Shocks in Heliophysics
Dana Longcope LWS Heliophysics Summer School & Montana State University Shocks in Heliophysics
Vasyliunas, v.1 ch.10 Shocks in Heliophysics
Tsuneta and Naito 1998
Forbes, T.G., and Malherbe 1986 (v.2 ch. 6) Shocks in Heliophysics
shock
Gold 1962
Cane, Reames, and von Rosenvinge 1988 (v. 2 ch. 7) Shocks in Heliophysics
Forbes 2000 (v. 2, ch. 6) Shocks in Heliophysics
Crooker, Gosling, et al. 1999 (v3, ch. 8) Shocks in Heliophysics
Opher v2, ch. 7
Shocks in the air Shocks are…
• Collision between 2 different plasmas
• A hydrodynamic surprise Shocks in Hydrodynamics Viscosity, exchanges ∂ρ mass = −∇⋅ [ρv] thermal & kine c energy ∂t ∂(ρv) momentum = −∇⋅ [ρvv + pI +σ ] ∂t € ⎛ ⎞ ⎡ ⎤ ∂ 1 2 p 1 2 γ energy ⎜ 2 ρv + ⎟ = −∇⋅ ⎢ 2 ρv v + pv +σ ⋅ v⎥ ∂t ⎝ γ −1⎠ ⎣ γ −1 ⎦ € kine c thermal
€ ⎛ ⎞ ∂vi ∂v j 2 viscous stress tensor σij = µ⎜ + − 3 δij∇⋅ v⎟ ⎝ ∂x j ∂xi ⎠
€ ∂ρ mass = −∇⋅ [ρv] ∂t ⎛ v ⎞ ∂(ρv) ∂vi ∂ j 2 momentum σij = µ⎜ + − 3 δij∇⋅ v⎟ = −∇⋅ [ρvv + pI +σ ] ⎜ ∂x ∂x ⎟ ∂t ⎝ j i ⎠ € ⎛ ⎞ ⎡ ⎤ ∂ 1 2 p 1 2 γ energy ⎜ 2 ρv + ⎟ = −∇⋅ ⎢ 2 ρv v + pv +σ ⋅ v⎥ ∂t ⎝ γ −1⎠ ⎣ γ −1 ⎦ € €
vs € collision vi
vi ∂ρ mass = −∇⋅ [ρv] ∂t ⎛ v ⎞ ∂(ρv) ∂vi ∂ j 2 momentum σij = µ⎜ + − 3 δij∇⋅ v⎟ = −∇⋅ [ρvv + pI +σ ] ⎜ ∂x ∂x ⎟ ∂t ⎝ j i ⎠ € ⎛ ⎞ ⎡ ⎤ ∂ 1 2 p 1 2 γ energy ⎜ 2 ρv + ⎟ = −∇⋅ ⎢ 2 ρv v + pv +σ ⋅ v⎥ ∂t ⎝ γ −1⎠ ⎣ γ −1 ⎦ € € pre-shock (1) post-shock (2) Assume € vi -vs -vs 1. Solu on is sta onary in v1 v2 shock frame
v 1 v2 2. Regions 1 & 2 are uniform: transform to ref. frame co-moving ρ1 v1 p1 ρ2 v2 p2 w/ shock - shock frame 0 = −∇⋅ [ρv] jump 0 = [[ρvn ]]
[[ f ]] = f 2 − f1 0 = −∇⋅ ρvv + pI +σ ˆ [ ] 0 = [[ρvn v + pn]] € ⎡ ⎤ € 1 2 γ 1 2 γ 0 = −∇⋅ ⎢ 2 ρv v + pv +σ ⋅ v⎥ 0 = [[ ρv v + pv ]] € 1 2 n γ −1 n ⎣ γ − ⎦ € nˆ € Jump condi ons pre-shock (1) post-shock (2) (Rankine-Hugoniot) € € € v1 v2
2. Regions 1 & 2 are v 1 v2 uniform: ⎛ ⎞ ∂vi ∂v j 2 σij = µ⎜ + − 3 δij∇⋅ v⎟ = 0 ρ1 ρ2 ⎝ ∂x j ∂xi ⎠
€ 0 = [[ρvn ]] ρvn = const. ˆ 0 = [[ρvn v + pnˆ ]] ρvn [[v]]+[[p]]n = 0 1 2 γ v [[ 1 v 2 γ (p/ )]] 0 0 = [[ 2 ρvnv + γ −1 pvn ]] ρ n 2 + γ −1 ρ = € € € € Case 1: ρvn = 0 - no flow across interface € p2=p1 pressure balance € 0 = [[ρvn ]] ρvn = const. ˆ 0 = [[ρvn v + pnˆ ]] ρvn [[v]]+[[p]]n = 0 1 2 γ v [[ 1 v 2 γ (p/ )]] 0 0 = [[ 2 ρvnv + γ −1 pvn ]] ρ n 2 + γ −1 ρ = € € € € Case 1: ρvn = 0 - no flow across interface € p2=p1 pressure balance €
v2 Contact HOT COLD discon nuity v1 p p 1 2 related to linear
T1 T2 waves w/ ω=0
entropy mode: [[ρ]]≠0 ρ1 ρ2 shear mode: [[vt]] ≠0 0 = [[ρvn ]] Case 2: ρvn = const.≠ 0 ρv [[v ]] = 0 0 = [[ρvn v + pnˆ ]] n ⊥
