Intensity variations of the equivalentSqcurrent system along the 210° magnetic meridian

Author:

Yamazaki Y.1,Yumoto K.12,Uozumi T.2,Cardinal M. G.1

Affiliation:

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

2. Space Environment Research Center; Kyushu University; Fukuoka 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

Reference49 articles.

1. The ionospheric disturbance dynamo;Blanc;J. Geophys. Res.,1980

2. Solar cycle dependence and long-term trends in the wind field of the mesosphere/lower thermosphere;Bremer;J. Atmos. Sol. Terr. Phys.,1997

3. Rocket measurements of the geomagnetic field above Woomera, South Australia;Burrows;J. Geophys. Res.,1965

4. Differences in geomagnetic Sq field representations due to variations in spherical harmonic analysis techniques;Campbell;J. Geophys. Res.,1990

5. Sq currents: A comparison of quiet and active year behavior;Campbell;J. Geophys. Res.,1982

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