Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/8559
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dc.contributor.authorBhatnagar, Aditi-
dc.contributor.authorvan der Voort, Luc Rouppe-
dc.contributor.authorJoshi, Jayant-
dc.date.accessioned2024-10-29T04:51:28Z-
dc.date.available2024-10-29T04:51:28Z-
dc.date.issued2024-09-
dc.identifier.citationAstronomy & Astrophysics, Vol. 689, A156en_US
dc.identifier.issn0004-6361-
dc.identifier.urihttp://hdl.handle.net/2248/8559-
dc.descriptionOpen Accessen_US
dc.descriptionOpen Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited-
dc.description.abstractContext. Quiet-Sun Ellerman bombs (QSEBs) are key indicators of small-scale photospheric magnetic reconnection events. Recent high-resolution observations have shown that they are ubiquitous and that large numbers of QSEBs can be found in the quiet Sun. Aims. We aim to understand the impact of QSEBs on the upper solar atmosphere by analyzing their spatial and temporal relationship with the UV brightenings observed in transition region diagnostics. Methods. We analyzed high-resolution Hβ observations from the Swedish 1-m Solar Telescope and utilized k-means clustering to detect 1423 QSEBs in a 51 min time series. We used coordinated and co-aligned observations from the Interface Region Imaging Spectrograph (IRIS) to search for corresponding signatures in the 1400 Å slit-jaw image (SJI) channel and in the Si IV 1394 Å and Mg II 2798.8 Å triplet spectral lines. We identified UV brightenings from SJI 1400 using a threshold of 5σ above the median background. Results. We focused on 453 long-lived QSEBs (> 1 min) and found 67 cases of UV brightenings from SJI 1400 occurring near the QSEBs, both temporally and spatially. Temporal analysis of these events indicates that QSEBs start before UV brightenings in 57% of cases, while UV brightenings lead in 36% of instances. The majority of the UV brightenings occur within 1000 km of the QSEBs in the direction of the solar limb. We also identify 21 QSEBs covered by the IRIS slit, four of which show emissions in the Si IV 1394 Å and/or Mg II 2798.8 Å triplet lines, at distances within 500 km of the QSEBs in the limb direction. Conclusions. We conclude that a small fraction (15%) of the long-lived QSEBs contribute to the localized heating observable in transition region diagnostics, indicating they play a minimal role in the global heating of the upper solar atmosphere.en_US
dc.language.isoenen_US
dc.publisherEDP Sciencesen_US
dc.relation.urihttps://doi.org/10.1051/0004-6361/202450070-
dc.rights© The Authors 2024-
dc.subjectSun: activityen_US
dc.subjectSun: atmosphereen_US
dc.subjectSun: magnetic fieldsen_US
dc.subjectSun: transition regionen_US
dc.titleTransition region response to quiet-Sun Ellerman bombsen_US
dc.typeArticleen_US
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