Space Plasmas as a Natural Laboratory R. J. Strangeway (IGPP/UCLA) PSTI Research Lectures – RJS–9 June 4, 2003 – 1 Space Plasmas as a Natural Laboratory Recap 1. Single particle dynamics –drifts, magnetization currents, adiabatic invariants, particle drift paths in the Earth’s magnetosphere. 2. Magnetohydrodynamics – moments of the Vlasov equation, truncating the hierarchy, “ideal MHD,” frozen in theorem, does MHD work? Introduction to reconnection. 3. The mechanical view of space plasmas, collisional MHD and magnetosphere-ionosphere coupling. PSTI Research Lectures – RJS–9 June 4, 2003 – 2 Space Plasmas as a Natural Laboratory Recap Continued 4. Waves in cold plasma –Alfven waves, “inertial effects,” Appleton-Hartree dispersion, the zoo of plasma waves. 5. Vlasov (kinetic theory) – inverse Landau damping and gyroresonance. 6. Auroral kilometric radiation – a fundamental plasma instability. PSTI Research Lectures – RJS–9 June 4, 2003 – 3 Particle Drifts Electric field drift: Gradient drift vE = E ×2 B B vG = W⊥ B × ∇B qB 3 ⋅ B× Β ∇ B Curvature Drift: vC = 2W || Polarization Drift: vP = m 2 dE qB dt qB 4 (Alfvén wave) Note: particle drifts do not necessarily imply current – Magnetization current must be included PSTI Research Lectures – RJS–9 June 4, 2003 – 4 PSTI Research Lectures – RJS–9 June 4, 2003 – 5 What Is Magnetohydrodynamics? Magnetohydrodynamics (MHD) is a formalism that describes a plasma in terms of fluid properties, such as density, flow velocity, pressure, etc. The basic assumption of MHD is that the plasma is “local” in its behavior. This means that the rates of change of fluid properties are dependent only on the local values of those properties. In a classical gas “localization” is provided by collisions. In a magnetized collisionless plasma, the gyration of particles around the field gives localization in the perpendicular direction. Along the field other processes (e.g., wave-particle interactions) have to be invoked to provide parallel localization. What happens when the mean free path is much larger than any gradient scales within the system? PSTI Research Lectures – RJS–9 June 4, 2003 – 6 Boltzmann Equation PSTI Research Lectures – RJS–9 June 4, 2003 – 7 Moment Equations - Closure? PSTI Research Lectures – RJS–9 June 4, 2003 – 8 Momentum Equations Electron Momentum Equation leads to generalized Ohm’s Law ∇ Pe dU e me = − e E + Ue × B − n dt e Sum of Electron and Ion Momentum Equations leads to total momentum equation – No electric field term! ρ DU = j × B − ∇P Dt PSTI Research Lectures – RJS–9 June 4, 2003 – 9 Frozen-in Field PSTI Research Lectures – RJS–9 June 4, 2003 – 10 Why Does MHD work so well? From Faraday’s Law, it is ∇×E that matters, not E Under assumption of scalar pressure, and a simple adiabatic relationship between pressure and density, the curl of the momentum equation reduces to mi B′ = B + e ω, ∂B′ − ∇ × U × B′ = 0 ∂t where ω is the vorticity. For “ideal MHD” ω = 0 PSTI Research Lectures – RJS–9 June 4, 2003 – 11 Magnetic Field Reconnection Mechanism by which energy and momentum are transferred to the magnetosphere. Requires local violation of MHD. PSTI Research Lectures – RJS–9 June 4, 2003 – 12 Force