By Jacques C.J. Nihoul (Eds.)
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Additional info for Hydrodynamics of The Equatorial Ocean, Proceedings of The 14th International Liege Colloquium on Ocean Hydrodynamics
Again t h e s u r f a c e d r i f t d i r e c t i o n s a r e i n agreement with t h e subsurface s t r u c t u r e ( F i g . 5 ) a n d w i t h t h e s u r f a c e s a l i n i t y w h i c h i s maximum b e t w e e n a n d 10'N of c o r r e s p o n d i n g t o t h e w e s t w a r d d r i f t of the northern ward d r i f t , eddy. ON. 6 < S < 3 6 % 0 ) s i m i l a r The v a l u e s l e s s t h a n 3 5 . 3 % 0 a p - N i n the eastward equatorial j e t . To s u m m a r i z e t h e s e o b s e r v a t i o n s seems t h a t t h e p r i n t o f a f t e r t h e o n s e t of 1°N the southern p a r t the northern i n t h e Somali b a s i n , it Somali eddy i s always t h e r e t h e SW monsoon w i t h a t r o u g h a s d e e p a s 1 5 0 me- t e r s and w i t h a s t e e p e r f r o n t i n t h e n o r t h which c o u l d be due t o t h e p r e s e n c e of the coast.
T h i s m e r i d i o n a l seasonal o s c i l l a t i o n o f t h e t h e r m o c l i n e i s s i t u a t e d approximat i v e l y under t h e mean p o s i t i o n o f t h e I n t e r t r o p i c a l Convergence Zone (ITCZ). The ITCZ p o s i t i o n v a r i e s s e a s o n a l l y o v e r a l a r g e l a t i t u d i n a l band which extends r o u g h l y f r o m t h e e q u a t o r t o 10-15' N o r t h ( F i g . 12 a - b ) and covers t h e oceanic r e - g i o n s where maximum a m p l i t u d e and phase changes i n t h e depth o f t h e t h e r m o c l i n e a r e observed.
46 F i g . 11 a : R a t e o f change o f h e a t c o n t e n t from 0 t o 50 m e t e r s i n June ( i n W/m2) F i g . 11 b : R a t e o f change of h e a t c o n t e n t from 0 t o 50 m e t e r s i n September ( i n 'l/m2). 47 Fig. 12 a and b : Seasonal m i g r a t i o n o f t h e I T C Z o b t a i n e d from t h e a t l a s o f HASTENRATH and LAMB ( 1 9 7 7 ) . 48 between 3 and 8' N. The zonal t i l t o f t h e t h e r m o c l i n e a t t h e e q u a t o r was a l r e a d y known (MERLE 1980b ) and c o n f i r m e d by e q u a t o r i a l models (CANE and SARACHIK 1980 PHILANDER and PACANOWSKY 1981).