Observation of F region irregularities near a northern equatorial anomaly crest during solar minimum using ionosonde, GPS receiver, and satellites
Author:
Affiliation:
1. General Education Center; Chien Hsin University of Science and Technology; Jhongli Taiwan
2. National Time and Frequency Standard Laboratory, Telecommunication Laboratories, Chunghwa Telecom Co., Ltd.; Yangmei Taiwan
Funder
National Science Council
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/jgra.50350/fullpdf
Reference32 articles.
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2. GPS phase fluctuations in the equatorial region during the MISETA 1994 campaign;Aarons;J. Geophys. Res.,1996
3. Two anomalies in the ionosphere;Appleton;Nature,1946
4. Ionospheric constraints on VHF/UHF communications links during solar maximum and minimum periods;Basu;Radio Sci.,1988
5. Spread-F at anomaly crest regions in the Indian and American longitudes;Chandra;Adv. Space Res.,2003
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1. The Simultaneous Observations of Nighttime Ionospheric E Region Irregularities and F Region Medium-Scale Traveling Ionospheric Disturbances in Midlatitude China;Journal of Geophysical Research: Space Physics;2018-06
2. Effects of sporadic E-layer characteristics on spread-F generation in the nighttime midlatitude ionosphere: A climatological study;Journal of Atmospheric and Solar-Terrestrial Physics;2018-04
3. Spread F occurrence and drift under the crest of the equatorial ionization anomaly from continuous Doppler sounding and FORMOSAT-3/COSMIC scintillation data;Earth, Planets and Space;2016-04-08
4. Effects of sporadic E-layer characteristics on spread-F generation in the nighttime ionosphere near a northern equatorial anomaly crest during solar minimum;Journal of Atmospheric and Solar-Terrestrial Physics;2015-06
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