Seasonal-latitudinal variation of the eastward-propagating diurnal tide with zonal wavenumber 3 in the MLT: Influences of heating and background wind distribution

Details Seasonal-latitudinal variation of the eastward-propagating diurnal tide with zonal wavenumber 3 in the MLT: Influences of heating and background wind distribution Seasonal-latitudinal variation of the eastward-propagating diurnal tide with zonal wavenumber 3 in the MLT: Influences of heating and background wind distribution

Apr 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012jastp..78...37z&link_type=abstract

Journal of Atmospheric and Solar-Terrestrial Physics, Volume 78, p. 37-43.

Physics

Scientific paper

This study demonstrates how the mean zonal wind affects the propagation of tidal energy from the troposphere to the mesosphere-lower thermosphere (MLT) region (60-120 km). We diagnose the seasonal-latitudinal variation of the eastward-propagating diurnal tide with zonal wavenumber 3 (DE3), which is a prominent tidal component and agrees well between model and observation in recent studies. It is shown that during the course of a year the seasonal-latitudinal variation of mean zonal wind modulates and filters DE3 energy propagating upwards from tropospheric radiative and latent heating sources. Our results are based upon ISCCP and TRMM troposphere heating rates, SABER-derived zonal mean gradient wind, SABER tidal signatures and GSWM (the global-scale wave model) diagnoses. The tropospheric tidal heating rates are derived from ISCCP (International Satellite Cloud Climatology Project) radiative fluxes and TRMM (Tropical Rainfall Measuring Mission) latent heating profiles together with TRMM rainfall rates. The zonal mean winds are derived from measurements of geopotential height from the SABER (sounding of the atmosphere with broadband emission radiometry) instrument on the TIMED (thermosphere, ionosphere, mesosphere energetics and dynamics) spacecraft, and the tidal signatures are determined from SABER temperature measurements.

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