Mars Global Surveyor radio science electron density profiles : Neutral atmosphere implications
By S. Bougher, S. Engel, D. Hinson, Jeff Forbes. 2001
164 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Statistical and Nonlinear Physics
View Paper: https://www.semanticscholar.org/paper/bd1bafb6adf7e16042f722ac5c100fefbf9b55e0
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In Astronomy and Astrophysics
- P. Withers
- Francois Forget
- J. Chaufray
- François Leblanc
- Jean-Loup Bertaux
- J. Fox
- M. López‐Valverde
- F. González-Galindo
In Statistical and Nonlinear Physics
Citations in the corpus
- MGS Radio Science electron density profiles: Interannual variability and implications for the Martian neutral atmosphere (2004, background): “In particular, nonmigrating tidal forcing is implicated by these high latitude ionospheric wave features [Bougher et al., 2001].”
- A review of observed variability in the dayside ionosphere of Mars (2009, methodology): “Electron densities at the altitude of the M1 layer change by the square root of 10, as expected for molecular ions lost by dissociative recombination (Rishbeth and Garriott, 1969; Bougher et al., 2001).”
- Martian dayglow as seen by the SPICAM UV spectrograph on Mars Express (2006, methodology): “…is significant, with diurnal Kelvin waves and semi-diurnal tides providing significant temperature and wind perturbations in the lower thermosphere [Bougher et al., 2000, 2001; Forbes et al., 2002; Wang and Nielsen, 2004; Withers et al., 2004] as well as nonmigrating tidal waves associated with…”
- Variation of the Martian Ionospheric Electron Density from Mars Express Radar Soundings (2008, methodology): “Modeling efforts based on MGS radio occultation include those of Bougher et al. [2000] and Fox and Yeager [2006]. More recently, Pätzold et al.”
- The plasma Environment of Mars (2004, background): “, 1998) and also provided additional radio occultation electron density profiles (Bougher et al., 2001).”
- Three‐dimensional Martian ionosphere model: I. The photochemical ionosphere below 180 km (2013, background): “The longitudinal variability of the main peak altitude and electron density predicted by the MTGCM is in agreement with that inferred from MGS measurements [Bougher et al., 2001], showing the importance of the coupling between the neutral atmosphere and the ionosphere [Bougher et al.”