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AGU: Journal of Geophysical Research, Space Physics

 

Keywords

  • ULF wave
  • magnetic conjugate
  • magnetosphere-ionsophere coupling
  • field line resonance
  • magnetic pulsation
  • Pc 3–5 pulsations

Index Terms

  • Magnetospheric Physics: Magnetosphere/ionosphere interactions
  • Magnetospheric Physics: MHD waves and instabilities
  • Magnetospheric Physics: Field-aligned currents and current systems
  • Ionosphere: Wave propagation
  • Magnetospheric Physics: General or miscellaneous
Abstract
Cited By (0)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, A10214, 9 PP., 2005
doi:10.1029/2003JA010242

North-south asymmetry of the amplitude of high-latitude Pc 3–5 pulsations: Observations at conjugate stations

Yuki Obana

Venture Business Laboratory, Kyushu University, Fukuoka, Japan

Akimasa Yoshikawa

Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University, Fukuoka, Japan

John V. Olson

Geophysical Institute, University of Alaska, Fairbanks, Alaska, USA

Ray J. Morris

Australian Antarctic Division, Department of the Environment and Heritage, Kingston, Tasmania, Australia

Brian J. Fraser

Department of Physics, University of Newcastle, Newcastle, New South Wales, Australia

Kiyohumi Yumoto

Space Environment Research Center, Kyushu University, Fukuoka, Japan

The north-south asymmetry of the amplitude of ULF pulsations in the Pc 3–5 band is studied using magnetic field data from the magnetically conjugate stations at L ∼ 5.4: Kotzebue (KOT) in the northern hemisphere and Macquarie Island (MCQ) in the southern hemisphere. We obtained the following results for the northward (H) component of magnetic pulsations: (1) The north to south power ratio shows a maximum in the northern winter and a minimum in the northern summer. This “seasonal variation” is stronger at higher frequencies (Pc 3 and Pc 4 frequencies). (2) The north to south power ratio for the Pc 4 and Pc 5 frequency band is basically greater than 1.0 for all seasons. This “positive offset” is stronger at lower frequencies. The “seasonal variation” implies that the magnetohydrodynamic (MHD) waves incident from the magnetosphere are more strongly shielded when the ionospheric conductivity is higher. The “positive offset” may result from the difference of the background magnetic field intensity between KOT and MCQ.

Received 16 September 2003; accepted 5 May 2005; published 28 October 2005.

Citation: Obana, Y., A. Yoshikawa, J. V. Olson, R. J. Morris, B. J. Fraser, and K. Yumoto (2005), North-south asymmetry of the amplitude of high-latitude Pc 3–5 pulsations: Observations at conjugate stations, J. Geophys. Res., 110, A10214, doi:10.1029/2003JA010242.

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