Observations m the Height of the Clouds. 41
4 )
-
A
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J
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to
60
js
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1 ■'
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jjj.
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t '
0
0
g
O
O
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0
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0
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O
£
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0
L
0
0
O
O
0
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in
O
O
O
O
O
O
O
0
0
0
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From
£
|
£
s
fe
1
fe
|
fe
1
fe
s
e
u.
s
2
tn
s
L
Z
Jan.
0
9
12
28
53
39
37
32
30
39
36
116
43 -
Feb.
5
10
5
15
4 i
45
45
27
43 ! 38
29
94
, 397
Mar.
2
I
6
11
22
40
32
36
24
32
44
184
1 434
Apr.
O
4
5
18
24
34
37
26
23! 38] 35
206
45 °
May
O
I
4
8
x 3
3 i
22
25
30
34 ! 27
270
' 465
June
0
2
2
a
24
24
29
21
34 ! 4 1
34
233
; 45 °
July
O
2
2
18
35
36
35
25
35 ! 48
38
191; 465
Aug.
O
4
5
l 3
27
39
35
26
25
45
3 °
215,' 464
Sep.
O
I
7
J 3
38
38
32
30
27
5 i
27
l86
45 °
Oct.
2
0
5
-3
26
49
3 1
31
a 6
61
37
164
■ 465
Nov.
O
O
3
13
3°
58
42
38
46
45
47
i 128! 450
Dec.
I
8
6
23
4i
53
39
50
47
46
35
III
1 46 O
Total 10
4262
179
1374
486
1416367
410
^181419^2098,;z8i
It may b& proper to observe, that the supposition ot thedouds rising or falling with the barometer, ar as the densityof the air increases or diminishes, is npt at all countenancedby these observations.—Also, that in very heavy and con-tinued rains, the clouds are mostly below the summit of themountain ; but it frequently rains when they are entirelyabove it.
G
SECTION