Statistical study of non-reconnection plasma jets as observed by the DOUBLE STAR spacecraft E. Amata 1, S. Savin 2, D. Ambrosino 1, L. Trenchi 1, M.F.

Slides:



Advertisements
Similar presentations
SuperDARN is a network of HF radars (8-20 MHz) used to study the convection in the Earth's ionosphere at altitudes between 90 and 400 km and at magnetic.
Advertisements

Generation of the transpolar potential Ramon E. Lopez Dept. of Physics UT Arlington.
Anti-Parallel Merging and Component Reconnection: Role in Magnetospheric Dynamics M.M Kuznetsova, M. Hesse, L. Rastaetter NASA/GSFC T. I. Gombosi University.
Cluster, THEMIS, & Geotail Conjunction Event on 11 July 2008 Hiroshi Hasegawa ISAS/JAXA.
Formation of the Magnetosphere 1 Solar Wind. Formation of the Magnetosphere 2 Solar Wind Bow Shock Magnetosheath.
E. Amata M. Candidi (1), M.F. Marcucci (1), S. Massetti (1), P. Francia (3), U. Villante (3) (1) Istituto di Fisica dello Spazio Interplanetario (IFSI),
Near-Earth Magnetotail Reconnection and Plasmoid Formation in Connection With a Substorm Onset on 27 August 2001 S. Eriksson 1, M. Oieroset 2, D. N. Baker.
The role of solar wind energy flux for transpolar arc luminosity A.Kullen 1, J. A. Cumnock 2,3, and T. Karlsson 2 1 Swedish Institute of Space Physics,
Weaker Solar Wind Over the Protracted Solar Minimum Dave McComas Southwest Research Institute San Antonio, TX With input from and thanks to Heather Elliott,
SuperDARN interhemispheric observations of reconnection signatures: a case study. Coco, I. (1), S. Massetti (1), E. Amata (1), M. F. Marcucci (1), and.
Anti-parallel versus Component Reconnection at the Magnetopause K.J. Trattner Lockheed Martin Advanced Technology Center Palo Alto, CA, USA and the Polar/TIMAS,
SuperDARN Workshop May 30 – June Magnetopause reconnection rate and cold plasma density: a study using SuperDARN Mark Lester 1, Adrian Grocott 1,2,
Five Spacecraft Observations of Oppositely Directed Exhaust Jets from a Magnetic Reconnection X-line Extending > 4.3 x 10 6 km in the Solar Wind Gosling.
Solar wind interaction with the comet Halley and Venus
Phase Coherence on Open Field Lines Associated with FLRs Abiyu Nedie, Frances Fenrich & Robert Rankin University of Alberta Edmonton, Alberta, Canada 2011.
OpenGGCM Simulation vs THEMIS Observations in an Dayside Event Wenhui Li and Joachim Raeder University of New Hampshire Marit Øieroset University of California,
O. M. Shalabiea Department of Physics, Northern Borders University, KSA.
In-situ Observations of Collisionless Reconnection in the Magnetosphere Tai Phan (UC Berkeley) 1.Basic signatures of reconnection 2.Topics: a.Bursty (explosive)
Location of the High-Latitude Reconnection Site on 14 February 2003 S. Eriksson 1, M. M. Kuznetsova 2, M. W. Dunlop 3, and H. Reme 4 1 LASP, University.
Solar system science using X-Rays Magnetosheath dynamics Shock – shock interactions Auroral X-ray emissions Solar X-rays Comets Other planets Not discussed.
Swedish National Graduate School of Space Technology Cluster multi-spacecraft measurements: applications on transition layer development and location of.
Plasma in the Heliosheath John Richardson M.I.T. Collaborators: J. Belcher, J. Kasper, E. Stone, C. Wang.
Observation and Theory of Substorm Onset C. Z. (Frank) Cheng (1,2), T. F. Chang (2), Sorin Zaharia (3), N. N. Gorelenkov (4) (1)Plasma and Space Science.
1 Dynamic Motion of Bow Shock and Magnetopause Observed by THEMIS Hui Zhang (BU) Q.-G. Zong (Umass Lowell) D. G. Sibeck (GSFC) T. A. Fritz (BU)
Solar System Physics Group Grande et al, Venus, RAS 2010 Solar wind interactions and Ionospheric loss mechanisms at Venus M Grande, A G Wood, I C Whittaker,
Hamrin, M., Norqvist, P., Marghitu, O., et al. Department of Physics, Umeå University, Sweden Nordic Cluster.
What DMSP Data Tell us About the Thermosphere Response to Solar Wind Forcing Delores Knipp CU Aerospace Engineering Sciences and NCAR HAO With Assistance.
Benoit Lavraud CESR/CNRS, Toulouse, France Uppsala, May 2008 The altered solar wind – magnetosphere interaction at low Mach numbers: Magnetosheath and.
A TMOSPHERIC, O CEANIC AND S PACE S CIENCES UNIVERSITY of MICHIGAN Daniel J. Gershman, James A. Slavin, Jim M. Raines, Thomas H. Zurbuchen, Brian J. Anderson,
