Using data from all four spacecraft during crossings of the outer cusp, I'll be examining electric field structures with scale sizes comparable to the satellite separation distance and larger. Particular attention will be paid to vorticity in the electric field, and to features where the measured divergence is not zero. I am expecting to have some initial results ready in time for the EGS meeting at the end of March.
Cluster instruments used: | EFW |
Time intervalls: |
Contact person: | cully@phys.ucalgary.ca | Chris Cully | ------------------------> Position in the EFW society: associate |
Further information can be found at: |
Project added 2001 - 2 - 23
We plan to use the CLUSTER wave observations to build global/statistical environmental models for the spatial distribution of VLF and ELF waves in the magnetosphere (mean intensities versus frequency, polarisation, propagation directions (!?), etc ...). These observations will be complemented with those from the DE mission already analysed at LPCE, Orleans, and Viking (currently under development at IASB).
Cluster instruments used: | WHISPER, STAFF, EFW, FGM |
Time intervalls: |
Contact person: | jl@oma.be & Fabien.Darrouzet@oma.be | Lemaire, J.F. & Fabien Darrouzet | ------------------------> Position in the EFW society: associate |
Further information can be found at: | http://www.magnet.oma.be/sevem/ |
Project added 2001 - 3 - 6
The electric field at the magnetopause is studied, in particular the tangential electric field. The field is put into the magnetopause frame of reference using the magnetopause geometrical characteristics and motion as determined from multi-spacecraft comparisons.
Cluster instruments used: | EFW, FGM, ...? |
Time intervalls: |
Contact person: | lindqvist@plasma.kth.se | Per-Arne Lindqvist | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 6
A search is done for large (> approx 100 mV/m) electric fields on auroral field lines. The relation to upward/downward field aligned current regions and auroral emissions is studied. Spatio-temporal characteristics are deduced from multi-spacecraft observations to discriminate between stationary structures and waves.
Cluster instruments used: | EFW, FGM, STAFF, ...? |
Intervall 1 | Intervall 2 | |
Time intervalls: | 2001-01-14 | 2001-01-18 |
Contact person: | lindqvist@plasma.kth.se | Per-Arne Lindqvist | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 6
Abstract submtitted to IAGA 2001: Field-line resonances are a direct consequence of the solar wind's interaction with a magnetized planet. They play a fundamental role in the coupling of the magnetosphere to the ionosphere. Initial results from multi-point observations by the Cluster spacecraft are presented. The emphasis is on the separation of temporal and spatial variations as well as on correlating the occurrence and characteristics of the resonances with the IMF.
Cluster instruments used: | EFW |
Time intervalls: |
Contact person: | blomberg@plasma.kth.se | Lars Blomberg | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 7
The s/c potential can provide high time resolution information about plasma density in solar wind, magnetosheath and inner magnetosphere/plasmasphere. In the plasmasheath and lobes and the outer cusp the spacecraft potential depends more on electron flux-this will require future calibrations with Cluster particle experiments.
Cluster instruments used: | WHISPER,CIS,PEACE,EFW |
Intervall 1 | |
Time intervalls: | many |
Contact person: | arne.pedersen@fys.uio.no | Arne Pedersen | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 7
Power conversion can be identified for selected crossings of the magnetopause where the current density is established from four Cluster s/c and EFW can observe a clear electric field direction in this current layer. Observation of magnetopause orientation and motion is important for transforming electric fields to the magnetopause reference frame.
Cluster instruments used: | EFW,FGM,CIS,PEACE |
Intervall 1 | |
Time intervalls: | Only preliminary looks;more specific later |
Contact person: | arne.pedersen@fys.uio.no | Arne Pedersen | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 7
By comparison of EFW data with flows from CIS, density from CIS, E-fields from EDI, etc., I will determine the quality, accuracy, and corrections for the EFW data. The corrections include a multiplying factor to account for the shorting of the field by the long, grounded, wire boom, an offset in the X-commponent of electric field, etc.
Cluster instruments used: | EFW, FGM, CIS, EDI, WHISPER |
Time intervalls: |
Contact person: | fmozer@ssl.berkeley.edu | Forrest Mozer | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 20
Comparisons of EFW determined electric fields with -VxB as determined from the FGM and CIS. These results will determine the effective antennae length.
