Migrating thermospheric tides

By M. E. Hagan, R. Roble, J. Hackney. 2001

181 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Oceanography

View Paper: https://www.semanticscholar.org/paper/21584dbf256830052223e773668db82cc4945d89

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Citations in the corpus

Control of equatorial ionospheric morphology by atmospheric tides (2006, methodology): “[7] Overlaid on this image are contours of the equinoctial amplitude of the diurnal temperature variation at 115 km determined from the Global Scale Wave Model (GSWM) [Hagan et al., 2001; Hagan and Forbes, 2002, 2003; Forbes et al., 2003].”
Longitudinal variability of low‐latitude total electron content: Tidal influences (2007, methodology): “[25] The Immel et al. [2006] study also reported a phase shift in the peak brightness of their nighttime UV observations of about 20 to the east when compared to the diurnal peak amplitudes of the temperature variation at 115 km as given by the Global Scale Wave Model (GSWM) [ Hagan et al., 2001; H”
A theory of ionospheric response to upward‐propagating tides: Electrodynamic effects and tidal mixing effects (2013, background): “When the lower-boundary forcing is off, the main tidal component resolved in the model is the vertically nonpropagating migrating diurnal component produced by solar ultraviolet heating in the thermosphere [Hagan et al., 2001].”
Modeling diurnal tidal variability with the National Center for Atmospheric Research thermosphere‐ionosphere‐mesosphere‐electrodynamics general circulation model (2001, methodology): “In the thermosphere it also varies with the solar cycle [e.g., Hagan et al., 2001].”
Impact of sudden stratospheric warmings on equatorial ionization anomaly (2010, unknown): “ionosphere [Forbes and Leveroni, 1992; Hagan et al., 2001; Abdu et al., 2006; Fuller‐Rowell et al., 2008].”
Causes of low thermospheric density during the 2007–2009 solar minimum (2011, methodology): “Tidal forcing at the lower boundary was specified by the Global Scale Wave Model [Hagan et al., 2001], and semiannual and annual density periodicities were obtained by applying seasonal variation of the eddy diffusivity coefficient at the lower boundary [Qian et al.”
Quiet variability of equatorial E × B drifts during a sudden stratospheric warming event (2009, background): “For example, atmospheric tides generated in the troposphere and stratosphere propagate upward and dominate the dynamics of the lower thermosphere [e.g., Hagan et al., 2001].”