[TS]-relationship and Connection with Mixing Processes and Large Water Masses 211 

 Table 82. Water masses of the South Atlantic between 33° S. and 11° N. 



Atlantic but solely for 400-1400 m depth. The values for L and h in the Jacobsen equa- 

 tion on p. 210 can be obtained immediately from the curves and in that way Table 

 82fl is obtained. 



The mean value of Ajpu is 0-74 and for ti = 10 cm/sec the quantity A is 7-4 cm^/sec 

 which is in good agreement with values determined by use of other methods. A 



2°° : West Atlantic Irouqh ^ y 



S=f(t) J.^ >^ ^'^ 



340 «» 3&0 



340 14 5 3S0 



340 M5 350 



34-0 M-5 350 



°f .'^ ™®^' J 'C '"• '"'^v -^ i-<'''''5''' /'^!c i[^' /ihU's^'^T 



i°t ■ Bs^ Bsa*- Bsv<c . . Bsy Bs«<5 



34 5-15 35 



Fig. 98. [rSJ-curves for a series of stations along the Western Trough of the Atlantic. 



Table 82a. Determination of Aj pii by 

 means of the Jacobsen method 



