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L1 observations and geoeffectivity consecutive to the frontside halo coronal mass ejections (CMEs) of year 2002

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    0558947 - ÚFA 2023 DE eng A - Abstract
    Grison, Benjamin - Cornilleau-Wehrlin, N. - Bocchialini, K. - Schmieder, B.
    L1 observations and geoeffectivity consecutive to the frontside halo coronal mass ejections (CMEs) of year 2002.
    EGU General Assembly 2022. Göttingen: European Geosciences Union, 2022. EGU22-4595.
    [EGU22 FAQs. 23.05.2022-27.05.2022, Vienna]
    EU Projects: European Commission(XE) 870437 - SafeSpace
    Institutional support: RVO:68378289
    Keywords : coronal mass ejection (CME) * halo CME * sudden storm commencements (SSCs)
    OECD category: Fluids and plasma physics (including surface physics)
    https://doi.org/10.5194/egusphere-egu22-4595

    Bocchialini et al. (2018) showed that among the 28 frontside halo coronal mass ejections (CMEs)
    with a visible source seen on the Sun in 2002, 21 are unambiguously associated with sudden
    storm commencements (SSCs). Based on velocity comparisons (LASCO, L1, and ballistic velocities),
    we look for association between these 28 halo CMEs and shock-like discontinuities observed in
    solar wind and interplanetary magnetic field (IMF) observations at L1. Geoeffectivity is tested on
    Dst, am, PCN, and auroral indices responses.
    The present work complements the Boochialini's study by analysing systematically all the 28 halo
    CMEs, including the seven halos CMEs not associated with SSCs. Source locations, potential L1
    signatures and geoeffectivity of these seven halo CMEs provide an overview of the properties
    related to halo CMEs in 2002, complementing Boccialini's et al. results. None of the discontinuities
    possibly associated to each of the seven halo CMEs corresponds to a clear ICME signature, based
    on our observations and on existing catalogs, showing that the central regions of the halo CMEs
    are not passing L1.
    From the L1 observations of frontside CME halos observed in 2002, we conclude that halo CMEs
    not associated with SSCs in 2002 are non-geoeffective. We also note that all halo CMEs observed in
    2002 and associated with ICMEs or magnetic clouds at L1 are also associated with SSCs. lders. The
    work leading to this paper has received funding from the European Union’s Horizon 2020 research
    and innovation programme under grant agreement No 870437 for the SafeSpace (Radiation Belt
    Environmental Indicators for the Safety of Space Assets) project.

    Permanent Link: https://hdl.handle.net/11104/0332429

     
     
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