Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/55965
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dc.contributor.authorMorris, Ray Jamesen
dc.contributor.authorHoldsworth, David Andrewen
dc.contributor.authorMurphy, Damian J.en
dc.contributor.authorMonselesan, D. M.en
dc.date.issued2005en
dc.identifier.citationGeophysical Research Letters, 2005; 32(23):23814-23814en
dc.identifier.issn0094-8276en
dc.identifier.urihttp://hdl.handle.net/2440/55965-
dc.description.abstractWe report on novel spectral characteristics of E-region backscatter acquired using a 1.94 MHz Medium Frequency (MF) radar above the high-latitude Antarctic station Davis (68.6°S). Two distinctive Doppler spectra are observed: one that exhibits bifurcation in Doppler velocity (or frequency) with one, or occasionally more, near symmetrical spectral side-bands (here labelled SSE); and a second that exhibits broad-band spectra related to the magnetic field topology (here labelled FRE). Both spectral forms reveal a characteristic quasi-hyperbolic spectral form that diverges in Doppler velocity with range. We discuss the properties of these two spectral forms including: Doppler spectral shape; power spectra; angle-of-arrival (AOA) of backscattered sources; and their diurnal and day-to-day occurrence distributions for our campaign interval. Interestingly, the E-region SSE observed at a height near 100 km were observed coincidentally with D-region polar mesosphere summer echoes (PMSE) in the height range 82–92 km, when colocated data were available.en
dc.description.statementofresponsibilityR. J. Morris, D. A. Holdsworth, D. J. Murphy and D. M. Monselesanen
dc.language.isoenen
dc.publisherAmerican Geophysical Unionen
dc.titleE-region bifurcation and magnetic field related Bragg backscattered spectral events observed at high-latitude by MF radaren
dc.typeJournal articleen
dc.contributor.schoolSchool of Chemistry and Physics : Physics and Mathematical Physicsen
dc.identifier.doi10.1029/2005GL024429en
Appears in Collections:Physics publications

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