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Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event

We report on the source of [Formula: see text] protons during the SOL2014-09-01 sustained gamma-ray emission (SGRE) event based on multi-wavelength data from a wide array of space- and ground-based instruments. Based on the eruption geometry we provide concrete explanation for the spatially and temp...

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Autores principales: Gopalswamy, N., Mäkelä, P., Yashiro, S., Akiyama, S., Xie, H., Thakur, N.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7004439/
https://www.ncbi.nlm.nih.gov/pubmed/32109973
http://dx.doi.org/10.1007/s11207-020-1590-8
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author Gopalswamy, N.
Mäkelä, P.
Yashiro, S.
Akiyama, S.
Xie, H.
Thakur, N.
author_facet Gopalswamy, N.
Mäkelä, P.
Yashiro, S.
Akiyama, S.
Xie, H.
Thakur, N.
author_sort Gopalswamy, N.
collection PubMed
description We report on the source of [Formula: see text] protons during the SOL2014-09-01 sustained gamma-ray emission (SGRE) event based on multi-wavelength data from a wide array of space- and ground-based instruments. Based on the eruption geometry we provide concrete explanation for the spatially and temporally extended [Formula: see text] -ray emission from the eruption. We show that the associated flux rope is of low inclination (roughly oriented in the east–west direction), which enables the associated shock to extend to the frontside. We compare the centroid of the SGRE source with the location of the flux rope’s leg to infer that the high-energy protons must be precipitating between the flux rope leg and the shock front. The durations of the SOL2014-09-01 SGRE event and the type II radio burst agree with the linear relationship between these parameters obtained for other SGRE events with duration [Formula: see text] . The fluence spectrum of the SEP event is very hard, indicating the presence of high-energy (GeV) particles in this event. This is further confirmed by the presence of an energetic coronal mass ejection with a speed [Formula: see text] , similar to those in ground level enhancement (GLE) events. The type II radio burst had emission components from metric to kilometric wavelengths as in events associated with GLE events. All these factors indicate that the high-energy particles from the shock were in sufficient numbers needed for the production of [Formula: see text] -rays via neutral pion decay.
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spelling pubmed-70044392020-02-25 Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event Gopalswamy, N. Mäkelä, P. Yashiro, S. Akiyama, S. Xie, H. Thakur, N. Sol Phys Editor’s Choice We report on the source of [Formula: see text] protons during the SOL2014-09-01 sustained gamma-ray emission (SGRE) event based on multi-wavelength data from a wide array of space- and ground-based instruments. Based on the eruption geometry we provide concrete explanation for the spatially and temporally extended [Formula: see text] -ray emission from the eruption. We show that the associated flux rope is of low inclination (roughly oriented in the east–west direction), which enables the associated shock to extend to the frontside. We compare the centroid of the SGRE source with the location of the flux rope’s leg to infer that the high-energy protons must be precipitating between the flux rope leg and the shock front. The durations of the SOL2014-09-01 SGRE event and the type II radio burst agree with the linear relationship between these parameters obtained for other SGRE events with duration [Formula: see text] . The fluence spectrum of the SEP event is very hard, indicating the presence of high-energy (GeV) particles in this event. This is further confirmed by the presence of an energetic coronal mass ejection with a speed [Formula: see text] , similar to those in ground level enhancement (GLE) events. The type II radio burst had emission components from metric to kilometric wavelengths as in events associated with GLE events. All these factors indicate that the high-energy particles from the shock were in sufficient numbers needed for the production of [Formula: see text] -rays via neutral pion decay. Springer Netherlands 2020-02-04 2020 /pmc/articles/PMC7004439/ /pubmed/32109973 http://dx.doi.org/10.1007/s11207-020-1590-8 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Editor’s Choice
Gopalswamy, N.
Mäkelä, P.
Yashiro, S.
Akiyama, S.
Xie, H.
Thakur, N.
Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title_full Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title_fullStr Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title_full_unstemmed Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title_short Source of Energetic Protons in the 2014 September 1 Sustained Gamma-ray Emission Event
title_sort source of energetic protons in the 2014 september 1 sustained gamma-ray emission event
topic Editor’s Choice
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7004439/
https://www.ncbi.nlm.nih.gov/pubmed/32109973
http://dx.doi.org/10.1007/s11207-020-1590-8
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