Discovery[1] | |
---|---|
Discovered by | Mariner 10 |
Discovery date | April 1974 |
Internal field[2][3] | |
Radius of Mercury | 2,439.7 ± 1.0 km |
Magnetic moment | 2 to 6 × 1012 T•m3 |
Equatorial field strength | 300 nT |
Dipole tilt | 0.0°[4] |
Solar wind parameters[5] | |
Speed | 400 km/s |
Magnetospheric parameters[6][7] | |
Type | Intrinsic |
Magnetopause distance | 1.4 RM |
Magnetotail length | 10–100 RM |
Main ions | Na+, O+, K+, Mg+, Ca+, S+, H2S+ |
Plasma sources | Solar wind |
Maximum particle energy | up to 50 keV |
Aurora |
Mercury's magnetic field is approximately a magnetic dipole, apparently global,[8] on the planet of Mercury.[9] Data from Mariner 10 led to its discovery in 1974; the spacecraft measured the field's strength as 1.1% that of Earth's magnetic field.[10] The origin of the magnetic field can be explained by dynamo theory.[11] The magnetic field is strong enough near the bow shock to slow the solar wind, which induces a magnetosphere.[12]
Magnetic Field and Magnetosphere
was invoked but never defined (see the help page).{{cite web}}
: CS1 maint: multiple names: authors list (link)