far Meteorologie und Erdmagnetismus (Seehohe 99-7 Toisen) 

 Mdrz 1870. 



91 



Bewolkuno; 



18^ 



IC- 



Elektricitiit 



Tagesmittel der magnetUchea 

 Yariationsbeobachtungen 



22' 



Decli- 

 nation 



Horizontal- 

 Intensitat 



Ozon 



Tag 



10 



1 



10 



1 



10 



10 

 10 

 2 

 10 

 10 



10 



7 

 10 



1 



3 







1 



10 



2 

 1 



I 

 10 

 10 

 10 

 10 



6 

 5 

 8 

 6 

 9 

 10 



6.6 



8 

 I 



8 



9 



10 



10 



10 



2 



9 



10 



10 

 4 



1 

 3 

 10 

 1 

 3 



2 

 10 

 10 

 10 

 10 



5 

 2 

 9 

 9 



10 

 10 



6.7 





 

 

 

 10 



10 

 10 

 10 

 10 

 9 



7 

 1 

 

 2 

 





 10 



8 

 



1 



10 

 10 

 10 

 10 



10 





 10 



9 

 10 

 10 

 10 



6.0 



6.0 

 0.7 

 6.0 

 3. 3 

 10.0 



10.0 



10.0 



4.7 



9.7 



9.7 



9.0 

 4.0 

 4.3 

 3.3 

 2.0 



0.3 

 4.7 

 9.3 

 1.0 

 1.7 



4.3 

 10.0 

 10.0 

 10.0 

 10.0 



3.7 

 5.7 

 8.7 

 8.3 

 9.7 

 10.0 



6.4 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 

 + 13.7 

 0.0 

 0.0 

 0.0 



0.0 

 0.0 



0.0 

 + 11.5 



+ 23.8 

 + 37.4 

 0.0 

 + 32.4 

 + 19.4 



+ 25.9 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 



0.0 



+ 14.4 



+ 23.8 

 0.0 

 0.0 



+ 6.74 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 

 0.0 



+ 12.2 

 + 16.6 



+ 31.7 

 + 25.2 

 0.0 

 + 26.6 

 + 16.2 



+ 21.6 

 0.0 

 0.0 

 0.0 

 0.0 



0.0 



0.0 



0.0 



+ 14.4 



0.0 



0.0 



+ 5.48 



76.13 

 76.68 

 78.68 

 79.53 

 80.40 



81.68 

 80.63 

 83.08 

 83.55 

 86.55 



85.48 

 85.27 

 87.37 

 84.05 

 89.05 



88.70 

 89.52 

 86.73 

 86.97 



86.52 



89.13 

 91.48 

 84.38 

 88.03 

 83.42 



83.70 

 84.32 

 87.07 

 86.57 

 85.93 

 83.23 



84.675 



3 

 3 



4 



7 

 5 

 5 

 1 



2 



3 

 3 

 4 

 4 

 2 



2 



4 

 3 

 2 



8 



2 

 3 

 2 

 2 

 3 

 2 



3.0 



n und n' sind Scalentheile der Variationsapparate fiir Declination und 

 horizontale Intensitat. 



t ist die Temperatur am Bifilarapparate in Graden Reaumur, T die Zeit 

 in Theilen des Jahres Yom 1. Jan. an gezahlt. 

 Zur Verwandlung der Scalentheile in absolutes Mass dienen folgendeFormeln: 



Declination D = 11° 19'. 59 + 0.763 (w- 100) 

 Horiz. Intensitat 7= 2.036-2 7 + 0.0000992 (400— F) + 0.00072 i!+ 0.0001 T. 



