“…In North America seasonal patterns in wet deposition are observed in both depositional flux and concentration with the highest values in the summer and lowest values in the winter (Sorensen et al, 1994;Mason et al, 2000;Guentzel et al, 2001;Keeler et al, 2005;VanArsdale et al, 2005;Choi et al, 2008;Prestbo and Gay, 2009). Explanations for this observation include more effective Hg scavenging by rain compared to snow (Sorensen et al, 1994;Mason et al, 2000;Keeler et al, 2005;Selin and Jacob, 2008), a greater availability of soluble Hg due to convective transport in summer events (Guentzel et al, 2001;Keeler et al, 2005), and a summer increase in Hg-containing soil derived particles in the atmosphere (Sorensen et al, 1994).…”