Chihiro Tao [1,2], Fouad Sahraoui [2], Dominique Fontaine [2], Judith de Patoul [2,3], Thomas Chust[2], Satoshi Kasahara [4], and Alessandro Retinò [2]

Slides:



Advertisements
Similar presentations
Statistical Properties of Broadband Magnetic Turbulence in the Reversed Field Pinch John Sarff D. Craig, L. Frassinetti 1, L. Marrelli 1, P. Martin 1,
Advertisements

Masuda Flare: Remaining Problems on the Looptop Impulsive Hard X-ray Source in Solar Flares Satoshi Masuda (STEL, Nagoya Univ.)
The Johns Hopkins University Applied Physics Laboratory SHINE 2005, July 11-15, 2005 Transient Shocks and Associated Energetic Particle Events Observed.
The Radial Variation of Interplanetary Shocks C.T. Russell, H.R. Lai, L.K. Jian, J.G. Luhmann, A. Wennmacher STEREO SWG Lake Winnepesaukee New Hampshire.
Session A Wrap Up. He Abundance J. Kasper Helium abundance variation over the solar cycle, latitude and with solar wind speed Slow solar wind appears.
Plasmas in Space: From the Surface of the Sun to the Orbit of the Earth Steven R. Spangler, University of Iowa Division of Plasma Physics, American Physical.
Seminar S 3, IMPRS, MPAeJanuary 9, 2003 N. Krupp Planetary Magnetospheres: Global Configuration and Dynamics of the Jovian Magnetosphere N. Krupp Solar.
Paul T.M. Loto’aniu 1,2 and H.J. Singer 1 NOAA Space Environment Center 1 CIRES, University of Colorado 2 Paul T.M. Loto’aniu 1,2 and H.J. Singer 1 NOAA.
Low-Frequency Waves Excited by Newborn Interstellar Pickup Ions H + and He + at 4.5 AU Charles W. Smith, Colin J. Joyce, Philip A. Isenberg, Neil Murphy,
Magnetopause flow vortices revealed during high speed solar wind streams Mona Kessel (NASA GSFC), Yaireska Collado-Vega (University of Puerto Rico), Xi.
Comparing the solar wind-magnetosphere interaction at Mercury and Saturn A. Masters Institute of Space and Astronautical Science, Japan Aerospace Exploration.
Solar wind interaction with the comet Halley and Venus
Solar Flare Particle Heating via low-beta Reconnection Dietmar Krauss-Varban & Brian T. Welsch Space Sciences Laboratory UC Berkeley Reconnection Workshop.
Or A Comparison of the Magnetospheres between Jupiter and Earth.
Reinisch_ Solar Terrestrial Relations (Cravens, Physics of Solar Systems Plasmas, Cambridge U.P.) Lecture 1- Space Environment –Matter in.
Solar system science using X-Rays Magnetosheath dynamics Shock – shock interactions Auroral X-ray emissions Solar X-rays Comets Other planets Not discussed.
Non-collisional ion heating and Magnetic Turbulence in MST Abdulgader Almagri On behalf of MST Team RFP Workshop Padova, Italy April 2010.
Tuija I. Pulkkinen Finnish Meteorological Institute Helsinki, Finland
Benoit Lavraud CESR/CNRS, Toulouse, France Uppsala, May 2008 The altered solar wind – magnetosphere interaction at low Mach numbers: Magnetosheath and.
Stuart D. BaleFIELDS iCDR – Science Requirements Solar Probe Plus FIELDS Instrument CDR Science and Instrument Overview Science Requirements Stuart D.
The Sun and the Heliosphere: some basic concepts…
1 Mirror Mode Storms in Solar Wind and ULF Waves in the Solar Wind C.T. Russell, L.K. Jian, X. Blanco-Cano and J.G. Luhmann 18 th STEREO Science Working.
