A reexamination of ATS 6 magnetometer data for radially polarized Pc 3 magnetic pulsations

Physics

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Geomagnetic Micropulsations, Magnetometers, Polarization Characteristics, Satellite Observation, Ats 6, Power Spectra, Satellite-Borne Instruments, Spectrum Analysis

Scientific paper

The polarization of Pc 3 (22-100 MHz) magnetic pulsations measured by the ATS 6 fluxgate magnetometer at synchronous orbit has been examined by using dynamic autospectral analysis. In contrast to the result obtained by Arthur et al. (1977) using the same data set, very few cases of radially polarized Pc 3 pulsations are found. It is suggested that satellite noise in the radial component, which depends on frequency f as 0.015/f (nT-squared/Hz), is responsible for this disagreement. In the presence of this type of noise, diagonalization of the spectral matrix can produce an erroneous major axis of polarization. Most Pc 3 pulsations classified as radially polarized by Arthur et al. appear to be a consequence of small amplitude azimuthal pulsations contaminated by satellite noise.

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