Hydrodynamics of Semi-Enclosed Seas, Proceedings of the 13th by Jacques C.J. Nihoul (Eds.)

By Jacques C.J. Nihoul (Eds.)

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I n s t e a d , t h e w a t e r s n e d w h i c h feeds i t i n t h e NH i s woody and humid, p a r t i c u l a r l y i n w i n t e r : t h e f l o w o f r i v e r s i n t o t h e sea i s m a i n l y i m p o r t a n t on t h e N o r t h e r n s h o r e and i n t o t h e B l a c k Sea ; t h e o n l y i m p o r t a n t r i v e r o f t h e Southern s n o r e i s t h e N i l e . I f t h e f l o w s f r o m t h e RhBne, t h e P6, t h e Danube and t h e N i l e a r e r e l d t i v e l y r e g u l a r , t h o s e f r o m t h e Russian r i v e r s t o t h e B l a c k Sea e x h i b i t a maximum volume a t t h e end o f s p r i n g and a t t h e b e g i n n i n g o f summer.

_ . _ . i + i n 92 001 00; Internal wave o f s a l i n i t y i n A4. 8 may 1967. Bathysonde yoyo-ing ( N / O "Jean C h a r c o t " ) . 41 The h y d r o l o g i c a l regime i s a l s o s u b j e c t t o i m p o r t a n t t i d a l e f f e c t s ; a determined i s o t h e r m , o r isohaline,changes F i g . 14 i s r e s u l t i n g i t s depth with t i n e ( f i g . 13 and 1 4 ) . f r o m t h e use of a y o - y o i n g bathysonde e v e r y 15 mn. I n t e r n a l waves a r e p r e s e n t ; t h e i r a m p l i t u d e i s 5 0 t o 60 m ; the "high water" o f the i n t e r n a l t i d e i s about one h o u r i n advance w i t h r e s p e c t t o t h e s u r f a c e t i d e , and c o i n c i d e s i n time w i t h t h e b e g i n n i n g o f t h e g l o b a l i n f l o w - c u r r e n t a t t h e s u r f a c e .

1 V e r t i c a l p r o f i l e o f mean v e l o c i t y and l o n g i t u d i n a l s l o p e o f t h e mean i n t e r f a c e . One o f t h e i m p o r t a n t c h a r a c t e r s o f t h e mean regime i s t h e v e r t i c a l mean v e l o c i t y p r o f i l e i n v a r i o u s p l a c e s . The w i d t h o f t h e channel f o r v a r i o u s depths on d i f f e r e n t c r o s s - s e c t i o n s , as w e l l as t h e d e p t h o f t h e " i n t e r f a c e " between t h e two superimposed waters,play a c o n s i d e r a b l e r o l e on t h e v e r t i c a l mean c u r r e n t p r o f i l e ( f i g .

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