1 Origin of Ion Cyclotron Waves in the Polar Cusp: Insights from Comparative Planetology Discovery by OGO-5 Ion cyclotron waves in other planetary magnetospheres.
Stuart D. BaleFIELDS iPDR – Science Requirements Solar Probe Plus FIELDS Instrument PDR Science and Instrument Overview Science Requirements Stuart D.
SPATIAL AND TEMPORAL MONITORING OF THE INTERMITTENT DYNAMICS IN THE TERRESTRIAL FORESHOCK Péter Kovács, Gergely Vadász, András Koppán 1.Geological and.
Space Research Institute Graz Austrian Academy of Sciences CERN, Geneve, June 2006 Helmut O. Rucker Exploring the Planets and Moons in our Solar System.
Cusp turbulence as revealed by POLAR magnetic field data E. Yordanova Uppsala, November, 2005.
9 May MESSENGER First Flyby Magnetospheric Results J. A. Slavin and the MESSENGER Team BepiColombo SERENA Team Meeting Santa Fe, New Mexico 11 May.
Large-Amplitude Electric Fields Associated with Bursty Bulk Flow Braking in the Earth’s Plasma Sheet R. E. Ergun et al., JGR (2014) Speaker: Zhao Duo.
1 Mars Micro-satellite Mission Japanese micro-satellite mission to Mars to study the plasma environment and the solar wind interaction with a weakly-magnetized.
Space Science MO&DA Programs - September Page 1 SS It is known that the aurora is created by intense electron beams which impact the upper atmosphere.
The role of the magnetodisk in the Jupiter's Magnetosphere Igor I. Alexeev 2MS3, 14:20-14:40 October 13th, 2011, SRI, Moscow1.
Why Solar Electron Beams Stop Producing Type III Radio Emission Hamish Reid, Eduard Kontar SUPA School of Physics and Astronomy University of Glasgow,
1 Multi-spacecraft, multi-scale investigation of intermittency and multifractal structure of turbulence in the terrestrial magnetosheath M. Echim (1,2),
Voyager 2 Observations of Magnetic Waves due to Interstellar Pickup Ions Colin J. Joyce Charles W. Smith, Phillip A. Isenberg, Nathan A. Schwadron, Neil.
A generic description of planetary aurora J. De Keyser, R. Maggiolo, and L. Maes Belgian Institute for Space Aeronomy, Brussels, Belgium
Earth’s Magnetosphere NASA Goddard Space Flight Center
Turbulence in the magnetosphere studied with CLUSTER data : evidence of intermittency Lamy H. 1, Echim M. 1,2, Darrouzet F. 1, Lemaire J. 3, Décréau P.
Kinetic Alfvén turbulence driven by MHD turbulent cascade Yuriy Voitenko & Space Physics team Belgian Institute for Space Aeronomy, Brussels, Belgium.
A. Vaivads, M. André, S. Buchert, N. Cornilleau-Wehrlin, A. Eriksson, A. Fazakerley, Y. Khotyaintsev, B. Lavraud, C. Mouikis, T. Phan, B. N. Rogers, J.-E.
1 Hybrid Simulations of the Callisto - Magnetosphere Interaction Stas Barabash and Mats Holmström Swedish Institute of Space Physics, Kiruna, Sweden.
Dec 1, FIELDS Top Level Requirements Review S. Harris (UCB)
Intermittency Analysis and Spatial Dependence of Magnetic Field Disturbances in the Fast Solar Wind Sunny W. Y. Tam 1 and Ya-Hui Yang 2 1 Institute of.
NASA NAG Structure and Dynamics of the Near Earth Large-Scale Electric Field During Major Geomagnetic Storms P-I John R. Wygant Assoc. Professor.
-1- Solar wind turbulence from radio occultation data Chashei, I.V. Lebedev Physical Institute, Moscow, Russia Efimov, A.I., Institute of Radio Engineering.
