Seasonally resolved ice core records from West Antarctica indicate a sea ice source of sea‐salt aerosol and a biomass burning source of ammonium. Issue 14 (21st July 2014)

• Record Type: Journal Article
• Authors: Pasteris, Daniel R.; McConnell, Joseph R.; Das, Sarah B.; Criscitiello, Alison S.; Evans, Matthew J.; Maselli, Olivia J.; Sigl, Michael; Layman, Lawrence
• Is Part Of: Journal of geophysical research. Volume 119:Issue 14(2014)
• Page Start: 9168
• Page End: 9182
• Publication Date: 2014-07-21
• Subjects: Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2013JD020720
• Languages: English
• ISSNs: 2169-897X

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>The sources and transport pathways of aerosol species in Antarctica remain uncertain, partly due to limited seasonally resolved data from the harsh environment. Here, we examine the seasonal cycles of major ions in three high‐accumulation West Antarctic ice cores for new information regarding the origin of aerosol species. A new method for continuous acidity measurement in ice cores is exploited to provide a comprehensive, charge‐balance approach to assessing the major non‐sea‐salt (nss) species. The average nss‐anion composition is 41% sulfate (SO<sub>4</sub><sup>2−</sup>), 36% nitrate (NO<sub>3</sub><sup>−</sup>), 15% excess‐chloride (ExCl<sup>−</sup>), and 8% methanesulfonic acid (MSA). Approximately 2% of the acid‐anion content is neutralized by ammonium (NH<sub>4</sub><sup>+</sup>), and the remainder is balanced by the acidity (Acy ≈ H<sup>+</sup> − HCO<sub>3</sub><sup>−</sup>). The annual cycle of NO<sub>3</sub><sup>−</sup> shows a primary peak in summer and a secondary peak in late winter/spring that are consistent with previous air and snow studies in Antarctica. The origin of these peaks remains uncertain, however, and is an area of active research. A high correlation between NH<sub>4</sub><sup>+</sup> and black carbon (BC) suggests that a major source of NH<sub>4</sub><sup>+</sup> is midlatitude biomass burning rather than marine biomass decay, as previously assumed. The annual peak in excess chloride (ExCl<sup>−</sup>) coincides with the late‐winter maximum in sea ice extent. Wintertime ExCl<sup>−</sup> is correlated with offshore sea ice concentrations and inversely correlated with temperature from nearby Byrd station. These observations suggest that the winter peak in ExCl<sup>−</sup> is an expression of fractionated sea‐salt aerosol and that sea ice is therefore a major source of sea‐salt aerosol in the region.</p> </abstract>