Structure and Detection of Rolled-up Kelvin-Helmholtz Vortices in the Tail Flank of the Magnetosphere H. Hasegawa, M. Fujimoto, T. K. M. Nakamura, K. Takagi.
1 Cambridge 2004 Wolfgang Baumjohann IWF/ÖAW Graz, Austria With help from: R. Nakamura, A. Runov, Y. Asano & V.A. Sergeev Magnetotail Transport and Substorms.
SPATIAL AND TEMPORAL MONITORING OF THE INTERMITTENT DYNAMICS IN THE TERRESTRIAL FORESHOCK Péter Kovács, Gergely Vadász, András Koppán 1.Geological and.
Space Weather from Coronal Holes and High Speed Streams M. Leila Mays (NASA/GSFC and CUA) SW REDISW REDI 2014 June 2-13.
Space Research Institute Graz Austrian Academy of Sciences CERN, Geneve, June 2006 Helmut O. Rucker Exploring the Planets and Moons in our Solar System.
The Magnetopause Back in 1930 Chapman and Ferraro foresaw that a planetary magnetic field could provide an effective obstacle to the solar-wind plasma.
Response of the Polar Cusp and the Magnetotail to CIRs Studied by a Multispacecraft Wavelet Analysis Axel Korth 1, Ezequiel Echer 2, Fernando L. Guarnieri.
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.
Response of the Magnetosphere and Ionosphere to Solar Wind Dynamic Pressure Pulse KYUNG SUN PARK 1, TATSUKI OGINO 2, and DAE-YOUNG LEE 3 1 School of Space.
Reconstruction of Reconnection Configurations From Spacecraft Data Bengt Sonnerup and Wai-Leong Teh Dartmouth College, Hanover, NH, USA Hiroshi Hasegawa.
5. Walen Test analysis The Walen Test results for Cluster 3 are as expected for a reconnection event. The test over the leading edge shows a positive correlation.
Energy conversion at Saturn’s magnetosphere: from dayside reconnection to kronian substorms Dr. Caitríona Jackman Uppsala, May 22 nd 2008.
Earth’s Magnetosphere NASA Goddard Space Flight Center
Conjugate response of the dayside magnetopause and dawn/dusk flanks using Cluster-THEMIS conjunctions and Ground based observations M W Dunlop, Q-H. Zhang.
E.E. Antonova1,2, I.P. Kirpichev2,1, Yu.I. Yermolaev2
Observation of high kinetic energy density jets in the Earth’s magnetosheath E. Amata 1, S. P. Savin 2, R. Treuman 3, G. Consolini 1, D. Ambrosino, M.F.
Ionospheric Convection during an extended period of Northward IMF
Simultaneous in-situ observations of the feature of a typical FTE by Cluster and TC1 Zhang Qinghe Liu Ruiyuan Polar Research Institute of China
Cluster and SuperDARN observations during a positive B y period D. Ambrosino, E. Amata, M.F. Marcucci, I. Coco Istituto di Fisica dello Spazio Interplanetario,
Space Weather in Earth’s magnetosphere MODELS  DATA  TOOLS  SYSTEMS  SERVICES  INNOVATIVE SOLUTIONS Space Weather Researc h Center Masha Kuznetsova.
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.
17th Cluster workshop Uppsala, Sweden , May 12-15, 2009
Compressibility and scaling in the solar wind as measured by ACE spacecraft Bogdan A. Hnat Collaborators: Sandra C. Chapman and George Rowlands; University.
A shock is a discontinuity separating two different regimes in a continuous media. –Shocks form when velocities exceed the signal speed in the medium.
Magnetic reconnection in the magnetotail: Geotail observations T. Nagai Tokyo Institute of Technology World Space Environment Forum 2005 May 4, 2005 Wednesday.
Shock heating by Fast/Slow MHD waves along plasma loops
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.
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.
Earth’s Magnetosphere Space Weather Training Kennedy Space Center Space Weather Research Center.
What influence the low-latitude boundary layer formation?
Lecture 12 The Importance of Accurate Solar Wind Measurements
Global MHD Simulations of Dayside Magnetopause Dynamics.
THEMIS multi-spacecraft observations of a 3D magnetic
Effects of Dipole Tilt Angle on Geomagnetic Activities
The Bow Shock and Magnetosheath
THEMIS SWG, Annapolis, Sept. 14, 2011 Supported by NSF grant #
H. Isobe, 2004/11/1, Taiyo zasshikai
THEMIS Dayside Lessons learned from the coast phase and the 1st dayside season Current plans for the 2nd dayside season and the extended phases.
Richard B. Horne British Antarctic Survey Cambridge UK
Presentation transcript:

