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Geospace Exploration Mission
Y. Miyoshi (1), T. Ono (2), T. Takashima (3), M. Hirahara (4), K. Asamura (3),
K. Seki (1), Y. Kasaba (2), A. Kumamoto (2), A. Matsuoka (3),
H. Kojima (5), K. Shiokawa (1) , M. Fujimoto (3), T. Nagatsuma (6)
and ERG working group
(1) STEL, Nagoya University, Japan, (2) Tohoku University, Japan
(3) ISAS/JAXA, Japan, (4) The University of Tokyo, Japan
(5) RISH, Kyoto University, (6) NICT, Japan
ERGEnergization and Radiation in Geospace
2010 RBSP-SWG
OUTLINE
1. Introduction
- science targets of the mission
2.ERG project
- ERG satellite
- ERG ground networks
- ERG simulation/integrated studies
- science coordination team/project science center
3. International collaboration
4. Collaboration with the RBSP mission (ERG pre-launch phase)
5. Summary
- Particle acceleration
(wave-particle interaction/
adiabatic radial diffusion)
- Particle transportation
(potential field/inductive field)
- Plasma waves
- M-I coupling via FAC
Acceleration via
radial diffusion
Whistler mode waves (kHz)
Acceleration via
W-P interaction
(NASA RBSP website)
1. Introduction ・・・ dynamical coupling in Geospace
RADIATION BELTS (MeV)
PLASMASPHERE (eV)
RING CURRENT (keV)
PLASMA SHEET
ULF pulsation (mHz)
plasmasphere
plasma sheet
inner belt outer belt
thermal
(~eV)
hot
(~ 100 keV)
relativistic
(~ MeV)
L=6L=3
en
erg
yParticles in the inner magnetosphere
distance from the earth
ring current
sub-relativistic
In the inner magnetosphere, widely differing energies over 6 orders
coexist same region.
plasmasphere
ring currentplasma sheet
inner belt outer belt
thermal
(~eV)
hot
(~ 100 keV)
relativistic
(~ MeV)
L=6L=3
en
erg
yExternal Source
external source (radial diffusion) --- violation of third invariant
large magnetic moment
MHD waves
Pc5
Transportation via MHD pulsations (drift-resonance) is
important for particle acceleration.
diffusion
sub-relativistic
PSD profile
(Green and Kivelson, 2004)
plasmasphere
ring current
plasma sheet
inner belt outer belt
thermal
(~eV)
hot
(~ 100 keV)
relativistic
(~ MeV)
L=6L=3
en
erg
y wave growth
acceleration
whistler
internal sources (w-p interactions) – violation of all invariants
Internal Source via wave particle interactions
ring current
sub-relativistic
Whistler mode waves act as a mediating agent via cyclotron resonance
- absorbing a fraction of the power of ring current electrons,
which results in wave growth
- its transfer to the acceleration of high energy electrons.
plasmasphere
ring current
plasma sheet
inner belt outer belt
thermal
(~eV)
hot
(~ 100 keV)
relativistic
(~ MeV)
L=6L=3
en
erg
y wave growth
acceleration
whistler
ring current
sub-relativistic
Variations of the plasmasphere are also essential to control the acceleration conditions,
because the plamasphere plays as an ambient media of plasma waves.
internal sources (w-p interactions) – violation of all invariants
Internal Source via wave particle interactions
plasmasphere
ring current
plasma sheet
inner belt outer belt
thermal
(~eV)
hot
(~ 100 keV)
relativistic
(~ MeV)
L=6L=3
en
erg
y wave growth
acceleration
whistler
ring current
sub-relativistic
Cross-Energy Coupling between particles of widely differing
energies over 6 orders via wave-particle interactions is
important to generate relativistic electrons in the inner
magnetosphere.
MeV electron acceleration is a manifestication of
cross-energy coupling.
internal sources (w-p interactions)
Internal Source via wave particle interactions
PSD profile
(Green and Kivelson, 2004)
2. The ERG project
project goal –
understanding cross-energy couplings for
generation and loss process of relativistic particles
&
variation of geospace during space storms
Target 1: Dynamics of the radiation belts
particle acceleration, transportation and loss
Target 2: Dynamics of the space storms
ring current and electro-magnetic field
variation associated with M-I coupling
Target 3: Dynamics of the plasmasphere
Significance of this project.
・ direct observations on generation of relativistic electrons
contribution to understanding of the particle acceleration
in the universe.
・ instrumental development to measure plasma and fields
under the incidence of radiation belt particles with small satellite
contribution to the future Jovian mission.
REMOTE SENSING
ERG-satelliteERG-ground networks
ERG Project Group
IN-SITU OBSERVATION
Science Coordination Team
Project Science Center
NUMERICAL SIMULATION/MODELING
ERG-simulation/integrated studies
ERG Working Group (~90 researchers in 20 universities/institutes, 2010/06)
PI: T. Ono (Tohoku Univ.),
Mission Manager: T. Takashima (ISAS/JAXA), Science Manager: Y. Miyoshi (STEL, Nagoya Univ.)