Balance - MI Coupling PSTI Research Lectures – RJS–9 June 4, 2003 – 13 Maxwell Stress and Poynting Flux PSTI Research Lectures – RJS–9 June 4, 2003 – 14 Currents and Ionospheric Drag PSTI Research Lectures – RJS–9 June 4, 2003 – 15 MI Coupling - FAST Observations PSTI Research Lectures – RJS–9 June 4, 2003 – 16 Auroral Currents PSTI Research Lectures – RJS–9 June 4, 2003 – 17 Alfvén Wave Governing Equations The electron momentum equation provides the “inertial” correction to the MHD modes. In particular electron inertia can allow the wave to carry a parallel electric field. PSTI Research Lectures – RJS–9 June 4, 2003 – 18 “Dungey Triads” PSTI Research Lectures – RJS–9 June 4, 2003 – 19 Shear (Alfvén) Mode PSTI Research Lectures – RJS–9 June 4, 2003 – 20 Fast Mode PSTI Research Lectures – RJS–9 June 4, 2003 – 21 Governing Equations – Recap Harmonic Perturbation, first order quantities only: ∂/∂t ≡ –iω ∇ ≡ ik Faraday’s Law: k × E = ωb Ampere’s Law: k × b = –iµ 0 j– ω2 E c i.e. PSTI Research Lectures – RJS–9 2 ω k – 2 E – k(k⋅E) = iωµ 0 j c 2 June 4, 2003 – 22 Cartesian Coordinates Assume: B 0 = B0z , Then: 2 ω k – 2 E x – k ⊥k || E z = iωµ 0 jx c k = (k ⊥, 0, k || ) 2 || 2 ω k – 2 E y = iωµ 0 j y c 2 2 ω k – 2 E z – k | |k ⊥E x = iωµ 0 jz c 2 ⊥ Alternative formalism replaces j with the equivalent dielectric tensor PSTI Research Lectures – RJS–9 June 4, 2003 – 23 Alfvén Waves (Again!) Frozen-in ions: E + U×B = 0 Momentum: – iωnmU = j×B – ikδ P δ P = C s2δρ Energy: Mass Conservation: Therefore i.e. [E x = –U yB0, E y = U xB0] [C s2 = γ P/nm] ωδρ = nmk⋅U C s2 j×B = –iωnm[U – 2 k(k⋅U)] ω k 2⊥C s2 2 j y = –iωnm(1 – )E /B y 0 ω2 j x = –iωnm E x /B02 [V a2 = B02 /nmµ 0] ω 2pe Electron momentum: j z = i ω ε 0 E z PSTI Research Lectures – RJS–9 June 4, 2003 – 24 Fast mode dispersion 2 ω k – 2 E y = iωµ 0 j y c 2 k 2⊥C s2 2 µ 0 j y = –iω(1 – )E /V y a ω2 Therefore: k 2V a2 + k 2⊥C 2s = ω 2(c 2 + V a2)/c 2 Aside: Slow mode comes from parallel component of momentum PSTI Research Lectures – RJS–9 C s2 2 U z – 2 k || U z = 0 ω June 4, 2003 – 25 Shear-mode dispersion 2 ω k – 2 E x – k ⊥k || E z = iωµ 0 jx c 2 || µ 0 j x = –iω E x /Va2 Therefore 2 2 ω ω k – 2 – 2 E x = k ⊥k | |E z c Va 2 || 2 ω k – 2 E z – k | |k ⊥E x = iωµ 0 jz c 2 ⊥ ω 2pe µ 0 jz = i 2 E z ωc Therefore k 2 ⊥ PSTI Research Lectures – RJS–9 (ω 2 pe– ω 2) + E z = k ||k ⊥ E x c2 June 4, 2003 – 26 Appleton-Hartree Maxwell’s equations again 2 ω k – 2 E x – k ⊥k || E z = iωµ 0 jx c 2 || 2 ω k – 2 E y = iωµ 0 j y c 2 2 ω k – 2 E z – k | |k ⊥E x = iωµ 0 jz c 2 ⊥ PSTI Research Lectures – RJS–9 June 4, 2003 – 27 Polarized Coordinates Force Law: –imωv = q(E + v×B 0) –imωv x = q(E x + v yB0) –imωv y = q(E y – v xB0) q –iω(v x ± iv y) = m (E x ± iE y) – v yΩ ± iv xΩ [Ω = – q B0 /m] (± i)(± i)v y = – v y Therefore PSTI Research Lectures – RJS–9 q –iωv± = m E± ± iΩv± June 4, 2003 – 28 Electrons only, parallel 2 ω k – 2 E± = iωµ0 j± c 2 iω 2 peε 0 E± j± = (ω – ±Ωe) Therefore 2 ω pe µ2 = 1 – ω (ω – ±Ωe) ω 2 E = –iωµ j 0 z c2 z ω 2pe j z = i ω ε0E z ω 2 = ω 2pe For parallel propagation modes split into R, L, and P modes PSTI Research Lectures – RJS–9 June 4, 2003 – 29 Electrons only, perpendicular O-mode: