GEOL/PHYS 6650 Geophysics Graduate Seminar: Geomagnetics
GEOL/PHYS 6650 Geophysics graduate seminar: Geomagnetics. Every Wed 11am in BESC 355.
Geomagnetism Class Spring 2016: 1 hour long lectures once in a week starting January, 2016, intended for graduate students of CU Earth Sciences and other interested researchers.
HISTORICAL MAIN FIELD CHANGE AND DECLINATION
The Earth is like a giant magnet, surrounded by a magnetic field. This magnetic field, which is a vector with both direction and intensity, is generated by a dynamo process in the fluid outer core of the Earth. Due to the chaotic movement of the core fluid, the Earth's magnetic field gradually changes over the years.
MAGNETOSPHERIC MAGNETIC FIELD
The magnetosphere is a large cavity produced by the Earth's main magnetic field. Essentially, the charged particles of the solar wind cannot move across magnetic field lines and are deflected around the Earth. The complex interactions of the Earth's magnetic field with the solar wind give rise to a multitude of electric current systems, which flow at typical distances of 2 to 20 Earth radii from the surface.