Summary
A compilation of sea salt data from East Antarctic ice cores are used to quantify the contribution of open ocean and sea ice to the sea salt budget. The ice cores used in this study are from Law Dome, Totten Glacier, Wilkes Land and Wilhelm II Land. Also included are ice cores from off the coast on Mill Island and iceberg B09B (which was grounded near the Mertz Glacier). Sea salt aerosols have two main sources, namely ocean sea spray (related to wind strength) and surface sea ice (due to frost flowers). Frost flowers sources are depleted in sulphate, and this contribution can be calculated from deviations to the expected sulphate:sodium ratio found in seawater. This was calculated for the array of ice cores, and we find that the frost flower source to the Antarctic ice sheet diminishes with elevation and distance inland.