fiir Meteorologie und Erdmagnetismus (Seehdhe 99°7 Toisen) 
113 
April 1867. 
Bewélkung Elektricitit Ge ee a Ozon me | 
| | 
~ i = es & h sth n || Decli- Horizontal- ae 
185} 25 | 10 23 18 2 10 mee Tatan atta 23 rae Nacht 
| nS n= ee ne 
4 {| 10 Sil Wad) 0.0 0.0 0.0) 113.58 |+ 8.1 | 295.78] — 6 9 
7 1 | 10 } 6.3 //+21.9|/+ 4.5)+13.9] 113.35 |-+ 7.6 | 297.08} — 6 9 
10 On| EoZ0 0.0 0.0 0.0) 115.10 |+ 7.7 | 286.70} — 8 | 10 
8 ol LO Sas 0.0 0.0 0.0] 112.45 |+ 8.0 | 281.77) — 6 | 10 
10 a OMe seid 0.0\-+ 5.8 0.0}| 109.80 + 8.3 | 291.15] — 8 | 10 
4/10] 10] 8.0|/+18.4 0.0 0.0] 113.08 |+ 7.6 | 293.50} — 6 0 
10 | 10 lL Bare 0.0 0.9 0.0|| 111.25 |+ 7.6 | 288.47] — 8) 10 
10 i recs 0.0 0.0 0.0)| 108.68 - 8.2 | 280:67| — 6 | 10 
9 6 le Dies 0.0 0.0 0.0) 112.23 |+ 8.6 | 298.25) — 9 9 
Z al NON || ato 0.0 0.0 0.0) 112.47 + 8.0 | 294.44) — 9 9 
6 9} 10) 8.3} 0.0/+20.8 0.0) 110 10 }+ 8.1 | 290.32] — 6 | 10 H 
J 8 Th) B3633 0.0 0.0)/+ 5.3) 113.13 |-++ 7.8 | 299.55}| — a 9 
0 1 1 | 0.7 ||4+30.2 0.0 0.0} 114.43 |}+ 8.0 | 302.30} — 4 8 
10 5 CON hos: 0.0/-++10.8 0.0} 113.87 |+ 8.8 | 299.17} — 6 6 
10 |} 10 3) |W od +18.4 0.0 0.0) 114.18/+ 9.6 | 303.55} — Lf 7 
9 & {1103 9.0 O 0.0 0.0) 113.85 '+- 9.3 | 305.38; — 9 9 
10] 10} 719.0] oo! .0| o.o/113.98|+ 8.7 | 295.82|—|| 6 | 10 
a 1 tht) ie) 0.0|/+24.2|/+ 7.8|| 114.47 a 8.4 | 298.08] — "if 9 
2 5 8 | 5.0 |+24.2)-+22.9 0.0) 113.75 |+ 9.5 | 304.38] — 4 6 
7 3 8 | 6.0 0.0/+ 8.1 0.0] 113.00 +11.3 | 305.02) — 7 2 
10-8. | 10 | 9.3] 0.0/+ 6.1] 0.0] 113.70/+12.2 | 318.02/—]} 8 | 2 
10 5 9 | 8.0 0.0)-+14.0 0.0] 113.55 |--11.8 | 320.87) — 8 | 10 
94) 7] 9 | 8.3 }+425.6)+ 4.5/+ 9.6] 116.58 }+11.7 | 333.53) — 7 8 
6 8 1 | 5.0)/4+15.5 0.0\+ 7.1] 114.77 +12.9 | 334.92] — 6 7 
6 2 | 10 | 6.0//+42.8 0.0 0.0|| 114.43 |-+14.0 | 346.87] — 5 1 
8 8 | 10 | 8.7/+16.6 0.0 0.0) 114.43 |+14.9 | 357.12] — a 3 
3 2/]10/] 5 O/+16.2 0.0)+ 4.3) 114.65 |+15.5 | 371.08} — fe 9 
4 vf 0 | 3.7 ||+26.3|/-+23.3/+ 7.8) 115.43 |+16.3 | 388.53} — 6 5 
5 9 Owes 0.0 0.0 0.0) 115.97 |+16.3 | 398.03) — 3 4 
10 6 2 620 0.0|-+18.0 + 4.9] 116.23 |+14.9 | 393.77) — 8 9 
6.9/6.5|6.7] 6.7 ]+8.54/+5.43 +-2.02/113.550] 10.32 |315.969| —||6.7 | 7.6 
Die Monatmittel der atmosphirischen Elektricitét sind ohne Riicksicht 
auf das Zeichen gebildet. 
n, n', n” sind Skalentheile der Variationsapparate fiir Declination, hori- 
zontale Tntensitat und Inclination. 
¢ ist die Temperatur am Bifilarapparate in Graden Réaumur. 
Zur Verwandlung der Skalentheile in absolutes Mafs dienen folgende Formeln: 
Declination D = 11°36 90 + 0° 763 (n—120) 
Horiz. Intensitit H =2:°0126 -+ 0°00009920 (600—n’) 
+ 0°000514 ¢ + 0°00128 7 
wo T die seit 1. Jaénner 1867 verflossene Zeit, in Theilen des Jahres ausgedriickt, 
bedeutet. 
