Part IV: Space Weather | Chapter 14

Solar Energetic Particles

Diffusive shock acceleration, first-order Fermi, Parker transport, and SEP event types

14.1 Diffusive Shock Acceleration (DSA)

Derivation 1: First-Order Fermi Acceleration at a Shock

DSA is the primary mechanism for accelerating particles to high energies at CME-driven shocks. Particles gain energy by bouncing back and forth across the shock.

Step 1. A particle crossing the shock from upstream to downstream sees the downstream plasma approaching at relative speed \(\Delta v = v_1 - v_2 = v_1(1 - 1/s)\) where\(s = \rho_2/\rho_1\) is the compression ratio.

Step 2. The average fractional energy gain per shock crossing cycle:

$$\frac{\Delta E}{E} = \frac{4}{3}\frac{v_1 - v_2}{c} = \frac{4}{3}\frac{v_1}{c}\frac{s-1}{s}$$

Step 3. The probability of escape per cycle is \(P_{\text{esc}} = 4v_2/(cv_s)\) for relativistic particles. The resulting spectrum is a power law:

$$\boxed{f(p) \propto p^{-q}, \quad q = \frac{3s}{s-1}}$$

For a strong shock with \(s = 4\) (adiabatic, \(\gamma = 5/3\)):\(q = 4\), giving a differential energy spectrum \(dN/dE \propto E^{-2}\). This is remarkably close to observed SEP spectral indices.

14.2 Parker Transport Equation

Derivation 2: Focused Transport in the Heliosphere

Step 1. The Parker transport equation describes the propagation of energetic particles in the heliosphere including diffusion, convection, and energy changes:

$$\boxed{\frac{\partial f}{\partial t} = \nabla \cdot (\kappa \cdot \nabla f) - \mathbf{v}_{\text{sw}} \cdot \nabla f + \frac{1}{3}(\nabla \cdot \mathbf{v}_{\text{sw}})\frac{\partial f}{\partial \ln p} + Q}$$

The terms represent: (1) spatial diffusion along and across \(\mathbf{B}\), (2) convection with solar wind, (3) adiabatic energy changes, and (4) source term.

Step 2. The parallel mean free path depends on the turbulence spectrum:

$$\lambda_\parallel = \frac{3v}{8}\int_0^1 \frac{(1-\mu^2)^2}{D_{\mu\mu}} d\mu$$

where \(D_{\mu\mu}\) is the pitch-angle diffusion coefficient from wave-particle interactions. Typical values: \(\lambda_\parallel \sim 0.1\text{--}1\) AU for ~10 MeV protons.

14.3 SEP Event Types

Derivation 3: Impulsive vs Gradual Events

Step 1. Impulsive events: accelerated in flare reconnection regions. Characterized by electron-rich, \({}^3\text{He}\)-rich (\({}^3\text{He}/{}^4\text{He} \sim 1\), vs 0.0004 in solar wind), heavy-ion enhanced. Duration: hours.

Step 2. Gradual events: accelerated at CME-driven shocks. Proton-rich, composition similar to corona/solar wind. Duration: days. Can fill the inner heliosphere.

Impulsive Events

  • • Source: Flare reconnection
  • • Duration: hours
  • \({}^3\text{He}\) enriched (\(\times 10^3\))
  • • Fe/O enhanced
  • • Electron-rich
  • • Small spatial extent

Gradual Events

  • • Source: CME-driven shock
  • • Duration: days
  • • Normal composition
  • • Proton-rich
  • • Fills heliosphere
  • • Radiation hazard

14.4 Maximum Energy and Acceleration Time

Derivation 4: Hillas Criterion

Step 1. A particle can be accelerated only as long as its gyroradius is smaller than the accelerator size:

$$\boxed{E_{\max} = ZeBR \approx 300 Z B[\mu\text{T}] R[\text{AU}] \text{ MeV}}$$

For a CME shock with \(B \sim 100\) nT, \(R \sim 0.5\) AU:\(E_{\max} \sim 15\) GeV for protons, consistent with ground-level enhancement (GLE) events.

14.5 Acceleration Timescale

Derivation 5: DSA Acceleration Time

Step 1. The characteristic time for DSA to accelerate a particle to momentum \(p\):

$$\boxed{\tau_{\text{acc}} = \frac{3}{v_1 - v_2}\left(\frac{\kappa_1}{v_1} + \frac{\kappa_2}{v_2}\right) \ln\frac{p}{p_0}}$$

For typical parameters (\(v_1 = 1000\) km/s, \(\kappa \sim 10^{18}\) m\(^2\)/s):\(\tau_{\text{acc}} \sim 10^4\) s for 10 MeV protons, consistent with the observed onset times of gradual SEP events.

Numerical Simulation

SEPs: DSA Spectra, Intensity Profiles, Energy Gain, Composition

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14.6 Detailed DSA Power-Law Derivation

Deriving \(f(p) \propto p^{-3r/(r-1)}\) from Compression Ratio

Step 1. Consider a plane shock with upstream velocity \(u_1\) and downstream velocity \(u_2 = u_1/r\) where \(r\) is the compression ratio. In the shock frame, particles scatter isotropically in each frame.

