139 



fiir Meteorologie und Erdmagnetismus (Seehohe 99*7 Toisen) 



Mai 1866. 



Bewolkung 



iSh 



8 

 10 

 10 

 10 







1 

 1 



9 

 4 



7 



9 



8 

 10 

 .1 



1 



10 

 8 

 9 

 5 

 



10 

 5 

 4 



8 

 6 



10 

 10 



3 

 10 



2 



10 

 6.4 



2h 



10" 





Elektricitat 



18^ 



2h 



10»> 



Tagesmittel dcr magnetischen 

 Variationsbeobachtungen 



Decli- 

 nation 



Horizontal- 

 Intensitat 





Ozon 



Tag 



9 

 3 



6 



1 

 1 

 1 

 1 

 5 



5 

 5 

 7 

 2 

 6 



9 

 6 

 8 

 2 

 2 



10 

 9 

 4 



10 

 5 



10 

 2 



b 



2 

 5 



2 



5.1 



10 

 10 







2 

 10 



2 

 2 

 



7 

 10 



4 

 10 

 1 

 2 

 3 



10 

 3 

 1 

 8 

 5 



9 

 7 

 1 

 9 

 8 



10 

 1 

 2 

 2 



7 



5 

 5.2 



8.0 

 9.3 

 6.3 

 5.0 

 5.3 



1.3 

 1.3 

 3.3 

 4.0 

 7.3 



6.0 

 7.7 

 6.0 

 1.7 

 3.3 



9.7 

 5.7 

 6.0 

 5.0 

 2.3 



9.7 

 7.0 

 3.0 

 9.0 

 6.0 



10.0 

 4.3 

 3.7 

 4.7 



4.7 



5.7 

 5.6 



+46 



0. 



0. 

 +64. 

 +67. 



+49. 

 + 16. 

 +19. 

 +45. 

 +23. 



+23, 

 +42, 

 + 18, 

 + 19 



+23, 



0, 

 +23, 

 +23, 



+29, 

 +27.7 



+ 19.1 

 +24.5 

 +32.8 

 +21.2 

 +31.0 



0.0 

 0.0 

 0.0 

 0.0 

 +26.3 



0.0 



+23.2 



+ 11.5 

 0.0 

 0.0 

 0.0 

 0.0 



+15.8 

 + 10.1 

 + 14.0 

 + 14.8 

 + 10.7 



+13.7 

 0.0 

 0.0 



+22.8 

 0.0 



+11.5 



+ 16.2 



0.0 



0.0 



+39.6 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 



+ 5.8 



+ 12.2 

 0.0 

 +30.7 

 + 12.1 

 + 9.0 



+34.1 



+28.4 

 + 11.0 

 +19.8 

 +20.4 



+20.4 

 + 6.5 

 +11-2 

 +20.4 

 +25.2 



+21.6 

 +23.4 

 +49.0 

 +31.2 

 +29.7 



+17.9 

 +24.5 

 +34.1 

 + 19.7 

 0.0 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



+ 10.7 



+16.9 



122.72 

 121.95 

 124.08 

 120 87 

 121.58 



122.67 

 123.52 

 123.97 

 124 95 

 124.10 



125.33 

 125.23 

 127.45 

 123.60 

 124.62 



124.10 

 125.00 

 125.23 

 125.67 

 125.60 



124.90 

 125.90 

 125.20 

 124.88 

 124.65 



121.92 

 120.27 

 120.43 

 119.20 

 118.59 



121.57 



123.543 



16.78 

 16.58 

 14.48 

 14.35 

 14.70 



14.27 

 13.68 

 14.10 

 14.82 

 15.52 



15.70 

 15.60 

 14.12 

 13.27 

 12.42 



12.13 

 11.27 

 10.88 

 11.05 

 11.18 



454.15 



458.28 

 455.37 

 451.42 

 453.78 



450.10 

 450.70 

 457.97 

 453.57 

 455.77 



463.87 

 462.13 

 461.88 

 459.08 

 457.30 



454.77 

 447.23 

 445.82 

 449.42 

 453.70 



10.42 442.98 



9.62 



9.43 



9.43 



10.67 



10.58 

 11.67 

 13.95 

 14.62 

 15.73 



17.02 



130.16 



438.20 

 441.92 

 443.67 

 446.63 



438.77 

 436.72 

 447.95 

 439.58 



428.48 



433.40 

 449504 



7 

 9 

 6 

 4 



7 



8 

 6 

 4 

 2 



5 

 4 

 9 

 8 

 5 



7 

 6 

 7 

 6 

 8 



8 



7 



5 

 5 



9 

 10 



7 

 8 



7 



6 

 6.5 



Nacht 



7 



4 



10 







8 



10 



7 

 5 

 1 



7 



9 





 10 

 10 

 10 



9 

 10 

 10 



8 

 9 



10 



10 

 10 



7 

 8 



10 

 9 



7 

 3 

 2 



9 



7.4 



n, n, n" sind Skalentheile der Variationsapparate fur Declination, hori- 

 zontale Intensitat und Inclination. 



t ist die Temperatur am Bifilarapparate in Graden Reaumur. 



Zur Verwandlung der Skalentheile in ab.solutes Mali dienen folgende 



Formeln : , ^^, 



Declination D = 1 1 36 * 29 + • 763 (w 120) 

 Horiz Intensitat if = 2-01498 + 0-000:)9920 (600 -w) 

 + 0-00(J651 t + 0-0()4()l T 

 wo T die seit 1. Janner I8(i6 verflossene Zeit, in Theilen des Jahres ausgedruckt, 

 bedeutet. 



