'Serpentine Emission' at the high latitude Antarctic station, Davis

Mathematics – Logic

Scientific paper

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Antarctic Regions, Auroral Arcs, Extremely Low Radio Frequencies, Oscillations, Radio Emission, Amplitudes, Frequency Modulation, Polarization Characteristics, Power Spectra, Time Response

Scientific paper

New observational and dynamical morphological results on the Serpentine Emission (SE) phenomenon observed at Davis, Antarctica during 1981 are discussed. Included are analyses of the amplitude-time structure, the maximum entropy power spectra, digital sonograms, and SE polarizations. Data revealed 0.8-10 sec individual oscillation periods, amplitude peaks at 0.4 nT, a carrier-frequency range between 0.05 and 0.4 Hz, and durations of several minutes to days. The Davis SEs were found to occur during magnetic quiescence and to exhibit left-handed polarization.

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