X. Note on the lunar-diurnal variation of magnetic declination
Author(s) -
John Allan Broun
Publication year - 1868
Publication title -
proceedings of the royal society of london
Language(s) - English
Resource type - Journals
eISSN - 2053-9126
pISSN - 0370-1662
DOI - 10.1098/rspl.1867.0013
Subject(s) - declination , magnetic declination , diurnal temperature variation , variation (astronomy) , equator , northern hemisphere , southern hemisphere , geodesy , geology , atmospheric sciences , physics , astronomy , climatology , earth's magnetic field , magnetic field , latitude , quantum mechanics
I received late last night No. 91 of the Proceedings of the Royal Society, and desire to offer the following remarks on the abstract of a paper by Mr. Neumayer which I find therein (vol. xv. p. 414). Mr. Neumayer is evidently unacquainted with the Note by me, read to the Royal Society of London in 1861 (Proc. Roy. Soc. vol. x. p. 475), in which I stated as result of the discussions of five years’ observations at Trevandrum (near the magnetic equator) that the lunar-diurnal variation of magnetic declination became inverted, like the solar-diurnal variation, when the sun passed from one hemisphere to the other, both the solar- and lunar-diurnal variations depending on the position of the sun.
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