Step 2. A particle crossing from upstream to downstream sees the downstream gas approaching at speed \(\Delta u = u_1 - u_2 = u_1(1-1/r)\). The fractional momentum gain per crossing (averaging over pitch angles):

$$\left\langle\frac{\Delta p}{p}\right\rangle_{\text{up}\to\text{down}} = \frac{2}{3}\frac{\Delta u}{v}$$

Step 3. Similarly crossing back from downstream to upstream gives the same gain. Per complete cycle (up\(\to\)down\(\to\)up):

$$\left\langle\frac{\Delta p}{p}\right\rangle_{\text{cycle}} = \frac{4}{3}\frac{u_1 - u_2}{v} = \frac{4}{3}\frac{u_1}{v}\frac{r-1}{r}$$

Step 4. The escape probability per cycle. Only particles moving away from the shock downstream can escape. The flux of particles crossing the shock from downstream to upstream vs escaping downstream:

$$P_{\text{esc}} = \frac{4u_2}{v} = \frac{4u_1}{rv}$$

Step 5. After \(n\) cycles: \(p = p_0(1+\epsilon)^n\) and\(N \propto (1-P_{\text{esc}})^n\). Eliminating \(n\):

$$N(>p) \propto \left(\frac{p}{p_0}\right)^{\ln(1-P_{\text{esc}})/\ln(1+\epsilon)}$$

Step 6. For small \(\epsilon\) and \(P_{\text{esc}}\):\(\ln(1-P_{\text{esc}})/\ln(1+\epsilon) \approx -P_{\text{esc}}/\epsilon\). Computing the ratio:

$$\frac{P_{\text{esc}}}{\epsilon} = \frac{4u_1/(rv)}{(4/3)(u_1/v)(r-1)/r} = \frac{3}{r-1}$$

Step 7. Therefore the differential spectrum:

$$\boxed{f(p) = \frac{dN}{dp} \propto p^{-q}, \quad q = \frac{3r}{r-1}}$$

For a strong adiabatic shock (\(\gamma=5/3\)): \(r=4\), \(q=4\), giving a differential energy spectrum \(dN/dE \propto E^{-2}\). This is remarkably universal: it depends only on the compression ratio, not on the details of the scattering or the shock speed.

14.7 Parker Transport Equation: Full Derivation

Physical Origin of Each Term

Step 1. Start from the focused transport equation for the phase-space density\(f(\mathbf{x}, p, t)\) of energetic particles in the solar wind:

$$\boxed{\frac{\partial f}{\partial t} = \underbrace{\nabla\cdot(\kappa\cdot\nabla f)}_{\text{diffusion}} - \underbrace{\mathbf{v}_{\text{sw}}\cdot\nabla f}_{\text{convection}} + \underbrace{\frac{1}{3}(\nabla\cdot\mathbf{v}_{\text{sw}})\,p\frac{\partial f}{\partial p}}_{\text{adiabatic cooling}} + \underbrace{Q}_{\text{source}}}$$

Term 1: Spatial diffusion. The diffusion tensor \(\kappa_{ij}\) has parallel and perpendicular components relative to \(\mathbf{B}\):

$$\kappa_\parallel = \frac{v\lambda_\parallel}{3}, \qquad \kappa_\perp \approx \frac{\kappa_\parallel}{1 + (\lambda_\parallel/r_g)^2}$$

Term 2: Convection. The solar wind carries particles outward at \(v_{\text{sw}} \sim 400\) km/s.

Term 3: Adiabatic cooling. In the expanding solar wind (\(\nabla\cdot\mathbf{v}_{\text{sw}} = 2v_{\text{sw}}/r > 0\)), particles lose energy as they do work against the expanding flow. This term causes spectral steepening at low energies.

Step 2. For a radial solar wind in 1D (neglecting perpendicular diffusion):

$$\frac{\partial f}{\partial t} = \frac{1}{r^2}\frac{\partial}{\partial r}\left(r^2\kappa_\parallel\frac{\partial f}{\partial r}\right) - v_{\text{sw}}\frac{\partial f}{\partial r} + \frac{2v_{\text{sw}}}{3r}\,p\frac{\partial f}{\partial p} + Q$$

This is the standard equation solved in SEP transport codes. The parallel mean free path\(\lambda_\parallel\) ranges from 0.01 AU (scatter-dominated) to 1 AU (nearly scatter-free) for 10-100 MeV protons, controlling the shape of the SEP intensity-time profile.

14.8 SEP Event Timeline: Impulsive vs Gradual

The diagram shows the characteristic intensity-time profiles of impulsive (flare) and gradual (CME-driven shock) SEP events.

Time after flare [hours]Particle Intensity061224364860Impulsive Event(flare electrons, 3He-rich)Gradual Event(CME-driven shock, proton-rich)ShockarrivalESP spikeFlareImpulsive (e-)Gradual (p+)

Comparison of impulsive and gradual SEP events. Impulsive events: rapid onset (minutes), short duration (hours), electron-rich, \({}^3\text{He}\)-enriched. Gradual events: slower onset, days-long duration, proton-rich, with ESP (energetic storm particle) enhancement at shock arrival.

Extended Simulation: DSA Spectra & SEP Intensity Profiles

Extended: DSA Spectra, Spectral Index, SEP Transport, Energy-Dependent Profiles

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