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dc.contributor.authorPagano, Paolo
dc.contributor.authorMackay, Duncan Hendry
dc.contributor.authorYardley, Stephanie Louise
dc.date.accessioned2019-10-10T11:30:05Z
dc.date.available2019-10-10T11:30:05Z
dc.date.issued2019-11-22
dc.identifier260661788
dc.identifier0634b9bd-1a39-461b-a28c-0afcaa3a3956
dc.identifier85077356630
dc.identifier000499380000001
dc.identifier.citationPagano , P , Mackay , D H & Yardley , S L 2019 , ' A space weather tool for identifying eruptive active regions ' , Astrophysical Journal , vol. 886 , no. 2 , 81 . https://doi.org/10.3847/1538-4357/ab4cf1en
dc.identifier.issn0004-637X
dc.identifier.otherORCID: /0000-0001-6065-8531/work/66069971
dc.identifier.urihttps://hdl.handle.net/10023/18639
dc.descriptionFunding: UK Science and Technology Facilities Council (UK) through the consolidated grant ST/N000609/1 and the European Research Council (ERC) under the European Union Horizon 2020 research and innovation program (grant agreement No. 647214); UK STFC via the Consolidated Grant SMC1/YST025 and SMC1/YST037 (S.L.Y.); UK STFC and the ERC (SynergyGrant: WHOLE SUN, Grant Agreement No. 810218) for financial support (DHM).en
dc.description.abstractOne of the main goals of solar physics is the timely identification of eruptive active regions. Space missions such as Solar Orbiter or future Space Weather forecasting missions would largely benefit from this achievement.Our aim is to produce a relatively simple technique that can provide real time indications or predictions that an active region will produce an eruption. We expand on the theoretical work of Pagano et al.(2019) that was able to distinguish eruptive from non-eruptive active regions.From this we introduce a new operational metric that uses a combination of observed line-of-sight magnetograms, 3D data-driven simulations and the projection of the 3D simulations forward in time. Results show that the new metric correctly distinguishes active regions as eruptive when observable signatures of eruption have been identified and as non-eruptive when there are no observable signatures of eruption. After successfully distinguishing eruptive from non-eruptive active regions we illustrate how this metric may be used in a “real-time” operational sense were three levels of warning are categorised. These categories are: high risk (red), medium risk (amber) and low risk (green) of eruption. Through considering individual cases we find that the separation into eruptive and non-eruptive active regions is more robust the longer the time series of observed magnetograms used to simulate the build up of magnetic stress and free magnetic energy within the active region. Finally, we conclude that this proof of concept study delivers promising results where the ability to categorise the risk of an eruption is a major achievement.
dc.format.extent323747
dc.language.isoeng
dc.relation.ispartofAstrophysical Journalen
dc.subjectSolar active regionsen
dc.subjectSolar coronal mass ejectionsen
dc.subjectSpace weatheren
dc.subjectSolar magnetic fieldsen
dc.subjectSolar active region magnetic fieldsen
dc.subjectQB Astronomyen
dc.subjectQC Physicsen
dc.subject3rd-NDASen
dc.subject.lccQBen
dc.subject.lccQCen
dc.titleA space weather tool for identifying eruptive active regionsen
dc.typeJournal articleen
dc.contributor.sponsorEuropean Research Councilen
dc.contributor.sponsorScience & Technology Facilities Councilen
dc.contributor.sponsorScience & Technology Facilities Councilen
dc.contributor.sponsorScience & Technology Facilities Councilen
dc.contributor.institutionUniversity of St Andrews. Applied Mathematicsen
dc.identifier.doi10.3847/1538-4357/ab4cf1
dc.description.statusPeer revieweden
dc.identifier.grantnumber810218en
dc.identifier.grantnumberN/Aen
dc.identifier.grantnumberST/S000402/1en
dc.identifier.grantnumberST/N000609/1en


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