1 2 γ ⇒ v⊥,1 = v⊥,2 = v⊥ 0 = [[ 2 ρvnv + γ −1 pvn ]] € € transform away € (ρv 2 + p)2 γ −1 (γM 2 +1€)2 = = F(M) 2( v) 1 v 3 γ pv γ 2 M 2 ( 1)M€2 2 € ρ ( 2 ρ + γ −1 ) [ γ − + ]
v M = Mach € γp/ρ number
F(M1) = F(M2 ) €
−1 M2 = F (F(M1)) €
€ pre-shock (1) post-shock (2) −1 M2 = F (F(M1)) super-sonic 2 sub-sonic (γ −1)M + 2 M = 1 2 2γM 2 −γ +1 v1 v2 € 1 c v1 s,2 2 v2 (γ −1)M1 + 2 v2 = 2 cs,1 € v1 (γ +1)M1 ρ (γ +1)M 2 ρ1 ρ2 2 1 = 2 ρ1 (γ −1)M1 + 2 € p 2 2 p 2γM − γ +1 2 = 1 p1 p γ +1 € 1 ⎛ ⎞ ⎛ ⎞ p2 ρ2 s1 s2 − s1 = ln⎜ ⎟ −γ ln⎜ ⎟ s ⎝ p1 ⎠ ⎝ ρ1 ⎠ 2 €
€ Hypersonic limit
M1 >> 1 γ = 5/3
2 (γ −1)M1 + 2 (γ −1) 1 M2 = 2 M2 → = 2γM1 −γ +1 2γ 5
2 v (γ −1)M + 2 v2 (γ −1) 1 2 = 1 → = 2 v (γ +1) 4 € v1 (γ +1)M1€ 1 € ρ (γ +1)M 2 ρ (γ +1) 2 = 1 2 → = 4 ρ (γ −1)M 2 + 2 ρ (γ −1) 1 1 1 € € € 2 p 2γ 2 p2 2γM1 − γ +1 2 → M 3 1 2 = € 1 p2 → 2 × 2 ρ1v1 p γ +1 p1 γ +1 € 1 €
€ € € Entropy’s tale
s2 ≥ s1 pre-shock must be supersonic fluid goes from super- to sub-sonic fluid slows down crossing shock fluid compresses crossing shock
viscosity = 0 s2 = s1 ⎛ ⎞ ⎡ ⎤ ∂ 1 2 p 1 2 γ ⎜ 2 ρv + ⎟ = −∇⋅ ⎢ 2 ρv v + pv +σ ⋅ v⎥ t 1 1 ∂ ⎝ γ − ⎠ ⎣ γ − ⎦ viscosity does not appear in jump condi ons (conserva on laws) but it is necessary for transi on from 1 to 2 € Q: what goes wrong if we set µ = 0 ? Q: is that diff. from taking µ 0 ? vs rarefac on
vi
vi
v -v i s -vs co-moving frame v1 v2
sa sfies conserva on v1 v 2 but violates 2nd law TD
What happens instead? ρ2 ρ1 cs rarefac on
vi
vi
vi
v t i
cs
vi A nearby shock M=1 asin(1/M∞) Mach cone
M∞
M∞=8 γ = 5/3
M=5.2
49o
8.0
M∞=8.0 Spreiter, Summers & Alksne 1966 Farther afield…
shock
contact discon nuity
shock
Opher v2, ch. 7 Hundhausen 1973 (v.3, ch.8) Q: which way is for each? Both move outward ( Forward shock 2 shocks: with slower wind creates High speed stream colliding Reverse shock € n ˆ v s >0) Shocks in MHD ∂ρ = −∇⋅ [ρv] ∂t
∂(ρv) 1 1 2 = −∇⋅ ρvv - 4π BB + (p + 8π B )I +σ ∂t [ ] € ∂ 1 2 1 1 2 1 2 γ 1 ( 2 ρv + γ −1 p + 8π B ) = −∇⋅ [ 2 ρv v + γ −1 pv − 4π (v × B) × B +σ ⋅ v] ∂ t € kine c thermal magne c
€ ∂B = −∇ × [v × B] ∂t
0 = ∇⋅ B
€
€ 0 = −∇⋅ [ρv] 0 = −∇⋅ ρvv - 1 BB + p + 1 B2 I +σ [ 4π ( 8π ) ] € 0 = −∇⋅ 1 ρv 2v + γ pv − 1 (v × B) × B +σ ⋅ v [ 2 γ −1 4π ] € 0 = −∇ × [v × B]
€ 0 = ∇⋅ B
€
€ v2
B1 B2
v1 0 = −∇⋅ [ρv] ρvn = const. B const. 0 = ∇⋅ B n = 0 = −∇⋅ ρvv - 1 BB + p + 1 B2 I +σ € [ 4π ( €8π ) ]
€ € 2 ρvn [[v]] − Bn[[B]]/4π +[[p + B /8π]]nˆ = 0 € ρvn [[v⊥]] = Bn[[B⊥]]/4π €
v2 € B1 B2
