Auroral electrojet current density deduced from the Chatanika Radar and from the Alaska Meridian Chain of magnetic observatories

Author:

Kamide Y.,Brekke A.

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

Reference21 articles.

1. Large-scale auroral motions and polar magnetic disturbances, 1, A polar disturbance at about 1100 hours on 23 September 1957;Akasofu;J. Atmos. Terr. Phys.,1960

2. Results from a meridian chain of observatories in the Alaskan sector;Akasofu;Planet. Space Sci.,1971

3. Electric field observations by incoherent scatter radar in the auroral zone;Banks;J. Geophys. Res.,1973

4. Birkeland , K. The Norwegian Aurora Polaris Expedition 1902-1903 1, sect. 2 H. Aschehoug Christiania, Norway 1913

5. A three-dimensional model current system for polar magnetic substorms;Bonnevier;J. Geophys. Res.,1970

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