The BT slides were processed and the data are on file at NODC 

 under reference number 06506. 



Oceanographic parameters are reported in the English or metric 

 units of measurement normal to the measuring instrument. For convenience, 

 equivalents are given in figures and tables where applicable. 



IV. PERSONNEL AND ACKNOWLEDGMENTS 



Personnel participating in the survey were Messrs. R. A. Schaeffer 

 (AGOR Coordinator), S. G. Tooma (Senior Scientist), H. Iredale, III, 

 L. E. Jarvela, P. Bockman, and L. S. Jordan of NAVOCEANO, Mr. K. 

 Hart of Seiscor Corporation, and Mr. R. K. Oser of the Geophysics 

 Division, Pacific Missile Range. 



Acknowledgment is given to Mr. R. A. Stewart for his interpretation 

 of the geological data and Mr. J. A. Bruce for his distribution analysis 

 of the biological data. 



V. DATA ANALYSIS 



A. Temperature. 



Temperature-depth profiles of the oceanographic stations showed 

 several interesting features. Representative profiles for both months 

 are presented in Figure 5. In September, an isothermal layer extended 

 to a depth of 15 meters. A sharp thermocline existed from this depth 

 to about 150 meters below which temperatures decreased gradually 

 to the lowest observed depth. The October data showed essentially 

 the same distribution with the exception of the surface isothermal 

 layer which was observed only to a depth of 5 meters. 



TEMPERATURE ° c TEMPERATURE 

 4 6 8 10 12 14 16 18 6 8 10 12 14 16 18 20 



100 



200 



300 



400 



w500 



til 



j600 



700 



800 



900 



































■300 

 -600 

 -900 

 -1200 

 -1500 

 -1800 £ 



IL 



-2100 

 -2400 



-2700 























/ 

































/ 















/ 

















J 



/ 















/ 

































/ 































/ 

















,/ 



1 































t 

























Grid Station No 11 

 22-24 September 1965 











Grid Station No.5 

 11-14 October 1965 



41 44 47 5 



53 56 59 62 65 P 41 44 47 5 



53 56 59 6 2 65 





FIGURE 5. REPRESENTATIVE TEMPERATURE VERSUS DEPTH PROFILES 



Two depths, 5 and 200 meters, were selected for presentation 

 of horizontal temperature distributions (Fig. 6). The 5-^neter depth 



