magnetic declination


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magnetic declination

[mag′ned·ik ‚dek·lə′nā·shən]
(astronomy)

Declination, Magnetic

 

(D), the angle between the magnetic and the true (geographic) meridians at a given point on the earth’s surface. The direction of the true meridian is usually determined with a gyroscopic theodolite or by astronomical observations. The direction of the magnetic meridian is found with the aid of instruments, such as magnetic declinometers and magnetometers, that make it possible to determine the position of a magnetic needle at the measurement site. If the north end of the magnetic needle is deflected to the east of the direction of the true meridian, the magnetic declination is called east, or positive; if it is deflected to the west, the magnetic declination is called west, or negative.

Magnetic declination is widely used in navigation, in geodetic and mine surveying, and in military work. Lines on a map connecting points with equal values of magnetic declination are called isoclinic lines. Since magnetic declination does not remain constant over long periods of time but undergoes slow changes, maps of magnetic declination are periodically revised based on measurements repeated every five to six years.

IU. A. BURTSEV

magnetic declination

At a particular location, the horizontal angle between true meridian (true north-south line) and magnetic meridian (direction of compass needle).

magnetic declination

magnetic declinationclick for a larger image
The angle between the magnetic and geographical meridians at any place, expressed in degrees east or west to indicate the direction of magnetic north from true north. Also called a magnetic variation.
References in periodicals archive ?
During the past 4 millennia, magnetic declinations in Britain have varied through an angle of 70[degrees] and their magnetic dips have ranged about 25[degrees], the researchers report.
d) Update raster maps to EC-135 helicopter and simulator - edition 2014 aktualnepoprawki incorporating magnetic declination.
The figures show that both sensors see quite small changes in magnetic declination (for the variometer) and the east-west field strength (for the fluxgate).
However, computation of this so-called magnetic declination was never completed.