Abstract
Abstract. Thermal tides play an important
role in the global atmospheric dynamics and provide a key mechanism for the
forcing of thermosphere–ionosphere dynamics from below. A method for
extracting tidal contributions, based on the adaptive filtering, is applied
to analyse multi-year observations of mesospheric winds from ground-based
meteor radars located in northern Germany and Norway. The observed seasonal
variability of tides is compared to simulations with the Kühlungsborn
Mechanistic Circulation Model (KMCM). It is demonstrated that the model
provides reasonable representation of the tidal amplitudes, though
substantial differences from observations are also noticed. The limitations
of applying a conventionally coarse-resolution model in combination with
parametrisation of gravity waves are discussed. The work is aimed towards the
development of an ionospheric model driven by the dynamics of the KMCM.
Funder
Deutsche Forschungsgemeinschaft
Leibniz-Gemeinschaft
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geology,Astronomy and Astrophysics
Cited by
24 articles.
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