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Air-sea exchange of gaseous elemental mercury (Hg() is influenced by different meteorological factors and the availability of Hg in seawater. Here, we use the MITgcm ocean model to explore the interannual variability of this flux and the influence of oceanographic and atmospheric dynamics. We apply the GEOS-Chem model to further simulate the potential impact of the evasion variability on the atmospheric Hg levels. We find a latitudinal pattern in Hg( evasion with a relatively small variability in mid-latitudes (3.1-6.7%) and a large on
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