Abstract
A common assumption in particle transport theory is the assumption of diffusive
propagation, corresponding to a linear increase of the mean square displacement of particle
orbits with time. In recent years, however, several authors have discovered nondiffusive
transport in observations and in test particle simulations. Some analytical theories also
predict subdiffusion or superdiffusion of charged particles. In this article, a recently
developed test particle code is employed to explore diffusive and nondiffusive transport
regimes. For slab, two‐component, and isotropic turbulence the simulations are performed
for different particle energies. It is demonstrated that, in most cases, cross‐field transport
is indeed subdiffusive. The level of subdiffusivity is sensitively controlled by the turbulence
geometry.
| Original language | English |
|---|---|
| Pages (from-to) | A03104/1-A03104/7 |
| Number of pages | 7 |
| Journal | Journal of Geophysical Research: Atmospheres |
| Volume | 115 |
| DOIs | |
| Publication status | Published - 2010 |
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