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Published byLorraine Snow Modified over 6 years ago
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The Role of the Atmosphere in Magnetosphere-Ionosphere Coupling
(at Saturn) N. Achilleos (Atmospheric Physics Laboratory, UCL) With thanks to colleagues: C. G. A. Smith (Brooksbank School), C. Tao, S. V. Badman (JAXA) and A. D. Aylward (UCL)
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Setting the Scene: Saturn’s Dynamic Aurora
HST images of Saturn’s southern UV aurora presented by Badman et al (JGR, 2005). Concurrent observations by Cassini planet’s auroral response to the passage of a solar wind compression / shock. Compression magnetic reconnection on the nightside, which closes of order 10 GWb of open magnetic flux. Polar cap boundary (main oval) strongly contracts to higher latitudes.
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(Expression from Cowley and Bunce PSS 2003)
Time scales ? Timescale for ‘dipolarization’ of a distended flux tube: <~ mins (observed by Bunce et al, GRL, 2005) How does this compare to the timescale on which the magnetospheric plasma can be accelerated by currents linking to the ionosphere / thermosphere ? tMI = 1/2 ( / P* Bi Bz) (e / i)2 (Expression from Cowley and Bunce PSS 2003) Surface density of plasma sheet in outer magnetosphere: ~ 30 / (2e) tonnes RS-2 (Arridge et al, GRL, 2007) Effective Pedersen conductance P*~ 1-2 mho (Bunce et al, Ann. Geo., 2003) Ionospheric field Bi~40000 nT Magnetospheric field Bz~3 nT MSP/ISP distance ratio (e / i) ~ 100 for e~30 RS Thus tMI ~ 1-2 hours, tMI ~ tdip
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Approach to Modelling Start with the UCL axisymmetric thermosphere model of Saturn (Smith and Aylward, Ann. Geo., 2008). Now uses the auroral profile by Tao et al. (Icarus, 2011). Modify the profile of plasma angular velocity M in the UCL model by shifting the position of the ‘polar cap boundary’ where M changes value from ~0.8 S to ~0.3 S (use the fit by Cowley et al. (JGR, 2004) to observations presented by Richardson, J. D. (JGR, 1995) and Stallard et al., Icarus, 2004). N.B. Since tMI ~ tdip for future work - ‘feedback’ from thermosphere on M evolution. In more detail: Start with a ‘contracting’ phase where the cap shrinks: D / Dt = -220 kV / radian (e.g. Badman et al., Ann. Geo. 2007) Follow with an ‘expansion phase’ where the cap expands: D / Dt = 70 kV / radian
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Angular velocity of magnetosphere and thermosphere
Thermosphere is ‘slow’ to respond to change in M Ionospheric current (T - M) At certain phases, T < M - this leads to interesting predictions for auroral current t=0 is most ‘contracted’ position of polar cap boundary.
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Field-Aligned Currents
(T - M) flow pattern leads to appearance and movement of a broad, higher-latitude oval or ‘ring’. The emission pattern may appear as a ‘bifurcation’. Here we use P = 1 mho, higher values produce higher current density. t=0 is most ‘contracted’ position of polar cap boundary.
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Field-Aligned Currents: Actual vs. ‘Constant K=0.5’
The grey profiles assume ionospheric current calculated using: (1 - T) = K(1 - M)
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Azimuthal Field B above Ionosphere
In certain regions, obtain negative B i.e. ‘leading’ field without any super-corotation of plasma. This happens when neutrals rotate slower than plasma T < M, but both subcorotate. Observations? Use axi-symmetric Ampere’s Law to calculate B following e.g. Cowley et al (Ann. Geo. 2008)
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Neutral Temperature ‘Wave fronts’ of temperature enhancement propagate outwards from sites of Joule heating. Observations?
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Proposal for UCL to host MOP 2013: (C. Jackman and N. Achilleos)
London is a vibrant city, also convenient for travel access to Europe, US. UCL campus is a 5 min walk from Eurostar terminal and a short train journey from Heathrow. Many possibilities for excursions near UCL - museums, art galleries, University of London observatory, visits to Royal Astronomical Society, London Eye, Thames riverboats, Tower Bridge, etc. UCL have planetary science teams at the Gower Street campus (Physics and Astronomy) as well as the Mullard Space Science Laboratory. We have experience in hosting international meetings, and a dedicated conference support team, to help organize venues, audiovisual needs, catering, etc. Other experience: UCL organized a small planetary meeting in 2008 at Windsor Great Park, which was successful. Accommodation: For restricted budgets, student halls of residence are an option during the Summer. Many hotel options, over a variety of budgets, in the Bloomsbury area. UCL have a special rate with the Tavistock hotel.
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