4.7 Article

2010 AUGUST 1-2 SYMPATHETIC ERUPTIONS. I. MAGNETIC TOPOLOGY OF THE SOURCE-SURFACE BACKGROUND FIELD

Journal

ASTROPHYSICAL JOURNAL
Volume 759, Issue 1, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/0004-637X/759/1/70

Keywords

magnetic reconnection; solar wind; Sun: coronal mass ejections (CMEs); Sun: flares; Sun: magnetic topology

Funding

  1. NASA
  2. SHINE under NSF [AGS-1156119]
  3. CISM (an NSF Science and Technology Center)
  4. Lockheed-Martin
  5. NSF [ATM-0837519]
  6. NASA [NNX09AG27G]
  7. Directorate For Geosciences
  8. Div Atmospheric & Geospace Sciences [1156119] Funding Source: National Science Foundation
  9. NASA [118073, NNX09AG27G] Funding Source: Federal RePORTER

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A sequence of apparently coupled eruptions was observed on 2010 August 1-2 by Solar Dynamics Observatory and STEREO. The eruptions were closely synchronized with one another, even though some of them occurred at widely separated locations. In an attempt to identify a plausible reason for such synchronization, we study the large-scale structure of the background magnetic configuration. The coronal field was computed from the photospheric magnetic field observed at the appropriate time period by using the potential field source-surface model. We investigate the resulting field structure by analyzing the so-called squashing factor calculated at the photospheric and source-surface boundaries, as well as at different coronal cross-sections. Using this information as a guide, we determine the underlying structural skeleton of the configuration, including separatrix and quasi-separatrix surfaces. Our analysis reveals, in particular, several pseudo-streamers in the regions where the eruptions occurred. Of special interest to us are the magnetic null points and separators associated with the pseudo-streamers. We propose that magnetic reconnection triggered along these separators by the first eruption likely played a key role in establishing the assumed link between the sequential eruptions. The present work substantiates our recent simplified magnetohydrodynamic model of sympathetic eruptions and provides a guide for further deeper study of these phenomena. Several important implications of our results for the S-web model of the slow solar wind are also addressed.

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