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  2. Earth's magnetic field - Wikipedia

    en.wikipedia.org/wiki/Earth's_magnetic_field

    The Earth and most of the planets in the Solar System, as well as the Sun and other stars, all generate magnetic fields through the motion of electrically conducting fluids. [54] The Earth's field originates in its core. This is a region of iron alloys extending to about 3400 km (the radius of the Earth is 6370 km).

  3. World Magnetic Model - Wikipedia

    en.wikipedia.org/wiki/World_Magnetic_Model

    World Magnetic Model. Magnetic declination map at sea-level for the year 2010 derived from WMM2010. The World Magnetic Model (WMM) is a large spatial-scale representation of the Earth's magnetic field. It was developed jointly by the US National Geophysical Data Center and the British Geological Survey. The data and updates are issued by the US ...

  4. File:World Magnetic Field 2015.pdf - Wikipedia

    en.wikipedia.org/wiki/File:World_Magnetic_Field...

    File:World Magnetic Field 2015.pdf. Size of this JPG preview of this PDF file: 800 × 533 pixels. Other resolutions: 320 × 213 pixels | 640 × 427 pixels | 1,024 × 683 pixels | 1,280 × 853 pixels | 2,560 × 1,707 pixels | 5,400 × 3,600 pixels. This is a file from the Wikimedia Commons. Information from its description page there is shown below.

  5. International Geomagnetic Reference Field - Wikipedia

    en.wikipedia.org/wiki/International_Geomagnetic...

    International Geomagnetic Reference Field. The International Geomagnetic Reference Field (IGRF) is a standard mathematical description of the large-scale structure of the Earth's main magnetic field and its secular variation. It was created by fitting parameters of a mathematical model of the magnetic field to measured magnetic field data from ...

  6. Magnetic declination - Wikipedia

    en.wikipedia.org/wiki/Magnetic_declination

    The angle between magnetic and grid meridians is called grid magnetic angle, grid variation, or grivation." [1] By convention, declination is positive when magnetic north is east of true north, and negative when it is to the west. Isogonic lines are lines on the Earth's surface along which the declination has the same constant value, and lines ...

  7. File:World Magnetic Field 2020.pdf - Wikipedia

    en.wikipedia.org/wiki/File:World_Magnetic_Field...

    File:World Magnetic Field 2020.pdf. Size of this JPG preview of this PDF file: 720 × 600 pixels. Other resolutions: 288 × 240 pixels | 576 × 480 pixels | 922 × 768 pixels | 1,229 × 1,024 pixels | 2,458 × 2,048 pixels | 5,400 × 4,500 pixels. Original file ‎ (5,400 × 4,500 pixels, file size: 3 MB, MIME type: application/pdf) Wikimedia ...

  8. Geomagnetic excursion - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_excursion

    A geomagnetic excursion, like a geomagnetic reversal, is a significant change in the Earth's magnetic field.Unlike reversals, an excursion is not a "permanent" re-orientation of the large-scale field, but rather represents a dramatic, typically a (geologically) short-lived change in field intensity, with a variation in pole orientation of up to 45° from the previous position.

  9. World Digital Magnetic Anomaly Map - Wikipedia

    en.wikipedia.org/wiki/World_Digital_Magnetic...

    The World Digital Magnetic Anomaly Map (WDMAM) was first made available by the Commission for the Geological Map of the World in 2007. Compiled with data from governments and institutes, [1] the project was coordinated by the International Association of Geomagnetism and Aeronomy, and was presented by Mike Purucker of NASA and Colin Reeves of ...