Mortons oF DIFFERENT CURRENTS OF AIR. clil 
24° more northerly than the surface wind; while there were only 58 results shewing a more southerly motion, 
and 19 in which both currents proceeded from the same point. It might be supposed that the regular differ- 
ence of these currents was due to some peculiar configuration of the surface of the country around the Obser- 
vatory, but this is disproved by the results of the comparison of the upper currents with each other ; thus, the 
cirro-stratous current, compared with the scud-current, shews on the average of 255 results that the upper 
current proceeds from a point 14° more northerly than the lower current: a similar result is obtained from a 
comparison of the cirrous current with the scud-current. 
TABLE 97.—Differences of the Directions of Motions of the Lower and Upper Currents of Air, as 
. deduced from the Comparisons of the Direction of the Wind, and the Motions of the Clouds, 
for the Years 1843-6. 
Quadrant N. to E. Quadrant E. to 8. Quadrant 8. to W. Quadrant W. to N. 
Currents. 
mee No. of Dee Mean || No. of en, -| Mean || No. of Ries -| Mean | No. of iar | Mean 
Results,|Di#fs- Of) Result. || Results. |Di#8- Of) Result, || Results. Di Of] Result, || Results.|D! 8. OF! Result. 
Motion. Motion. Motion. Motion. 
Biden 227 +23 76 +24 664 +24 166 +20 
aa 111 | —25| +71]} 20 | —23] 413} 58 | -13 | +20] 57 | -18| + 9 
12 0 9 0 19 0 15 0 
64 +40 46 +31 371 +40 113 +27 
46 -51 +2 11 —25 | +20 43 -19 | +33 38 —35 | +11 
3) 0 1 0 12 0 6 0 
+ 36 41 +21 190 +27 107 + 26 
Cir.-str. minus 
Wind. 
Cir.-str. minus 
Oe Oe SS 
or or 
No 
| 
oo 
Oey 
| 
_ 
_ 
_ 
i 
bo 
lor) 
Ee 
Ne) 
a 
= 
: e381} -a214IP zo 9a" | pay 
Seud- 16 0 15 0 34 0 27 0 
: ; 20 | +58 15 | +60 190 | +45 Bl (ean 
Cirrus minus 165) S59uleeesG 0 Breet oD ieee Gr at eae oGal| aS) ie —alglece 1s 
ieee ont 0 1 0 10 0 P 0 
: . 20 | +35 1g | +54 107 | +36 gi | +27 
Alaa 17. |eoagee || 9 | sa] 49g] 33 | 96.) +90 1 33 | —41.| 44.7 
cue 2 0 1 0 12 0 13 0 
219. It happens frequently that comparisons of the motions of two currents are obtained when the others 
do not exist, or are not evident from the absence of clouds within them or from the masses of clouds in the lower 
current ; it is for this reason that the comparison of motions above, obtained from observations partly simul- 
taneous and partly not, are to a considerable extent independent of each other ; yet it will be seen that they in 
general confirm each other. Thus, the differences of the mean results for the first two comparisons (in Table 
97) should give the difference for the third; so in the quadrant S. to W. we have 33°—20°= + 13°; and the 
_ partly independent comparisons for the cirro-stratous minus the scud-current, give + 14°; and as the differ- 
ences of the first and fourth comparisons should give the fifth (in Table 97), we have 36°—20°= +16°; and 
the partly independent comparisons for the cirrus minus scud, give + 20°. We obtain similar results in the 
quadrants E. to 8. and W. to N., but the differences of the motions are less marked. This appears to be due 
chiefly to the greater proportion of negative results in these two quadrants. The means for the positive results 
- do not differ greatly in any of the quadrants. In the quadrant N. to E. we find all the three cloud-currents 
positive of the surface-current, but only to the extent of 2° in the case of the cirro-stratous current; while the 
cirro-stratous and cirrous currents appear on the whole 1° or 2° negative of the scud-current. These differences 
appear due to causes belonging chiefly to the sudden appearances of the north-east winds, which are chiefly sur- 
face-winds, and are nearly or altogether unconnected with the upper currents. 
220. When we combine the results in the four quadrants for each class of comparisons, we have the fol- 
lowing means :— 
Seud-current minus surface-current, mean of 1434 results, = +14%5 
Cirro-stratous current minus surface-current, mean of 754 results, = +422°:8 
Cirrous current minus surface-current, mean of 349 results, = +29°6 
Cirro-stratous current minus scud-current, mean of 683 results, =-+ 6°9 
Cirrous current minus scud-current, mean of 339 results, = +137 
MAG. AND MET. obs. 1845 anp 1846. Qe 
