502 REPORT—1868. 
Table of Corrections of the 6 x 16 Coefficients A,, B,, &c. (continued). 
K L M N O 
(y—) (vy)  (y-30-3@) (y-9) (y-$e+30) (y—20) 
A, —*0005 +0043 +0067 —‘oool +0015 —*0046 
B; —"0013 +'0026 —"0041 —"0013 +'0016 —"0003 
A, +°0105 —‘o1or +°0037 + "0009 —"0052 + ‘0024 
B, —"o184 +°0075 +0020 —‘ooI4 +:0088 —‘o1og 
A, —'0198 +oo12z —‘oorr — ‘0007 —"0004. —'0097 
B, — ‘0042 +0009 +0017 + °Oo17 —"0020 —*0067 
AY —*0030 +°'0039 —"O145 —*0002 +:0021 +:0086 
B, —*0035 +'0042 +0014 —"‘oolo —'0031 —"0103 
A, +0002 — "0009 —"0431 + "0005 + "0008 +°0029 
B, -+-*oool +0064 +°0362 —‘Ool4 —‘oolo —*0030 
Values of A,, A,, &c., to second Approximation. 
8 K L M N O 
(y—7) (y) (y-0-3e) (7-9) (y-$0+4%) (y—20) 
A, +0'0256 —0°2050 —0'0284 +0'0136 +0'0332 —0'2931 
5, —0'0270 —0°0237 —0'0070 —0°0055 +0°'0016 +0'0631 
A, +1°5616 —0'4227 —0'2341 —4°3167 +0°8098 —o'0716 
Is +1°0027 —o'0166 +0°3007 +4 5004 —0°7443 -+o°0001 
A, +0°0077 —o'0050 —0'0022 —o'01l3 —0'0007 —o’oo1o 
B, +0°0008 +0°0089 —0'0059 +0°0423 +0°0067 +0°0046 
AN, +0°0300 —o’oI70 —0'°0524. —0°5442 —o*o1og +0°0076 
B, -+0°0022 —0'0047 —o0'0886 —o'0865 —0'0138 +0°0037 
A, —O'OIOS -+0°0050 —o'0060 +0°0023 -+-0°0039 —o"0002 
B, +0°0213 —0°0003 +0°0026 +0°0033 —0'0036 +0°0035 
A, +0'0215 —0'0020 —0°0039 —O'lI2§ —0'0283 +0°0035 
Bs +o'o110 +o0'0018 —o'0096 —O'li3I —0°0004. +0'0107 
A, +0°0038 —0*0009 +0°0089 +0°0023 —0°0042 +oo116 
B, +o0'0081 —0'0053 -+0°0029 —o'0021 +0'0027 +0°0019 
A, +0'0009 +0°'0067 +o'ooro +0'0290 +0'0040 —0'0086 
B, +0'0027 — 0°0097 —0'0050 — 00402 -+-0°0009 +0°0103 
‘A. 10°1988 10°1989 10°1843 I0°1g992 10°1853 IO°I1971 
22. The values A,, B, in columns § and M express the mean solar semi- 
diurnal and mean lunar semidiurnal tides. 
A,, B, of column K express the lunar declinational semidiurnal tide. 
A,, B, of columns L and N express two constituents of the lunar elliptic 
semidiurnal tide. 
A,, B, of column O express zero tolerably well*. 
A,, B, of columns K and O express the two constituents of the lunar 
diurnal tide. é 
A,, B, of column § express one constituent of the solar elliptie diurnal 
tide. 
A,, B, of column M express one constituent of the lunar elliptic diurnal 
tide t. 
A,, B, of columns L and N possibly depend on the elliptic lunar diurnal 
tides, but will no doubt be found a better approximation to zero when 
* There being no theoretical tide of the period corresponding to them. 
_ t Being the resultant of the two corresponding angular velocities y—o+m and y—o—@, 
inasmuch as for a single year the effect of the +m may be neglected. 
