Abstract

Abstract. In this paper we present the results from the observation of ultra low frequency (ULF) pulsations in the Doppler velocity data from SuperDARN HF radar located at Goose Bay (61.94° N, 23.02° E, geomagnetic). Fourier spectral techniques were used to determine the spectral content of the data and the results show Pc 5 ULF pulsations (with a frequency range of 1 to 4 mHz) where the magnetic field lines were oscillating at discrete frequencies of about 1.3 and 1.9 mHz. These pulsations are classified as field lines resonance (FLR) since the 1.9 mHz component exhibited an enhancement in amplitude with an associated phase change of approximately 180° across a resonance latitude of 71.3°. The spatial and temporal structure of the ULF pulsations was examined by investigating their instantaneous amplitude which was calculated as the amplitude of the analytic signal. The results presented a full field of view which exhibit pulsations activity simultaneously from all beams. This representation shows that the peak amplitude of the 1.9 mHz component was observed over the longitudinal range of 13°. The temporal structure of the pulsations was investigated from the evolution of the 1.9 mHz component and the results showed that the ULF pulsations had a duration of about 1 h. Wavelet analysis was used to investigate solar wind as a probable source of the observed ULF pulsations. The time delay compared well with the solar wind travel time estimates and the results suggest a possible link between the solar wind and the observed pulsations. The sudden change in dynamic pressure also proved to be a possible source of the observed ULF pulsations.

Highlights

  • Ultra low frequency (ULF) pulsations are magnetohydrodynamic (MHD) waves that are excited on and propagate along and across the earth’s magnetic field within the magnetosphere (Hughes, 1994)

  • In this paper we present the results from the observation of ULF pulsations

  • The analysis was conducted using Doppler velocity data collected from HF radar which is located at Goose Bay (61.94◦ N, 23.02◦ E, geomagnetic)

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Summary

Introduction

Ultra low frequency (ULF) pulsations are magnetohydrodynamic (MHD) waves that are excited on and propagate along and across the earth’s magnetic field within the magnetosphere (Hughes, 1994). The lack of observational evidence of the cavity mode led Walker et al (1992) to propose another new model that could be responsible for the excitation of the ULF pulsations They assumed that the magnetospheric cavity is not closed but represents an open-ended waveguide with boundaries at the magnetopause and the turning point where the Alfven waves are reflected. This mechanism is similar to the one where solar wind excites ULF pulsations through KelvinHelmholtz instabilities.

Instrumentation and data acquisition
Results and discussion
Amplitude spectra
Possible source of the ULF pulsations
Full Text
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