SXAXION 1097 1 1 00 



45576910 234567 



, rr— [— I — 1 ■'■('■' 1 ! \ p— t — I T' i'l 



STATiOH 355 59 1041 



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"Oi—j — I I ' yr , 1 T"! ' r ' t - vi e ' V fv t yy i } i (r ri'-r t 



Representative Temperature Curves of Water Columns in Davis Strait 



AND Baffin Bay 



Figure 120. — The degree of solar warming of the surface hiyers, to a depth of 150 

 meters or less, in vari'ous parts of Davis Sti-ait and Baffin Bay, is shown on the 

 shaded areas above. The temperature Centigrade is recorded as the abcissa and 

 the depth in metei's as the ordinate. The greatest increase in temperature, as nat- 

 urally should be expected, occurs in the southern stations of this region, such as 

 1125 and 355, while the least affected are Baffin Bay stations', such as 100 and 

 1015. The geographical position of the stations is shown on Figure 121, p. 200. 



198 