Cluster instruments used: | EFW, CIS, FGM |
Time intervalls: |
Contact person: | fmozer@ssl.berkeley.edu | Forrest Mozer | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 3 - 24
In the March-May time frame Cluster measurements concentrate on the cusp and mantle. At the same time in many cases, Polar will be skimming the magnetopause near apogee within a few hours in local time. These measurements may be nearby in the cusp, nearer the nose of the magnetopause, or in the cusp and boundary layers in the opposite hemisphere. Combining these data sets will provide new tools to address questions such as high-latitude versus subsolar merging, pulsed verses continuous merging, and the formation of and the open/closed character of the boundary layers.
Cluster instruments used: | EFW, FGM, CIS, PEACE |
Intervall 1 | Intervall 2 | |
Time intervalls: | 2001.03.12.11.00.00.000 - 2001.03.12.13.00.00.000 | 2001.03.31.11.00.00.000 - 2001.03.31.18.00.00.000 |
Contact person: | nmaynard@mrcnh.com | Nelson Maynard | ------------------------> Position in the EFW society: co-i |
Further information can be found at: |
Project added 2001 - 4 - 4
To determine the power radiated from the tail in the form of low frequency electromagnetic waves and to assess its propagation down the field lines. Two point conjuctions with Geotail and POLAR spacecraft provide measurements of the Poynting flux at another altitude (other than Cluster's). IMAGE auroral oval images help place the events in global context.
Cluster instruments used: | EFW, FGM, CIS, PEACE |
Time intervalls: |
Contact person: | vassilis@ssl.berkeley.edu | Vassilis Angelopoulos | ------------------------> Position in the EFW society: other |
Further information can be found at: |
Project added 2001 - 4 - 12
I will study the density and electric field structure at the bow shock. I plan to compare the cross-shock potential with PEACE observations of electron heating. Part of this work will involve calculating shock speeds and thickness. I will also do a study of the (whistler?) turbulence observed in the layer.
Cluster instruments used: | EFW |
Time intervalls: |
Contact person: | bale@ssl.berkeley.edu | Stuart D Bale | ------------------------> Position in the EFW society: associate |
Further information can be found at: |
Project added 2001 - 4 - 13
It is shown in a statistical study using POLAR data that anisotropic midenergetic electrons correlate well with broadband waves (1-10 Hz). The wavemodes are still however unknown. By using CLUSTER data we hope to be able to classify the wavemodes and in more detail study a possible interaction between the electrons and the waves.
Cluster instruments used: | EFW,FGM,STAFF |
Intervall 1 | Intervall 2 | Intervall 3 | Intervall 4 | Intervall 5 | |
Time intervalls: | 2001.01.18.20.30.000-2001.01.18.21.10.000 | 2001.02.14.00.30.000-2001.02.14.01.10.000 | 2001.02.21.04.00.000-2001.02.21.04.20.000 | 2001.02.14.06.00.000-2001.02.14.06.30.000 | 2001.03.12.07.05.000-2001.03.12.07.40.000 |
Contact person: | ao@irfu.se | Annika Olsson | ------------------------> Position in the EFW society: associate |
Further information can be found at: | http://repo.irfu.se/~ao/ |
Project added 2001 - 4 - 18
We will carry out an investigation of the particle flows in the Earth's magnetosphere using ion plasma and ExB velocity measurements on the Cluster spacecraft. We hope to determine the accuracy with which these correlative observations can be made in order to set limits on the identification of non-MHD flows and boundary motions.
Cluster instruments used: | CIS, EFW |
Time intervalls: |
Contact person: | mcfadden@ssl.berkeley.edu | Jim McFadden | ------------------------> Position in the EFW society: associate |
Further information can be found at: |
Project added 2001 - 4 - 20
The Cluster quartet crosses the plasmasphere every ~2 days if the geomagnetic activity is not too high (in this case the plasmasphere may shrink to altitudes below L=4). The goal of this study is to detect and analyze the large fluctuations of the high resolution Spacecraft Potential, considered as a proxy of the electron density, measured by EFW near the plasmapause. The Whisper relaxation sounder data will be used as a complement below 100 e-/cc. From these data, different analysis tools will be used to check for the presence of 2-D MHD turbulence. This two-dimensional MHD turbulence could be produced by velocity shear at the flow separatrix which can be detected using the electric field data. The use of the 4 satellites facility will be used to look for spatial extension and temporal evolution of this turbulence. Finally, the relation between these large amplitude fluctuations and low frequency emissions observed by STAFF will be investigated.
