Dr. Grossmann: Ueber die Anwendung der Bessel’schen Formel in der Meteorologie etc.
9
A
1.29
1.15
0.94
0.81
0.67
0.56
B
3.96
3.36
2.56
1.77
1.07
0.68
c
4.54
4.76
4.84
4.73
4.42
3.90
D
1.53
1.80
2.11
2.43
2.82
3.30
M= A+C
5.83
5.91
5.78
5.54
5.09
4.46
N = B+B
5.49
5.16
4.67
4.20
3.89
3.98
S = M+N
5.49
10.99
10.58
9.98
9.43
9.07
4.46
(8)
D = M-N
—5.49
0.67
1.24
1.58
1.65
1.11
4.46
M 1 = A—C
—3.25
—3.61
—3.90
—3.92
—3.75
—3.34
w 1 — B—B
—2.43
—1.56
—0.45
0.66
1.75
2.62
S l = A/1+W 1
—2.43
—4.81
—4.06
—3.24
—2.17
—1.13
—3.34
TU = M l -N l
+ 2.43
—1.69
—3.16
—4.56
—5.67
—6.37
—3.34
—2.43
—4.6461
—3.5161
—2.2910
— 1.0850
—0.2925
0
Oi)
0
—0.4374
— 1.5800
—3.2244
—4.9104
—6.1530
—3.3400
(aO
5.49
0
9.5177
0.3350
5.2900
1.0739
0
1.5800
—4.7150
1.4290
—7.8549
0.5550
4 4600
(Pi)
fe)
(B) .
0
ß)
—2.4300
—3.4012
0
2.2910
2.1700
0.7990
0
(Pi)
0
—1.1950
—3.1600
3.2244
0
4.5043
3.3400
(ffs)
5.4900
5.4950
—5.2900
—9.9800
—4.7150
4.5350
4.4600
(Pi)
0
0.5802
1.0739
0
—1.4290
—0.9613
0
(Qi) .
Ans diesen (72) berechnen sich in angegebener Weise die p®* und man erhält durch wenig Rechnung:
Pi = p’f 41
=
—1.1884
Qi = Qi U)
—1.6371
y/ 2)
=
—1.1718
Q'r
—
— 1.6384
pT
—
—1.1802
qT
=
—1.6411
pT
—1.1717
qf
=
—1.6368
Pi'
—
—1.2150
Ql'
=
—1.6700
pf
=
—0.9133
Qi'
—
—2.1131
p (2)
=
—1.2150
Q?
—
0
P2 = pT :)
=
0.2723
q-2 = qT'
=
0.4144
Pi 2)
=
0.2675
qß'
—
0.4172
pf
—
0.2575
qf
=
0.3950
pf
=
0.2583
qT
=
0.4763
pf
=
0.2575
qf
—
0
Ps = P'i 4)
—
—0.0476
Q 3 == q { i 4)
—
0.0221
p ( r
=
—0.0433
Q i r
=
0.0300
pf
—
—0.0348
qf
—
0.0289
pf
=
—0.0433
Q?
=
0
sowie
p 1 ^ = 2.5000
¿tf 2 ’ = 2.4967
jf 0 81 = 2.4912
pf = 2.4867
pf = 2.4875
pf = 2.4433
jo ( 0 2) = 2.7450
pf — 1.5300
Pi = pT 1 =
—0.0004
Qi = =
—0.0614
Mittelst der Formel 10) be
Pi 2) =
—0.0092
q'ß' =
—0.0592
rechnet man sofort die Koeffizienten
pT =
Archiv 1S94. 5.
—0.0038
►Q
II
0
mit 4 übersteigendem Index:
2
9
