699 
| ‘ | | : | 
| Time- . | | Period. | ; 
Year Date | | ae Longitude | Synod. arc | a aes 
| | fo) d 
46 é 34 285's/ | 
236 VIIL22 | | 9505’ HH | 13 22 
ee. eee | 33 143/ 
ISP hie ae BS | 13°58 apes, I 8 
had A2 KON: 
238 | X 20 | REED 1 20 
| 42). Cl | 30 0 
239 ee ik 1e HAS ty, Mea cae 19 2 
00 | 30 0 
240* XIII14 | (3u Set a Be Net 
Ps: | 30 305/ 
Dames es AAG. \ | 13 355, "| 13 26 
| BT? hs | 33 45 
243° "| IH, 33 AT 20 FP) 26 13 
| AT “il eee Ca | 
244%) IE 30 | eee = 8 „ls (80 
adt 1; 3620 | | 
245 | Vi018 | 2822 HE 20 18 
| [FOSS val 1360 | | 
246+ | Vib 6 | cecaneear Ee AMS dl | Ze 6 
| (oe ), 36 0 | | 
BAT y MLAB | MO’ 224 7. Or a iy cia 24 a 
| 45 Pa BA Om on | 
Brul IX, TO 14 3175.) Lt) A ue arto 
The time-intervals, derived in the same way using 304 for each 
month, show the same character as the synodie ares: the 48¢ and 
424 occur repeatedly several times in succession, just as the synodic 
ares are 36° and 30°. The number of intermediate values is in these 
tables greater than in those of the first kind. Here also it is natural 
to assume that the intermediate values of the time-interval are cal- 
culated in the same way as those of the synodic arc, but the devia- 
tions between the first and 12¢ + the last are here even more 
numerous and larger than in the tables of the first kind. Even in 
the constant extreme values deviations occur; now and then 43 
(once 41) and 49 stand in place of 42 and 48. 
In order to be able to see, if at least on the average the values 
for the time-interval increase in the same way as the synodic ares, 
they were combined into groups of full degrees and the mean was 
taken. This showed that 
with 30°22’ corresponded a mean of 42.47 ( 6 values) 
pee: iy 5 he Ba dv eae 
„ 3222 4 Ms De Ea Caen 
A id ¥ 45.2 (4 And’ 
„ 3345 ri 856 NE UD 
„… 34 32 us * CBG PEW a 
5, 95 23 ie 5 ot Se es OE) 
