On Flare-CME Characteristics from Sun to Earth Combining Remote-Sensing Image Data with In Situ Measurements Supported by Modeling

• Published in: Solar physics 2017-07, Vol.292 (7), p.93-93, Article 93
• Main Authors: Temmer, Manuela, Thalmann, Julia K., Dissauer, Karin, Veronig, Astrid M., Tschernitz, Johannes, Hinterreiter, Jürgen, Rodriguez, Luciano
• Format: Article
• Language: English
• Subjects: Astronomical instruments; Astrophysics and Astroparticles; Atmospheric models; Atmospheric Sciences; Coronal mass ejection; Cylindrical shells; Dimming; Earth-affecting Solar Transients; Erosion; Evolution; Fluctuations; Ground-based observation; Helicity; In situ measurement; Interplanetary space; Magnetic clouds; Magnetic fields; Magnetic flux; Magnetic reconnection; Magnetism; Measurement; Nonlinear dynamics; Observatories; Physics; Physics and Astronomy; Reconstruction; Remote sensing; SOHO Mission; Solar activity; Solar corona; Solar flares; Solar observatories; Solar physics; Space Exploration and Astronautics; Space Sciences (including Extraterrestrial Physics; Sun; Three dimensional models
• ISSN: 0038-0938; 1573-093X
• DOI: 10.1007/s11207-017-1112-5

We analyze the well-observed flare and coronal mass ejection (CME) from 1 October 2011 (SOL2011-10-01T09:18) covering the complete chain of effects – from Sun to Earth – to better understand the dynamic evolution of the CME and its embedded magnetic field. We study in detail the solar surface and atmosphere associated with the flare and CME using the Solar Dynamics Observatory (SDO) and ground-based instruments. We also track the CME signature off-limb with combined extreme ultraviolet (EUV) and white-light data from the Solar Terrestrial Relations Observatory (STEREO). By applying the graduated cylindrical shell (GCS) reconstruction method and total mass to stereoscopic STEREO-SOHO ( Solar and Heliospheric Observatory ) coronagraph data, we track the temporal and spatial evolution of the CME in the interplanetary space and derive its geometry and 3D mass. We combine the GCS and Lundquist model results to derive the axial flux and helicity of the magnetic cloud (MC) from in situ measurements from Wind . This is compared to nonlinear force-free (NLFF) model results, as well as to the reconnected magnetic flux derived from the flare ribbons (flare reconnection flux) and the magnetic flux encompassed by the associated dimming (dimming flux). We find that magnetic reconnection processes were already ongoing before the start of the impulsive flare phase, adding magnetic flux to the flux rope before its final eruption. The dimming flux increases by more than 25% after the end of the flare, indicating that magnetic flux is still added to the flux rope after eruption. Hence, the derived flare reconnection flux is most probably a lower limit for estimating the magnetic flux within the flux rope. We find that the magnetic helicity and axial magnetic flux are lower in the interplanetary space by ∼ 50% and 75%, respectively, possibly indicating an erosion process. A CME mass increase of 10% is observed over a range of ∼ 4 – 20 R ⊙ . The temporal evolution of the CME-associated core-dimming regions supports the scenario that fast outflows might supply additional mass to the rear part of the CME.