13 14 13 22 14 14 14 15 6 67 00 Direct. Retrograde. ེ་ བ་ ེ་ ི ་ ེ་ ི་ ེ་ ི ་ ི ་ ི་་ྷ་ ེ་ ེ་ ེ་ ི་རྟ; 16 8 16 22 23 10 24 20 25 14,, 25 18 >> 25 22 26 4 " 27 20 28 18 28 20 124 67 112 90 22 79 17 16 8 559 67 67 4 124 67 29 22 5 12 5 18 7 20 4 22 5 о 5 2 2 5 8 191 5 14 112 མི་ ༢་ ༢ ་༤ ་ ་ ་ ེ་ ་ བ་ ༢ ་ ེ་ ི ་ རྟ་ རྟ་ བ ་ ེ་ ༢ ་ ི་ ༢་ ༢་༢ 45 56 39 24 8 » 25 6 " 25 622 7268 2 135 25 8 8 112 18 4 90 19 28 22 29 14, 29 16 124 30 O "9 30 6 24 6 26 о 26 18 ,, 27 27 20 II 14 " 12 22 17 16 17 22 18 18 20 18 21 18 22 12 22 16 22 22 23 14 23 22 10 12 རྟ ་ ་ པ ་ བ ་ ༢ ་ བ ་ ེ་ ྷ་ ི ་ ི ་ བ ་ ི ་ བ ་ ི ་ བ ་ བ ་ བ ོ ་ ི ་ ༢ 67 II 14 23 22 ,, 24 O 157 79 25 18 26 2 26 2 27 8 67 2 14 3 14 56 67 3 14, 67 The following is an abstract of the results, the negative sign denoting retrograde motion : And, for the year, there is an excess of direct motion amounting to 189°. It will be observed that the near approach to equality of direct and retrograde motion is due mainly to the very large amount of retrograde motion in November. The same fact of large retrograde motion in this month is observable in the Observations of 1860, but it does not apply to the years 1858 and 1859. |