After correcting for seasonal variations and long-term (linear or quad
ratic) trends, the residual interannual anomalies (variations) of the
trace elements and surface aerosol show periodicities in the Quasi-bie
nnial Oscillation (2-3 years) and 3-5 years range. Quasi-biennial Osci
llations (QBO) of some elements match with the QBO of equatorial 50-hP
a wind, but for some others, matching is not good. For some elements,
matching with Southern Oscillation index is good. The relationship is
probably through the sea-surface temperature changes, which affect the
role of the ocean as a source/sink for these trace elements. Interact
ion between equatorial wind QBO and extratropical phenomena should als
o be involved.