Seasonal variations in Antarctic non-migrating tides

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[3332] Atmospheric Processes / Mesospheric Dynamics, [3389] Atmospheric Processes / Tides And Planetary Waves

Scientific paper

Atmospheric radars operated in Antarctica by Australia (Davis), Japan (Syowa), the United Kingdom and the United States of America (Rothera) and New Zealand (Scott Base) form a network of observing sites that allow decomposition of tidal wind variations in the mesosphere and lower thermosphere (MLT, 70-100km) into three westward and one standing wavenumber. These tides exhibit variations on both seasonal and multi-day time scales. In the case of the semidiurnal westward-one tide, there is evidence that the summertime short term variability is due to changes in their forcing and that this forcing occurs in the opposite (northern) hemisphere. Less is known about the variations at other wavenumbers. Data obtained between 2002 and the present have allowed the compilation of a climatology of southern polar MLT tides. Strong seasonal variations are apparent in a number of the extracted wavenumbers for both the diurnal and the semidiurnal tides. The nature of these seasonal variations will be described and discussed. The relationship between the global planetary wave field (from assimilated data sets) and the short-term variations in tidal amplitude and phase will also be considered.

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