The Cryosphere (Mar 2021)

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

  • G. Shi,
  • G. Shi,
  • H. Ma,
  • Z. Hu,
  • Z. Chen,
  • C. An,
  • S. Jiang,
  • Y. Li,
  • T. Ma,
  • J. Yu,
  • D. Wang,
  • S. Lu,
  • B. Sun,
  • M. G. Hastings,
  • M. G. Hastings

DOI
https://doi.org/10.5194/tc-15-1087-2021
Journal volume & issue
Vol. 15
pp. 1087 – 1095

Abstract

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To better understand snow chemistry in different environments across the Antarctic ice sheet, we investigated snow ions on a traverse from the coast to Dome 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 nssSO42- on the coast indicates sea salts from the sea ice, and marine biogenic emissions dominate snow SO42- in interior areas throughout the year.