TheFregion and topside ionosphere response to a strong geomagnetic storm at Arecibo

Author:

Gong Yun123,Zhou Qihou14,Zhang Shao Dong3,Aponte Néstor5,Sulzer Michael5,González Sixto A.5

Affiliation:

1. Electrical and Computer Engineering Department; Miami University; Oxford Ohio USA

2. State Key Laboratory of Space Weather; Chinese Academy of Sciences; Beijing China

3. School of Electronic Information; Wuhan University; Wuhan China

4. School of Electrical Engineering; Zhengzhou University; Zhengzhou China

5. Arecibo Observatory; SRI International; Arecibo Puerto Rico USA

Funder

National Science Foundation

NSF

National Basic Research Program of China

Chinese Natural Science Foundation

Specialized Research Fund for State Key Laboratories

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Reference37 articles.

1. Modeling the midlatitude F-region ionospheric storm using east-west drift and a meridional wind;Anderson;Planet. Space Sci.,1976

2. Behnke , R. A. 1970 Vector measurements of the ion transport velocity with application to the F-region dynamics Ph D thesis

3. Properties of traveling atmospheric disturbances (TADs) inferred from CHAMP accelerometer observations;Bruinsma;Adv. Space Res.,2009

4. Ionospheric storms-A review;Buonsanto;Space Sci. Rev.,1999

5. Effects of magnetospheric electric fields and neutral winds on the low-middle latitude ionosphere during the March 20-21, 1990 storm;Buonsanto;J. Geophys. Res.,1993

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