Electrodynamics in the low and middle latitude ionosphere: a tutorial

By R. Heelis. 2004

384 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/fce2ab9f64d8b9b5c675020153484d9ed3afc6ce

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. B. Fejer
3. Han-Li Liu
4. Astrid Maute
5. Jorge L. Chau
6. L. P. Goncharenko
7. R. Roble
8. J. Oberheide

In Geophysics

1. J. Oberheide
2. Han-Li Liu
3. B. Fejer
4. L. P. Goncharenko
5. Jorge L. Chau
6. Astrid Maute
7. Hermann Lühr
8. M. E. Hagan

In Molecular Biology

1. B. Fejer
2. M. Purucker
3. Liying Qian
4. B. Langlais
5. T. Immel
6. S. Solomon
7. J. Oberheide
8. T. Sabaka

Citations in the corpus

• Lunar‐dependent equatorial ionospheric electrodynamic effects during sudden stratospheric warmings (2010, background): “[2] The quiet time low‐latitude ionospheric electric fields are generated by dynamo action of thermospheric neutral winds [e.g., Richmond, 1995a; Heelis, 2004 ].”
• Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, methodology): “For a comprehensive review on the physical principles underlying the electrodynamic properties of the equatorial and low-latitude ionosphere, we recommend reading Heelis (2004).”
• WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “[8] The daytime plasma drifts in the equatorial F layer are generated by the dynamo action of tidal winds in the E region between about 100–150 km [Martyn, 1953;Heelis et al., 1974; Anderson, 1981; Heelis, 2004].”
• Control of equatorial ionospheric morphology by atmospheric tides (2006, background): “and neutrals are much more frequent, with the result that the layer recombines and is reduced in density a hundredfold soon after sunset [Rees, 1989; Heelis, 2004].”
• The Magnetic Field of the Earth’s Lithosphere (2010, methodology): “Moreover, toroidal currents flow in the F-region of the ionosphere crossing the satellite orbit (see Heelis 2004); Maus and Lühr (2006) proposed a method for correcting CHAMP satellite data for them.”
• Longitudinal structure of the vertical E × B drift and ion density seen from ROCSAT‐1 (2007, background): “It is well established that these fields are present both at night and during the day [Kelley, 1989; Heelis, 2004].”
• Longitudinal variation of the E‐region electric fields caused by atmospheric tides (2006, background): “[12] The E-region dynamo is driven by poleward neutral winds in the thermosphere at E-region altitudes [see Heelis, 2004 and references therein].”
• Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, positive): “[5] The tides and planetary waves are known to affect the ionospheric variability through wind dynamo processes [e.g., Richmond, 1983; Heelis, 2004].”