A LOFAR observation of ionospheric scintillation from two simultaneous travelling ionospheric disturbances

dc.bibliographicCitation.firstPage10eng
dc.bibliographicCitation.volume10eng
dc.contributor.authorFallows, Richard A.
dc.contributor.authorForte, Biagio
dc.contributor.authorAstin, Ivan
dc.contributor.authorAllbrook, Tom
dc.contributor.authorArnold, Alex
dc.contributor.authorWood, Alan
dc.contributor.authorDorrian, Gareth
dc.contributor.authorMevius, Maaijke
dc.contributor.authorRothkaeh, Hanna
dc.contributor.authorMatyjasiak, Barbara
dc.contributor.authorKrankowski, Andrzej
dc.contributor.authorAnderson, James M.
dc.contributor.authorAsgekar, Ashish
dc.contributor.authorAvruch, I. Max
dc.contributor.authorBentum, Mark
dc.contributor.authorBisi, Mario M.
dc.contributor.authorButcher, Harvey R
dc.contributor.authorCiardi, Benedetta
dc.contributor.authorDabrowski, Bartosz
dc.contributor.authorDamstra, Sieds
dc.contributor.authorde Gasperin, Francesco
dc.contributor.authorDuscha, Sven
dc.contributor.authorEislöffel, Jochen
dc.contributor.authorFranzen, Thomas M.O.
dc.contributor.authorGarrett, Michael A.
dc.contributor.authorGriessmeier, Jean-Matthias
dc.contributor.authorGunst, Andre W.
dc.contributor.authorHoeft, Matthias
dc.contributor.authorHorandel, Jorg R.
dc.contributor.authorIacobelli, Marco
dc.contributor.authorIntema, Huib T.
dc.contributor.authorKoopmans, Leon V.E.
dc.contributor.authorMaat, Peter
dc.contributor.authorMann, Gottfried
dc.contributor.authorNelles, Anna
dc.contributor.authorPaas, Harm
dc.contributor.authorPandey, Vishambhar N.
dc.contributor.authorReich, Wolfgang
dc.contributor.authorRowlinson, Antonia
dc.contributor.authorRuiter, Mark
dc.contributor.authorSchwarz, Dominik J.
dc.contributor.authorSerylak, Maciej
dc.contributor.authorShulevski, Aleksander
dc.contributor.authorSmirnov, Oleg M.
dc.contributor.authorSoida, Marian
dc.contributor.authorSteinmetz, Matthias
dc.contributor.authorThoudam, Satyendra
dc.contributor.authorToribio, M. Carmen
dc.contributor.authorvan Ardenne, Arnold
dc.contributor.authorvan Bemmel, Ilse M.
dc.contributor.authorvan der Wiel, Matthijs H.D.
dc.contributor.authorvan Haarlem, Michiel P.
dc.contributor.authorVermeulen, Rene C.
dc.contributor.authorVocks, Christian
dc.contributor.authorWijers, Ralph A.M.J.
dc.contributor.authorWucknitz, Olaf
dc.contributor.authorZarka, Philippe
dc.contributor.authorZucca, Pietro
dc.date.accessioned2021-07-22T08:39:43Z
dc.date.available2021-07-22T08:39:43Z
dc.date.issued2020
dc.description.abstractThis paper presents the results from one of the first observations of ionospheric scintillation taken using the Low-Frequency Array (LOFAR). The observation was of the strong natural radio source Cassiopeia A, taken overnight on 18–19 August 2013, and exhibited moderately strong scattering effects in dynamic spectra of intensity received across an observing bandwidth of 10–80 MHz. Delay-Doppler spectra (the 2-D FFT of the dynamic spectrum) from the first hour of observation showed two discrete parabolic arcs, one with a steep curvature and the other shallow, which can be used to provide estimates of the distance to, and velocity of, the scattering plasma. A cross-correlation analysis of data received by the dense array of stations in the LOFAR “core” reveals two different velocities in the scintillation pattern: a primary velocity of ~20–40 ms−1 with a north-west to south-east direction, associated with the steep parabolic arc and a scattering altitude in the F-region or higher, and a secondary velocity of ~110 ms−1 with a north-east to south-west direction, associated with the shallow arc and a scattering altitude in the D-region. Geomagnetic activity was low in the mid-latitudes at the time, but a weak sub-storm at high latitudes reached its peak at the start of the observation. An analysis of Global Navigation Satellite Systems (GNSS) and ionosonde data from the time reveals a larger-scale travelling ionospheric disturbance (TID), possibly the result of the high-latitude activity, travelling in the north-west to south-east direction, and, simultaneously, a smaller-scale TID travelling in a north-east to south-west direction, which could be associated with atmospheric gravity wave activity. The LOFAR observation shows scattering from both TIDs, at different altitudes and propagating in different directions. To the best of our knowledge this is the first time that such a phenomenon has been reported.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6304
dc.identifier.urihttps://doi.org/10.34657/5351
dc.language.isoengeng
dc.publisherLes Ulis : EDP Scienceseng
dc.relation.doihttps://doi.org/10.1051/swsc/2020010
dc.relation.essn2115-7251
dc.relation.ispartofseriesJournal of space weather and space climate : SWSC 10 (2020)eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectIonospheric scintillationeng
dc.subjecttravelling ionospheric disturbanceseng
dc.subjectinstability mechanismseng
dc.subject.ddc550eng
dc.subject.ddc520eng
dc.titleA LOFAR observation of ionospheric scintillation from two simultaneous travelling ionospheric disturbanceseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleJournal of space weather and space climate : SWSCeng
tib.accessRightsopenAccesseng
wgl.contributorAIPeng
wgl.subjectPhysikeng
wgl.typeZeitschriftenartikeleng
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