v1 0 = −∇⋅ [ρv] ρvn = const. B const. 0 = ∇⋅ B n = 0 = −∇⋅ ρvv - 1 BB + p + 1 B2 I +σ € [ 4π ( €8π ) ] € € ρvn [[v⊥]] = Bn[[B⊥]]/4π 0 = Bn[[B]]
€ Case 1: ρvn = 0
Case 1a: Bn = 0 € Case 2: Bn = 0 €
v2 Tangen al Discon nuity
B1 B2 Case 1b: [[ B ]] = 0
v1 Contact Discon nuity Case 1a: Tangen al Disc. 0 = −∇⋅ [ρv] ρvn = const.
vn = 0, Bn = 0 0 = ∇⋅ B Bn = const.
0 = −∇⋅ ρvv - 1 BB + p + 1 B€2 I +σ € 2 [ 4π ( 8π ) ] [[p + B /8π]]nˆ = 0 € €
J € €
An equilibrium current B1 v2 sheet separa ng uniform B fields w/ different angles. v 1 B2 • total pressure balance • possible shear
2 B1 /8π p2 p 2 1 B2 /8π Case 1b: Contact Disc. 0 = −∇⋅ [ρv] ρvn = const.
vn = 0, [[ B ]] = 0 0 = ∇⋅ B Bn = const. 0 = −∇⋅ ρvv - 1 BB + p + 1 B2 I +σ ˆ [ 4π ( 8π € ) ] € [[p]]n = 0 € € 0 = −∇ × [v × B] [[v⊥]] = 0 € € B € HOT COLD €
p p2 1 related to linear
T1 T2 waves w/ ω=0
entropy mode: [[ρ]]≠0 ρ1 ρ2 shear mode: [[vt]] ≠0 Case 2: perpendicular shock ρvn [[v⊥]] = Bn[[B⊥]]/4π
Bn = 0, vn ≠ 0 ⇒ v⊥,1 = v⊥,2 = v⊥ transform away 0 = −∇⋅ ρvv - 1 BB + p + 1 B2 I +σ 2 2 [ 4π ( 8π ) ]€ [[ρv + p + B /8π]] = 0
1 2 γ 1 € 0 = −∇⋅ ρv v + pv − (v × B) × B +σ ⋅ v [ 2 γ −1 4π ] 1 2 γ 1 2 € [[ 2 ρvnv + 1 pvn + 4 B vn ]] = 0 € γ − π
€ 0 = −∇ × [v × B] [[Bvn ]] = 0 v v 1 €2 € HD shock w/ 2 ``fluids’’ B1 B 2 €• plasma: γ=5/3 • mag. field: γ=2 p B1 B2 2 p1 Gabriel 1976
hot Bn = 0 Bn ≠ 0 vn = 0 Tangen al Contact discon nuity discon nuity cold vn ≠ 0 Perpendicular General shock MHD shock Case 3: General MHD shock ρvn [[v⊥]] = Bn[[B⊥]]/4π Bn ≠ 0, vn ≠ 0 ⇒ v⊥,1 ≠ v⊥,2
ρvn = const.≠ 0 0 = −∇⋅ [ρv] cannot transform away v⊥ € 0 = ∇⋅ B Bn = const.≠ 0 can transform to 1 1 2 € deHoffman-Teller frame 0 = −∇⋅ ρvv - 4π BB + (p + 8π B )I +σ [ € ] € vn,1 1 2 γ 1 v €= v − B € 0 = −∇⋅ 2 ρv v + γ −1 pv − 4π (v × B) × B +σ ⋅ v dHT ⊥,1 ⊥,1 [ € ] Bn,1 0 = −∇ × [v × B] € In dH-T frame: • v || B € 1 1 B2 € • E1 = v1 X B1 = 0 v1 € • E 2 = v2 X B2 = 0 B v2 1 • v2 || B2 • flow is parallel to field lines on both sides Shock characterized by 3 dimensionless Jump condi ons in pre-shock parameters: de Hoffman-Teller frame
v1 v1n ρvn [[v⊥]] − Bn[[B⊥]]/4π = 0 M = = 1A B / 4πρ B / 4πρ 2 2 1 1 1n 1 [[ρvn + p + B⊥ /8π]] = 0 ⎛ B ⎞ 1 2 γ −1 ⊥1 θ1 = tan ⎜ ⎟ [[ 2 ρvnv + γ −1 pvn ]] = 0 € ⎝ Bn1 ⎠ € p1 € β1 = 2 B1 /8π B2 € v1 € Use 3 jump. conds B v2 β β1 1 2 to solve for € θ2 downstream parameters θ1 MA2 θ2 β2 2 2 ρvn [[v⊥]] − Bn[[B⊥]]/4π = 0 [[(MA −1)tan θ]] = 0
2 2 eliminate θ2 in terms of θ1, MA1 and MA2 etc. un l… € €
B2 v1 B v2 β β1 1 2
θ2
θ1 NB: 2 2 0 • ρ2/ρ1 = MA1 / MA2 θ1 =30 β1=0.05 • region M A2 > MA1 (ρ2 < ρ1) disallowed by 2nd law thermo.
