Electrostatic solitary waves in current layers: from Cluster observations during a super-substorm to beam experiments at the LAPD

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dc.contributor.author Pickett, J.S.
dc.contributor.author Chen, L.-J.
dc.contributor.author Santolík, O.
dc.contributor.author Grimald, S.
dc.contributor.author Lavraud, B.
dc.contributor.author Verkhoglyadova, O.P.
dc.contributor.author Tsurutani, B.T.
dc.contributor.author Lefebvre, B.
dc.contributor.author Fazakerley, A.
dc.contributor.author Lakhina, G.S.
dc.contributor.author Ghosh, S.S.
dc.contributor.author Grison, B.
dc.contributor.author Décréau, P.M.E.
dc.contributor.author Gurnett, D.A.
dc.contributor.author Torbert, R.
dc.contributor.author Cornilleau-Wehrlin, N.
dc.contributor.author Dandouras, I.
dc.contributor.author Lucek, E.
dc.date.accessioned 2015-10-26T06:39:30Z
dc.date.accessioned 2021-02-12T09:37:49Z
dc.date.available 2015-10-26T06:39:30Z
dc.date.available 2021-02-12T09:37:49Z
dc.date.issued 2009
dc.identifier.citation Nonlin. Processes Geophys., v.16, p.431–442, 2009, doi: 10.5194/npg-16-431-2009 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/638
dc.description.abstract Electrostatic Solitary Waves (ESWs) have been observed by several spacecraft in the current layers of Earth's magnetosphere since 1982. ESWs are manifested as isolated pulses (one wave period) in the high time resolution waveform data obtained on these spacecraft. They are thus nonlinear structures generated out of nonlinear instabilities and processes. We report the first observations of ESWs associated with the onset of a super-substorm that occurred on 24 August 2005 while the Cluster spacecraft were located in the magnetotail at around 18–19 RE and moving northward from the plasma sheet to the lobes. These ESWs were detected in the waveform data of the WBD plasma wave receiver on three of the Cluster spacecraft. The majority of the ESWs were detected about 5 min after the super-substorm onset during which time 1) the PEACE electron instrument detected significant field-aligned electron fluxes from a few 100 eV to 3.5 keV, 2) the EDI instrument detected bursts of field-aligned electron currents, 3) the FGM instrument detected substantial magnetic fluctuations and the presence of Alfvén waves, 4) the STAFF experiment detected broadband electric and magnetic waves, ion cyclotron waves and whistler mode waves, and 5) CIS detected nearly comparable densities of H+ and O+ ions and a large tailward H+ velocity. We compare the characteristics of the ESWs observed during this event to those created in the laboratory at the University of California-Los Angeles Plasma Device (LAPD) with an electron beam. We find that the time durations of both space and LAPD ESWs are only slightly larger than the respective local electron plasma periods, indicating that electron, and not ion, dynamics are responsible for generation of the ESWs. We have discussed possible mechanisms for generating the ESWs in space, including the beam and kinetic Buneman type instabilities and the acoustic instabilities. Future studies will examine these mechanisms in more detail using the space measurements as inputs to models, and better relate the ESW space measurements to the laboratory through PIC code models. en_US
dc.language.iso en en_US
dc.subject Electrostatic solitary waves en_US
dc.subject Current layers en_US
dc.subject Earth's magnetosphere en_US
dc.subject Super-substorm en_US
dc.subject ESW en_US
dc.subject LAPD en_US
dc.title Electrostatic solitary waves in current layers: from Cluster observations during a super-substorm to beam experiments at the LAPD en_US
dc.type Article en_US
dc.identifier.accession 091302


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