Observation of a Non Thermal Continuum radio event during the CLUSTER Tilt campaign 17th CLUSTER...
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Observation of a Non Thermal Continuum radio event during the CLUSTER Tilt campaign
17th CLUSTER Workshop
Uppsala, Sweden, 12 – 15 May 2009
Uppsala May 2009 1/13
Pierrette Décréau (1), Séna Kougblenou (1), Jean –Louis Rauch (1), Jean – Gabriel Trotignon (1), Xavier Vallières (1),Sandrine Grimald (2) and Patrick Canu (3)
(1) LPC2E, Orléans, France(2) MSSL , Holmbury St Mary, United Kingdom(3) LPP, Vélizy, France
Y
X
Y
X
Gurnett, 1975
Pioneer studies show that NTC radiation emerges from sources at PlasmaPause boundary layer, beaming predominantly near equatorial plane.
The lower frequency band is trapped inside the magnetospheric cavity.
26/02/2001
Magnetosphere
Trapped NTC
Cusp
Escaping NTC
20
40
60
Magnetosheath
F (kHz)
2 00:30 03:50 07:10 UT
• Cluster observations largely confirm this view
Introductory remarks
1) Observations: Non Thermal Continuum form analyzed
Uppsala May 2009 3/13
• Cluster revealed a new form of NTC: banded emissions (Grimald et al., 2008)The plasmapause radiates over a large latitudinal range.Waves emitted (at local plasma frequencies) are banded at local Fce.
Medium latitude plasmasphere
28 August 2008
X
Z
Y
C4 C3
C3
C4
A new form of NTC revealed by CLUSTER
1) Observations: Non Thermal Continuum form analyzed
Uppsala May 2009 4/13
Case event presentation : spectral and orbit characteristics
• Date: 18/05/2008 (tilt campaign); 12:00 -12:30 UT
• Spectral features: bands in the 15 – 25 kHz range; df ~ 2.5 kHz (< local fce = 3 kHz)
• Observer’s position: dawn lobes; Cluster heads toward dusk plasmasphere
Fuh
DawnDawn
DuskDusk
Z
Y
X GSM
Polar cap
1) Observations: Non Thermal Continuum form analyzed
Fp
Uppsala May 2009 5/13
• Magnetic activity: quiet period, preceding a moderate perturbation
• Expanded plasmasphere (outer boundary at L ~ 8 in dusk sector)
Case event presentation : geophysical context
1) Observations: Non Thermal Continuum form analyzed
Uppsala May 2009 6/13
• NTC bands provide remote information of a plasmapause knee feature (at source) which we attempt to localize, in order to learn about plasmaspheric dynamics.
• In this event, geomagnetic conditions announce a possible drainage of the plasmaspheric body. The frequency range of NTC is associated to a PPause knee at low densities (< 10 cm-3). Such features could not be observed by IMAGE, which nevertheless revealed complex plasmasphere contours (plume, shoulder, fingers …).
Motivation
2) Analysis
After Carpenter, 1970
Shoulder ?
Plume
Shoulder
Plume
Uppsala May 2009 7/13
•The frequency distance between bands gives access to magnetic field magnitude local to the source, i. e. an ‘iso-fce’ surface which can be modeled in 3D;
• 3D ray path orientation (from tilted SC pair) points to the source position
• Directivity in spin planes of the two other SC add supporting information
2) Analysis
Strategy
1
2
43
Iso-fce surface
Uppsala May 2009 8/13
2) Analysis
Wave measurements from a tilted pair• Assumption: E field combines two linear fields, au and bv, oscillating in quadrature. Same conditions at C3 and C4.
Processing: The signal intensity measured in spin plane, modulated with antenna orientation, is characterized by three parameters (E0
2, α2, ), leading to possible orientations of meridian planes P4a & P4b.
Combining C3 and C4 possible meridian planes lead to candidates au / bv pairs, tested regarding the main assumption. Either no solution is obtained, or an optimal solution validated.
• Results: test the assumption; estimate au and bv quantities; obtain k orientation (all vectors with sign ambiguity)
k
Uppsala May 2009 9/13
azimuth
Uppsala May 2009 10/13
3) Results
Spin modulation on all SCE field analysis on C3-C4 pair: coherent with plane wave elliptic polarization (e = 0.85) kel within a cone of ~10° half angleAssumption of circular polarization: kcirc at ~ 10° from kel
Directivity analysis
azimuth ( [0, π[)
k orientation (GSE coordinates)
zenith angle ([0, π[ )
90 100 110 120 130 140 (deg)
400
40
20
20
0
k orientation is measured at (C3_C4) position at 4.6 MLT, 12:20 U : = 126° ; = 119° in the band 15 – 25 kHz.
a rectilinear ray path (free space approximation) cuts successive meridian planes (SM coordinates) until the gyro-frequency of a modeled magnetic field meets the df band spacing
the (unrealistic) dipole model indicates a source near the equator beaming in an unrealistic way towards the observatory
Tsyganenko model – not including By IMF component - points to a source at L=11, MLT = 6.6, beaming in a realistic way
directivity on other SC indicates similar values –compatible with above
all uncertainty factors cumulated lead to an unprecise source position – could be refined
3) Results
Uppsala May 2009 11/13
Source position
Ray path in rotating meridian plane of SM coordinate system
Iso-fce
1 kHz2
34
B Tsyganenko
df
Wave source position: questions raised
3) Results
Uppsala May 2009 12/13
The source is found at L = 11, not far from a connection with the low latitude boundary layer. What is the actual topology? Are field lines at source close/open? (could be checked with Superdarn)
The ray path orientation between source and Cluster indicates the presence of a shoulder, ~ MLT aligned. . What is the actual 3D shape of plasmasphere?
?
C4 MLT
Conclusion
• Search of the source of a banded NTC wave observed from the polar cap (4.6 MLT) by CLUSTER tilted pair
• Tilted pair allows to measure wave polarization characteristics, confirming propagation in an L_O mode
• Path direction is estimated in 3D (with a 180° ambiguity)• Use of a realistic static magnetic field model points to a region
source at high L value in the dawn (6.6) MLT sector• the low average density (~ 5 cm -3) at the source, is observed at
medium latitudes (Z = -4.5 RE) along a (closed?) flux tube connected to the low latitude boundary layer (LLBL)
• Those results confirm that the plasmapause radiates NTC waves at medium latitudes, in this case in the MI coupling region.
Uppsala May 2009 13/13