Longitudinal variability of low‐latitude total electron content: Tidal influences

By L. Scherliess, D. Thompson, R. Schunk. 2007

168 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/d0b6bca9c937966374cb5c0732bdd0a1c17a8b59

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In Astronomy and Astrophysics

1. B. Fejer
2. Shin-Yi Su
3. R. Akmaev
4. J. W. Jensen

In Geophysics

1. Shin-Yi Su
2. B. Fejer
3. J. W. Jensen
4. R. Akmaev

Citations in the corpus

• Seasonal and longitudinal dependence of equatorial disturbance vertical plasma drifts (2008, background): “It has also been shown that the global ionospheric densities in the F-layer and TEC from high to equatorial latitudes have larger values in December solstice than in June solstice [e.g., Rishbeth and Müller-Wodarg, 2006; Scherliess et al., 2008].”
• Quiet time equatorial F region vertical plasma drift model derived from ROCSAT‐1 observations (2008, unknown): “The seasonal and longitudinal variations of our daytime upward drifts are fully consistent with global distribution of low latitude TEC derived from TOPEX satellite data [Scherliess et al., 2008].”
• WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “The amplitude of wave number 4 of about 4% is comparable to TEC estimates [Scherliess et al., 2008] but substantially lower than in other observations [e.g., Lin et al., 2007; Liu et al., 2009b], while the interhemispheric asymmetry appears to be overestimated by the model.”
• Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, background): “altimeter, Scherliess et al. [2008] found that the wavenumber-4 patterns created during the daytime hours undergo a remarkable seasonal variation, but are largely”
• The International Reference Ionosphere 2012 – a model of international collaboration (2014, unknown): “A good example is the recently discovered four maxima structure in the longitudinal variation of F-peak electron density and of ionospheric electron content that was first observed with IMAGE/EUV observations (Immel et al. 2006), and then confirmed with data from CHAMP (Lühr et al. 2007) and TOPEX (”