16T 



fill' Meteorologie mid Erdmagnetismus (Seehohe 99-7 Toisen) 



Juli 1869. 



Bewblkung 



18" 



10" 



e2 a 



10 

 10 

 10 

 9 

 10 



2 

 9 

 7 

 9 

 5 



8 

 1 

 

 5 



7 



9 



10 

 2 





 9 



7 

 

 1 

 

 1 



4 

 9 

 1 

 

 2 

 1 



5.1 



9 

 6 

 9 

 9 

 2 



6 

 6 

 1 

 5 

 2 



9 



1 





 10 

 10 



4 



10 



3 



4 



4 



7 

 1 

 6 

 1 

 1 



3 



8 

 1 

 9 

 1 

 9 



4.8 



9 



10 

 10 



9 



9 



1 



8 

 



7 

 10 



3 







1 



10 



8 



10 

 1 







7 

 



10 



1 



4 

 

 



7 

 

 

 

 



1 



4.4 



9.3 

 8.7 

 9.7 

 9.0 

 7.0 



3.0 

 7.7 

 2.7 

 7.9 

 5.7 



6.7 

 0.7 



9.3 

 8.3 

 8.3 



7.7 

 7.0 

 1.7 

 3.7 



4.3 



8.0 

 0.7 

 3.7 

 0.3 

 0.7 



4.7 

 5.7 

 0.7 

 0.0 

 1.0 

 3.7 



4.8 



Elektricitat 



18" 



2h 



Tagesmittel der magnetischen 

 Variationsbeobaehtungen 



Decli- 

 nation 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



+ 



0.0 



0.0 

 0.0 

 0.0 

 4.7 



0.0 +15.8 

 O.O! 0.0 



0.0 

 

 0.0 



0.0 

 0.0 

 0.0 



0.0 0.0 

 +24.8 +10.1 

 +26.9i+ 9.0 

 + 18.4 0.0 



0.0 0.0 



15.0 

 0.0 

 0.0 

 0.0 



0.0 



0.0 



0.0 

 + 10.4 

 + 0.0 



+14.6 0, 



28.4 + 6. 

 0.0+19 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 





 0.0 

 0.0 

 0.0 

 0.0 



0.0 

 + 10.3 

 0.0 

 0.0 

 0.0 



0.0 



0.0 



+ 5.4 



0.0 



+22 

 +47. 



24.1 



0.0 



+38.9 



+34.2 



+ 0.0 



50.4 



+ 11.0 



+ 12.2 +15.8 



0.0 



1 0.0 

 2+12.6 



+19.8 +15.5 

 0.0 00 



0.0 0.0 

 + y.4+ 7.2 

 +24.8 19.8 

 + 9.4 +11.9 

 + 15.1 +15.5 

 +24.5 +19.4 



+ 6.3 + 4.3 



94.08 

 93.75 

 95.05 

 96. 37 

 95.25 



93.75 

 94.00 

 95.42 

 94.43 

 95.35 



94.43 

 97.12 



99.42 

 99.27 

 97.80 



98.03 

 96.92 

 96 35 

 98.83 

 98.60 



97.85 

 100.05 

 101.58 

 100.18 

 100.13 



101.33 

 99.62 

 99.27 

 100.25 

 100.40 

 100.45 



97.59 



Horizontal- 

 Intensitat 



Ozon 



Tag 



n' = 

 444.07 

 436 . 70 

 433.52 

 434.90 

 406.37 



405.18 

 404.23 

 406.22 

 410.55 

 416.77 



423.65 

 436.28 

 436.27 

 430 58 

 423.05 



420.62 

 410.85 

 416.45 

 424.20 

 436.92 



433.62 

 436.13 

 442.13 

 451.80 

 446. 48 



453.75 

 452.25 

 451.80 

 461.37 

 464.62 

 465.77 



432.82 



t = 

 17.] 

 17.7 



17.8 

 18.0 

 18.9 



19.1 



19.7 

 20.1 

 20.6 

 21 3 



21.7 

 21.1 

 20.5 

 20.1 

 18.7 



17.7 

 17.3 

 17.1 

 17.3 

 18.2 



19.2 

 19.5 

 19 8 

 20.4 

 21.1 



21.4 

 21.5 

 21.9 



22.8 

 23.6 

 23.8 



19.82 



7 

 2 

 8 

 8 

 5 



6 

 1 

 3 

 5 



7 



4 

 5 

 4 

 5 

 3 



4 

 2 

 7 

 4 

 6 



6 

 4 

 4 

 5 

 6 



6 

 7 

 6 

 6 

 6 

 7 



5.1 



Nachl 



5 

 5 



8 

 4 

 8 



7 

 6 

 2 

 6 

 4 



8 

 6 

 2 

 4 



8 



9 

 7 

 8 

 6 

 5 



3 

 5 

 3 

 4 

 3 



3 



8 

 2 

 3 

 8 

 3 



5.2 



n und n' sind Skalentheile der Variationsapparate fur Declination und 

 horizontale Intensitat. 



t ist die Temperatur am Bifilarapparate in Graden R(5aumur. 

 T die Zeit in Theilen des Jahres vom 1. Januer an gezahlt. 

 i6ur Verwaudliing der Skalentheile in absolutes MaB dienen folgende Forineln: 

 Declination: i) = Jl" 15M4 + 0.763 (n-lOO), 

 Horiz.-inteusitat: H = 202886 + (40U n') U. 000099 + 0.00107 I + 



+ 0-00402 T. 



