Using two ground stations to identify magnetospheric field line eigenfrequency as a continuous function of ground latitude-Reference-Cited by-同舟云学术

Using two ground stations to identify magnetospheric field line eigenfrequency as a continuous function of ground latitude

Published:2002-08 Issue:A8 Volume:107 Page:SMP 25-1-SMP 25-12
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res.

Author:

Kawano H.¹,Yumoto K.¹,Pilipenko V. A.²,Tanaka Y.-M.¹,Takasaki S.¹,Iizima M.³,Seto M.⁴

Affiliation:

1. Department of Earth and Planetary Sciences; Kyushu University; Fukuoka Japan

2. Institute of the Physics of the Earth; Moscow Russia

3. Geophysical Institute; Tohoku University; Miyagi Japan

4. Tohoku Institute of Technology; Miyagi Japan

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference29 articles.

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2. Two simple methods for the determination of the resonance frequencies of magnetic field lines;Baransky;Planet. Space Sci.,1990

3. Gradient and polarization methods of ground-based monitoring of magnetospheric plasma;Baransky;J. Geomagn. Geoelectr.,1995

4. A theory of long-period magnetic pulsations, 1, Steady state excitation of field line resonance;Chen;J. Geophys. Res.,1974

5. Plasmaspheric depletion and refilling associated with the September 25, 1998 magnetic storm observed by ground magnetometers at L = 2;Chi;Geophys. Res. Lett.,2000

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