Space Weather Imaging by the EPIC Small Explorer Mission
Jerry
Goldstein
Southwest Research Institute
Poster
Exploration of Plasma Interactions and Circulation (EPIC) is a Heliophysics imaging mission
to reveal the life cycle of core magnetospheric plasma. Core plasma is a fundamental
magnetospheric population comprising the majority of the magnetosphere’s mass, 100 to 1,000
metric tons. Core plasma is initially cold (<10 eV) within the plasmasphere and oxygen torus.
During storms it is transported throughout geospace and heated to 100 eV – keV energies.
EPIC is the first mission to target the critical core plasma life cycle (CPLC), by imaging four
fundamental geospace populations: plasmasphere, dense oxygen torus, neutral hydrogen
exosphere, and ring current. Continuous, multi-species, multi-region imaging from EPIC’s high
(>70º) inclination 20 RE circular orbit achieves a coordinated system-level view of the CPLC,
including imaging of core plasma circulated to both dayside and nightside outer magnetosphere.
This continuous, multi-region imaging is also extremely well suited to space weather
monitoring/backcasting that can greatly improve predictive models. Continuous 30.4 nm
EUVHe plasmaspheric He+ imaging provides a global monitor of the cold plasma, a population
with several big space weather effects: (1) it controls the waves that can increase or decrease the
outer radiation belt, (2) it reduces spacecraft charging, and (3) it enables estimation of inner
magnetospheric convection. The first-ever 83.4 nm EUVO oxygen ion imaging will finally
observe the formation and global distribution of the dense oxygen torus whose mass loading
controls the Alfven speed that is fundamental to magnetosphere-ionosphere coupling, and
reconnection. A high-resolution (200 km) geocoronal imager (GCI) captures the neutral H
exosphere that affects atmospheric escape. Low-energy neutral atom (LENA) imaging captures
the macroscale dynamics of ENA spectra to measure how core ion recirculation feeds storms.
Core plasma is an essential and central component of geospace weather. EPIC improves
prediction of extreme conditions driven by the many CPLC-affected plasmas and phenomena
throughout geospace.
EPIC's science and space weather impacts are cross disciplinary (both "Ionosphere and
Thermosphere" and "Geospace/Magnetosphere" categories), targeting a plasma population
whose origin is ionospheric, whose home is the inner magnetosphere, and whose fate is to be
circulated to the outer magnetosphere, both dayside and nightside.
to reveal the life cycle of core magnetospheric plasma. Core plasma is a fundamental
magnetospheric population comprising the majority of the magnetosphere’s mass, 100 to 1,000
metric tons. Core plasma is initially cold (<10 eV) within the plasmasphere and oxygen torus.
During storms it is transported throughout geospace and heated to 100 eV – keV energies.
EPIC is the first mission to target the critical core plasma life cycle (CPLC), by imaging four
fundamental geospace populations: plasmasphere, dense oxygen torus, neutral hydrogen
exosphere, and ring current. Continuous, multi-species, multi-region imaging from EPIC’s high
(>70º) inclination 20 RE circular orbit achieves a coordinated system-level view of the CPLC,
including imaging of core plasma circulated to both dayside and nightside outer magnetosphere.
This continuous, multi-region imaging is also extremely well suited to space weather
monitoring/backcasting that can greatly improve predictive models. Continuous 30.4 nm
EUVHe plasmaspheric He+ imaging provides a global monitor of the cold plasma, a population
with several big space weather effects: (1) it controls the waves that can increase or decrease the
outer radiation belt, (2) it reduces spacecraft charging, and (3) it enables estimation of inner
magnetospheric convection. The first-ever 83.4 nm EUVO oxygen ion imaging will finally
observe the formation and global distribution of the dense oxygen torus whose mass loading
controls the Alfven speed that is fundamental to magnetosphere-ionosphere coupling, and
reconnection. A high-resolution (200 km) geocoronal imager (GCI) captures the neutral H
exosphere that affects atmospheric escape. Low-energy neutral atom (LENA) imaging captures
the macroscale dynamics of ENA spectra to measure how core ion recirculation feeds storms.
Core plasma is an essential and central component of geospace weather. EPIC improves
prediction of extreme conditions driven by the many CPLC-affected plasmas and phenomena
throughout geospace.
EPIC's science and space weather impacts are cross disciplinary (both "Ionosphere and
Thermosphere" and "Geospace/Magnetosphere" categories), targeting a plasma population
whose origin is ionospheric, whose home is the inner magnetosphere, and whose fate is to be
circulated to the outer magnetosphere, both dayside and nightside.
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Geospace/Magnetosphere Research and Applications
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