Variabilities of mesospheric tides during sudden stratospheric warming events of 2006 and 2009 and their relationship with ozone and water vapour

The present study demonstrates how the relationship between the high latitude northern hemispheric major sudden stratospheric warming (SSW) events of 2006 and 2009 and low-latitude mesospheric tidal variability in zonal winds observed by the MF radar at Tirunelveli (8.7°0N, 77.8°E) exists. It is found that the ozone mixing ratio increases at low latitudes during the SSW and it could probably be due to the SSW induced reversal of meridional circulation towards southward, which may aid the transport of ozone from high to low latitudes, but prevent the same from low to high latitudes. As semi-diurnal tide is produced due to solar insolation absorption of ozone and the increase in the ozone mixing ratio could be a reason for the increase in the semi-diurnal tidal amplitude. The variabilities of diurnal tide appear to be governed mostly by variation of specific humidity at 300 hPa over equator and intraseasonal variability dominates the variabilities in both the parameters.

► Demonstrated the relationship between SSW events and low-latitude mesospheric tides.
► Enhancement in the ozone mixing ratio at low-latitude stratosphere during the SSW events.
► Suggested that it could be a reason for the increase of semi-diurnal tidal amplitudes.
► Diurnal tidal variabilities governed mostly by tropospheric specific humidity variabilities.