摘要
Previous theoretical models showed that, in the middle geomagnetic latitudes the oscillations in the Doppler frequency shift lag and lead the H component of ULF pulsations field on the ground, owing to the advection and compression mechanisms by 90°, respectively. On March 24, 1991, measurements obtained from a CW-HF Doppler sounding system and a fluxgate magnetometer show phase differences of 15°‒77° between the Doppler frequency shift oscillations and the H component of ULF pulsations field at ground level, which indicates that the Doppler velocity arises from predominant changes due to the compression mechanism.
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 109-114 |
頁數 | 6 |
期刊 | Journal of Geomagnetism and Geoelectricity |
卷 | 45 |
發行號 | 1 |
DOIs | |
出版狀態 | 已出版 - 1993 |