Induction From Satellite Data
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-4423-6_146
In addition to sources of internal origin, magnetic satellites record the variations in Earth's external magnetic field caused by interaction of the ionosphere and magnetosphere with the solar wind and radiation, along with the secondary magnetic fields induced in Earth. The ratio of the internal to external field may be used to probe the electrical conductivity structure of the planet. Satellite induction studies date from Didwall's (
1984) early work with the POGO satellite data. Olsen (
1999a) and Constable and Constable (
2004a) provide reviews of satellite induction methods. Table
I3 presents a list of past, present, and future magnetic satellite missions that are relevant to induction studies (see
MAGSAT,
Ørsted,
POGO).
Table I3
Satellite missions relevant to magnetic induction studies, as of July, 2005
Satellite |
Type |
Launch date |
Data to |
Inclination |
Altitude (km) |
|
|---|---|---|---|---|---|---|
POGO 2 |
Scalar |
October 14, 1965 |
October 2, 1967 |
87.3° |
410–1510 |
|
POGO 4 |
Scalar |
July 28, 1967 |
January 19, 1969 |
86.0° |
410–910... |
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