Runaway electrons from a 'beam-bulk' model of streamer: Application to TGFs

dc.bibliographicCitation.articleNumber055003
dc.bibliographicCitation.firstPage055003
dc.bibliographicCitation.issue5
dc.bibliographicCitation.journalTitleEnvironmental Research Letters
dc.bibliographicCitation.volume9
dc.contributor.authorChanrion, O.
dc.contributor.authorBonaventura, Z.
dc.contributor.authorÇinar, D.
dc.contributor.authorBourdon, A.
dc.contributor.authorNeubert, T.
dc.date.accessioned2025-03-03T12:23:10Z
dc.date.available2025-03-03T12:23:10Z
dc.date.issued2014
dc.description.abstractThe generation of x- and gamma-rays in atmospheric discharges has been studied intensively since the discovery of terrestrial gamma-ray flashes (TGFs) by the Compton gamma-ray Observatory in 1991. Emissions are bremsstrahlung from high energy particles accelerated in large scale atmospheric electric fields associated with thunderstorms. Whereas observations now are many, both from lightning and the laboratory, the phases of the discharge where emissions are generated are still debated and several processes for electron acceleration have been put forward by theorists. This paper address the electron acceleration in streamer region of lightning. We present the first 'beam-bulk' model of self-consistent streamer dynamics and electron acceleration. The model combines a Monte Carlo Collision code that simulates the high-energy electrons (>100 eV) and a fluid code that simulates the bulk of the low-energy electrons and ions. For a negative streamer discharge, we show how electrons are accelerated in the large electric field in the tip of the streamer and travel ahead of the streamer where they ionize the gas. In comparison to the results obtained with a classical fluid model for a negative streamer, the beambulk model predicts a decrease of the magnitude of the peak electric field and an increase of the streamer velocity. Furthermore, we show that a significant number of runaway electrons is lost by diffusion outside of the streamer tip. The results presented here do not yet include extra amplification nor acceleration far away from the streamer to explain the electron energies seen in TGFs. Still, in the light of those results, we emphasize that the production of runaway electrons from streamers needs to be simulated including the self-consistent feedback of runaways on the streamer. Simulations with a beam-bulk model may not only help to understand the fundamental atmospheric processes behind TGFs, but also pave the way for the interpretation of remote sensing of the most energetic discharges in the Earth's atmosphere and thus help to address their environmental impact. © 2014 IOP Publishing Ltd.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/18721
dc.identifier.urihttps://doi.org/10.34657/17740
dc.language.isoeng
dc.publisherBristol : IOP Publ.
dc.relation.doihttps://doi.org/10.1088/1748-9326/9/5/055003
dc.relation.essn1748-9326
dc.rights.licenseCC BY 3.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/3.0
dc.subject.ddc690
dc.subject.otheratmospheric electricityeng
dc.subject.otherdrift diffusion methodseng
dc.subject.otherMonte Carlo methodseng
dc.subject.otherstreamer dischargeeng
dc.subject.otherTGFeng
dc.titleRunaway electrons from a 'beam-bulk' model of streamer: Application to TGFseng
dc.typeArticle
dc.typeText
tib.accessRightsopenAccess
wgl.contributorINP
wgl.subjectPhysikger
wgl.typeZeitschriftenartikelger
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