Cluster instruments used: | EFW, WHISPER, STAFF |
Time intervalls: |
Contact person: | Arnaud.Masson@esa.int | Arnaud Masson | ------------------------> Position in the EFW society: associate |
Further information can be found at: |
Project added 2001 - 6 - 18
I intend to investigate the evolution and dispersion of electromagnetic wave packets with distance from the bow shock and turbulence at the shock (fpe Cluster instruments used: EFW, WHISPER, STAFF Intervall 1 Intervall 2 Time intervalls: 2001.01.24.02-09 2001.02.19.10-20.18 Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 7 - 5 We investigate waves by reconstructing the wave distribution function from observed power and cross spectra. We use data from two or more of the Cluster II spacecrafts to reconstruct the distribution of wave energy in k-space.
Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 8 - 27 Using a combination of electric field and particle data, the attributes
and regions of occurrence of Electron-Phase-Space-Holes (EPSH) will be
investigated and categorized, with particular attention to propagation and
possible generation regions and/or mechanisms. Boundary layers such as the shock transition region as well as the cusp, plasma sheet , and the boundary layer plasma sheet will be investigated for EPSH, possible sources, and evidence of propagation. Cluster instruments used: EFW,WBD, PEACE Intervall 1 Time intervalls: TBD Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2001 - 8 - 28 We are interested in studying the orientations, propagation speeds, thicknesses, and relative locations of electric field and density structures in the high-altitude auroral region, with the goal of understanding how the electric field and density structures are linked, and how the two together may control the mid-altitude auroral acceleration processes. Cluster instruments used: EFW Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 8 - 29 Simultaneous measurements by the Cluster satellites and ground-based auroral cameras and photometers, magnetometers and radars (especially EISCAT Mainland and Svalbard radars) from the auroral oval will be looked for. The four spacecraft will allow to study the extent and temporal characteristics of auroral cavities and electric field fluctuations. Additional information about FACs, particles and high frequency waves would be valuable. Cluster instruments used: EFW, FGM, PEACE,... ? Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 9 - 4 The electromagnetic ion cyclotron (EMIC) waves are among the most common waveforms in space, appearing in the different parts of the magnetosphere, magnetosheath and solar wind. The four Cluster satellites can give information about EMIC wave generation, their spatial extent, temporal development and propagation as well as their effects on particle populations.
Cluster instruments used: EFW, STAFF, FGM, CIS...? Time intervalls: Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2001 - 9 - 4 We are studying the polarization, dispersive, propagation and poynting flux characteristics of low frequency Alfvénic and broadband ELF emissions (<300 Hz) within the auroral zone (including cusp). We will relate these emissions to current and density structures and look for the origin of these emission. Furthermore we hope to relate the observations to lower-altitude auroral acceleration processes.
