Seasonal variations of the terdiurnal tide in the mesosphere and lower thermosphere: a model study

Observations of the terdiurnal (8-hour) tidal wind oscillations in the meso sphere and lower thermosphere (MLT) reveal strong seasonal and latitudinal variations. The tidal amplitudes reach a maximum of about 15-20 m s(-1) at midlatitudes in winter. The vertical phase progression corresponds to very long vertical wavelengths. During summer the amplitudes are typically weake r and the phases are less regular. First simulations of the terdiurnal tide with the Spectral Mesosphere/Lower Thermosphere Model are presented. The m odel explicitly accounts for the solar thermal excitation in the middle and upper atmosphere and reproduces the salient features of the terdiurnal win d oscillations well. The preferential solar excitation of antisymmetric ter diurnal modes capable of propagating into the MLT combined with an asymmetr ic atmospheric response appears to be primarily responsible for the observe d seasonal variations. Nonlinear interactions of the diurnal and semidiurna l tides are demonstrated to make a noticeable in situ contribution to the e xcitation of the terdiurnal tide at 95-100 km, especially during equinox.