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Abstract. To better understand snow chemistry in different environments across theAntarctic ice sheet, we investigated snow ions on a traverse from the coast toDome A. Results show that the non-sea-salt (nss) fractions of K+ , Mg2+ , and Ca2+ are mainly from terrestrial particle mass and nssCl− is associated with HCl. Spatially, the non-sea-salt fractions of ions to the totals are higher in the interior areas than on the coast, and seasonally, the proportions are higher in summer than in winter. Negative nssSO 4 2 - on the coast indicatessea salts from the sea ice, and marine biogenic emissions dominate snow SO 4 2 - in interior areas throughout the year.

the cryosphere

Brief communication: Spatial and temporal variations in surface snow chemistry along a traverse from coastal East Antarctica to the ice sheet summit (Dome A)