Therefore X-mode: ω 2pe j z = i ω ε0E z 2 ω k – 2 E z = iωµ 0 jz c 2 ω 2pe µ =1– 2 ω 2 2 ω k – 2 E y = iωµ 0 j y c 2 ω 2 E = –iωµ j 0 x c2 x iω 2 peε 0 E± j± = (ω – ±Ωe) PSTI Research Lectures – RJS–9 June 4, 2003 – 30 A-H Dispersion Relation ω 2pe ω 2 pe 2 2 1– 2 ω ω µ2 = 1 – ω 2pe Ωe2 2 2 1 – 2 – 2 sin θ ± Γ ω ω Γ= PSTI Research Lectures – RJS–9 2 ω 2pe Ω Ω 4 sin θ +4 1 – 2 cos 2θ ω ω ω 4 e 4 2 e 2 June 4, 2003 – 31 Appleton-Hartree PSTI Research Lectures – RJS–9 June 4, 2003 – 32 Quasi-longitudinal Approximation ω 2 pe Ω Ω 4 sin θ << 4 1 – 2 cos 2θ ω ω ω 4 e 4 µ2 = 1 – 2 e 2 2 ω 2 pe ω 2pe 2 2 1– 2 ω ω ω 2pe Ωe2 2 ω 2pe Ωe 2 1 – 2 – 2 sin θ ± 2 ω 1 – 2 cosθ ω ω ω ω 2 pe Ωe2 2 sin θ << 2 1 – 2 ω2 ω PSTI Research Lectures – RJS–9 ω 2pe 2 ω 2 µ =1– Ω 1 ± ωe cosθ June 4, 2003 – 33 Quasi-transverse Approximation ω 2 pe Ω Ω 4 sin θ >> 4 1 – 2 cos 2θ ω ω ω 4 e 4 2 2 e 2 µ2 = 1 – PSTI Research Lectures – RJS–9 ω 2 pe 1– 2 ω ω 2 pe 2 1 – 2 cos θ ω June 4, 2003 – 34 Appleton-Hartree Including Ions PSTI Research Lectures – RJS–9 June 4, 2003 – 35 Vlasov Equation Vlasov Equation (Collisionless Boltzmann): ∂f + v⋅∇ ∇ f + a⋅∇ ∇v f = 0 ∂t Liouville’s theorem: phase space density is constant along a particle trajectory, define Liouville operator L: L = ∂ + v⋅∇ ∇ + a⋅∇ ∇ v, ∂t Lf = 0 Jeans’s theorem: Any phase distribution that satisfies the Vlasov equation is a function of the constants of the motion (αi): n Lf = Σ Lα i ∂f ∂α i i=1 PSTI Research Lectures – RJS–9 June 4, 2003 – 36 Linearized Vlasov Equation ∂ f1 q q + v⋅∇ ∇ f1 + v × B0 ⋅∇ ∇ v f1 = − E + v × B1 ⋅∇ ∇v f0 m m 1 ∂t The left hand side of this equation is the rate of change in f1 following an unperturbed particle trajectory. Formally f1 r,v,t = − t −∞ q dt′ m E 1 + v × B1 ⋅∇ ∇ v f0 Where the time integral is over the “past history” of the particle that passes through r, v at time t. PSTI Research Lectures – RJS–9 June 4, 2003 – 37 Wave Solutions Having obtained f1, the coupled Maxwell’s equations require either charge density (ρ1) [electrostatic] or current density (j1) [electromagnetic] ρ 1 r,t j1 r,t PSTI Research Lectures – RJS–9 = Σ species = Σ species q f1dv q v f 1dv June 4, 2003 – 38 Harmonic perturbation Past history integral: ⋅ × ∇ q q v ω + k v⋅E1 ω ⋅∇ ∇v f0 ∇v f1 = m E1 1 − k⋅v i ω − k⋅v f1 − m v × B0 ⋅∇ ⋅ ⋅ ∇ Note that this form implicitly assumes that integrals converge at t = -∞ PSTI Research Lectures – RJS–9 June 4, 2003 – 39 Landau Damping Parallel Propagation, electrostatic waves q2 ∂ f0 ∂v|| ρ = − i m E || dv|| ω − k ||v|| PSTI Research Lectures – RJS–9 June 4, 2003 – 40 Beam Generated Instabilities PSTI Research Lectures – RJS–9 June 4, 2003 – 41 Gyro-resonance Parallel Propagation, electromagnetic waves iq 2 jr = − E 2m r iq 2 jl = − E 2m l PSTI Research Lectures – RJS–9 dvv⊥ dvv⊥ k ||v|| ∂ f0 k ||v⊥ ∂ f0 1− ω + ω ∂v⊥ ∂v|| ω − k ||v|| − Ωe k ||v|| ∂ f0 k ||v⊥ ∂ f0 1− ω + ω ∂v⊥ ∂v|| ω − k ||v|| + Ωe June 4, 2003 – 42 Auroral Currents PSTI Research Lectures – RJS–9 June 4, 2003 – 43 Liouville’s Theorem and Aurora Liouville’s theorem states that phase space density is constant along a particle trajectory. For an auroral flux tube with a parallel potential drop constants of the