A theory of ionospheric response to upward‐propagating tides: Electrodynamic effects and tidal mixing effects

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Sq and EEJ—A Review on the Daily Variation of the Geomagnetic Field Caused by Ionospheric Dynamo Currents (2017, background): “Yamazaki and Richmond (2013), and Yamazaki et al. (2014b) showed that about one third of Sq currents and about one-half of EEJ are driven by the upward-propagating tides.”
Sudden Stratospheric Warmings (2020, background): “This altered mean meridional circulation leads to an increase of [O] and a decrease of [N 2 ] in the lower thermosphere that is then communicated to the upper thermosphere via molecular dif-981 fusion (e.g., Yamazaki & Richmond, 2013).”
Variability and predictability of the space environment as related to lower atmosphere forcing (2016, background): “On the other hand, tidal modulation of atomic oxygen recombination rate [Akmaev and Shved, 1980; Forbes et al., 1993] is found to be insignificant in the MLT region, probably due to the very long chemical lifetime of atomic oxygen therein [Yamazaki and Richmond, 2013].”
Internal wave coupling processes in Earth's atmosphere (2014, unknown): “Their impacts can be estimated by turning on and off the tidal activity in the lower atmosphere (Yamazaki and Richmond , 2013).”