If a compass needle is weighted so as to swing horizontally it takes up a definite direction at each place, usually not agreeing with the geographical or true north. The deviation from true north is called the declination, D, if eastward is reckoned as positive, if westward as negative. The end of the needle which, over most of the earth points nearly northward, is called the north-seeking or positive end; the compass direction from the centre to this end is called the Eggggtic north, and the vertical plane through this direction is called the local magnetic meridian plane
International audienceRegular magnetic daily quiet time (Sq) variations in total intensity of about ...
We use data from several geomagnetic observatories to derive a series of Fourier harmonic models of ...
Intermagnetic data was used to obtained hourly values of solar quiet variation of horizontal compone...
The daily amplitude of the solar quiet (Sq) magnetic variation of the horizontal intensity, H, of ob...
The daily amplitude of the solar quiet (Sq) magnetic variation of the horizontal intensity, H, of ob...
Seasonal features that are not related in a simple way to solar declination occur in the daily varia...
Equinoctial asymmetry of the range of the solar quiet day variation (Sq) of the horizontal geomagnet...
Solar geomagnetic variations on quiet days (Sq), neglecting the small lunar contribution (L), are co...
today) of the horizontal component of the Earths magnetic field varies systematically during the day...
Summary. It is well known that the time of occurrence of the minimum in the horizontal component of ...
The latitudinal distributions of delta H, delta X, delta Y, and delta Z were studied for quiet and d...
Solar geomagnetic variations on quiet days (Sq), neglecting the small lunar contribution (L), are co...
The daily variation of the horizontal intensity of the earth's magnetic field at Honolulu exhibits s...
An empirical model of the quiet daily geomagnetic field variation has been constructed based on geom...
The relation of F2 layer noon critical frequency with magnetic dip and geomagnetic latitude is studi...
International audienceRegular magnetic daily quiet time (Sq) variations in total intensity of about ...
We use data from several geomagnetic observatories to derive a series of Fourier harmonic models of ...
Intermagnetic data was used to obtained hourly values of solar quiet variation of horizontal compone...
The daily amplitude of the solar quiet (Sq) magnetic variation of the horizontal intensity, H, of ob...
The daily amplitude of the solar quiet (Sq) magnetic variation of the horizontal intensity, H, of ob...
Seasonal features that are not related in a simple way to solar declination occur in the daily varia...
Equinoctial asymmetry of the range of the solar quiet day variation (Sq) of the horizontal geomagnet...
Solar geomagnetic variations on quiet days (Sq), neglecting the small lunar contribution (L), are co...
today) of the horizontal component of the Earths magnetic field varies systematically during the day...
Summary. It is well known that the time of occurrence of the minimum in the horizontal component of ...
The latitudinal distributions of delta H, delta X, delta Y, and delta Z were studied for quiet and d...
Solar geomagnetic variations on quiet days (Sq), neglecting the small lunar contribution (L), are co...
The daily variation of the horizontal intensity of the earth's magnetic field at Honolulu exhibits s...
An empirical model of the quiet daily geomagnetic field variation has been constructed based on geom...
The relation of F2 layer noon critical frequency with magnetic dip and geomagnetic latitude is studi...
International audienceRegular magnetic daily quiet time (Sq) variations in total intensity of about ...
We use data from several geomagnetic observatories to derive a series of Fourier harmonic models of ...
Intermagnetic data was used to obtained hourly values of solar quiet variation of horizontal compone...