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pro vyhledávání: '"H. W. Fisk"'
26. The effects are especially noticeable at stations where the normal diurnal variation of the Earth's magnetism at the time was large—for example, near the morning or afternoon elongations of the declination-needle. Kakioka, Japan, was somewhat f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0dd600ba658c7cda536d9cdca546875
https://zenodo.org/record/1560476
https://zenodo.org/record/1560476
Autor:
H. W. Fisk
Magneticians generally will welcome the appearance of this publication, both because of its excellent presentation of the essentials of field and office practice and because of its general suggestiveness. Its aim is “to present the subject matter i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f9153ee3cdf96fcdca24c957295894ab
https://zenodo.org/record/1827876
https://zenodo.org/record/1827876
GENERAL PLAN FOR MAGNETIC AND ALLIED OBSERVATIONS DURING THE TOTAL SOLAR ECLIPSE OF JANUARY 24, 1925
Publikováno v:
Science (New York, N.Y.). 60(1563)
Autor:
H. W. Fisk
Publikováno v:
Science. 58:123-124
General Plan for Magnetic and Allied Observations During the Total Solar Eclipse of January 24, 1925
Autor:
J. P. Ault, H. W. Fisk
Publikováno v:
Science. 60:547-548
Autor:
H. W. Fisk, C. R. Duvall
Publikováno v:
Journal of Geophysical Research. 30:1
For the computation of the horizontal component of the Earth's magnetic field from the observed angle of deflection of one magnet by a second in Lamont's first position a factor, intrinsically a function of the dimensions of the magnets employed, is
Autor:
H. W. Fisk
Publikováno v:
Journal of Geophysical Research. 14:183
By a fortunate chance I went on the morning of September 25 to one of the small non-magnetic houses used for testing instruments, belonging to the Department of Terrestrial Magnetism. My purpose was to test the magnetization of some compass needles,
Autor:
J. A. Fleming, H. W. Fisk
Publikováno v:
Journal of Geophysical Research. 33:37
It is well recognized that the accumulation of additional reliable data in terrestrial magnetism and electricity in the polar regions is of first importance to the definite solution of unsolved problems both from the statistical and laboratory method