Global Structure of the Inner Solar Wind and it's Dynamic in the Solar Activity Cycle from IPS Observations with Multi-Beam Radio Telescope BSA LPI Chashei.
Satellites and interactions
RPWI Team Meeting, Sep. 2010, Roma Magnetic Loop Antenna (MLA) Scientific Objectives A. Marchaudon, V. Krasnoselskikh, T. Dudok de Wit, C. Cavoit,
Magnetic reconnection in the magnetotail: Geotail observations T. Nagai Tokyo Institute of Technology World Space Environment Forum 2005 May 4, 2005 Wednesday.
The Suprathermal Tail Properties are not well understood; known contributors Heated solar wind Interstellar and inner source pickup ions Prior solar and.
Stuart D. BaleFIELDS SOC CDR – Science Requirements Solar Probe Plus FIELDS SOC CDR Science and Instrument Overview Science Requirements Stuart D. Bale.
Inherent Length Scales and Apparent Frequencies of Periodic Solar Wind Number Density Structures Nicholeen Viall 1, Larry Kepko 2 and Harlan Spence 1 1.
Turbulence in the Solar Wind
Jupiter’s 2-D Magnetosphere- Ionosphere-Thermosphere coupling model Chihiro Tao 1,2, Michel Blanc 1 1. IRAP, Univ. de Toulouse/UPS-OMP/CNRS 2. now at NICT.
MULTI-INSTRUMENT STUDY OF THE ENERGY STEP STRUCTURES OF O + AND H + IONS IN THE CUSP AND POLAR CAP REGIONS Yulia V. Bogdanova, Berndt Klecker and CIS TEAM.
Particle precipitation has been intensely studied by ionospheric and magnetospheric physicists. As particles bounce along the earth's magnetic fields they.
HISAKI mission – ひさき – Chihiro Tao 1,2, Nicolas Andre 1, Hisaki/EXCEED team 1. IRAP, Univ. de Toulouse/UPS-OMP/CNRS 2. now at NICT
Solar Wind Propagation Tool Chihiro Tao 1,2, Nicolas Andre 1, Vincent Génot 1, Alexis P. Rouillard 1, Elena Budnik 1, Arnaud Biegun 1, Andrei Fedorov 1.
SEPT/STEREO Observations of Upstream Particle Events: Almost Monoenergetic Ion Beams A. Klassen, R. Gomez-Herrero, R. Mueller-Mellin and SEPT Team, G.
ASEN 5335 Aerospace Environments -- Magnetospheres 1 As the magnetized solar wind flows past the Earth, the plasma interacts with Earth’s magnetic field.
1 CSSAR Center for Space science and Applied Research Chinese academy of Sciences FAC in magnetotail observed by Cluster J. K. Shi (1), Z. W. Cheng (1),
Multi-Fluid/Particle Treatment of Magnetospheric- Ionospheric Coupling During Substorms and Storms R. M. Winglee.
R. Maggiolo 1, M. Echim 1,2, D. Fontaine 3, A. Teste 4, C. Jacquey 5 1 Belgian Institute for Space Aeronomy (IASB-BIRA); 2 Institute.
Earth’s Magnetosphere Space Weather Training Kennedy Space Center Space Weather Research Center.
Exploring reconnection, current sheets, and dissipation in a laboratory MHD turbulence experiment David Schaffner Bryn Mawr College Magnetic Reconnection:
A Global Hybrid Simulation Study of the Solar Wind Interaction with the Moon David Schriver ESS 265 – June 2, 2005.
Modulation of chorus wave intensity by ULF waves from Van Allen Probes Observation Lunjin Chen 1, Zhiyang Xia 1, Lei Dai 2 1 Physics Dept., The University.
ARTEMIS – solar wind/ shocks
Third-Moment Descriptions of the Interplanetary Turbulent Cascade, Intermittency, and Back Transfer Bernard J. Vasquez1, Jesse T. Coburn1,2, Miriam A.
Richard B. Horne British Antarctic Survey Cambridge UK
Presentation transcript:

