Planetary waves in coupling the lower and upper atmosphere

By A. Pogoreltsev, A. Vlasov, K. Fröhlich, C. Jacobi. 2007

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Ionospheric variability due to planetary waves and tides for solar minimum conditions (2010, background): “…that ultrafast Kelvin waves and short‐period planetary waves can propagate up to 150 km and capable of causing ionospheric perturbations, while long‐period and quasi‐stationary planetary waves cannot penetrate to the thermosphere [Forbes, 2000; Takahashi et al., 2007; Pogoreltsev et al., 2007].”
Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, background): “The former is difficult to conceive since quasi-stationary PWs are mostly limited to high and middle latitudes (e.g., Pogoreltsev et al. 2007) and their vertical propagation is confined below the critical layer near the mesopause where the zonal wind reverses (e.g., Sassi et al. 2002).”
Unexpected connections between the stratosphere and ionosphere (2010, background): “latitudes of the winter hemisphere, and are mostly limited to high and middle latitudes [Pogoreltsev et al., 2007; Pancheva et al., 2009].”
Impact of sudden stratospheric warmings on equatorial ionization anomaly (2010, background): “The quasi‐stationary planetary waves originate from high latitudes of the winter hemisphere,andthoughtheycanpropagatehorizontally,they are mostly confined to high and middle latitudes, as was shown in both simulations and observations [ Pogoreltsev et al., 2007; Pancheva et al., 2009].”