310 The Geophysical Structure of the Sea 



The numerical value of 035,0,0, is 0-97264 so that 



J„ , = 0-02736 - -, "!' ^ ^^in . . 

 *' * 1 + (^< X 10-3 



The specific volume anomaly S can then be determined quickly and easily using three 

 small tables. 

 The pressure /? at a dynamic depth D is by definition 



CD 

 /? = Ps,t,D 



dD. 



Table 111. Example of the dynamic evaluation of oceanographic observations of a single 



station 

 ("Meteor" St. 267, 18.11.27; (p = 13-7° N., A = 19-8° W., 4206 m) 



