Diurnal Variation of the Earth's Magnetic Field at Sea

Nature ◽  
1962 ◽  
Vol 195 (4839) ◽  
pp. 365-366 ◽  
Author(s):  
M. N. HILL ◽  
C. S. MASON
Keyword(s):  
Magnetic Field ◽  
Diurnal Variation ◽  
Earth’S Magnetic Field ◽  
Earth's Magnetic Field

scholarly journals II. The lunar diurnal magnetic variation at Greenwich and other observatories

1926 ◽  
Vol 225 (626-635) ◽  
pp. 49-91 ◽  
Keyword(s):  
Magnetic Field ◽  
Electrical Conductivity ◽  
Diurnal Variation ◽  
Solid Earth ◽  
Upper Atmosphere ◽  
Earth’S Magnetic Field ◽  
Terrestrial Magnetism ◽  
Magnetic Variation ◽  
Earth's Magnetic Field ◽  
The Subject

§ 1. The present research forms part of a wider investigation of terrestrial magnetism, the main object of which is the study of certain electrical phenomena that are associated with solar emissions absorbed in the upper atmosphere, and with the systematic motions of the upper atmosphere. The subject also bears on the electrical conductivity of the solid earth and oceans. The results are briefly discussed from this standpoint in Part IV. The immediate subject of the paper is the lunar diurnal variation of the earth’s magnetic field, and particularly that of the declination at Greenwich, although the results of extensive reductions for other elements, at Batavia, Zikawei, and Pavlovsk, are also included.

scholarly journals On certain average characteristics of world wide magnetic disturbance

1927 ◽  
Vol 115 (771) ◽  
pp. 242-267 ◽  
Keyword(s):  
Magnetic Field ◽  
Diurnal Variation ◽  
Local Time ◽  
World Wide ◽  
Magnetic Storms ◽  
The Other ◽  
Magnetic Disturbance ◽  
Earth’S Magnetic Field ◽  
Earth's Magnetic Field ◽  
Three Components

1. This paper forms a sequel to one entitled “An Outline of a Theory of Magnetic Storms,” published several years ago. In that paper I determined the average additional variations in the three components of the earth's magnetic field (for observatories in magnetic latitudes up to about 60°N.) which during times of considerable magnetic disturbance—commonly called magnetic storms —are superposed on the normal variations. The storms dealt with were such as had a commencement sufficiently definite for its epoch to be estimated to within an hour. The average additional variations of the field were shown to be separable into two parts, one depending on “storm-time” (that is, time reckoned from the commencement of the storm), and the other being a “diurnal” variation depending on local time. Besides these average variations there are, of course, less regular features peculiar to each individual storm.

The Atlas of the Earth's Magnetic Field

2012 ◽  
Author(s):  
A. Soloviev ◽  
A. Khokhlov ◽  
E. Jalkovsky ◽  
A. Berezko ◽  
A. Lebedev ◽  
...  
Keyword(s):  
Magnetic Field ◽  
Earth’S Magnetic Field ◽  
Earth's Magnetic Field
Sign in / Sign up

Export Citation Format

Share Document