SH32B-08
Dropouts, spreading, and squeezing of solar particle distributions and space weather variability
Wednesday, 16 December 2015: 12:05
2009 (Moscone West)
David J Ruffolo, Department of Physics, Faculty of Science, Mahidol University, Bangkok, 10400, Thailand, William H Matthaeus, Department of Physics and Astronomy, University of Delaware, Newark, DE, United States, Achara Seripienlert, Rajamangala University of Technology Thanyaburi, Division of Physics, Faculty of Science, Pathum Thani, Thailand, Paisan Tooprakai, Chulalongkorn University, Department of Physics, Faculty of Science, Bangkok, Thailand and Piyanate Chuychai, School of Science, Mae Fah Luang University, Chiang Rai, 57100, Thailand
Abstract:
In the past 15 years, observations and theories concerning dropouts of solar energetic particles have made it clear that the lateral spread of field lines and particles from a given location near the Sun is not a purely diffusive process. Particles of low energy from impulsive solar events exhibit abrupt changes in flux (dropouts) due to filamentation of magnetic connection from the Sun, indicating that magnetic flux tube-like structures at least partially persist to Earth orbit. Our simulations based on a corresponding spherical two-component model of Alfv\’enic (slab) and 2D magnetic fluctuations indicate that such particles mostly follow field lines, which spread over ∼25∘ at Earth orbit, and exhibit dropout features. On the other hand, gradual solar events are of practical interest because they can produce greatly enhanced high-energy ion fluxes, which can cause radiation damage to satellites, spacecraft, and astronauts. While gradual events do not exhibit dropouts in the above sense, we show that the distribution of high-energy (E≥1 GeV) protons is squeezed toward magnetic flux tube-like structures with a specific polarity due to the structures’ conical shape. Since it is difficult to observationally determine what polarity of flux structure the Earth is in at a given time, this transport phenomenon contributes to event-to-event variability in ground level enhancements of GeV-range ions from solar storms, presenting a fundamental uncertainty in space weather prediction. Partially supported by the Thailand Research Fund (Grant BRG5880009), a Postdoctoral Fellowship from the Thailand Center of Excellence in Physics, a Research Fellowship from the Faculty of Science at Mahidol University, the U.S. NSF (AGS-1063439 and SHINE AGS-1156094), NASA (Heliophysics Theory NNX14AI63G, and LWS NNX15AB88G), and the Solar Probe Plus/ISIS project (D99031L).