motion are (subscript “0” indicates top of the acceleration region, where Φ = 0): W + qΦ = W 0, W ⊥ = µB = W ⊥0B B0 i.e., for electrons W || = W ||0 + W ⊥0 1 − B B0 + eΦ PSTI Research Lectures – RJS–9 June 4, 2003 – 44 Flux into atmosphere Electrons in the loss-cone are the current carriers eΦ Flux at atmosphere = flux in local loss cone x BI/B (flux-tube area) PSTI Research Lectures – RJS–9 June 4, 2003 – 45 Phase Space Mapping Theoretical and Observed Distributions (Ergun et al., GRL, 27, 4053-4056, 2000) Acceleration Ellipse and Loss-cone Hyperbola PSTI Research Lectures – RJS–9 June 4, 2003 – 46 Current Density – Flux in the Loss-Cone The auroral current is carried by the particles in the loss-cone. Without any additional acceleration the current carried by the electrons is the precipitating flux at the atmosphere: j0 = nevT/2π1/2 ≈ 1 µA/m2 for n = 1 cm-3, Te = 1 keV. A parallel electric field can increase this flux by increasing the flux in the loss-cone. Maximum flux is given by the flux at the top of the acceleration region (j0) times the magnetic field ratio (flux conservation - with no particles reflected). jm = nevT/2π1/2 × (BI/Bm). PSTI Research Lectures – RJS–9 June 4, 2003 – 47 Knight Relation j/j0 Asymptotic Value = BI /Bm 1+eΦ/T eΦ/T [Knight, PSS, 21, 741-750, 1973; Lyons, 1980] PSTI Research Lectures – RJS–9 June 4, 2003 – 48 Consequences of Low Density: 1 Because of low density electrons can be in direct gyroresonance with faster-than light R-X mode waves PSTI Research Lectures – RJS–9 June 4, 2003 – 49 Consequences of Low Density: 2 Resonance condition must be modified to include relativistic corrections [Wu and Lee, 1979] Non-relativistic (R-mode gyro-resonance) : iq 2 jr = − E 2m r dvv⊥ k v ∂ f0 k ||v⊥ ∂ f0 1 − ω|| || + ω ∂v⊥ ∂v|| ω − k ||v|| − Ωe For non-relativistic gyro-resonance waves damped because of tail of distribution at large v⊥ Relativistic Resonance condition is ω − k ||v|| = Ωe an ellipse in velocity space: PSTI Research Lectures – RJS–9 1 − v2 c2 June 4, 2003 – 50 Consequences of Low Density: 3 Dispersion relation must be modified to include relativistic corrections [Pritchett, 1984; Pritchett and Strangeway, 1985] Resonance condition: ω − k ||v|| = Ωe In a cold plasma R-X mode cut-off = Weakly relativistic: ωr = Ωe 1 − v2 c2 ωr = Ωe + ω pe2 Ωe 1 − v 2 c 2 + ω pe2 Ωe Modified dispersion relation allows k|| = 0 PSTI Research Lectures – RJS–9 June 4, 2003 – 51 Free Energy Source "Horseshoe" Distribution 1997-01-31/06:43:48.899 - 06:44:25.617 1ï10 5 -12.0 Resonance ellipse, k = 0 Resonance circle, k = 0 5ï10 4 -13.4 0 -14.9 -5ï10 4 -16.3 Loss-cone Hyperbola -1ï10 5 -1ï10 5 PSTI Research Lectures – RJS–9 -5ï10 4 Acceleration Ellipse 0 Para. Velocity (km/s) 5ï10 4 1ï10 5 -17.8 June 4, 2003 – 52 Energy flow in the AKR Source Region Electron Distribution in Density Cavity -1x105 -12.0 Upgoing to Magnetosphere -5x104 -13.4 2 3 Energy Flow Loss Cone -14.9 0 1 5x104 1. Acceleration by Electric Field 2. Mirroring by Magnetic Mirror 3. Diffusion through Auroral Kilometric Radiation -16.3 Downgoing to Ionosphere 1x105 -1x105 -5x104 0 Parl. Velocity (km/s) PSTI Research Lectures – RJS–9 5x104 1x105 -17.8 June 4, 2003 – 53