Longitudinal variation of the E‐region electric fields caused by atmospheric tides

By Scott L. England, Stefan Maus, T. Immel, S. Mende. 2006

253 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/2703ef1068336ca6db411fa4dffc17baa2aa520d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Astronomy and Astrophysics

1. R. Akmaev
2. Jeff Forbes
3. B. Fejer
4. Han-Li Liu
5. J. Oberheide
6. Jorge L. Chau
7. L. P. Goncharenko
8. N. Pedatella

In Molecular Biology

1. R. Akmaev
2. K. Häusler
3. Sean Bruinsma
4. Jeff Forbes
5. J. Oberheide
6. M. E. Hagan
7. C. Liu
8. L. Scherliess

Citations in the corpus

• The global electrical circuit: A review (2009, background): “Preliminary interpretations of the wavenumber-4 observations in the upper ionosphere (England et al., 2006) are based on tidal forcing originating in tropospheric weather.”
• Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, background): “These ionospheric signatures have been identified before in measurements of the nighttime equatorial ionization anomaly (e.g., Immel et al. 2006) and noontime equatorial electrojet (England et al. 2006) using far ultraviolet images.”
• Quiet time equatorial F region vertical plasma drift model derived from ROCSAT‐1 observations (2008, unknown): “by Scherliess and Fejer [1999] is probably more realistic than that shown in our model.”
• Tropospheric tidal effects on the middle and upper atmosphere (2009, background): “, 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 wind data [Häusler et al., 2007; Lühr et al., 2007] with four-peaked structures. In their report on the ”
• FORMOSAT-3/COSMIC observations of seasonal and longitudinal variations of equatorial ionization anomaly and its interhemispheric asymmetry during the solar minimum period (2009, background): “[2006], Forbes et al. [2006], England et al.”
• Longitudinal variability of low‐latitude total electron content: Tidal influences (2007, methodology): “England et al. [2006b] have used noontime equatorial electrojet observations from the CHAMP, Orsted, and SAC-C satellites and demonstrated that a similar wave number four variation exists in the daytime electrojet sheet current density during geomagnetically quiet periods near equinox.”
• Longitudinal structure of the equatorial ionosphere: Time evolution of the four-peaked EIA structure (2007, methodology): “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): “[12] As suggested by previous works [Sagawa et al., 2005; England et al., 2006a; Immel et al., 2006; Hagan et al., 2007], the longitudinal wavenumber-4 structure in the EIA region may be caused by the longitudinal modulation of the F-region ion drifts which is created in turn by the longitudinal…”
• Tropospheric tides from 80 to 400 km: Propagation, interannual variability, and solar cycle effects (2009, background): “…electron densities [Liu and Watanabe, 2008; Pedatella et al., 2008], total electron content [Scherliess et al., 2008; Wan et al., 2008], O+ airglow [England et al., 2006a], equatorial electrojet [Lühr et al., 2008], daytime electric fields [England et al., 2006b], and ~E ~B drift velocities…”
• Electrodynamics of the formation of ionospheric wave number 4 longitudinal structure (2008, background): “[2] A wave number 4 longitudinal structure has recently been found in the low-latitude ionospheric density distribution by a number of satellite observations, both for the nighttime [Sagawa et al., 2005; Immel et al., 2006; England et al., 2006a, 2006b; Lin et al., 2007a] and daytime [Lin et al., ”
• Plausible effect of atmospheric tides on the equatorial ionosphere observed by the FORMOSAT‐3/COSMIC: Three‐dimensional electron density structures (2007, methodology): “[7] The most likely wave mode responsible for the fourpeaked longitudinal structure is the eastward wavenumber three (E3) diurnal nonmigrating tide [Sagawa et al., 2005; Immel et al., 2006; England et al., 2006a, 2006b].”
• Connections between deep tropical clouds and the Earth's ionosphere (2007, background): “[3] Recent analyses of IMAGE FUV observations reveal four longitudinal EIA enhancements in the early evening, which can be attributed to comparatively stronger equatorial plasma fountain effects at each of these locations [Sagawa et al., 2005; Immel et al., 2006; England et al., 2006a, 2006b ].”
• WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “The plasma density peaks are also shifted farther poleward, both features indicative of stronger plasma drifts at these longitudes [Sagawa et al., 2005; England et al., 2006].”
• The influence of atmospheric tide and planetary wave variability during sudden stratosphere warmings on the low latitude ionosphere (2013, background): “Longitude dependent vertical plasma drift velocities result from nonmigrating tides as well as the interaction between migrating tides and the geomagnetic main field [England et al., 2006; Fang et al., 2012].”
• Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, unknown): “For this reason, the Sq-EEJ separation is a common practice for EEJ studies based on satellite data analysis (e.g., Le Mouël et al. 2006; England et al. 2006; Manoj et al. 2006; Alken and Maus 2007; Tomás et al. 2008; Alken et al. 2015).”