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Using wildland fire tracer molecules to investigate fire frequency and vegetative combustion sources archived in the Juneau Icefield of Alaska

Dates

Publication Date
Time Period
2016
Time Period
2017

Citation

Jasmann, J.R., Kehrwald, N.M., Dunham, M.E., Ferris, D.G., Osterburg, E.C., Kennedy, J., and Barber, L.B., 2020, Using wildland fire tracer molecules to investigate fire frequency and vegetative combustion sources archived in the Juneau Icefield of Alaska: U.S. Geological Survey data release, https://doi.org/10.5066/P9DNAN1M.

Summary

The past decade includes some of the most extensive boreal forest fires in the historical record. Environmental drivers include warming temperatures, changing precipitation patterns, desiccation of thick organic soil layers, and increased ignition frequency from lightning. Wildland fires produce smoke aerosols that can travel thousands of kilometers, before blanketing the surfaces on which they fall, such as the Juneau Icefield of Alaska. This data release presents chemical constituent and physical particulate results from investigations of wildland fire smoke deposits and other atmospheric deposition characteristics stored in layers of ice in the Juneau Icefield of Alaska, USA (Tables 1 and 2). We drilled a series of four firn cores [...]

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Attached Files

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Juneau Icefield Alaska Map.jpg thumbnail 757.33 KB image/jpeg
Table 1 Site Locations.xlsx 12.31 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet
Table 2 Constituents Analyzed.xlsx 13.34 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet
Table 3 Quality Assurance.xlsx 143.32 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet
Table 4 Constituent Data.xlsx 253.58 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet

Purpose

The deposition of black carbon onto glaciers is known to increase the melting rate which has severe implications on sustainability of fresh water availability and water quality to downstream communities in certain regions. The source of black carbon and other co-transported smoke aerosols and particulates can not be distinguished to have come from wildland fires or industrial fossil fuel burning without the use of other chemical tracer molecules. This study uses the monosaccharide anhydride stereoisomers (also called anhydrosugars) combustion products levoglucosan, mannosan, and galactosan as specific indicators of biomass burning to unambiguously demonstrate that wildland 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. Our smoke aerosol tracer method informs water and land resource managers on source locations of recent and historic fire aerosol and particulate deposits archived in the ice, along with revealing historical trends and links between climate, shifts in local vegetation type, and wildland fire activity frequency and intensity.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9DNAN1M

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