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The Earth’s Magnetic Field
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Source: NASA http://www.nasm.si.edu/research/ceps/etp/earth/img/dipole_earth.gif
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Source: NASA http://www.nasm.si.edu/research/ceps/etp/earth/img/magneto.gif
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spher. harmonic analyses
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magnetic reversals, secular variation
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Earth’s Magnetic Field Mostly a dipole field (modern and paleomagnetic evidence) Can change direction (polarity) Secular variation (small-scale changes in direction and magnitude)
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Magnetic Units: Magnetic field – Tesla field mostly described in micro-Tesla or gamma (γ) 1γ = 10 -9 T
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http://geophysics.ou.edu/solid_earth/notes/mag_earth/earth.htm
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Mathematical description: Spherical harmonic analyses
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Short-term changes: Careful measurements since 1600 Navigational purposes
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http://gsc.nrcan.gc.ca/geomag/nmp/early_nmp_e.php
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Paleomagnetism – history of the earth’s magnetic field Earth is dipole field –Relationship between Inclination and latitude tan I = 2 tan λ
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Identification of magnetic minerals in rocks Rocks are assemblages of diamagnetic, paramagnetic, and ferrimagnetic minerals. Concentration of ferrimagnetic minerals is usually very small (< 1 %) Microphotograph of a thin section of norite dolomite limestone sandstone shale Sedimentary rocks Volcanic rocks granite gabbro basalt 1 10 -1 10 -2 10 -3 10 -4 10 -5 Magnetic susceptibility, κ (SI units) Median values and ranges of the magnetic susceptibility in common rock types Modified from Lowrie, 1997
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Magnetic Polarity
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Duration of a Polarity Chron
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Generation of the Magnetic Field No big fat bar magnet Dynamic processes inside the outer core
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Early (Simplistic) Model
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Ultimate driver of magnetic field ?
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Magnetic Field of Other Planets Mercury – yes, but weak Venus – no, or very weak Mars – no clear evidence for field, but might have had field in the past Jupiter – yes, very strong (20,000 times earth) Saturn – yes 500 times earth Uranus – yes, strong tilt with respect to rotational axis
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Source: NASA http://photojournal.jpl.nasa.gov/jpeg/PIA02008.jpg
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