Earth's Magnetic Field: Peak Altitude & Value

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SUMMARY

The Earth's magnetic field does not have a peak altitude above the equator; instead, it decreases with elevation. The magnetic flux is strongest near the poles, where phenomena such as auroras occur. The field is primarily generated by the Earth's liquid outer core, with 95% of the magnetic field being internal and only 5% external, as established by Carl Friedrich Gauss in 1838. The approximate surface value of the magnetic field at the equator is around 0.3 Gauss.

PREREQUISITES
  • Understanding of Earth's magnetic field dynamics
  • Familiarity with dipole magnetic fields
  • Knowledge of geomagnetic phenomena such as auroras
  • Basic principles of geophysics and magnetic field measurement
NEXT STEPS
  • Research Earth's magnetic field mapping tools and simulators
  • Explore the effects of altitude on magnetic field strength
  • Study the principles of geomagnetism and its applications
  • Investigate the historical contributions of Carl Friedrich Gauss to geophysics
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Geophysicists, educators in Earth sciences, students studying geomagnetism, and anyone interested in the dynamics of the Earth's magnetic field.

drag
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Greetings !

I'd like to know the approximate altitude above the equator
where the Earth's magnetic field has a peak value and what is
that value (assuming approximate surface value there is 0.3 Gauss).

Also, I'd appreciate any links including Earth's magnetic field
maps/simulators at and aspecialy above the surface (in LEO for example).

Thanks. :smile:

Live long and prosper.
 
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The magnetic field decreases as elevation increases. There is no peak, unless you are talking subterranean.
 
I don't think that's the case, you don't expect the greatest
magnetic flux right near the external surface of a coil for example, do you ?
Also, from the rough field line plots I've seen here and there
it looks like it should be at some distance.

Peace and long life.
 
The greatest flux will be near the poles. That's why we have the auroras at high latitudes. Earth's magnetic field is essentially a dipole field which varies inversely with the cube of the distance from the dipole. (Of course as you get closer to the center of the Earth the structure of the field becomes more complicated.)
 
Thanks. But, like I said, I'm more interested in the equator.
 
drag said:
Thanks. But, like I said, I'm more interested in the equator.

In that case you have your answer!
 
drag said:
I don't think that's the case, you don't expect the greatest
magnetic flux right near the external surface of a coil for example, do you ?
Also, from the rough field line plots I've seen here and there
it looks like it should be at some distance.

Peace and long life.
The surface of the Earth does not function as a coil. In fact, the main source of the magnetic field is a long ways under you feet; it's in the (liquid) outer core. In 1838, Carl Friedrich Gauss proved 95% of Earth's magnetic field is internal, 5% external.
http://geophysics.ou.edu/solid_earth/notes/mag_earth/earth.htm
 
Last edited by a moderator:
Thanks. Good link too.
 

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