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Multi-thermal atmosphere of a mini-solar flare during magnetic reconnection observed with IRIS

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    SYSNO ASEP0548092
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleMulti-thermal atmosphere of a mini-solar flare during magnetic reconnection observed with IRIS
    Author(s) Joshi, R. (IN)
    Schmieder, B. (FR)
    Tei, A. (JP)
    Aulanier, G. (FR)
    Lörinčík, Juraj (ASU-R) ORCID
    Chandra, R. (IN)
    Heinzel, Petr (ASU-R) RID, ORCID
    Number of authors7
    Article numberA80
    Source TitleAstronomy & Astrophysics. - : EDP Sciences - ISSN 0004-6361
    Roč. 645, January (2021)
    Number of pages19 s.
    Publication formOnline - E
    Languageeng - English
    CountryFR - France
    Keywordsvariable source function ; cloud-model ; explosive events
    Subject RIVBN - Astronomy, Celestial Mechanics, Astrophysics
    OECD categoryAstronomy (including astrophysics,space science)
    R&D ProjectsGA19-09489S GA ČR - Czech Science Foundation (CSF)
    Method of publishingOpen access
    Institutional supportASU-R - RVO:67985815
    UT WOS000609886600001
    EID SCOPUS85099714631
    DOI10.1051/0004-6361/202039229
    AnnotationThe aim of this work is to study the fine structure and dynamics of the plasma at a jet base forming a mini-flare between two emerging magnetic fluxes (EMFs) observed with IRIS and the Solar Dynamics Observatory instruments.Methods. We proceed to a spatio-temporal analysis of IRIS spectra observed in the spectral ranges of Mg II, C II, and Si IV ions. Doppler velocities from Mg II lines were computed using a cloud model technique.Results. Strong asymmetric Mg II and C II line profiles with extended blue wings observed at the reconnection site (jet base) are interpreted by the presence of two chromospheric temperature clouds: one explosive cloud with blueshifts at 290 km s(-1) and one cloud with smaller Doppler shift (around 36 km s(-1)). Simultaneously at the same location (jet base), strong emission of several transition region lines (e.g. O IV and Si IV), emission of the Mg II triplet lines, and absorption of identified chromospheric lines in Si IV broad profiles have been observed and analysed.Conclusions. Such observations of IRIS line and continuum emissions allow us to propose a stratification model for the white light, mini-flare atmosphere with multiple layers of different temperatures along the line of sight in a reconnection current sheet. It is the first time that we could quantify the fast speed (possibly Alfvenic flows) of cool clouds ejected perpendicularly to the jet direction via the cloud model technique. We conjecture that the ejected clouds come from plasma which was trapped between the two EMFs before reconnection or be caused by chromospheric-temperature (cool) upflow material similar to a surge during reconnection.
    WorkplaceAstronomical Institute
    ContactRadka Svašková, bibl@asu.cas.cz, Tel.: 323 620 326
    Year of Publishing2022
    Electronic addresshttp://hdl.handle.net/11104/0324208
Number of the records: 1  

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