Electron acceleration above thunderclouds

Autor: Andrew Mezentsev, Christiane Helling, Oscar van der Velde, Giles Harrison, Michel Parrot, Radek Lan, Serge Soula, Ludek Uhlir, William Rison, Declan A. Diver, Alec Bennett, Ondrej Santolik, Enrico Arnone, Ivana Kolmasova, Jean Louis Pinçon, Martin Füllekrug, Ferruccio Zanotti, Thomas Farges, József Bór
Přispěvatelé: Department of Electronics and Electrical Engineering [Bath], University of Bath [Bath], Institute of Atmospheric Physics [Prague] (IAP), Czech Academy of Sciences [Prague] (CAS), Faculty of Mathematics and Physics [Praha/Prague], Charles University [Prague] (CU), DAM Île-de-France (DAM/DIF), Direction des Applications Militaires (DAM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Research Centre for Astronomy and Earth Sciences [Budapest], Hungarian Academy of Sciences (MTA), Bristol Industrial and Research Associates Ltd, Portishead, Bristol, UK, Laboratoire de physique et chimie de l'environnement (LPCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), New Mexico Institute of Mining and Technology [New Mexico Tech] (NMT), Italian Meteor and TLE Network, Ferrara, Italy, Laboratoire de Génie Civil et Génie Mécanique (LGCGM), Université de Rennes (UR)-Institut National des Sciences Appliquées - Rennes (INSA Rennes), Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA), Department of Meteorology [Reading], University of Reading (UOR), Laboratoire d'aérologie (LAERO), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Electrical Engineering Departement, Technical University of Catalogna, SUPA School of Physics and Astronomy [University of St Andrews], University of St Andrews [Scotland]-Scottish Universities Physics Alliance (SUPA), SUPA School of Physics and Astronomy [Glasgow], University of Glasgow, European Research Council, Science & Technology Facilities Council, University of St Andrews. School of Physics and Astronomy, Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut National des Sciences Appliquées - Rennes (INSA Rennes), Institut National des Sciences Appliquées (INSA)-Université de Rennes (UNIV-RENNES)-Institut National des Sciences Appliquées (INSA), Centre National de la Recherche Scientifique (CNRS)-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées
Jazyk: angličtina
Rok vydání: 2013
Předmět:
Zdroj: Environmental research letters 8 (2013). doi:10.1088/1748-9326/8/3/035027
info:cnr-pdr/source/autori:Fullekrug M.; Kolmasova I.; Santolik O.; Farges T.; Bor J.; Bennett A.; Parrot M.; Rison W.; Zanotti F.; Arnone E.; Mezentsev A.; Lan R.; Uhlir L.; Harrison G.; Soula S.; Van Der Velde O.; Pincon J.-L.; Helling C.; Diver D./titolo:Electron acceleration above thunderclouds/doi:10.1088%2F1748-9326%2F8%2F3%2F035027/rivista:Environmental research letters/anno:2013/pagina_da:/pagina_a:/intervallo_pagine:/volume:8
Environmental Research Letters
Environmental Research Letters, 2013, 8 (3), pp.035027. ⟨10.1088/1748-9326/8/3/035027⟩
Environmental Research Letters, IOP Publishing, 2013, 8 (3), pp.035027. ⟨10.1088/1748-9326/8/3/035027⟩
Fullekrug, M, Kolmasova, I, Santolik, O, Farges, T, Bor, J, Bennett, A J, Parrot, M, Rison, M, Zanotti, F, Arnone, E, Mezentsev, A, Lan, R, Uhlir, L, Harrison, G, Soula, S, van der Velde, O A, Pincon, J-L, Helling, C & Diver, D 2013, ' Electron acceleration above thunderclouds ', Environmental Research Letters, vol. 8, no. 3, 035027 . https://doi.org/10.1088/1748-9326/8/3/035027
ISSN: 1748-9326
DOI: 10.1088/1748-9326/8/3/035027
Popis: The work of MF andAMis sponsored by the Natural Environment Research Council (NERC) under grant NE/H024921/1. IK, OS, RL, and LU are supported by the international cooperation program of the ASCR grant M10042120 and by the GACR project 205-09-1253. JB is supported by the Earth-system project TAMOP-4.2.2.C-11/1/KONV-2012-0015 sponsored by the EU and European Social Foundation. OV is supported by the Spanish Ministry of Science and Innovation under project AYA2011-29936-C05-04. ChH acknowledges an ERC starting grant from the European Union. The acceleration of electrons results in observable electromagnetic waves which can be used for remote sensing. Here, we make use of similar to 4 Hz-66 MHz radio waves emitted by two consecutive intense positive lightning discharges to investigate their impact on the atmosphere above a thundercloud. It is found that the first positive lightning discharge initiates a sprite where electrons are accelerated during the exponential growth and branching of the sprite streamers. This preconditioned plasma above the thundercloud is subsequently exposed to a second positive lightning discharge associated with a bouncing-wave discharge. This discharge process causes a re-brightening of the existing sprite streamers above the thundercloud and initiates a subsequent relativistic electron beam. Publisher PDF
Databáze: OpenAIRE