(Yes, we are in contact with John Bonnell) Cluster instruments used: EFW, STAFF, FGM, CIS, PEACE Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 9 - 10 Utilizing Image and DMSP data to identify theta aurora (transpolar arcs) we will use Cluster to identify the magnetotail signatures associated with the TPAs. Cluster instruments used: EFW Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2001 - 9 - 20 To use FAST and Cluster s/c to the propagation of Alfven waves in the near Earth magnetotail and cusp into the auroral oval. In this study observations from FAST and Cluster of Alfven waves and electron accleration will be compared and simulated to develop a model for energy transport by these waves in the high latitude magnetosphere Cluster instruments used: EFW, Peace, Cis, FGM Intervall 1 Time intervalls: 2001/01/1-2003/01/1 Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2002 - 1 - 10 The electric field and potential structure of Short Large Amplitude Magnetic Structures (SLAMS) at the Earth´s quasi-parallel bow shock is studied. Cluster instruments used: EFW, FGM Intervall 1 Intervall 2 Time intervalls: 2001.02.02.20.50.00 - 2001.02.02.21.00.00 2001.03.12.14.50.00 - 2001.03.12.15.00.00 Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 1 - 14 We will seek observational evidence for magnetosheath plasma inside the magnetopause that is flowing sunward on magnetic field lines that map to low-altitude regions of sunward lobe cell convection and investigate whether particle precipition in these regions may cause signatures of transpolar aurora Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 4 - 3 We are examining the response of the magnetosphere to pressure pulses, including the excitation of low frequency MHD waves and changes in the convection. In some cases, the waves are observed by Polar with Cluster as an upstream monitor in the magnetosheath. In some cases, the prime observations are on Cluster. This study uses the electric field, spacecraft potential and ExB velocities Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2002 - 4 - 4 We are studying the waveform capture observations made through out the magnetosphere. Our prime focus are waveforms in the magnetotail and low altitude plasma sheet. We are making comparisons with both plasma sheet crossings, the speed of the plasma sheet, and regions of large ExB flows. We are looking for cases where the near earth neutral line passed the satellite to examine the small-scale structures. This work is an outgrowth of our ISEE, Geotail and Polar studies. A paper is accepted in Tromso proceedings and one is submitted to ICS6 proceedings. Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2002 - 4 - 4 Investigation of the magnetopause from small scales (electron gyroradius and electron inertial length) up to mesoscales (ion gyroradius and ion inertial length) Cluster instruments used: EFW, FGM, STAFF, WHISPER, DWP, CIS, PEACE Intervall 1 Time intervalls: see webpage for time intervalls Contact person: ------------------------> Position in the EFW society: pi Further information can be found at: Project added 2002 - 6 - 13 We investigate the role of Broadband ELF emissions for energy transport in the polar cusp by analysis of
electric and magnetic field wave data. The four spacecraft with small separation distances makes it plausible
to infer some spatial information on the waves from cross-spectral analysis. Together with calculated
Poynting flux, polarization and combined with particle data we try to answer questions like: the importance
of these waves for energy transport to the ionosphere, the nature of the wave modes, the generation mechanism of broadband waves and the coupling of these phenomena to magnetic reconnection. Cluster instruments used: EFW, STAFF, FGM, CIS, PEACE Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 6 - 13 Using magnetic and electric field data collected by the Cluster satellites near apogee, combined with ground-based observations from Canada and Scandinavia, I will try to identify signatures of predicted substorm instabilities in the mid-distant tail. By computing the spatial gradient tensors, large-scale field perturbations can be identified, and their relative motion established. Cluster instruments used: EFW, FGM, CIS Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 6 - 13 It is known that the precipitating electrons are accelerated to downward by the strong parallel electric fields above the auroral region. This acceleration process occurs on not only the night side auroral region but on the dayside with high occurrence frequencies. Using the conjugated points observation between high altitudes (Cluster) satellite and low altitude (DMSP, FAST, Akebono etc.) satellite, we will see witch regions of the magnetosphere are related to the dayside auroral particle acceleration phenomena, and discuss their generation mechanisms. Cluster instruments used: EFW,STAFF,FGM,CIS,PEACE Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 6 - 13 People: Anders Tjulin, Anders Eriksson, ...
Object: Small-scale (ion gyroradius size) density depletions with enhanced wave activity in the lower hybrid frequency range.
