Postsunset rise of F layer height in the equatorial region and its relation to the F layer dynamo polarization fields

Author:

Goel M. K.,Singh S. S.,Rao B. C. N.

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

Reference36 articles.

1. Modeling the total electron content observations above Ascension Island;Anderson;J. Geophys. Res.,1983

2. Effect of vertical ExB ionospheric drifts on F region neutral winds in the low-latitude thermosphere;Anderson;J. Geophys. Res.,1974

3. Calculated nighttime eastward plasma drift velocities at low latitudes and their solar cycle dependence;Anderson;Ann. Geophys.,1987

4. Appleton, E. V., , Equatorial anomalies in the F2 layer of the ionosphere, Some Ionospheric Results obtained During the IGY, 3 Elesevier Publishing Company, Amsterdam, 1960,

5. Electric fields in the equatorial ionosphere: A review of techniques and measurements;Balsley;J. Atmos. Terr. Phys.,1973

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