formation of hot channels in pre-cme coronal flux ropes and their role in the onset of eruptions

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Formation of hot channels in pre- CME coronal flux ropes and their role in the onset of eruptions Yuhong Fan and Piyali Chatterjee High Altitude Observatory, National Center for Atmospheric Research

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Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions . Yuhong Fan and Piyali Chatterjee High Altitude Observatory, National Center for Atmospheric Research. Simulation set up. - PowerPoint PPT Presentation

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Page 1: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Formation of hot channels in pre-CME coronal flux ropes and their role in the

onset of eruptions

Yuhong Fan and Piyali ChatterjeeHigh Altitude Observatory, National Center for Atmospheric Research

Page 2: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Simulation set up• Numerically solve the following MHD equations, assuming a perfect gas

with adiabatic index g = 1.1 for the coronal plasma:

• Solve the total energy equation in conservative form and include thermal conduction along magnetic field lines

• The domain is resolved by a non-uniform grid of 432x192x240

• Initially the corona is a static isothermal atmosphere at 1MK with a pre-existing potential arcade field, with cs=135 km/s, va0=1951km/s.

• At the lower boundary, we impose (kinematically) the emergence of a twisted torus for t=0 to t=tstp after which the emergence is stopped and the field lines are rigidly anchored subsequently

Spherical coronal simulationdomain :

r∈ Rs, 5.496Rs[ ],

θ ∈ 5π /12, 7π /12[ ],

φ∈ −π /9.6, π /9.6[ ]

Fan (2012)

Page 3: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions
Page 4: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Hyperbolic flux tube (HFT) (e.g. Titov 2002, Savcheva et al. 2012)

• Strongest current layers form along QSLs with very large squashing factor Q, which measures the “squashing” of the flux tube cross-section as it is mapped from one foot point to the other (Titov et al. 2002; Titov 2007; Pariat & Demoulin 2012).

Orange surfaces : iso - surfaces of J/B = 1/(10 gridsize),Pink surface : iso - surface of T =1.2 MK

Page 5: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions
Page 6: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

AIA 171 AIA 193

Reversed AIA images from Regnier et al. (2011)

AIA 211

Page 7: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Berger (2012)Regnier et al. (2011)

U-shape or horns

Page 8: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions
Page 9: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Observation of a hot channel prior to and during a CME: “driver” of the eruption (Zhang et al. 2012, Cheng et al. 2013)

Page 10: Formation of hot channels in pre-CME coronal flux ropes and their role in the onset of eruptions

Summary

• A sigmoid-shaped vertical current layer forms along the QSL underlying the pre-eruption coronal flux rope

• Reconnections in the current layer effectively add twisted flux to the flux rope and thus allow it to rise quasi-statically

• As a result of such tether-cutting reconnections a central hot, low-density channel containing reconnected, twisted flux threading under the flux rope axis form on top of the central current layer.

• When viewed in the line of sight roughly aligned with the hot channel, the current layer appears as a high-density vertical column with upward extensions as a “U” shaped dense shell (or “horns”) enclosing a central hot, low-density void.