1980
DOI: 10.1016/0032-0633(80)90098-7
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High-latitude Pc1–2 geomagnetic pulsations and their connection with location of the dayside polar cusp

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Cited by 33 publications
(17 citation statements)
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“…Stations located in the auroral zone (63° and 64°) also show two maxima but at significantly different times: a peak at 16:00–17:00 MLT and a secondary peak in the early morning sector. Bolshakova et al [1980] suggested the existence of the two occurrence peaks is attributed to the position of the stations with respect to the dayside polar cusp since the stations approach the cusp twice in the course of their diurnal rotation. The MLT occurrences observed by Plyasova‐Bakounina et al [1996] using a ground network of six stations at latitudes 65° to 76° appear to be similar to those in the Bolshakova et al [1980] study.…”
Section: Discussionmentioning
confidence: 99%
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“…Stations located in the auroral zone (63° and 64°) also show two maxima but at significantly different times: a peak at 16:00–17:00 MLT and a secondary peak in the early morning sector. Bolshakova et al [1980] suggested the existence of the two occurrence peaks is attributed to the position of the stations with respect to the dayside polar cusp since the stations approach the cusp twice in the course of their diurnal rotation. The MLT occurrences observed by Plyasova‐Bakounina et al [1996] using a ground network of six stations at latitudes 65° to 76° appear to be similar to those in the Bolshakova et al [1980] study.…”
Section: Discussionmentioning
confidence: 99%
“…Ground observations [e.g., Bolshakova et al , 1980; Menk et al , 1992; Neudegg et al , 1995] suggested the dayside cusp as the magnetospheric source regions of Pc1–2 wave activity. Fraser [1975a] estimated the general location of the injection region near the dawn terminator in the range 58°–66° ILAT ( L = 3.5–6) using the polarization ellipse major axis azimuthal directions and direction of arrival triangulation method.…”
Section: Discussionmentioning
confidence: 99%
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“…The theoretical estimates of the periods and amplitudes in the transition region (A<lOr, TN2-5sec) and on the ground (AN300-500mr) have the same order of magnitude as the experimentally obtained values in space and on the ground. The suggested mechanism explains the localization, quasipermanence and the absence of conjugacy for these pulsations (BoLSHAKOVA et al, 1980). The main properties of Pc 1-2 are given in the Table 1.…”
Section: Geomagnetic Pulsations Pc 1-2mentioning
confidence: 81%
“…After some time dt, particles with greater velocities will be concentrated on the front of the beam, and particles with lower velocities on the tail (i. e. Vifr>Vitaii). The main bulk of the particles will be located in the middle of the beam (BOLSHAKOVA et al, 1980). On the front of such beams oscillations with smaller periods will be amplified, and on the tails, oscillations with greater periods.…”
Section: Pulsations Iprp (Intervals Of Pulsations With Rising Periods)mentioning
confidence: 99%