fiir Meteorologie und Erdmagnetismus (Seehohe 99*7 Toisen) 

 August 1868. 



2or 



Bewolkung 



18^ 



10^ 





Elektricitat 



18'' 



6*^ 



Tagesmittel cler raagiietischen 

 Viiriatioiisbeobaciuungen 



Decli- 

 nation 



Horizontal- 

 Iiitensitat 



Tag 



Nacht 



8 



3 



10 







9 



1 

 4 

 1 

 2 

 





 

 

 1 









 

 9 

 10 

 9 



10 

 10 

 10 

 10 

 3 



10 

 



1 

 8 

 9 



4.7 



9 

 7 

 6 

 9 



8 

 3 

 10 

 3 

 





 1 

 

 6 

 1 





 

 10 

 5 

 4 



5 

 9 

 10 

 3 

 



9 

 2 

 4 

 6 

 3 

 3 



4.6 





 10 

 

 2 

 



8 

 

 2 





 





 

 

 

 







1 



9 



3 



10 



10 

 



1 



2 

 



9 



7 



10 



10 



3.3 



5.3 

 7.3 

 5.3 



2.7 

 6.0 



5.7 

 2.3 

 4.3 

 1.7 



0.0 



0.0 

 0.3 

 0.0 

 2.3 

 0.3 



0.0 

 0.3 

 9.3 



6.0 



7.7 



8.3 

 6.3 

 7.0 

 4.7 

 3.3 



7.0 

 0.7 

 4.7 

 7.0 

 7.3 

 7.3 



4.2 



0.0 

 +2^.6 



0.0 

 +31 3 

 +24.7 



-j-21.8 



-[-29.4 



-f-23 



0.0 



0.0 



+20 9 



4-23.8 

 -i-47.7 

 + 22.2 

 +22.9 



0.0 

 0.0 

 0.0 

 0.0 

 +20.0 



0.0 

 0.0 



-1-10.8 

 + 18.0 

 -[-12 2 



+ 16.6 

 +21.6 



0.0 

 +10.1 



0.0 



+ 12.0 



+ 16 6 

 +18.0 

 -[-23.4 

 -(- 0.0 



+ 14.3 



+ 30.6 



0.0 

 0.0 

 4-23.6 

 U.O 

 0.0 



+ 17.3 



4-20.0 



-1-72.0 



0.0 



0.0 



4-15.8 



+ 15.8 



+ 13.7 



0.0 





 



4-50 

 +24 

 4-39 







+42, 



4-42, 



4-24 











4-17.3 



4-15.8 

 4-:8.4 

 0.0|+ 5.0 

 0.0 4-22.0 

 0.0+14.4 



+ 12 

 4-21.6 

 0.0 

 + 21.2 

 + 9.4 



0.0 

 -f-18.0 

 0.0 

 0.0 

 

 4-13.7 



+ 97 



61+61.2 



+ 12.2 

 + 10.4 



+18.4 

 + 18.0 

 0.0 

 + 10.1 

 + 14.4 

 + 11.5 



4-14.3 



6 



7 

 8 



6 

 10 

 2 

 6 

 1 



7 

 2 



2 



7 

 6 



5.8 



n und n sind Skalentheile der Variationsapparate fiir Declination und 

 horizontale Intensitat. 



t ist die Temperatur am Bifilarapparate in Graden Reaumur. 

 Zur Verwandlung der Skalentheile in absolutes Maft dienen folgende Formein: 

 Declination i> = 1 1 '' 17'* 25 -f- 0'- 763 (n— 100) 

 Horiz. Intensitat fi'= 2-03648 + 0*00039920 (500— w') + 0'00074 5 ^ 



