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By Jacques C. J. Nihoul

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Extra info for Marine Forecasting: Predictability and Modelling in Ocean Hydrodynamics, Proceedings of The 10th International Liége Colloquium on Ocean Hydrodynamics

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R a t c l i f f e and Murray (1970) d i s c u s s some evidence of a r e l a t i o n s h i p between l a r g e s c a l e S S T anomalies south of Newfoundland and weather p a t t e r n s over Europe during t h e following month, mainly during t h e fall. Near t h e equator, t h e a i r - s e a i n t e r a c t i o n s a r e s t r o n g e r . For example, Newel1 and Weare (1976) found t h a t t h e t r o p i c a l SSTIanomalies i n t h e P a c i f i c were leading t h e g l o b a l l y averaged temperature i n t h e t r o p i c a l troposphere by 6 months.

1 9 7 1 . An e x p e r i m e n t a l i n v e s t i g a t i o n o f t u r Moore, M . J . , b u l e n t s t r a t i f i e d s h e a r i n g f l o w . J. , 49:635-656. 1977. E n t r a i n m e n t . Chap. 7. B. , M o d e l l i n g and P r e d i c t i o n o f t h e u p p e r l a y e r s i n t h e o c e a n . Pergamon Press. , R h i n e s , P . B . , Thompson, R . O . R . V . , 1973. The d e e p e n i n g o f t h e w i n d - m i x e d l a y e r . G e o p h . , 3 : 3 8 1 - 4 0 4 . , 1975. P a r a m e t r i z a t i o n o f t h e i n t e g r a l t u r b u l e n t energy d i s s i p a t i o n i n t h e upper quasi-homogeneous l a y e r o f t h e o c e a n .

Fig. 10 shows the computed values of I[ times ft = ; i , II and 2II = EL D, as a function o f the at three different non-dimensional 30 -_ L, f 80 10 80 50 40 30 20 10 F i g . 8. T h e o r e t i c a l curve S ( f t ) f o r d i f f e r e n t v a l u e s of t h e s u r f a c e h e a t f l u x so i n t h e c a s e y = 0 . T h e c u r v e s I , 2 , 3 w e r e c a l c u l a t e d f o r R i w ( o ) = 5 0 , us = 1 , 5 1 0 - 2 m / s e c , D ( o ) = lm a n d so = 0 ; 2 . 1 0 - 5 a n d 1 0 - 4 0 C m / s e c , r e s p e c t i v e l y .

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