JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

P (Space and Planetary Sciences) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM12] [EE] Space Weather, Space Climate, VarSITI

Tue. May 23, 2017 1:45 PM - 3:15 PM A01 (Tokyo Bay Makuhari Hall)

convener:Ryuho Kataoka(National Institute of Polar Research), Antti A Pulkkinen(NASA Goddard Space Flight Center), Kanya Kusano(Institute for Space-Earth Environmental Research, Nagoya University), Kazuo Shiokawa(Institute for Space-Earth Environmental Research, Nagoya University), Chairperson:Ryuho Kataoka(National Institute of Polar Research)

1:45 PM - 2:00 PM

[PEM12-34] Numerical study of solar prominence formation: the reconnection-condensation model

★Invited papers

*Takafumi Kaneko1, Takaaki Yokoyama1 (1.Graduate School of Science,The University of Tokyo,Department of Earth and Planetary Science)

We propose a model in which magnetic reconnection triggers radiative condensation for solar prominence formation and demonstrate it by three-dimensional magnetohydrodynamic (MHD) simulations including anisotropic nonlinear thermal conduction and optically thin radiative cooling.
Solar prominences are cool dense plasma clouds in the hot tenuous corona. Because prominences suddenly erupt and evolve into coronal mass ejections, they have potential to give an impact on the solar-terrestrial plasma environment. The formation mechanims of prominences as well as the eruption mechanism is still unclear. We propose a reconnection–condensation model in which the topological change of a coronal magnetic field via reconnection triggers radiative condensation for prominence formation. Previous observational studies suggested that reconnection at a polarity inversion line of a coronal arcade field creates a flux rope sustaining a prominence; however, the origin of the cool dense plasmas of a prominence was not clear. Using three-dimensional MHD simulations including anisotropic nonlinear thermal conduction and optically thin radiative cooling, we demonstrate that reconnection leads not only to flux rope formation but also to radiative condensation under a certain condition. This critical condition in our model is described by the Field length, which is defined as the scale length for thermal balance between radiative cooling and thermal conduction. This critical condition has a weak dependence on the artificial background heating. The extreme ultraviolet emissions through the filters of the Solar Dynamics Observatory Atmospheric Imaging Assembly synthesized with our simulation results have good agreement with observational signatures in previous studies.