arXiv subjects

A. Sahade

Publications and source records attributed to A. Sahade.

4 recordsLinked to original sources

arXiv2025

Helmet streamer influence on the evolution of magnetic flux ropes

Context: Solar eruptions are crucial for space weather studies. Understanding the mechanisms influencing their evolution is key to improving predictions of their geoeffectiveness. Helmet streamers (HSs) are persistent structures in the solar corona, present in both minimum and maximum solar activity periods. These structures contain a current sheet of low magnetic energy, where coronal mass ejections (CMEs) tend to deflect. However, they also feature a closed magnetic field region beneath this sheet, often confining eruptions. Their complexity makes predicting eruptions challenging. Aims: This study examines how HSs influence the evolution and potential confinement of magnetic flux ropes (MFRs). We explore magnetic configurations where the MFR is more likely to rise through the overlying field, aiming to establish simple parameters that help predict whether an MFR will ascend or remain confined. Methods: Using 2.5D MHD simulations, we model MFR dynamics in the presence of an HS, analyzing different magnetic configurations and focusing on the mechanisms that enable ascent or confinement. Results: Null-point reconnection plays a key role in MFR dynamics. Depending on the initial configuration, it can either disrupt the MFR, preventing ascent, or reduce the strapping flux, facilitating upward motion. We identify a critical threshold: if the strapping flux above the MFR is less than two-thirds of its poloidal flux, the MFR ascends successfully. Conclusions: Our simulations show that null-point reconnection significantly impacts MFR ascent. A key predictor of successful rise is the initial ratio of the MFR's poloidal flux to the strapping flux above it.

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arXiv2024

Analysis of solar eruptions deflecting in the low corona: influence of the magnetic environment

Coronal mass ejections (CMEs) can exhibit non-radial evolution. The background magnetic field is considered the main driver for the trajectory deviation relative to the source region. The influence of the magnetic environment has been largely attributed to the gradient of the magnetic pressure. In this work, we propose a new approach to investigate the role of topology on CME deflection and to quantify and compare the action between the magnetic field gradient (`gradient' path) and the topology (`topological' path). We investigate 8 events simultaneously observed from Solar Orbiter, STEREO-A and SDO; and, with a new tracking technique, we reconstruct the 3D evolution of the eruptions. Then, we compare their propagation with the predictions from the two magnetic drivers. We find that the `topological' path describes the CME actual trajectory much better than the more traditional `gradient path'. Our results strongly indicate that the ambient topology may be the dominant driver for deflections in the low corona, and that presents a promising method to estimate the direction of propagation of CMEs early in their evolution.

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arXiv2022

Pseudostreamer influence on flux rope evolution

A critical aspect of solar activity is the coupling between eruptions and the surrounding coronal magnetic field, which determines the trajectory and morphology of the eruptive event. Pseudostreamers (PSs) are coronal magnetic structures formed by arcs of twin loops capped by magnetic field lines from coronal holes of the same polarity that meet at a central spine. They contain a single magnetic null point in the spine, potentially influencing the evolution of nearby flux ropes (FRs). To understand the net effect of the PS on FR eruptions is first necessary to study diverse and isolated FR-PS scenarios, which are not influenced by other magnetic structures. We performed numerical simulations in which a FR structure is in the vicinity of a PS magnetic configuration. The combined magnetic field of the PS and the FR results in the formation of two magnetic null points. We evolve this scenario by numerically solving the magnetohydrodynamic equations in 2.5D. The simulations consider a fully ionised compressible ideal plasma in the presence of a gravitational field and a stratified atmosphere. We find that the dynamic behaviour of the FR can be categorised into three different classes based on the FR trajectories and whether it is eruptive or confined. Our analysis indicates that the magnetic null points are decisive in the direction and intensity of the FR deflection and their hierarchy depends on the topological arrangement of the scenario. Moreover, the PS lobe acts as a magnetic cage enclosing the FR. We report that the total unsigned magnetic flux of the cage is a key parameter defining whether the FR is ejected or not.

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arXiv2020

Analysis of large deflections of prominence-CME events during the rising phase of solar cycle 24

Motivated by the need to improve the ability to forecast whether a certain coronal mass ejection (CME) is to impact Earth, and by the insufficiency of statistical studies that analyze the whole erupting system with the focus on the governing conditions under CME deflections, we performed a careful analysis of 13 events along a one-year time interval showing large deflections from their source region. We used telescopes imaging the solar corona at different heights and wavelengths on board the Project for Onboard Autonomy 2 (PROBA2), Solar Dynamics Observatory (SDO), Solar TErrestrial RElations Observatory (STEREO), Solar and Heliospheric Observatory (SOHO) spacecraft and from National Solar Observatory (NSO). By taking advantage of the quadrature position of these spacecraft from October 2010 until September 2011, we inspected the 3D trajectory of CMEs and their associated prominences with respect to their solar sources by means of a tie-pointing tool and a forward model. Considering the coronal magnetic fields as computed from a potential field source surface model, we investigate the roles of magnetic energy distribution and kinematic features in the non-radial propagation of both structures. The magnetic environment present during the eruption is found to be crucial in determining the trajectory of CMEs, in agreement with previous reports.

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