ERG-satellite
Particle Instrument: M. Hirahara (U. Tokyo), T. Yanagimachi (Rikkyo Univ.) T. Takashima, K. Asamura,
Y. Saito, T. Abe, H. Matsumoto, S. Kasahara, M. Shimoyama , N. Higashio (JAXA), W. Miyake(Tokai Univ.),
K. Ogasawara (SwRI), Y. Kazama, C. Z. Cheng (NCKU)
Plasma Wave& Electric Field Instrument: Y. Kasaba, T. Ono, A. Kumamoto, Y. Kato (Tohoku Univ.),
Y. Kasahara, S. Yagitani, T. Imachi, Y. Goto (Kanazawa Univ.), H. Kojima, Y. Omura, Y. Ueda (Kyoto Univ.),
M. Iizima (Daijyo Syukutoku), H. Hayakawa, T. Muranaka (JAXA), T. Okada, K. Isisaka, S. Miyake
(Toyama Pref. Univ)
Magnetic Field Instrument: A. Matsuoka (JAXA), M. Tanaka, H. Shirasawa (Tokai Univ.), K. Shiokawa
(Nagoya Univ.), Y. Tanaka (NIPR), K. Yumoto (Kyushu Univ.), T. Nagatsuma (NICT), M. Shinohara
(Kagoshima Tech. College)
ERG-ground networks
K. Shiokawa, N. Nishitani, T. Kikuchi, Y. Otsuka, R. Fujii (Nagoya Univ.), K. Yumoto, H. Kawano, A. Yoshikawa
(Kyushu Univ.), N. Sato, A. Yukimatsu, H. Yamagishi, A. Kadokura, Y. Ogawa (NIPR), M. Taguchi
(Rikkyo Univ.), K. Hosokawa (U. of Electro-Communications), K. Hashimoto (KUHW),
K. Kitamura (Tokuyama Tech. College) , F. Tsuchiya (Tohoku Univ.)
ERG-simulation/integrated studies
K. Seki, Y. Miyoshi, A. Ieda, Y. Ebihara, Y. Miyashita, T. Umeda, S. Masuda, Y. Matsumoto, T. Hori,
S. Saito, T. Amano (STEL, Nagoya Univ.), K. Murata, H. Shimazu, T. Tanaka, H. Shinagawa, H. Jin (NICT),
M. Nakamura (Osaka Pref. Univ.), N. Terada (Tohoku Univ.) , M. Nose, T. Iyemori, Y. Omura, S. Machida,
A. Shinbori (Kyoto Univ.), M. Fujimoto, I. Shinohara, H. Hasegawa, K. Maezawa, T. Obara, M. Yamada (JAXA),
S. Watanabe, K. Komatsu (Hokkaido Univ.), T. Higuchi, G. Ueno, S. Nakano (ISM), M. Hoshino,
T. Terasawa (U. of Tokyo), T. Nagai, K. Asai, R. Kataoka (TITEC), S. Arvelius (IRF), T. Takada (Koch Tech. College)
The ERG satellite
・apogee geocentric distance: 5.0 Re (L~10) ・perigee altitude: 300 km
・ inclination angle: 31 deg
・MLT of initial apogee: 9:00 (± 1:00)
・planned launch date: FY2014 -2015
・mission line: > 1yr
Size: 0.95 m X 0.95 m X 1.705 m (w/o projection)
Weight: 350 kg
Spin: Sun-oriented spin (7.5 RPM)
Attitude accuracy: less than 0.5 deg (star sensor)
Appearance of the ERG satellite
plasmasphere
ring current
plasma sheet
inner belt outer belt
1 eV
100 keV
1 MeV
ERG : plasma & particles
LEP-i
MEP-i
1 keVLEP-e
MEP-e
HEP-e
XEP
10 MeV
PPE: Plasma and Particle Experiment (PI: M. Hirahara, U. Tokyo)
ion electron
-ERG/ PPE measure widely differing energies with ion mass discriminations
(H+, O+, He+, He++).
- The energy coverage of particle instruments overlaps each other.
ring current
sub-relativistc
XEP FOVMEP FOV
DC
1 Hz
1 kHz
Whistler
(~kHz)
MHD waves
(~mHz)
Convective
Field
PWE
Magnetic
Field
1mHz MGF(fluxgate)
PWE
(search coil)
10 kHz
PWE: Plasma Wave and Electric Field Experiment (PI: Y. Kasaba, Tohoku. U.)
MGF: Measurement of Geomagnetic Field (PI: A. Matsuoka, ISAS)
electric field magnetic field
- ERG/ PWE and MGF measure electric and magnetic field for wide frequency
range from DC to MHz.
- Frequency spectrum and wave-form observations (E: ~100 kHz/B:~20kHz)
EMIC
(~Hz)
magnetosonic
wave
(~100Hz)
100 kHz UHR
1 MHz
ERG: Field and Waves
・Magnetometer Network:MAGDAS/CPMN, Silk-Road, Antarctic Network, ULTIMA
・Radar Network: SuperDARN network (HOK, KSR, SWE, SWS), FM-CW radar
- global convective electric field
- ULF pulsation (Pc5)
- Electric field penetration
- ionospheric current /ring current.
