1974
DOI: 10.1029/ja079i031p04709
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Radar auroral echo characteristics as seen by a 398-MHz phased array radar operated at Homer, Alaska

Abstract: In this paper we present the first results of the mapping of the spatial distribution of auroral echoes by a 398‐MHz phased array radar recently installed at Homer, Alaska. The results are shown in the form of two‐dimensional spatial maps of auroral echoes. These maps are classified into types that are extensions of the ‘diffuse’ and ‘discrete’ echo types introduced by Leadabrand et al. (1959) and Presnell et al. (1959) for narrow beam radars. The auroral echo signatures typically seen during the afternoon and… Show more

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Cited by 46 publications
(39 citation statements)
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“…Small‐scale plasma structures, or so‐called field‐aligned plasma irregularities, in the auroral E region ionosphere, whose scale size ranges from a few meters to a few tens of meters, have mainly been studied using ground‐based radar measurements. In particular, the spatial collocation of optical auroral forms and plasma irregularities (i.e., radar aurora) in the auroral E region was investigated extensively using coherent radars at VHF frequencies [ Balsley et al , 1973; Greenwald et al , 1973; Tsunoda et al , 1974]. These studies in the 1970s demonstrated that, rather than being co‐located, backscatter echoes from meter‐scale irregularities were observed to be adjacent to auroral arcs.…”
Section: Introductionmentioning
confidence: 99%
“…Small‐scale plasma structures, or so‐called field‐aligned plasma irregularities, in the auroral E region ionosphere, whose scale size ranges from a few meters to a few tens of meters, have mainly been studied using ground‐based radar measurements. In particular, the spatial collocation of optical auroral forms and plasma irregularities (i.e., radar aurora) in the auroral E region was investigated extensively using coherent radars at VHF frequencies [ Balsley et al , 1973; Greenwald et al , 1973; Tsunoda et al , 1974]. These studies in the 1970s demonstrated that, rather than being co‐located, backscatter echoes from meter‐scale irregularities were observed to be adjacent to auroral arcs.…”
Section: Introductionmentioning
confidence: 99%
“…Considerable work was conducted in the 1970s concerning the relationship between optical auroral arcs and VHF coherent radar backscatter echoes from the E-region Greenwald et al, 1973Greenwald et al, , 1975Romick et al, 1974;Tsunoda et al, 1974Tsunoda et al, , 1976Hunsucker et al, 1975;Tsunoda and Fremouw, 1976a, b). In general, it was found that backscatter was observed adjacent to auroral arcs as opposed Correspondence to: S. E. Milan (steve.milan@ion.le.ac.uk) to the two phenomena being co-located.…”
Section: Introductionmentioning
confidence: 99%
“…Two mechanisms for the generation of metre-scale ionospheric irregularitiesthe targets from which VHF coherent radars scatter -were suggested to explain this interrelationship. In the first, it was the electron density gradients at the edges of auroral arcs that provided the seed for irregularity formation by the gradient drift instability Tsunoda et al, 1974). The growth rate of this instability becomes positive when the local electron density gradient has a component parallel to the background electric field.…”
Section: Introductionmentioning
confidence: 99%
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“…They showed that the bright aurora and the auroral radar backscatter prefer to be in close spatial contact and/or common motion (Greenwald et al, 1973;Tsunoda et al, 1974. A number of papers that described the pre-substorm, substorm or post-substorm behaviour of the aurora and the auroral radar backscatter supported or even ®tted well within a scheme (Ecklund and Unwin, 1971;Tsunoda and Fremouw, 1976;Uspensky et al, 1982Uspensky et al, , 1983Uspensky et al, , 1992Starkov and Uspensky, 1988).…”
Section: Introductionmentioning
confidence: 99%