Plausible effect of atmospheric tides on the equatorial ionosphere observed by the FORMOSAT‐3/COSMIC: Three‐dimensional electron density structures
By Chien‐Hung Lin, Wenbin Wang, M. E. Hagan, C. Hsiao, T. Immel, M. M. Hsu, Jann‐Yenq Liu, Larry J. Paxton, Tzu‐Wei Fang, C. H. Liu. 2007
178 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/6f20c7d2414e16f04010990ec1a5c73b36792c1b
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- Electrodynamics of the formation of ionospheric wave number 4 longitudinal structure (2008, background): “During the daytime, wave number 4 structure has been observed both in the ionospheric density and the vertical E � B drift [Lin et al., 2007b; Kil et al., 2007]; thus, the longitudinal variation of E � B drift is probably the primary driver for that of the ionospheric density, whereas in the evening”
- Tidal propagation of deep tropical cloud signatures into the thermosphere from TIMED observations (2008, background): “…attention because there is a growing observational evidence that DE3 is the main source of the prominent four-peaked longitudinal variation of the equatorial ionization anomaly (EIA) in F-region electron density [Lin et al., 2007], wind [Häusler et al., 2007], and UVemission [Immel et al., 2006].”
- Tropospheric tidal effects on the middle and upper atmosphere (2009, background): “…variations in 1356 nm airglow brightness measurements [e.g., Sagawa et al., 2005; Immel et al., 2006; England et al., 2006b], electron density [Lin et al., 2007; Lühr et al., 2007], electric field [England et al., 2006a; Kil et al., 2007], electrojet [Lühr et al., 2008], and thermospheric…”
- Wave-driven variability in the ionosphere-thermosphere-mesosphere system from TIMED observations: What contributes to the wave 4 ? (2011, background): “It has been frequently observed by(quasi‐) Sun‐synchronous satellites in a variety of ionospheric and neutral parameters such as F‐region airglow [i.e., Sagawa et al., 2005; England et al., 2006], electron density [i.e., Lin et al., 2007; Pedatella et al., 2008], ~ E × ~ drifts [i.e., Hartman and ”
- Exploring earth's atmosphere with radio occultation: contributions to weather, climate and space weather (2011, unknown): “Figure 39 shows the vertically integrated electron content in two layers, between 100 and 500 km and 300–350 km altitude (Lin et al., 2007c).”
- FORMOSAT-3/COSMIC observations of seasonal and longitudinal variations of equatorial ionization anomaly and its interhemispheric asymmetry during the solar minimum period (2009, background): “tudinal structure in EIA [Sagawa et al., 2005; Immel et al., 2006; Lin et al., 2007b, 2007c; Liu and Watanabe, 2008; Kil et al., 2008]; hence the underlying physical mechanisms for this four-peaked structure will not be discussed here.”
- Longitudinal structure of the equatorial ionosphere: Time evolution of the four-peaked EIA structure (2007, result): “The hypothesis put forward by previous authors [e.g., Sagawa et al., 2005; Immel et al., 2006; England et al., 2006a, 2006b; Lin et al., 2007] suggests that the stronger EIA zones are produced by a stronger plasma fountain effect in those four regions.”
- Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, background): “Lin et al. [2007a] analyzed the electron density profiles observed by radio occultation from FORMOSAT-3/COSMIC satellites and found that the wavenumber-4 patterns occurs usually at altitudes above 250 km. Lin et al. [2007b] also studied the diurnal variation of the wavenumber-4 patterns and pointed”