1. Fate of cold ions in the inner magnetosphere: energization and drift inferred from morphology and mass dependence M. Yamauchi 1, I. Dandouras 2, H. Reme 2, Y. Ebihara 3 (1) Swedish Institute of Space Physics (IRF), Kiruna, Sweden (2) CNRS and U. Toulouse, IRAP, Toulouse, France (3) Kyoto University, Uji, Japan Geospace2014@Rhodos, 2014-9-17 1

2. North-south symmetry of trapped particle motion for fixed MLT ⇒ inbound-outbound asymmetry = temporal change of 1-2 hour a zoo of various patterns 2

3. Decay in time partly came from rapid degradation of the sensor Cluster Statistics 3

4. (a) Vertical stripes: Nearly vertical in the spectrogram, extending from the about 10 keV to sub-keV (dispersion is very weak). Only found near midnight during substorms. Mostly inbound-outbound asymmetric (life time~1h), indicating substorm injection. (b) Wedge-like energy-latitude dispersed sub-keV ions: Stronger dispersion than (a), at slightly lower energy (up to few keV). Often found in the morning to noon sectors some hours after a substorm. Often inbound-outbound asymmetric, but can yet be explained by ion drift (next figure) of <0.1 keV ion source. (c) Short bursts of low-energy ions: a peak energy flux less than 100 eV but not thermal. Found all local time without clear relation to geomagnetic activities. Often inbound-outbound asymmetric (life time~1h), indicating a local phenomena. (d) Warm trapped ions confined near equator: tens eV to a few hundred eV without dispersion. Found all local time without clear relation to geomagnetic activities. Comparison to different SC indicates life time~1h, indicating a local phenomena. 4

5. Comparison of observation and ion drift simulation. 0.1 keV t ≈ 6 hr t ≈ 4 hr Cool source (<0.1 keV, but not cold) can cause wedge-like dispersed sub-keV ions with its inbound-outbound asymmetry even at noon, and hot source can cause ion band (keV). Due to different drift velocity, two population has different O/H ratio. 5

6. Next: O + /H + and He + /H + differences (a) Vertical stripes Appearances of H +, He +, and O + are not correlated types (a)-(c) 2001-2006 (~300 relatively clean data out of ~760 traversals) 6

7. (b) Wedge-like energy-latitude dispersed ions Timing & energy are quite different among H +, He +, and O + (drift theory predicts same energy-time diagram for all species). 7

8. (c) Short bursts of low- energy ions: Unlike most H + bursts, He + bursts (time scale~1h) are in perpendicular direction. It is also independent from O +, indicating local heating of He + only. (d) Warm trapped ions confined near equator Equatorially-confined hot ions sometime show E(H + ) < E(He + ) while majority is E(H + ) = E(He + ). 8

9. Conclusions & Future Observations There must be filtering mechanisms that select only cold He + and separates them from H + and O + for both energization and transportation. We need more investigation on Mass dependency  Nitrogen Ion TRacing Observatory (NITRO) for next ESA's M-class call Sprinter meeting: Saturday 11:30-16:00 (after coffee break) 9

10. In-situ spacecraft start with 6-7 Re apogee outside the radiation belts during the first 2 years, and then gradually decrease the apogee altitude to explorer the “dangerous” region. Monitoring satellite flies just above the polar ionosphere at altitude ~2000 km. 3-spacecraft mission (high inclination) North In-situ (spinning) Cold ion mass spectrometer Hot ion (3~4 different types) Energetic ions Photoelectron Magnetometer+Waves (Ω N ) Langmuir Probe (plus alpha) UV/visible (narrow FOV) IR (narrow FOV) Cold ion mass spectrometer Hot ion mass analyser Photolectron Magnetometer Langmuir Probe (plus alpha) South FOV Imaging (3-axis) & monitoring Daughter (gradient) 10

11. In-situ #1 mother (spinning) * Mass spectrometer (cold) (Bern) * Ion analyzers (0.03 – 30 keV): (1) Narrow mass range (Kiruna) (2) Wide mass range (Toulouse) (3) No mass (LPP) (4) low G-factor mass (Japan) * Ion mass analyzer (> 30 keV) (UNH) * Electron (photoelectron) (London) * Magnetometer (Graz) * Waves (Ω N ≠Ω O ) (Prague) * Langmuir Probe (Brussels) * ENA monitoring substorm (Berkeley) * (Potential Control=SC subsystem) Payloads Remote sensing & monitoring (3-axis) * Optical (emission) (LATMOS & Japan) (1) N + : 91 nm, 108 nm (2) N 2 + : 391 nm, 428 nm (3) NO + : 123-190 nm, 4.3 µm (4) O + : 83 nm, 732/733 nm * Mass spectrometer (cold) (Goddard) * Ion analyzer (< 0.1 keV) (Kirina) * Electron (photoelectron) (London) * Langmuir Probe (Brussels) * Ionospheric sounder (Iowa) * Magnetometer (Graz/UCLA) * Waves (Ω N ≠Ω O ) (Prague) * Ionospheric optical emission (???) Optical imager needs a scanner keep in- situ spacecraft within FOV. * underline: core, * colored: important, * black: optional Possible methods for ion analyzers: Magnet, Magnet-TOF, reflection-TOF, MCP-MCP TOF, shutter-TOF 11

12. Yamauchi, et al. (2012), GRL, doi:10.1029/2012GL052366. Yamauchi, et al. (2013), AnnGeo, doi:10.5194/angeo-31-1569-2013. Yamauchi, et al. (2014), AnnGeo, doi:10.5194/angeo-32-83-2014. Yamauchi, et al. (2014), JGR, doi:10.1002/2013JA019724. End 12

13. Next: O + /H + and He + /H + differences (a) Vertical stripes Appearances of H +, He +, and O + are not correlated types (a)-(c) 2001-2006 (~300 relatively clean data out of ~760 traversals) 13

14. (b) Wedge-like energy-latitude dispersed ions p/a < 45° p/a ≈ 90° cf. drift theory predicts same energy-time diagram for all species 14

15. (c) Short bursts of low-energy ions: Unlike majority of H + bursts, He + bursts are mostly in perpendicular direction and time scale ~ 1h. Even independent from O +, indicating local heating of He + only. 15

16. (d) Warm trapped ions confined near equator equator Equatorially-confined hot ions sometime show E(H + ) < E(He + ) while majority is E(H + ) = E(He + ). He+ is certainly heated e.g. by He cyclotron waves (1980’s) 16