Background: Previously observed on Freja and several auroral sounding rockets, and in fact also found in the old Viking data set. We use the Cluster EFW internal burst data to study these in detail. Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 9 - 27 Study of bow shock motions from normal and speeds
determined by the timing methos and EFW SC potentiel Cluster instruments used: EFW Time intervalls: Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2002 - 10 - 9 We will investigate the variations of electric fields and related flow events in the magnetotail during periods with simultaneous (conjugate) ground-based (MIRACLE) observations. The large-structure and temporal evolution of the flow events will be examined by comparison with global MHD simulations. Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2002 - 10 - 14 To explain the increase of bulk velocity of O+ ions parallel to the magnetic field, I'm estimating the ponderomotive force which affects on field-aligned motion of O+ ions under E-field waves existing. If there are E-field waves with frequencies of less than O+ ion gyrofrequency or around 0.1 Hz, the increase of field-aligned bulk velocity can be explained well. And with high time resolution data, for instance 0.04-sec interval, fine structure of bursty velocity increase can maybe explained also. Cluster instruments used: CIS Intervall 1 Time intervalls: 2001.04.12.07.30 - 2001.04.12.09.30 Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2003 - 2 - 4 Using data from all 4 Cluster S/C we study how electric field properties behave in and near the neutral sheet. Parameters to be investigated are 1) dawn-dusk electric field amplitude and 2) coherence/correlation of Edusk between spacecraft, both sorted by Bx and magnetic activity. The aim is to understand the characteristic temporal and spatial scales of E-field/plasma flow structures and how these are distributed around the neutral sheet. Cluster instruments used: FGM Intervall 1 Time intervalls: All magnetotail crossings during 2001 and 2003 Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2003 - 2 - 14 We plan to investigate potential generator regions in the high latitude auroral magnetosphere using conjugate data from Cluster and FAST. We shall examine the diversion of perpendicular currents into field-aligned currents and the current / energy transfer between the magnetosphere and the auroral ionosphere. Cluster instruments used: Time intervalls: Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2003 - 10 - 31 The aim of this project is to combine EFW electric field data with FGM magnetic field data to extend on-going investigations into the properties of ion driven ULF waves in the terrestrial foreshock. The project will examine wave polarization, pointing flux, and use E and B data to determine intrinsic wave properties. The project will be limited to the study of ion driven foreshock wave phenomena, including shocklets and discrete wave packets, but not SLAMS. This project is complementary to Behlke's study of SLAMS, and also Moullard's project to study electron driven waves.
Cluster instruments used: EFW, FGM, CIS Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2004 - 3 - 16 We have begun a preliminary investigation using FGM data into the nature of shock crossings where the profile at each spacecraft is not the same and the shock transition is often extended. This often corresponds to oblique/ quasi-parallel shock front geometry. We propose to use the EFW electric field and potential data together with magnetic data to study these extended shock transitions where a timing analysis cannot necessarily be applied. The projects of Bale and Maksimovic concentrate on the perpendicular shock where a timing analysis can be used; this project is complementary. Results from this project may also be of relevance to Behlke's study of SLAMS.
Cluster instruments used: EFW, FGM, CIS, PEACE Time intervalls: Contact person: ------------------------> Position in the EFW society: associate Further information can be found at: Project added 2004 - 3 - 16 We plan to study the distribution of electric fields in the inner magnetosphere, in the region of possible overlap of cold plasmaspheric and hot RC/PS plasmas, in the context of SAPS and related phenomena in the ionoshere and the equatorial plane during disturbed conditions. Cluster instruments used: EFW, FGM,CIS,RAPID,EDI Time intervalls: Contact person: ------------------------> Position in the EFW society: co-i Further information can be found at: Project added 2004 - 10 - 25 Sonnerup et al. [GRL 2004] have described a flux transfer event (FTE) seen by Cluster on 2003/03/08. Using C1, C2, and C4 which were on the magnetosheath side of the magnetopause they could indentify FTE consisting of a flux rope of approximate size 1Re and irregular in shape embedded in the MP. The de Hoffmann-Teller (HT) frame mainly moves anti-sunward and northward, and is well anchored in the magnetosheath flow. They used C3 as well on the magnetospheric side, but the results are quite different. C3 saw a temperature minimum and gave a different HT frame. Several measured quantites with C3 not noted by the authors give a different view. CIS saw a burst of solar wind plasma (indentified by He++) at the time chosen by Sonnerup et al, coincident with plasma wave emissions detected by WHISPER. Electron data from PEACE varied also, with some field aligned flux. EFW showed electric field data which varied in unison with the ion and electron measurements suggesting a close relationship. AE had moderate acitivity reaching 100 nT. All these C3 and ground-based data are in agreement with a plasma transfer event (PTE) [Heikkila, JGR, 1997; Space Sci. Rev. 1998].
