Boreal blazes: Biomass burning and vegetation types archived in the Juneau Icefield

Warming temperatures, changing precipitation patterns, vegetation marching northward, the desiccation of thick organic soil layers, and increased ignition from lightning all contribute to a combustive combination. The past decade includes some of the most extensive boreal forest fires in the historical record. Smoke aerosols travel thousands of kilometers, before blanketing the surfaces on which they fall, including locations far from fire, such as the Juneau Icefield. However, many aerosols found in fire are also produced by other processes and therefore can be ambiguous indicators of fire activity. Here, we use the monosaccharide anhydrides levoglucosan, mannosan, and galactosan as specific indicators of biomass burning to unambiguously demonstrate that fire aerosols reach the Juneau Icefield and are integrated into the snowpack. Back trajectories and satellite observations demonstrate that smoke plumes originating in central Alaska and eastern Siberia affect the Juneau Icefield. These regional sources of fire differ from other combustion aerosols deposited on the Juneau Icefield, such as black carbon, that originate from local fossil fuel burning. Ratios of levoglucosan/mannosan (L/M) and levoglucosan/(mannosan + galactosan) (L/(M+G)) demonstrate that while the majority of fire aerosols reaching the Juneau Icefield originate from softwood burning, grasslands and hardwood forests are also sources. The presence of these hardwoods suggests that fire aerosols may reach the Juneau Icefield from locations as far away as East Asia.