This payer uses dissipation values derived from UARS/HRDI observations
in a recently published diurnal-tide model. These model structures co
mpare quite well with the UARS/HRDI observations with respect to the a
nnual variation of the diurnal tidal amplitudes and the size of the am
plitudes themselves. It is suggested that the annual variation of atmo
spheric dissipation in the mesosphere-lower thermosphere is a major co
ntrolling factor in determining the annual variation of the diurnal ti
de.