Current Conqxment 



20 



1 0- 



-20 



1 1 1 1 1 1 1 1 1 1 1 1 1 1 r 



h 



I I I I I I I I LJ—U 



T 1 1 1 r 



11/16 11/19 11/22 11/25 11/28 11/31 12/03 12/06 



Figure 3-32. Enlargement of the period during which the largest SMC 



perturbations were observed, November 16 to December 6, 1993. 

 Concentration data are compared with wind and current data. 