Statistical study of non-reconnection plasma jets as observed by the DOUBLE STAR spacecraft E. Amata 1, S. Savin 2, D. Ambrosino 1, L. Trenchi 1, M.F. Marcucci 1 1) Istituto di Fisica dello Spazio Interplanetario, INAF, Roma, Italia 2) IKI RAN, Moscow, Russian Federation Istituto di Astrofisica e Planetologia Spaziali: IAPS

A vast literature has been produced in the last decades on the observation of accelerated jets close to the Earth’s magnetopause, which have been commonly ascribed to magnetic reconnection at the magnetopause between the magnetic field convected by the shocked solar wind and the magnetic field of the magnetosphere. Nemecek et al. (1998) described abrupt strong ion flux increases or decreases in the flank magnetosheath, which they called Transient Flux Events (TFE). Savin et al. (2008) presented observations of non reconnection jets, argued that such jets are accompanied by plasma super-diffusion and suggested that they are important for energy dissipation and plasma transport. Shue et al. (2009) presented an event during which a fast magnetosheath jet impinged on the subsolar magnetopause and produced an indentation of the magnetopause which resulted in the reflection of the jet so as to produce a sunward flow in the magnetosheath. Finally, non reconnection jets have been described by Amata et al. (2008), Hietala et al. (2009, 2011), Savin et al. (2011).

Outline Some examples: - Nemecek et al. - March 17, 2001, Cluster - March 2, 2004, Double Star - March 17, 2005, Cluster + Double Star Statistical study of DS jets Conclusions

Nemecek et al (GRL,1998) found a number of events, in the Interball data set, when unusually large flow fluxes were observed in the MSH. Transient Flux Enhancement: TFE. F (t) > 1.5 (t-5min,t) WIND ion flux. N ~ 6cm -3 ; V ~ 490 km/s WIND clock angle WIND M A I.Ball ion flux I.Ball mag. field v - At all latitudes of the flank MSH. - Steady solar wind flow. - Highly supercritical SW (M A >7). - Not correlated with magnetic field changes (thus, no link with the slow mode transitions reported by Song et al. [1992]).

Cluster SC1 (red lines) and ACE (black lines) magnetic field data. Cluster (HIA SC1) omni-directional ion energy spectrograms from 09:10 to 12:10 UT on March 17, IMP 8 (dots), WIND (blue solid line) and SC1 ion density (red line). SC1 T // (black line) and T ┴ (red line). Solar wind V x measured by IMP 8 (dots) and by ACE (solid line). Bulk ion kinetic energy density, measured by IMP 8 (dots), WIND (blue) and SC1 (red). SC1 magnetosonic Mach number.

Possible interaction of the A and B jets with the magnetopause (GSM XZ plane): -Shue et al., 1998, magnetopause (dashed curve), - deformed magnetopause (thin solid line), - jet peak velocity vectors, - Cluster orbit (solid thick line), - the H jet and the bow shock are also shown.

XZ GSE XY GSE March 17, 2005, Cluster + Double Star

ACE V z ~ -30 km/s ACE V x ~ -690 km/s

(km/s) DS VxDS VyDS VzCl VxCl VyCl Vz Jet MSH XZ GSEXY GSE MSH/Jet flow Angle Double Star Cluster 10° 14° W k_jet ~ 3. W k_MSH ~ 1.5 W k_SW β MSH β jet M ms_MSH M ms_jet D.Star Cluster

Outline Some examples: - Nemecek et al. - March 17, 2001, Cluster - March 2, 2004, Double Star - March 17, 2005, Cluster + Double Star Statistical study of DS jets Conclusions

Triggered bt the previous results, we decided to look at the whole DS data base. We identified jets in the DS MSH data in the period (winter and spring tiimes)

We considered all cases when Pdyn_msh > Pdyn_omni Alternatively, we considered all cases when Mms_msh > 1. The results I will describe in the following slides did not change.

Clock angle

Plasma data provided by the HIA were examined searching for high dynamic pressure plasma jets in the Earth’s magnetosheath (Pdyn > Pdyn_SW). The study was limited to portions of the spacecraft orbit such that the angle between the position vector in GSE and the Sun-Earth line was steadily below 20°. More than 500 such jets were identified. Therefore, we can suggest that such jets are a permanent feature of MSH dynamics. We found that: 1)such jets occur at all distances from the bow shock and from the magnetopause; suggesting that they are somehow generated at the bow shock and propagate in the MSH, 2)they are not due to magnetic reconnection; 3)about 1/3 of jets occur without changes in the solar wind conditions (TD, RD etc.); 4)they have Mms > Mms_msh: usually, Mms > 1. 5)no clear dependence is observed on the average IMF Bz component 6)no dependence is observed on the average IMF clock angle. 7)dependence on the average IMF Bx component to br further investigated. Further studies are required to fully explain the mechanism(s) by which they are generated Summary and conclusions