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Title: High-lattitude ground observations of PC 1/2 micropulsations

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JA02539· OSTI ID:183252
;  [1];  [2]
  1. Univ. of New Hampshire, Durham, NH (United States)
  2. Augsburg College, Minneapolis, MN (United States); and others

A ground-based survey of Pc 1/2 (0.1-0.4 Hz) and Pc 1 micropulsations throughout 1986 has provided evidence for the location of the Pc 1/2 source region. Data were taken from three high-latitude stations, located at South Pole ({minus}75{degrees} geomagnetic latitude; 1530 UT local noon), Sondre Stromfjord (+74{degrees}, 1330 UT LN) and Siple ({minus}61{degrees}, 1700 UT LN). The study revealed a diurnal occurrence patterns of the waves above and below 0.4 Hz, it is concluded that the waves observed on the ground above 0.4 Hz come primarily from plasmapause latitudes, while the source of the Pc 1/2 lies between the plasmapause and the magnetopause. The estimate of source locations for waves above and below this frequency, combined with the typically sharp upper frequency limit of waves in the 0.1-0.4 Hz band (Pc 1/2) are interpreted as evidence that He{sup +} ions in the outer magnetosphere influence propagation and possibly wave growth. These results are compared with those of Anderson, who showed with a spacecraft study that Pc 1 are more commonly observed beyond L=7 than in regions closer to the Earth. It is concluded that many of the waves above the He{sup +} gyrofrequency from the outer magnetosphere do not always reach the ground. An extensive search for correlations between Pc 1/2 occurrence and solar wind pressure and magnetic field orientation showed no direct connection between solar wind parameters and Pc 1/2 generation. They may instead be amplified by plasma sheet ions that drift sunward on the dusk side of the magnetosphere and undergo ion-cyclotron resonance in the afternoon sector. This mechanism is consistent with the diurnal pattern and apparent source location of the Pc 1/2. 39 refs., 12 figs., 1 tab.

Sponsoring Organization:
USDOE
OSTI ID:
183252
Journal Information:
Journal of Geophysical Research, Vol. 98, Issue A12; Other Information: PBD: 1 Dec 1993
Country of Publication:
United States
Language:
English

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