• M A2 = MA1 reps. 3 linear waves of MHD • each shock: flow faster (slower) than lin.
wave in region 1 (2) 3 MHD shocks
fast: MA1 > MA2 > 1 intermediate: MA1 > 1 > MA2 slow: 1 > MA1 > MA2 3 MHD shocks
fast: MA1 > MA2 > 1 intermediate: MA1 > 1 > MA2 slow: 1 > MA1 > MA2
2 2 [[(MA −1)tan θ]] = 0 2 B⊥2 tanθ2 MA1 −1 = = 2 B⊥1 tanθ1 MA 2 −1 € fast intermediate slow B2 B B2 B1 B1 2 B € 1
θ 2 θ 2 θ θ1 θ1 2 θ1
θ2 > θ1> 0 B1 < B2 θ1 > 0 > θ2 θ1 > θ2> 0 B1 > B2 B1 B1 FMW
SMW SAW θ1 θ1 quasi-parallel quasi-perpendicular o, o, θ1=20 β1=0.2 θ1=70 β1=0.2 B1 B1 FMW
SMW SAW θ1 θ1 quasi-parallel quasi-perpendicular o, o, θ1=20 β1=2.0 θ1=70 β1=2.0 Hypersonic limit
Magne c 4 pressure: only x16
Plasma pressure, no limit H-sphere: θ =84o, β =15 Fast Shocks 1 1 Observed Voyager I @ r=1.6 AU
(vesc = 34 km/s) T R 282 km/s 321 N 305 km/s
-3 7.6 cm-3 19 cm
M = 8.0/cos(θ ) A1 1 Vinas & Scudder 1986 ISEE-1 crosses bow shock
MA1 = 8.1/cos(θ1) o, θ1=74 β1=6
Vinas & Scudder 1986 Forward shock
Voyager 2 at r=2.17 AU
o, θ1=23 β1=1.7, MA1=2.4 Scudder et al. 1984
upstream downstream Gosling et al. 1994
=3.5 AU r
@ Ulysses 2 (1?) TDs 2 FM shocks Solar Fast Shocks
Type II Liu et al. 2009
n =107 cm-3 e Band spli ng reveals both 6 -3 ne=10 cm ne1 & ne2 Type III ne2/ne1=1.59
MA1~ 1.26-1.47 Solar Fast Shocks
Type II Liu et al. 2009
ground
7 -3 ne=10 cm 6 -3 ne=3 x 10 cm Band spli ng reveals both n =106 cm-3 n & n e Space (STEREO) e1 e2 Type III ne2/ne1=1.59
MA1~ 1.26-1.47 Slow shocks: reconnection
SS’ Lin & Lee 1999
p Model reconnection
Tsuneta and Naito 1998
Forbes, T.G., and Malherbe 1986 (v.2 ch. 6) Walthour et al. 1994
magnetopause: SS from reconnec on ISEE-1 at the B Intermediate Shocks z By Reconnec on between skewed fields Lin & Lee 1999
Petschek & Thorne 1967 Entropy’s Tale … the sequel
• A shock converts kinetic to thermal energy • How? What is the µ-physics? – Collisions (i.e. viscosity) – high enough density – Otherwise…(story not finished yet) • Instabilities, chaotic particle motion, … • Related to acceleration of non-thermal particles • Easier if particles gyrate near shock: quasi-perp. thermalizes easier than quasi-parallel Summary