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DOUBLE STAR IMAGE CONJUNCTIONS: OPPORTUNITY FOR NEW SCIENCE

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Title: DOUBLE STAR IMAGE CONJUNCTIONS: OPPORTUNITY FOR NEW SCIENCE


1
DOUBLE STAR IMAGE CONJUNCTIONSOPPORTUNITY FOR
NEW SCIENCE
  • Pontus Cson Brandt, D. G. Mitchell, S. Ohtani,
    E. C. Roelof, R. Demajistre JHUAPL, MD
  • R. A. Wolf Rice, TX
  • M. C. Fok NASA GSFC, MD

2
OUTLINE
  • WHY ENA IMAGING?
  • WHAT HAVE WE LEARNED?
  • MI-coupling at work
  • WHY gt2 VANTAGE POINTS?
  • CONJUNCTIONS

3
Charge Exchange
A magnetically trapped ion captures an electron
from a neutral hydrogen atom...
creating an energetic neutral atom (ENA) that is
no longer trapped.
4
THE IMAGE MISSION
  • Lifetime 2000-2005
  • 800 x 8 Re solar inertial orbit (more later on
    orbit)
  • LENA 50 eV-10 keV
  • MENA 1-50 keV
  • HENA 10-200 keV (hydrogen) 50-180 keV (oxygen)
  • FUV auroral imager (proton and electron aurora)
  • EUV plasmaspheric imager. Images light
    resonantly scattered sunlight scattered on He.

5
High-Energy Neutral Atom (HENA) Imager
Lead Investigator D. Mitchell, Applied Physics
Lab
6
STORM AS SEEN BY HENA March 31 2001 (60-119 keV
protons)
-40 nT
21 nT
26 nT
0730 UT
0830 UT
0930 UT
7
WHY ENA IMAGING?
  • The only way to image proton plasma.
  • The hot plasma (ring current/plasma sheet) in the
    Terrestrial magnetosphere has proven to be more
    dynamic than anticipated.
  • Need to measure global pressure on timescales lt
    10-20 min.
  • All of the region 2 and probably a large portion
    of the nightside region 1 current system is
    PRESSURE DRIVEN.

8
MEASURED/COMPUTED QUANTITIES
SCIENTIFIC UNDERSTANDING
ENA
STORM, SUBSTORM DYNAMICS
PRESSURE
CURRENTS
MI-COUPLING
B-FIELD TOPOLOGY
DB (Biot-Savarts)
ADIABATIC EFFECTS ON RADIATION BELTS
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WHAT HAVE WE LEARNED SO FAR?
  • The morphology of the storm-time ring current
    depends heavily on the ionospheric conductivity.
  • Storm main phase ring current peaks around
    midnight.
  • Storm-time ring current penetrates always deeper
    than geosynchronous.
  • Heavy ions (O) are energized dramatically during
    storm-time substorms.
  • Storm-time substorm injections can have an
    extreme local time extent (to noon).

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18
MI-COUPLING AT WORK
  • Old picture storm-time ring current peaks at
    dusk, because thats where the Alfven layer comes
    closest to the Earth in a dawn-dusk E-field.
  • New picture Wolf, 1980 Fok et al., 2001
    storm-time ring current peaks at midnight.
    Consistent with IMAGE results Cson Brandt et
    al., 2002.
  • Mechanism
  • The convectional E-field (dawn-dusk) try to force
    Hall currents to flow across the terminators
    (conductivity jump)?positive charge
    build-up?skewing of potential pattern.
  • Probably some additional intricate effects.

19
SubAuroral Polarization Stream (SAPS) (Foster et
al., EOS and JGR, 2002)
20
WHY gt2 VANTAGE POINTS?
  • ANSWER one polar vantage point and on at the
    equator can resolve large-scale pitch-angle
    distributions (PAD) for the first time! ? Effects
    on all results discussed above.
  • Specifically is there a high-energy (100 keV)
    component of trapped ions during storm main
    phase?
  • Perigee passes with IMAGE and simultaneous apogee
    passes with DSP will give essential information
    on upper atmosphere interactions during different
    phases of the storm/substorm.
  • Note tomography requires far more vantage points
    than just a couple.

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22
CONJUNCTIONS
JAN 2001
JAN 2002
JAN 2003
JAN 2004 Mostly equatorial vantage point
JAN 2005 Mostly polar
23
PAD AND VANTAGE POINTS60-119 keV hydrogen ENA
EQUATORIAL VANTAGE POINT Dst-54 nT
POLAR VANTAGE POINT Dst-71 nT
Note a factor of 2 stronger flux for equatorial
vantage point?Anisotropy2.
24
3rd (and 4th) CONJUNCTION ?
  • NASA S/C TWINS launch in mid 2003.
  • 2 ENA imagers in 2 opposing Molnyia orbits.
    1000km x 7.2 Re. 64 deg incl.
  • Based on IMAGE/MENA design.
  • H and O
  • 1-70 keV

25
CONCLUSIONS
  • At mid-2004 IMAGE apocenter will be at 30-40 deg
    lat (southern hemi)?PAD resolved for first time!!
  • Later in 2005 IMAGE apocenter towards southern
    pole.
  • Perigee-Apogee combinations essential for
    detailed information on upper atmospheric
    interactions.
  • Ring current see effects of magnetospheric
    E-fields? in-situ measurements (E-fields and
    particles) essential. Also for intercalibrating
    DSP/NUADU and IMAGE/HENA.
  • Third (and fourth) conjunction with TWINS. Launch
    in 2003.

26
LAUNCH END OF 2003?
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29
R1 HIGH CONDUCTIVITY R2 LOW CONDUCTIVITY Sp
HIGH, SH LOW ? NORTHWARD E-FIELDS WE THINK.
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