Author: T. Laitinen, S. Dalla and J. Kelly,

Jeremiah Horrocks Institute, University of Central Lancashire, Preston

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### Introduction

Energetic ions and electrons accelerated during solar flares and coronal mass ejections constitute a significant component in eruption energetics and phenomena. When propagating away from the Sun in the interplanetary medium, to be observed near the Earth, the charged particles scatter due to magnetic field turbulence. In order to use particle observations to understand how the particle acceleration and release are related to eruption characteristics at the Sun, we must also understand the effects of interplanetary particle transport in the turbulent field.

Recent observations of solar energetic particle events at large longitudinal separation, as shown in Figure 1, reveal that the particles can be detected over a very wide longitudinal range [1]. This presents a challenge to current theoretical models of particle transport, in particular for particle propagation across the mean interplanetary magnetic field.

Typically, studies of solar energetic particles use a very idealised description of the interplanetary magnetic field through which the particles propagate. In this nugget we investigate how a moreT realistic model of the field, which includes structured, nonlinearly evolving turbulence, affects energetic particle transport. We investigate particle propagation in this field, and compare our results on cross-field propagation to those obtained from an idealised field description. To describe the field, we have introduce the concept of turbulent envelopes [3].

### Model of Enveloped Turbulence

Idealised descriptions of the interplanetary turbulence usually assume uniform, homogeneous magnetic turbulence, overlaid on a constant background magnetic field. In reality, solar wind turbulence is evolving non-linearly and is permeated by transient structures [2]. In our model of ‘enveloped turbulence’, the field perturbations are structured, with varying amplitude in the direction along the magnetic field. The composition of the turbulence is allowed to vary from one envelope to another, mimicking non-linear evolution.

The turbulence is enveloped into cosine-shape envelopes, which introduces spatial variation in the amplitude of the turbulence in the mean field direction, characterised by envelope length *L _{p}* and density

*ρ*(Figure 2). In this description, the homogeneous turbulence model would be described by infinite values of these parameters, and a spatially constant total amplitude (thick solid curve in Figure 2). The turbulent envelopes contain a sum of Fourier modes that form a Kolmogorov wavenumber spectrum (see [3] and [4] for details).

_{p}The phase of the waves can also be varied between envelopes, and we consider two models for this. In the *modulated wavefield* model, the phases of the waves are coherent throughout the simulation space, and thus the amplitude of the turbulence is only modulated by the sum of the envelopes (the thick black curves in Figure 2). In the *random envelope* model, we break the coherence by randomising phases and wave vector directions in the different envelopes.

In Figure 3, we plot magnetic field lines to show how the enveloping affects the spreading of the field. The *modulated amplitude* model (middle panel) does not differ qualitatively from the homogeneous model (top panel). In the *random envelope* model (bottom panel), the field lines have a considerably smaller spread. This is caused by the loss of coherence of the 2D wave modes, which have their wave vectors perpendicular to the mean magnetic field [3].

### Effect of the structured turbulence on energetic particles

We use full-orbit test particle simulations to study the particle propagation in these turbulence models, and collect particle statistics so that we can investigate the spreading – or diffusion – of the energetic particle distribution. The diffusion coefficients κ_{ζζ} are calculated from the definition:

κ_{ζζ}=<Δζ²>/2*t*, ζ=*x, y, z*,

where Δζ² is the square of the particle displacement in direction ζ at time *t*, *z* is the direction of the mean magnetic field, and the <> denotes ensemble average over the simulated particles. Our results are also compared to those obtained using the homogeneous model. We set the mean magnetic energy density over a large spatial range to be the same in all cases.

*random envelope*model has a significant effect, and is most pronounced for short envelopes (small

*L*). Strong overlap of the envelopes, characterised by larger

_{p}*ρ*, results in a less pronounced effect, as the turbulence approaches the homogeneous description, in particular with the

_{p}*modulated wavefield*model.

### Conclusions

The characteristics of the interplanetary turbulence affect the energetic particle propagation parameters significantly. In this work, we have shown that the inclusion of structuring is very important and reduces the perpendicular diffusion coefficient by up to an order of magnitude. In particular, the effect is strong when, with the help of the spatially changing random wave phases, we break the large-scale coherence of the waves. Our work demonstrates that treatments which ignore the presence of structure and non-linear evolution of the field can significantly overestimate the perpendicular diffusion coefficient. As a result, structuring of the turbulence does not provide an explanation for the observed widely-separated particle events, and perhaps we must look to other properties of the interplanetary magnetic field and turbulence.

The work is described in detail in [3].

### References

- [1] Dresing, N., et al., 2012, Solar Physics, In Press, DOI: 10.1007/s11207-012-0049-y
- [2] Rouillard, A. P., et al., 2010, Journal of Geophysical Research (Space Physics), 115, A04103
- [3] Laitinen, T., Dalla, S., & Kelly. J., 2012, ApJ, 749, 103
- [4] Giacalone, J., & Jokipii, J. R., 1999, ApJ, 520, 204