Prof. Loomis’s Remarks upon Prof. Everett's Article. 31 
Conversely, i 
a,=A, poe = A,X 10115 
d,=A, ba = A, x 10472 
m 
a,=A, a a8 = A,X11107 
a,=A, — a = A, x 12092 
&e. &e. 
Hence, to reduce monthly to daily results it will simply be 
necessary to multiply the amplitudes A,, A,, &c., as above indi- 
cated. The logarithms of the multipliers for A,, A,, A, and A, 
are as under. 
are 15° 
log. "5 = “0040725 
log: = -0200286 
log. ona = -0456049 
log. pe = 0824980. 
Arr. IIl.—Remarks upon the Article of Prof. J. D. Everett; by 
E. Loomis, Professor of Natural Philosophy and Astronomy 
in Yale College. 
Iy the preceding article, page 18, Prof. Everett has adopted 
the formula 
y=A+asin (x+e); 
to represent the annual fluctuation of temperature at any place, 
i urve has 
one maximum and one minimum in the year, which ote; sheorat 
half a year asunder ; and the curve is bisected symmetric ly at the 
ature. 