Cluster instruments used: EFW, FGM, STAFF, WHISPER, WBD, DWP, CIS, PEACE and RAPID Intervall 1 Intervall 2 Time intervalls: 2003.03.08.07.07 - 2003.03.08.07.14 2003.03.08.07.07 - 2003.03.08.07.08.15 Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2004 - 11 - 8 The onset of an isolated substorm of 2002/09/11 began at 1600 UT in far north Finland (Kilpisjarvi). Cluster near apogee ~19 Re at midnight at z = -2 Re and saw nothing (except a decreasing value of Bz from 15 to 5 nT)until it apparently crossed a shock at 1623 UT into a plasmoid. RAPID data shows an immediate response with high fluxes of electrons and ions with high energies which lasted until 1740 UT. The data from the 4 s/c showed a nested structure. All instruments showed unique data (FGM, EFW, CIS, PEACE, and a variety of plasma emissions. A remarkable event! Cluster instruments used: All instruments Intervall 1 Intervall 2 Time intervalls: 2002.09.11.15.00.00 - 2002.09.11.18.00.00 2002.09.11.16.20.00 - 2002.09.11.17.40.00 Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2004 - 11 - 9 Multi-instrumental survey in the magnetotail of physical properties across the thickness of current sheets (with accurately known normals), moving quickly over the Cluster tetrahedron during intense flapping motions of the magnetotail plasma sheet. Cluster instruments used: FGM+CIS+PEACE + EFW Intervall 1 Intervall 2 Time intervalls: 2001.07.24.17.20 -2001.10.20.10.40 (~40events) 2004.07.03.11.40 -2004.10.20.11.20 (~50events) Contact person: ------------------------> Position in the EFW society: other Further information can be found at: Project added 2005 - 10 - 11om@so.estec.esa.nl Olivier Moullard Wave Distribution Function Analysis on several spacecrafts
stenberg@space.umu.se Gabriella Stenberg Investigation of Electron Phase Space Holes
pmk1@cornell.edu/klatt@ece.cornell.edu Paul Kintner/Eric Klatt Auroral Zone Electric Fields and Density Irregularities
jbonnell@ssl.berkeley.edu John Bonnell Crossings of auroral oval during ground-based observations
Anita.Aikio@oulu.fi Anita Aikio Electromagnetic ion cyclotron waves
kalevi.mursula@oulu.fi Kalevi Mursula Auroral Alfén waves and broadband ELF emissions
jwe@irfu.se Jan-Erik Wahlund Magnetotail signatures of theta aurora
cumnock@plasma.kth.se Judy Cumnock Multi-spacecraft study of energy transport by alfven waves
ccc@ssl.berkeley.edu Chris Chaston Electric field and satellite potential measurements at the bow shock
rico@irfu.se Rico Behlke http://cluster.irfu.se/rico Lobe cell convection and polar cap precipitation
eriksson@lasp.colorado.edu Stefan Eriksson The response of the magnetosphere to pressure pulses
Cattell Cynthia Studies of waveforms in the magnetotail and psb
cattell@fields.space.umn.edu Cynthia Cattell http://ham.space.umn.edu/cattell/NPG/tromso_paperfinalall.pdf The magnetopause at small scales
mats.andre@irfu.se Mats André http://www.cluster.irfu.se/magnetopause/ Broadband ELF emissions and energy transport in the cusp
david.sundkvist@irfu.se David Sundkvist Electric fields in the tail at substorm onset
chris@irfu.se Chris Cully Particle acceleration process above the dayside auroral region
morooka@irfu.se Michiko Morooka Lower hybrid cavities in plasmasphere and auroral zone
at@irfu.se Anders Tjulin Bow shock motions
milan.maksimovic@obspm.fr Milan Maksimovic Comparison of magnetospehric and ionospheric processes
Petri.Toivanen@fmi.fi Petri Toivanen field-aligned accelration of O+ ions by the ponderomotive force
sachiko@irf.se Sachiko Joko Electric field properties in and near neutral sheet
Petri.Toivanen@fmi.fi Petri Toivanen Energy and current transfer in the auroral magnetosphere
hamrin@space.umu.se Maria Hamrin Electric and magnetic field properties of foreshock ULF waves
jeastwood@lepvax.gsfc.nasa.gov Jonathan Eastwood Structure of oblique and non-laminar shock crossings
jeastwood@lepvax.gsfc.nasa.gov Jonathan Eastwood Electric field in the inner magnetosphere
bpop@cbk.waw.pl Barbara Popielawska Observation of plasma transfer event (PTE) seen by Cluster
heikkila@utdallas.edu Walter J. Heikkila Substorm of 2002/09/11 - 911 Plasmoid
heikkila@utdallas.edu Walter J. Heikkila Structure of tail current sheet in flapping events
victor@geo.phys.spbu.ru Victor Sergeev