Noon‐time equatorial electrojet: Its spatial features as determined by the CHAMP satellite

By Hermann Lühr, S. Maus, Martin K. A. Rother. 2004

170 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/6dbc3cc0206772f96b2ca836cfa60d33f774977b

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Citations in the corpus

Generation of 100‐year geomagnetically induced current scenarios (2012, background): “The maximum values occurred between 08:00–12:00 magnetic local time (not shown), which indicates that the enhancement may be associated with the equatorial electrojet that is a localized band of ionospheric current between about 5 to 5 of geomagnetic latitude [Lühr et al., 2004].”
Plausible effect of atmospheric tides on the equatorial ionosphere observed by the FORMOSAT‐3/COSMIC: Three‐dimensional electron density structures (2007, background): “…and Rishbeth [2000]) stimulate great interest in studying the physical mechanism responsible for the observed longitudinal structure [Vladimer et al., 1999; Jadhav et al., 2002; Lühr et al., 2004; Sagawa et al., 2005; Henderson et al., 2005; Immel et al., 2006; England et al., 2006a, 2006b].”
Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, unknown): “Earlier attempts to observe geomagnetic solar eclipse effects can be found in review articles by Matsushita (1966) and Rastogi (1982).”
Lunar‐dependent equatorial ionospheric electrodynamic effects during sudden stratospheric warmings (2010, methodology): “and ambient field geometry [e.g., Luhr et al., 2004; Manoj et al., 2006].”
Longitudinal variation of the E‐region electric fields caused by atmospheric tides (2006, methodology): “[8] The EEJ current densities are estimated by an improved version of the method used by Lühr et al. [2004]. From the magnetic measurements of each satellite”
Connections between deep tropical clouds and the Earth's ionosphere (2007, result): “These results complement related upper atmospheric diagnostics that also reveal longitudinal variability with 4 peaks [Vladimer et al., 1999; Jadhav et al., 2002; Lühr et al., 2004; Lin et al., 2007].”
Control of equatorial ionospheric morphology by atmospheric tides (2006, methodology): “Recent studies using space-based magnetometers [Ivers et al., 2003; Lühr et al., 2004] or ionospheric density measurements [Vladimer et al., 1999] have found some new indications of longitudinal ionospheric structure, but those studies discussed no causal mechanisms.”