Modeling diurnal tidal variability with the National Center for Atmospheric Research thermosphere‐ionosphere‐mesosphere‐electrodynamics general circulation model

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

168 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/4ca14531e3cf588fb50ca69a651d5bf7df76dbc0

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Citations in the corpus

Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, background): “The tidal amplitudes in the MLT do not show a clear dependence on solar activity, while the thermospheric tides are strongly dependent on the solar activity.”
Impact of sudden stratospheric warmings on equatorial ionization anomaly (2010, result): “[30] Earlier studies showed that a strong semidiurnal tide can result from nonlinear interaction between tides and the quasi‐stationary planetary wave [ Hagan and Roble, 2001; Liu and Roble, 2002; Liu et al., 2007], and this mechanism is supported by growing observational and modeling evidence of e”
Unexpected connections between the stratosphere and ionosphere (2010, background): “Since the occurrence of SSWs is related to the growth of quasi‐stationary planetary waves [Matsuno, 1971], such a strong semidiurnal tide could result from nonlinear interaction between tides and a quasi‐stationary planetary wave [ Hagan and Roble, 2001; Liu and Roble, 2002].”
Ionospheric variability due to planetary waves and tides for solar minimum conditions (2010, result): “It is also found in previous studies that QSPWs can nonlinearly interact with atmospheric tides, leading to global responses of both migrating and nonmigrating components [e.g., Hagan and Roble, 2001; Liu et al., 2007; Fuller‐Rowell et al., 2008; Chang et al., 2009].”
Tropospheric tidal effects on the middle and upper atmosphere (2009, result): “[13] Evidence of the excitation of so-called secondary waves resulting from nonlinear interactions between primary waves from data analyses and in modeling investigations was previously reported [e.g., Teitelbaum and Vial, 1991; Hagan and Roble, 2001; Pancheva et al., 2002].”
Tidal perturbations and variability in the mesopause region over Fort Collins, CO (41N, 105W): Continuous multi‐day temperature and wind lidar observations (2004, background): “[9] The variability of the apparent tidal amplitudes and phases could be caused by interactions with planetary waves on global scales [Hagan and Roble, 2001] or interactions with gravity waves, or combination of both.”
The first 80‐hour continuous lidar campaign for simultaneous observation of mesopause region temperature and wind (2003, background): “Though the nature of the observed second wave with longer vertical wavelength is not clear, the excitation of secondary waves resulting from the mean wind effect or from W1 tide/S1 planetary wave interaction was confirmed in model studies [Hagan and Roble, 2001].”
Troposphere-Thermosphere Tidal Coupling as Measured by the SABER Instrument on TIMED during July-September, 2002 (2006, background): “Non-linear tide-tide interactions (Teitelbaum and Vial 1991; Smith and Ortland 2001) and tideplanetary wave interactions (Hagan and Roble 2001; Yamashita et al. 2002; Angelats i Coll and Forbes 2002; Lieberman et al. 2004; Grieger et al. 2004) in the stratosphere and mesosphere are also known to…”
Solar tides as revealed by measurements of mesosphere temperature by the MLS experiment on UARS (2006, background): “…observational analyses spawned a number of modeling investigations seeking to explain the origins and characteristics of nonmigrating tides in the MLT (i.e., Ekanayake et al. 1997; Miyahara et al. 1999; Forbes et al. 2001; Hagan and Roble 2001; Grieger et al. 2002; Hagan and Forbes 2002, 2003).”