Chihiro Tao [1,2], Fouad Sahraoui [2], Dominique Fontaine [2], Judith de Patoul [2,3], Thomas Chust[2], Satoshi Kasahara [4], and Alessandro Retinò [2] [1] IRAP, CNRS/OMP/Université de Toulouse, France [2] LPP, CNRS/Ecole Polytechnique, France [3] EMPS/CGAFD, University of Exeter, UK [4] ISAS, JAXA, Japan Characteristics of Jupiter's magnetospheric turbulence observed by Galileo STORM2015, Constanta, Romania, 2015/9/6-12 International Workshop and School on Solar system plasma turbulence, intermittency and multifractals

1. Intro. Turbulence and Space Plasma [Bourouaine et al., 2012] (for fluid) *Turbulence is a ubiquitous phenomenon seen both in fluid and plasma *Turbulence couples multi-scales *Space plasma in various regions provides various parameters solar wind -- planetary environment 2

1. Intro.: Jovian magnetosphere solar wind Jovian magnetosphere Io plasma torus current sheet magnetic field Io plasma torus 3 lobe Rotation-dominant, energetic particle accelerator ・Fast rotation (9h55m) ・Strong magnetic field (momentum x20,000 Earth’s) ・Plasma source at Io locating inner magnetosphere  Sulfur ion, Oxygen ion, …, Proton  Plasma rotate in the vast magnetosphere region ・Planetary magnetosphere would provides turbulence under unique environment with parameters (e.g., Jupiter magnetosphere 0.01<β<1000) + dawn-dusk asymmetry (rot. + solar wind)

1. Intro.: Jovian magnetosphere Voyager data [Glassmeier, 1995] Galileo data [Saur et al., 2002, 2003] “Turbulence-like field fluctuations” in the Jovian magnetosphere ◆ less resonant peak  turbulence is dominant feature and a good index of activity ◆ spectral index ~ -5/3 [Glassmeier, 1995] ◆ small δb/B 0 & index~2 at the inner magnetosphere (< 26 R J ), [Saur et al., 2002] cf. solar wind δb/B 0 ~1 Effect of turbulence on ◆ heating the expanding plasma from Io [Saur et al., 2004] ◆ electric potential drop which accelerates electrons & create Jovian aurora [Saur et al., 2003] Power at 2.4 mHz [nT 2 /Hz] 4 P(f) ∝ f –5/3 aurora

1. Intro.: Motivation of this study Fig. Spectral power of 1 hour interval at 20 R J [Saur et al., 2002] Previous works used low time-resolution data in the limited radial distance and time. Questions: (1) Spectral feature, existence of break point? (2) How turbulence feature varies in global various region? (3) Relation between turbulence characteristics and magnetospheric phenomena? (4) Comparison among different planetary magnetospheres We use high time-resolved magnetometer data observed by Galileo  Characterize Jovian magnetospheric turbulence feature and its relation with magnetospheric dynamics 5

2. Data set : Galileo Jovian magnetospheric orbiter Dec Sep covering many radial and local time (LT) magnetopause bow shock [Khurana and Schwarz, 2005] 6

2. Data set : MAG data Galileo in the magnetosphere MAG: flux gate magnetometer [e.g., Kivelson et al., 1992] High resolution (HR) data : moon flyby: 24 events (not used in this study) magnetosphere: 23  11 events (above noise level) Δt~0.33 sec., min. Low resolution (LR) data : Δt~24 sec.  June 23, 1996 – Nov. 11, Wavelet analysis (using Morlet function) LR/HR obs. plasma obs. Spectra

3. Analysis: Spectrum (ex.1997/07/04 14:09) Low resolution data High resolution data 8 Br BθBθ BΦBΦ |B| Br BθBθ BΦBΦ Wavelet analysis B-perpen. B-aligned

4. Spectrum: over view (HR+LR) Fig. An example of spectrum from HR and LR data breaking frequency spectral index -Spectral break is seen at ~0.01 Hz in both LR and HR data -Spectral index is 1.3 (2.4) at lower (higher) frequency range -B // (B ⊥ ) is dominant at lower (higher) frequency range 9 Radial distance 64.6 RJ

3. Analysis: Plasma parameters Characteristic plasma parameters -ion cyclotron frequency (fci) -ion inertial length (di) -ion gyro-radius (ρi) -plasma beta (βi)  From ion inertia length and ion gyro-radius, corresponding characteristic frequencies are obtained as follows by Taylor Assumption: -ion inertial length (fdi) -ion gyro-radius (fρi) Magnetic field : directly observed value Ion density and temperature : -If data exists: PLS [Frank et al., 1992] observation -If not: refer to an empirical model [Bagenal and Delamere, 2011]. Energetic particle profile based on EPD observation [e.g., Mauk et al., 2004] is added. Fig. Observed and modeled radial profiles of density (upper) and temperature (lower) radial profiles [Bagenal and Delamere, 2011] GLL Observation 10

4. Spectrum: intermittency 11 Br BθBθ BΦBΦ |B| Intermittency  dissipation self- similary or not δB ≡ δB(t+τ)-δB(t) S m (τ)= ∝ τ ξ(m) m: order S m (τ): structure function Intermittent feature is seen in the inertial frequency range of current sheet less in the lobe

