Page:Scientific Memoirs, Vol. 2 (1841).djvu/68

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56
GAUSS AND WEBER ON TERRESTRIAL MAGNETISM.

Mean value of the Westerly Magnetic Declination at Göttingen.

8, a.m. 1, p.m.
1834. March, second half 18 38 16·0 18 46 40·4
April 36 6·9 47 3·8
May 36 28·2 47 15·4
June 37 40·7 47 59·5
July 37 57·5 48 19·0
August 38 48·1 49 11·0
September 36 58·4 46 32·3
October 37 18·4 44 47·2
November 37 38·4 43 4·3
December 37 54·8 41 32·7
1835. January 37 51·5 42 14·4
February 37 3·5 42 29·4
March 34 47·5 44 55·2
April 32 57·7 46 31·6
May 32 13·4 45 17·1
June 32 56·4 44 41·3
July 34 8·0 44 42·8
August 34 12·4 46 56·8
September 33 21·2 44 27·6
October 33 23·0 43 5·3
November 36 15·3 43 49·5
December 35 25·9 40 19·1
1836. January 35 2·4 40 34·6
February 33 26·7 41 15·2
March 31 1·4 43 16·4
April 26 32·9 43 42·6
May 28 0·8 44 37·2
June 27 35·1 42 52·4
July 26 54·2 42 26·0
August 25 42·4 41 45·0
September 26 14·6 40 59·6
October 27 34·0 40 32·8
November 29 21·0 36 54·3
December 29 13·7 35 46·8
1837. January 27 35·3 37 46·2
February 27 35·6 36 28·3
March 24 44·2 39 4·2

Some combinations of these observations may now be noticed.

The difference between the declination of the morning and afternoon has one sign all through in the monthly means; the dependence of its magnitude on the season of the year will be perceived in the following tabular view: