



200 





50 



>100 FATHOMS 



5U 



<100 FATHOMS 











40 



1 



40 



— 







150 









^ 





1 

 1 











30 



_ 



1 





30 



_jn 





AREA E 





100 



1 







1 













1952 







i 



20 



- 



j; 





20 



- 











50 





1 



























i 

 il III *" ^' 



10 

 



.JlUi 





^1 



10 

 



_[r 



_J 



1 1 1 















0/>/A 





z 



zOO ''^ 





z 



^100 FATHOMS 



z 



100 FATHOMS 





o 







o 





o 







1- 







^- 40 



- 



1- 40 



- 





< 



150 



_ 



< 





< 







> 







> 





> 







q: 







Qi 





cc: 





AREA C 



LU 







i^ 30 



1 



[^ 30 



1 



1953 



CQ 

 O 



u_ 

 O 



100 



± 



CQ 



o 

 fe 20 



n 





CO 

 o 



- 20 



- A 







a: 





r^ ' ^ 



h- 







1— 





1 



n 





LU 



SO 



J ' 



Z 







z 





1 1 





CD 



z 







^U^ 



^ 10 

 u 



Q^ 

 LU 



a. 



"/l\ 



LU 10 



u 



a: 



LU 



°- 



if 



i^ 



















50 











200 







100 FATHOMS 



50 



• 100 FATHOMS 













40 





40 



_ 







150 



- 







L 







AREA B 









'- 



30 



- 







30 



r-H 







100 



— 



















1954 











20 



" r 



1- 





20 



1 



L 









50 



- 1 



1 ^ 



10 



J ; 





10 



r-l 













Jj 



i^ 



n 



^, ! 



7^ 



n 



r4, fl 1 1 



S 



1 



-4 



DIFFERENCE, DEGREES F 



49 



Figure 10. Differences befween observed and computed sea-surface temperatures for 

 water depths greater than and less than 100 fathoms. 



