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. 2018 Jul 20;39(5):817–859. doi: 10.1007/s10712-018-9487-x

Table 2.

Major particle populations (subsystems) in the magnetosphere; parameters of the populations can be found in Fig. 2

Plasma population What and where Origin Roles in the system
Ionosphere Ionized upper atmosphere Sunlight on atmosphere and electron impact on atmosphere Supplies plasma to magnetosphere
Source of the plasmasphere and warm plasma cloak
Dissipates system energy by Joule heating
Hinders magnetospheric convection
Magnetosheath Shocked solar-wind plasma bathing the outer surface of the magnetosphere Solar wind Plasma properties govern dayside reconnection rate
Supplies solar-wind-origin plasma
Transfers momentum into magnetosphere
Generates ULF waves
Plasmasphere Cold ionospheric-origin plasma in the dipolar region Ionosphere Provides home for whistler-mode hiss waves
Provides home for EMIC waves
Feeds drainage plume
Feeds back on dayside reconnection
Ion plasma sheet (includes ring current) Hot ions in magnetotail
and dipolar region
Mantle,
LLBL,
Ionosphere
Diamagnetically distorts magnetic field
Drives EMIC waves in dipole
Can mass load dayside reconnection rate
Electron plasma sheet Hot electrons in magnetotail and dipolar region Solar wind Home of the aurora and auroral currents
Provides enhanced ionization of ionosphere
Drives chorus waves
May control ionospheric outflows to the warm plasma cloak
Seed population for substorm-injected electrons
Electron radiation belt Relativistic electrons in the dipolar region Substorm-injected electrons Energy sink for plasma waves
Spacecraft damage
Alters atmospheric chemistry
Ion radiation belt Very energetic protons in dipolar region Neutron decay, Solar wind
Ion plasma sheet
not much is known about the origin and interactions of the outer proton belt
Substorm-injected electrons Energetic electrons in the dipolar region Electron plasma sheet Drives whistler-mode chorus waves
Seed population for electron radiation belt
Warm plasma cloak Cool oxygen-rich plasma in
dipolar region
Ionosphere Mass loading of dayside reconnection rate
Controls properties of ULF waves
Low-latitude boundary layer (LLBL) Solar-wind plasma flowing tailward inside the magnetopause Magnetosheath Feeds plasma into the ion and electron plasma sheets
Mantle Solar-wind plasma and cusp-ionosphere plasma moving into the magnetotail Magnetosheath Feeds plasma into the ion and electron plasma sheets
Impacts reconnection rate in magnetotail
Plasmaspheric drainage plume Cold plasma flowing from plasmasphere to dayside magnetopause Plasmasphere Loss of plasmasphere
Mass loading of dayside reconnection rate
Home of EMIC and hiss waves at larger radii than plasmasphere
Atmosphere Neutral gas gravitationally bound to the Earth Absorbs electrons and ions from the magnetosphere
Hydrogen geocorona Neutral hydrogen evaporating off of atmosphere Atmosphere Causes charge-exchange loss of ion-plasma-sheet ions
Has a charge-exchange interaction with the plasmasphere
Is affected by magnetospheric energy input into upper atmosphere

EMIC: electromagnetic ion-cyclotron