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Generation of intense quasistatic fields at high altitudes by the Ionospheric Alfvén Resonator Bill Lotko, Jon Watts, Anatoly Streltsov Thayer School of.

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Presentation on theme: "Generation of intense quasistatic fields at high altitudes by the Ionospheric Alfvén Resonator Bill Lotko, Jon Watts, Anatoly Streltsov Thayer School of."— Presentation transcript:

1 Generation of intense quasistatic fields at high altitudes by the Ionospheric Alfvén Resonator Bill Lotko, Jon Watts, Anatoly Streltsov Thayer School of Engineering Dartmouth College

2 Multiple resonant cavities Standing Alfvén waves confined by gradients and conducting boundaries Ionospheric Alfvén Resonator Field Line Resonator IAR ~ 1- 10 sec (Polyakov ‘76; Trakhtengerts, Feldstein ’81; Belyaev et al ’87; Lysak ‘88) FLR ~ 1 – 10 min (Samson ‘72; Southwood ‘74; Chen, Hasegawa, ‘74)

3 Multiple resonant cavities IAR ~ 1- 10 sec (Polyakov ‘76; Trakhtengerts, Feldstein ’81; Belyaev et al ’87; Lysak ‘88) FLR ~ 1 – 10 min (Samson ‘72; Southwood ‘74; Chen, Hasegawa, ‘74) MIAR ~ 1 min Standing Alfvén waves confined by gradients and conducting boundaries Ionospheric Alfvén Resonator M-I Alfvén Resonator Field Line Resonator

4 Atkinson ’70, Sato ’78, Lysak ’91, Trakhtengerts and Feldstein ’91 Feedback-gain in an active ionosphere: Resonator

5 Atkinson ’70, Sato ’78, Lysak ’91, Trakhtengerts and Feldstein ’91

6 Alfvén resonator frequency (fundamental) Constructive interference Ion mobility Alfvén Resonance Condition (for an “insulating” reflector) f = 1 / 4  = V A / 4L  = V  4  = 4L (V  / V A ) V  = M i E  M i = ion mobility insulator conductor

7 Active Ionization and Depletion Upward current Ionization  Conductance  Electric field  Downward current Ionization  Conductance  Electric field 

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9 Observations from low-altitude satellites (FAST) Paschmann et al. ‘03 polar cap

10 Observations at higher altitude Intense electromagnetic activity in the “PSBL” ~ 1-min oscillations Oscillations confined mainly to downward current channel Integrated Poynting flux is upward Johansson et al. ‘04 polar cap plasmasheet down up M-I Alfvén resonator?

11 Opgenoorth et al. ‘02 Aikio et al. ‘04 Active Ionization and Depletion

12 Two-fluid Alfvénic Response of the Magnetosphere Electron parallel momentum Density continuity Current continuity v ||e - electron parallel speed; IC - electron collision frequency; AR - effective collision frequency representing wave-particle interactions. ρ i - ion Larmour radius. 0

13 Coupling to Ionospheric Conducting layer Density Continuity Equation n = n 0 + n 1 E-region plasma number density; S 1 =  n 0 2 ionization source maintaining equilibrium n 0 j || field-aligned current;  recombination coefficient. Current Continuity Equation  P,  H height-integrated Pedersen and Hall conductances. 0 0

14 Modeling Region − Plasmasheet boundary layer Computational Domain − Dipole + Rectangle − Nonuniform grid in altitude NUMERICAL SIMULATIONS Streltsov et al., 2002

15 Density, Alfven speed / refractive index IAR MIAR

16 Resonator “keyogram”

17 Resonator keyogram − zoom view

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19 Variation with altitude

20 Simple Layered Model

21 Resonator stability properties How does the growth rate change with cavity size? Longer cavities  − larger || AND  − unstable at higher  P − lower frequency − lower growth rate k  cutoffs regulated by: high-k  − parallel resistivity low-k  − recombination

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24 Conclusions High V A region  lossy Alfvén resonator cavity Fundamental period ~ 1 minute Feedback unstable resonator modes in  currents – Onset near current maximum – Decelerating propagation toward  current channel – Mode decays when it enters  current channel Strong coupling ion sound- IAR mode coupling – Pondermotive force creates ionospheric upwelling –  n/n ~ 1 holes (bottomside) and patches (topside)


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