- ULF pulsation (Pc5).
- EMIC (Pc1).
- diagnostics of plasmasphere
・Optical Imager Network:Canada, Norway, Siberia, Antarctica
- Measurement of electron/proton precipitations
- Estimation of ionospheric conductivity
The ERG ground networks (PI: K. Shiokawa, STEL)
Sakaguchi et al. JGR, 2008
・Riometer observations:Antarctica
・VLF observations: Antarctica
- whistler (chorus, hiss) observations
- Imaging of precipitation of tens keV electrons
・LF-wave observations : Svalbard
- Estimation of MeV electron precipitations
The ERG ground networks
The ERG simulation/integrated studies (PI: K. Seki, STEL)
Saito, Miyoshi, and Seki. JGR, 2010
-High-precision test particle simulation
code in realistic 3D magnetic fields
during storm time.
( calculation error less than 1% over 24 hour)
Ring Current Model Radiation Belt Model
Amano, Seki, Miyoshi et al., submitted to JGR.
-Self-consistent simulation with 5-D Boltzmann
equation/Maxwell equation.
- It is possible to simulate ULF waves (fast/slow/
Alfven mode waves) in the inner magnetosphere.
Comprehensive simulations which can be compared with the observations
are necessary for the ERG project. STEL/GEMSIS project is one of core
activities of the ERG simulation/integrated study group.
・Science Coordination Team (Ld. Y. Miyoshi, STEL)
-Planning and coordination of science program of the ERG project.
-Making an arrangement of the international collaborations.
Science Coordination Team/Project Science Center
Science Coordination Team/Project Science Center
・Project Science Center (Ld. K. Seki)
- The science data of the ERG project will be archived in the CDF file.
- We are developing software package based on the THEMIS-IDL tool
to analyze observations and modeling/simulation data.
- We start the collaboration with the THEMIS mission about
the development of the software.
210 MM magnetic field data
SuperDARN data HOK
KSR
3. International Collaboration: international fleet of satellites
US/RBSP
Canada/ORBITALS
Japan/ERG
US/THEMIS
Russia/RESONANCE
Sun
Solar Wind
Optical Imager
Geospace-
Ionosphere
Aurora
Magnetometer
ORBITALS
Radiation Belts
Ring Current
RBSP
ERG
Radar
RESONANCE
LANL
GOES
POES
Geospace-
Magnetosphere
THEMIS
Geotail
Cluster
Reimei
FORMOSAT-5
CASSIOPE
CINEMA
3. International Collaboration: coordinate studies
SAMPEXDSX
BARREL
FOV of SuperDARN
Hokkaido Radar
Outer radiation belt
Footprint of
the satellite
4. Collaboration with RBSP (ERG-pre launch phase)
Magnetic Bay/Pc5/Pc1 observations Global convective electric field / Pc5
Proton/Electron aurora observations
1. Ground network observations at sub-auroral latitudes :Coordinated observations between the ground based observations and the RBSP satellites.
The CDF files of the related data will be downloaded from the ERG-science center.
Pc1
5577
6300
H beta
Sakaguchi et al., 2008
4. Collaboration with RBSP (ERG-pre launch phase)
2. Comparative study between the simulations and the RBSP observations
Self-consistent ULF wave (fast mode) simulation is important to
understand the shock accelerations of MeV electrons.
Evolution of plasma flow and current (RC and FAC) Evolution of MHD mode waves
Spatial / pitch angle distribution of energetic particles
Simulation in the realistic magnetic field is important
to understand the dynamics of the trapped particle.
e.g., pitch angle distributions at different positions.
Amano et al.
Saito et al., 2010
4. Collaboration with RBSP (ERG-pre launch phase)
3. Coordinated studies with the Akebono satellite (1989-present)
Coordinated observations between the equatorial plane and
middle-latitudes.
- wave observations (1 Hz – 5000 kHz)
- energetic electrons (300keV, 900 keV, 2500 keV)
Plasma wave observations (1Hz -5000 kHz)
Tadokoro et al., 2009
Radiation Monitor
>2500 keV 950 keV 300 keV
Seki et al., 2005
Akebono
CRRES--RBSP
5. Summary
- The ERG satellite has been nominated as the second mission of
the small satellite program of ISAS/JAXA. Further approval by JAXA/HQ
will be required. The planned launch will be FY 2014-15.
- The ground network observations/integrated studies/science center
have started their activity.
- International collaboration with RBSP, ORBITALS, RESONANCE,
THEMIS, GOES/POES, LANL, DSX, SAMPEX, ground networks etc.
would be very good chance for study of geospace during the solar maximum.
- We hope to collaborate on the coordinate observations between
the RBSP satellites and ERG ground observations as well as
comparative studies with the simulations.