magnetic declination oor Noorse Bokmål
magnetic declination
en
(military, nautical, navigation) 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. In nautical and aeronautical navigation, the term magnetic variation is used instead of magnetic declination and the angle is termed variation of the compass or magnetic variation. Magnetic declination is not otherwise synonymous with magnetic variation which refers to regular or irregular change with time of the magnetic declination, dip, or intensity.
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misvisning
en
the angle on the horizontal plane between magnetic north and true north
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The local angular difference between magnetic north and true north is called the magnetic declination.
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Humboldt had devised a calendar for observations of magnetic declination .
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As the compass is moved closer to one of the magnetic poles, the magnetic declination, the difference between the direction to geographical north and magnetic north, becomes greater and greater.
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Lindbergh also used special navigation instruments such as the Earth Inductor Compass as its main instrument, allowing Lindbergh to navigate while taking account of the magnetic declination of the earth.
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- Use it as a simple compass with declination correction and magnetic field strength display.
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Some scientists argue that the magnetic field of the earth has declined over time.
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Because magnetic North and true North are not at the same location, you must set the declination on your compass.
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The angle of declination is primarily determined by the fluctuations in the earth's magnetic field — closer to the poles, the different positions of the geographical and magnetic north are also used.
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The book is known under the name De magnete (the actual title being much longer) - About the magnet - and was written by the Englishman William Gilbert (1540-1603), a renowned doctor in Elizabeth I's England, and appointed as her personal physician until the plague took his life two years later. In De magnete, Gilbert follows the thread from Petrus Perengrinius Epistola de magnete going through magnets and their properties, magnetic poles, describing deviation and declination and arriving at the result that the Earth has the same properties as a sphere of magnetite.
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