| 
fiir Meteorologie und Erdmagnetismus (Seehohe 99°7 Toisen) 
Juni 1867. 
| Tag 
167 
Ozon 
Nacht 
Bewolkung 
18; 25 | 105 
| 
9 8 1 
0 1 8) 
O 1 1 
1 Tf 2 
10 8 1 
1 1 0) 
1 6 6 
3 || AO 
6 2 0 
2 3 | 10 
10 8 1 
1 0 2 
1 3 | 10 
LO ko) |) 0 
B) |) NO |) 10) 
10 a 2 
ie | 8 | 4/ 
8 a 3 
a 8 1 
I 1 1 
1 1 1 
if 9 10 
10 3 1 
0 3 6 
2 8 4 
3 4 9 
2 8 7 
1 Bl ©) 
3 8 1 
10 a 0) 
4.3|5.0]4.5 
Blekivertit || Te eeucashedbactescen 
2 = 1g Qh 10" | Decli- Horizontal- aé 
é = nation Intensitit as 
| | mn = 1 ne nS] 
6.0 | 0.0,+27.4 0.0) 113.97 |+19.0 | 463.68) — 
0.3 | 0.0\/+11.2 0.0)| 113.70 |-+19.5 | 463.15} — 
0.7 ||-+14.8 +20.2 0.0|| 114.18 | +20.6 | 477.23) — 
G0) 0.0|—85.0 0.0|| 116.25 |+20.8 | 478.15) — 
6.3 0.0 0.0 0.0) 115.07 |-+19.3 472.50) — 
0.7 || +42.1 0.0 0.0) 116.02 |+19.0 | 473.32} — 
4.3 /+19.7|—31.7|/+20.4] 117.55 |+19.7 | 468.37) — 
6.7|-+17.6|-+ 5.8] 0.0] 116.60 |4+19.1 | 473.97] — 
6.0 17.3 + 9.4 0.0) 116.85 |+18.4 | 476.03} — 
5.0 0.0 0.0 0.0]| 118.25 +17.6 474.53] — 
6.3 ||+11.5)+27.2 0.0) 117 O7 |-+17.4 | 471.35) — 
1.0 423.8] 0.0/+18 9] 118.95 |--17.5 | 476.78] — 
ALT +11.2 0.0) —40.0|| 117.27 |+-18.1 | 478.13} — 
10.0 0.0 0.0 0.0) 116.95 |+17.9 | 462.90} — 
8.3 0.0 0.0 0.0) 116.03 |}+16.6 | 455.90) — 
6.3 0-0)7-54-1 +22.5 115.95 |+15.1 | 451.45; — 
7.3|+36.7! 0.0l  0.0l 117.30 [414.4 | 452.10| — 
6.0 |-+20.5 +47 .5|-+21.5|/ 116.55 +13.5 446.80] — 
ire 4-20 .5 0.0 +19.8 115.97 |+13.9 | 448.93) — 
1.0 |-+-44.3)+22.7|/+ 0.0 116.27 |-414.5 | 465.93; — 
TON geese eee Nata eats eh Ge 
a ee pe) ee see ere: 7) | 4e0.Onle 
4.7 — = — 115.65 |-+17.7 | 481.60} — 
SONU aa i eee hte igre, | ae4e ole 
4.7 — = a 114.53 |}+19.1 | 486.65) — 
Bea Se al) ell Meee 19) 5) ao0sma hes 
Be | ee Se ee 50/9. 72 49307 
4.3) — — — 115.03 |+19.3 | 499.55] — 
4.0 = — — 117.03 |+17.9 | 498.23] — 
| ee hh 2 nage ber eiy P4903. 42 
4.7] — _ — || 116.10) 17.00 || 473.86 | — 
— 
Ono Os 
—_ 
— 
— 
TIAIOOS OCOONDM COMOONW 
— 
WOOoMmHow wOMmMm-0r 
-T 
—_ 
=] 
fon) 
Die Beobachtungen der Elektricitit vom 21. angefangen fielen aus, weil 
eine Reparatur des Elektrometers nothwendig geworden war. 
n, n,n’ sind Skalentheile der Variationsapparate fiir Declination, hori- 
zoutale Intensitét und Inclination. 
¢t ist die Temperatur am Bifilarapparate in Graden Réaumur. 
Zur Verwandlung der Skalentheile in absolutes Mafs dienen folgende Formeln: 
Declination D =11°33 81 + 0° 763 (n—120) 
Horiz. Intensitiit H = 2-02258 + 0-00009920 (600—n’) 
+ 0:°000514¢ + 0°00128 T 
wo T die seit 1. Jiénner 1867 verflossene Zeit, in Theilen des Jahres ausgedriickt, 
bedeutet. 
