An investigation into the influence of tidal forcing on F region equatorial vertical ion drift using a global ionosphere‐thermosphere model with coupled electrodynamics

By G. Millward, I. Müller‐Wodarg, A. Aylward, T. Fuller‐Rowell, Arthur D. Richmond, R. Moffett. 2001

180 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Astronomy and Astrophysics

View Paper: https://www.semanticscholar.org/paper/44fd456394f0c942c73d048e74b23e402676da8b

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In Aerospace Engineering

1. Y. Yamazaki
2. T. Fuller‐Rowell
3. Han-Li Liu
4. H. Frey
5. Arthur D. Richmond
6. N. Pedatella

In Astronomy and Astrophysics

1. Scott L. England
2. T. Immel
3. M. E. Hagan
4. H. Frey
5. Arthur D. Richmond
6. Han-Li Liu
7. Y. Yamazaki
8. Larry J. Paxton

Citations in the corpus

• The influence of atmospheric tide and planetary wave variability during sudden stratosphere warmings on the low latitude ionosphere (2013, background): “…significantly to the ionosphere electrodynamics [e.g., Liu and Richmond, 2013]; however, the DW1 contribution to the electrodynamics is primarily due to the in situ component generated by solar forcing and not the upward propagating tide generated in the lower atmosphere [Millward et al., 2001].”
• A theory of ionospheric response to upward‐propagating tides: Electrodynamic effects and tidal mixing effects (2013, background): “Although most tidal waves from the lower and middle atmosphere are not able to propagate into the F region ionosphere, they can influence the distribution of F region plasma by modulating the ionospheric E region wind dynamo and equatorial plasma fountain [Millward et al., 2001].”
• Quiet time equatorial F region vertical plasma drift model derived from ROCSAT‐1 observations (2008, unknown): “Millward et al. [2001] examined the global effects of tidal forcing on F region equatorial vertical ion drifts using the Coupled”
• Interaction between direct penetration and disturbance dynamo electric fields in the storm‐time equatorial ionosphere (2005, methodology): “[7] In this study, we used the Coupled ThermosphereIonosphere-Plasmasphere-Electrodynamics (CTIPe) model [Millward et al., 2001; Fuller-Rowell et al., 2002] and the Rice Convection Model (RCM) [e.g., Wolf, 1983].”
• Control of equatorial ionospheric morphology by atmospheric tides (2006, background): “Recent simulations performed to study the effect of upward-propagating tidal energy in a global circulation model showed that several of the major diurnal tidal modes have a significant influence on the vertical plasma drifts in the F-region during the daytime [Millward et al., 2001].”
• Longitudinal structure of the equatorial anomaly in the nighttime ionosphere observed by IMAGE/FUV (2005, background): “However, because the prereversal enhancement of vertical plasma drift over the equator is controlled by both E layer and F layer dynamos, it is quite possible that the EA during the night is also affected by the E layer dynamo [Millward et al., 2001].”