new results in polarimetry of planetary thermospheric emissions: earth and jovian cases
DESCRIPTION
New results in polarimetry of planetary thermospheric emissions: Earth and Jovian cases. M. Barthelemy (1), J. Lilensten (1), C. Simon (2), H. Lamy(2), G Gronoff (3), H. Menager (1), S. Miller (4), M. Lystrup (5), H. Rothkael (6), J. Moen (7). IPAG, France BIRA-IASB, Belgium - PowerPoint PPT PresentationTRANSCRIPT
New results in polarimetry of planetary thermospheric emissions: Earth and Jovian cases.
M. Barthelemy (1), J. Lilensten (1), C. Simon (2), H. Lamy(2), G Gronoff (3),
H. Menager (1), S. Miller (4), M. Lystrup (5), H. Rothkael (6), J. Moen (7).
(1)IPAG, France(2)BIRA-IASB, Belgium(3)NASA, Langley,VA, USA(4)UCL, UK(5)University of Colorado, USA(6)Polish Space Research Center, Poland(7)University in Oslo, Norway
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Polarization processes
• Impact polarizationPolarization rate
depends of:– Pitch angle
distribution
– Kind of particles
– Energy
– Depolarization processes as collisions.
• Emission in an anisotropic region: for ex Electric field.
Ex. Lyman alpha polarization rate by electron impact. Laboratory measurement (from James et al 1998).
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Earth case: POLARLIS, or the measurement of the POLarization of the Oxygen thermospheric Red Line In Svalbard.
• Photo-polarimeter: SPP at KHO in Longyearbyen (Svalbard) and at Hornsund .
Steerable Polarization Photometer (SPP) built at the Oslo University (UiO). It includes 2 channels and a pan-tilt unit. Aperture is 2°.
Channel 1: Photomultiplier.
Red filter centered on 6300 A with a FHWM of 1 nm.
Linear polarization analyser. One rotation of the analyser every 4.02 s.
Channel 2: Same, without the polarization filter.
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17 jan 2007 late afternoon. From Lilensten et al. 2008. GRL
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Reassessment
-Error in calibration angles. Correction around 45°
-New measurements at Hornsund (no light pollution)
-Confirmation of the detection-But rates around 1% after data processing-Direction close to the vertical (difference was due to the pollution)
-Compatible with Bommier et al. 2011-Raw polarisation before depolarizing collisions: ~18%-Vertical ie //B
- Barthelemy et al. submitted 2010.
Jovian case
• H3+ emissions in the IR.
• The emission process is different: No emission due to electronic impact because of the chemical process of formation, but…
• Possibility to get alignment due the electric fields in the auroral region.
2 half nights observation for August 2008 at the UKIRT with the instrument UIST-IRPOL in the Long L band (3.6-4.2 µm). Barthelemy et al. 2010, submitted
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Seventh data set:I at 3.95µm
q (Normalized Stokes parameter)
u (Normalized Stokes parameter)
p (%) (Debiaised)
Θ (°) (ref is the slit direction)
v (Normalized Stokes parameter)
The polarization direction are difficult to interpret…
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Interpretation:
Conclusion and Perspectives
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Jovian case.
•Auroral UV emissions.•Lyman , the most promising:
•Very intense (100 kR)
•Emission due to electrons and/or protons. Various polarization rate and direction with the energy.
•Radiative transfer in a presence of magnetic field for an allowed transition.
•Due to this, possible variation of the polarization rate along the line profile. Need for very high resolution.
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Needed in a dream world
• Spatial resolution around 100km2• Width of the oval ~200km.
• Spectral resolution• Lyman alpha width is 0.02 nm and it exists H2 lines in
coincidence with H-Lyman alpha.• Typical lyman alpha filter width (~5nm) Some lines of
H2 but faint compared to H-Lyman alpha
• Polarimetric accuracy under 1%• Only in the night side (dayside emission can
reach 10% of the auroral emission!)
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Feasability• Flux (at Ly alpha)
• Expected spatial resolution:100 km2
• 100 kR in the oval (i.e. 1e11 ph.cm-2.s-1 averaged in all directions).• Orbit : for example EJSM in resonance 2:1 with Europa i.e. around
106km for the centre of the planet
i.e. 7.9 10-1 ph.cm-2.s-1
Need an effective area of the instrument of 12.5 cm2 on a basis of 10ph.s-1. pix-1 (with an efficiency of the optics of 0.05, this correspond to an aperture of 250cm2)
Pb moving pieces!!!
• With a “better” orbit (more flux) : example of JUNO.Polar orbit.Closest point 4000km~12000km above the oval.
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Spectra/Lyman alpha filter
• Interest of spectra:• H2 lines
• No mixing between H2 and Lyman alpha lines if sufficient resolution.
– But not enough flux considering EJSM orbits to get H2 lines.
– And possible problem with the grating.
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Optical solution?
• Exemple: SMESE-Lyot like design (mirrors)
From Auchere et al. 1st SMESE workshop.
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Conclusions
• Difficult design due to the short wavelength– But
• Strong interest
• Best solution?• Mission to the planet (EJSM; too late for Juno)VS• Space telescope
• Rq: Saturn has Ly alpha aurora 10 times fainter.
Perspectives and needs.• Diversity of processes,diversity of emissions
→Specific information for each line and planet.• Others examples :
– O 8446 Å, O 1304 Å* (Earth, Venus, Mars)– Na I 5890 Å (Mercury)….in progress
– Needs for the jovian case– Ab initio calculation of the link between H3+ lines
polarization and the fields (E and/or B).– Lab experiment.
– In EJSM frame: Difficult to have a Ly alpha polarimeter. H3+ measurement as combined measurements
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Polarisation as a tool to study the Solar System and beyond
Hervé Lamy1 & Mathieu Barthélemy2
1 Belgian Institute for Space Aeronomy (BISA)2 Institut de Planétologie et d’Astrophysique de
Grenoble (IPAG)
COST proposal reference: oc-2010-2-8667