A longitudinal variation in the mesopause semi-annual oscillation (SAG
) is documented from wind observations made by the High Resolution Dop
pler Imager satellite instrument. The asymmetry is dominated by a wave
number 1 pattern with a variable phase. During the easterly phase of t
he mesopause SAO (equinoxes), maximum tropical easterlies occur over e
astern South America and the Atlantic Ocean in the longitude band 300
degrees-360 degrees. During the westerly phase (solstices), the wester
ly winds descend more rapidly and are larger below similar to 80 km in
this same (Atlantic) longitude band. To the best that can be determin
ed with sparse data, the longitudinal asymmetries near the stratopause
are weak and are in phase with those in the mesosphere.