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Earth's magnetic field, also known as the geomagnetic field, is the magnetic field that extends from Earth's interior out into space, where it interacts ...
gov. Retrieved on 2012-01-27. ^ a b c d McElhinny, Michael W. ; McFadden, Phillip L. (2000). Paleomagnetism: Continents and Oceans. Academic Press. ISBN 978-0-12-483355-5. ^ Opdyke, Neil D. ; Channell, James E. T. (1996). Magnetic Stratigraphy. ISBN 978-0-12-527470-8. ^ Mussett, Alan E. ; Khan, M. Aftab (2000). Looking into the Earth: An introduction to Geological Geophysics. Cambridge University Press.
"Tesla". National High Magnetic Field Laboratory. Archived from the original on 21 March 2013. Retrieved 20 October 2013. ^ a b Chulliat, A. ; Brown, W. ; Alken, P. ; Nair, M. ; Cox, G. ; Woods, A. ; Meyer, B. ; Paniccia, M. (2020). The US/UK World Magnetic Model for 2020–2025 (Report). Retrieved 30 August 2023. ^ "Ancient lava reveals secrets of Earth's magnetic field cycle". Cosmos Magazine. 2021-08-31. Retrieved 2021-09-03. ^ Casselman, Anne (28 February 2008). "The Earth Has More Than One North Pole". Scientific American. Retrieved 21 May 2013. ^ Serway, Raymond A. ; Chris Vuille (2006). Essentials of college physics. USA: Cengage Learning. p. 493.
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This model truncates at degree 12 (168 coefficients) with an approximate spatial resolution of 3, 000 kilometers. It is the model used by the United States Department of Defense, the Ministry of Defence (United Kingdom), the United States Federal Aviation Administration (FAA), the North Atlantic Treaty Organization (NATO), and the International Hydrographic Organization as well as in many civilian navigation systems.
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[12] Common coordinate systems used for representing the Earth's magnetic field. Intensity[edit] The intensity of the field is often measured in gauss (G), but is generally reported in microteslas (μT), with 1 G = 100 μT. A nanotesla is also referred to as a gamma (γ). The Earth's field ranges between approximately 25 and 65 μT (0.
1) Bow shock. 2) Magnetosheath. 3) Magnetopause. 4) Magnetosphere. 5) Northern tail lobe. 6) Southern tail lobe. 7) Plasmasphere. Earth's magnetic field, predominantly dipolar at its surface, is distorted further out by the solar wind. This is a stream of charged particles leaving the Sun's corona and accelerating to a speed of 200 to 1000 kilometres per second. They carry with them a magnetic field, the interplanetary magnetic field (IMF). [25] The solar wind exerts a pressure, and if it could reach Earth's atmosphere it would erode it.
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ISBN 978-0-521-78085-8. ^ Temple, Robert (2006). The Genius of China. Andre Deutsch. ISBN 978-0-671-62028-8. ^ a b c d e f g h i j Merrill, McElhinny & McFadden 1996, Chapter 2 ^ a b "Geomagnetism Frequently Asked Questions". National Geophysical Data Center. Retrieved 21 October 2013. ^ Palm, Eric (2011).
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Earth's magnetic field Earth's magnetic field, also known as the geomagnetic field, is the magnetic field that extends from Earth's interior out into space, where it
Dynamo Ceske Budejovice ReviewAt the moment, Dynamo Ceske Budejovice has 6 scored points, and for such a competitive championship as this, alas, is too little. The 13 line in the table is the result that this team fully deserved with its game. The level of their play is clearly shown by their statistics - 2 wins, 0 draws, 5 defeats. In these matches, they score on average 1.
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