Arctic source for elevated atmospheric mercury (Hg0) in the western Bering Sea in the summer of 2013


Tom Sizmur

DOI:10.1016/j.jes.2016.12.022

Received April 18, 2016,Revised November 30, 2016, Accepted December 27, 2016, Available online February 20, 2017

Volume 68,2018,Pages 114-121

Measurements of gaseous elemental mercury (Hg0) in the marine boundary layer of the western Bering Sea were performed using an automatic mercury analyzer RA 915 + (Ltd. “Lumex”, St. Petersburg, Russia) aboard the Russian research vessel Academician M.A. Lavrentev from 3 to 20 August 2013. Hg0 concentrations varied from 0.3 to 2.1 ng/m3 (n = 4783); the average value (1.1 ± 0.3 ng/m3) was lower than both the background range of the Northern Hemisphere (1.5–1.7 ng/m3) and average values previously observed in the Bering Sea, and corresponded to the background concentrations of the Southern Hemisphere (1.1–1.3 ng/m3). Maximum Hg0 concentrations were observed within air masses that came from the lower troposphere of the central Arctic. Under these conditions, Hg0 ranged between 1.1 and 2.1 ng/m3 with an average of 1.5 ± 0.2 ng/m3 (n = 1183). Except for these periods, Hg0 concentrations during the rest of the study varied from 0.3 to 1.8 ng/m3, with an average value of 1.0 ± 0.2 ng/m3 (n = 3600). Our results support the hypothesis that, in the summer, air masses from the central Arctic Ocean can be an exporter of mercury to lower latitudes. Perhaps the atmospheric transport of elevated concentrations of Hg0 into lower latitudes may have implications for the biologic and economic health of important fisheries, such as the Bering Sea.

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