Continuous measurements of atmospheric dimethylsulfide (DMS) have been perf
ormed over a IO-year period (1990-1999) at Amsterdam Island in the southern
Indian Ocean. Atmospheric DMS ranges from 5 to 1930 parts per trillion by
volume (pptv) and shows a clear seasonal variation with a factor of 20 in a
mplitude between its maximum in January (austral summer) and minimum in Jul
y-August (austral winter). Important deviations from the IO-year monthly me
an as high as 100% have been detected, which could not be explained by chan
ges in meteorology and/or oxidation capacity of the atmosphere. Comparison
with a three dimensional (3-D) chemistry/transport model revealed that chan
ges in the source strength of DMS as high as a factor of 2 were required to
account for such DMS interannual variations. In addition, DMS variability
was found to be closely related to sea surface temperature anomalies, clear
ly indicating a link between DMS and climate changes.