HR events #Start timeGalileo (x,y,z) JSE [RJ]R [RJ]LT [h]βindex 1index /06/30 02:00(-25.9, 8.57, 0.186) /09/11 02:38(-39.2, 1.5, -0.22) /03/30 18:49(-14.7, -43.9, ) /05/06 13:00(-0.2, -25.3, -0.38) /08/23 14:07(-125.8, -31.9, -0.52) /07/04 14:09(-56.6, 30.9, -0.12) /07/28 13:50(-0.7, 18.2, -0.04) /05/03 15:59(8.5, -3.8, -0.02) /07/01 23:52(3.6, -6.9, 0.00) /11/03 15:27(17.2, 23.5, -0.29) /11/04 21:48(2.4, 9.9, -0.12) events (of 23) with power well above the “minimum” level

4. Spectrum : spectral index Spectral index for f < fb for f > fb Histogram of spectral index 13 Spectra from LR and HR data

4. Spectrum: break point Spectral breaking frequency is -close to frequency at ion inertial length and gyro radius Spectra from LR and HR data Ion characteristic (x-axis) and break frequencies (y-axis) 14

4. Spectrum: small spectral index Spectra from LR and HR data Small slope events Small slope cases are seen in the dawnside observations ■ slope >1.36 ■ slope <

LR/HR obs. plasma obs. 5. Statistical analysis Galileo in the magnetosphere Low resolution (LR) data : Δt~24 sec.  June 23, 1996 – Nov. 11, 2002 *Separate current sheet & lobe (automatically) Fig. An example of CS/lobe separation 16 |B| [nT] Br [nT]

17 x-axis: frequencynormalized by fci normalized by fρi normalized by fdi 5. Statistics: Radial dependence [Bourouaine et al., 2012] LF α HF α (for fluid) -Most concentration of PSD by normalization with fci.

5. Statistics: Radial dependence 2 Radial distance [Rj] -Large deviation of flatness from Gaussian (=3) for plasma sheet case than lobe. -PSD is large in the plasma sheet with enhancement at ~50 R J and ~100 R J. -PSD enhancements at ~50 R J is seen in the duskside and ~100 R J in the dawnside. Plasma sheet lobe dawn dusk 18

6. Discussion 1. Dependence of the breakpoint frequency on the ion gyrofrequency, than ion scales (cf. Ion inertial scale for solar wind)  Possible role of ion cyclotron waves and resonance in the dissipation of magnetic energy into particle heating *There is also an ambiguity in the plasma data, model, and Taylor assumption  Expect to JUICE (future mission 2030-) (Intermittency at current sheet) > (Intermittency at lobe) This regional dependence is similar as seen in the Earth magnetotail [Weygand et al., 2005]  reflecting local structures (i.e., reconnection and resulting flow).

6. Discussion 3. Large total power in the duskside (dawnside) at 80 R J ) 4. Small spectral index at the dawnside is close to -1 in the “energy- containing scale” *Reconnection-like magnetic features is observed at these locations, while ion flow and density change is associated with those in the dawnside [Kasahara et al., 2013]. *Large slope variation in the low-frequency range is due to the magnetospheric dynamics, as suggested in the case of Saturn [von Papen et al., 2014]. 20 [Kasahara et al., 2013]

7. Summary and Conclusions We analyze Galileo/MAG high and low resolution data using a wavelet method. (1) Spectral feature, existence of break point? ★ We confirmed (at least) two spectral index. -- The spectral index is for lower and for higher range of break point. -- Spectrum break is close to frequency at ion gyrofrequency and ion scales. (2) How turbulence feature varies in global various region? ★ The turbulence power and intermittency is strong in the plasma sheet than lobe. ★ The power enhances at ~50 R J at the duskside and ~100 R J at the dawnside. (3) Relation between turbulence characteristics and magnetospheric phenomena? ★ Dawn-dusk asymmetries of PSD radial profile and slope at “energy-containing scales” would be related with magnetospheric reconnection and ion flow features. statistical distribution so far.  event study? (4) Comparison among different planetary magnetospheres ★ Dominance of intermittency in the plasma sheet is the same with Earth. ★ Spectral feature is due to plasma parameter. Detail  accurate obs. by JUICE etc. Tao et al., Properties of Jupiter’s magnetospheric turbulence observed by the Galileo spacecraft, J. Geophys. Res. Space Physics,