PHYSICAL OCEANOGRAPHY OF THE GULF OF MAINE 
577 
so that the temperature curves for the two dates recall those off Mount Desert for 
May 10 and June 14, 1915, in their mutual relationship. A similar seasonal rela- 
tionship also obtains between serials taken in the Fundy Deep near by on March 22, 
1920 (station 20079), and June 10, 1915 (station 10282). 
Temperature, Centigrade 
1 ° 2 ° 3 ° 4 ° 5 ° 6 ° 7 ° 8 ° 9 ° 10 ° 11 ° 12 ° 13 ° 
Fig. 40 — Vertical distribution of temperature in the Bay of Fundy in 1917, from Mavor (1923, 
Prince station 3, 1916-17). A, February 28; B, May 4; C, June 15; D, July 4; E, July 31; F, 
September 4. 
In 1917 the surface temperature had risen only to 8.68° at the Prince station by 
July 4 (Mavor, 1923, p. 375); the 50-meter level to 5.06°, the 100-meter level to 
4.5°, and the 150-meter level to 4.21°; but warming either took place more rapidly 
in the Bay of Fundy in 1904, or the temperature did not fall so low there during the 
preceding winter, because Dawson (1922, p. 82, station F) found the deeper strata of 
the Fundy Deep about 2° warmer than this a week earlier in the season, as follows: 
