Altitude variations of the horizontal thermospheric winds during geomagnetic storms

Author:

Wang W.1,Burns A. G.1,Wiltberger M.1,Solomon S. C.1,Killeen T. L.1

Affiliation:

1. High Altitude Observatory; National Center for Atmospheric Research; Boulder Colorado USA

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

Reference39 articles.

1. A mathematical model of the Earth’s plasmasphere and its application in a study of He+ at L = 3;Bailey;Ann. Geophys.,1990

2. Thermospheric heating away from the auroral oval during geomagnetic storms;Burns;Can. J. Phys.,1992

3. The solar-cycle-dependent response of the thermosphere to geomagnetic storms;Burns;J. Atmos. Sol. Terr. Phys.,2004

4. The ionospheric and thermospheric response to CMEs: Challenges and successes;Burns;J. Atmos. Sol. Terr. Phys.,2007

5. Meridional neutral winds in the thermosphere at Arecibo: Simultaneous incoherent scatter and airglow observations;Burnside;J. Geophys. Res.,1983

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