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Boreal blazes

Biomass burning and vegetation types archived in the Juneau Icefield

Datos Bibliográficos

ID15548464
AutoresNatalie Kehrwald (0000-0002-9160-2239, Denver Federal Center, autor de correspondencia), Jeramy R Jasmann (0000-0002-5251-6987, United States Geological Survey), Melissa E Dunham (Dartmouth College), D G Ferris (0000-0003-2336-6163, Dartmouth College), E C Osterberg (0000-0002-0675-1230, Dartmouth College), Joshua A Kennedy (0000-0002-2265-4799, South Dakota State University), Jeremy C Havens (0000-0002-8685-2823, United States Geological Survey), Larry B Barber (0000-0002-0561-0831, United States Geological Survey), Sarah K Fortner (0000-0002-7075-1825, Wittenberg University)
Año2020
Volumen15
Número8
Páginas085005-085005
Fecha de publicación2020-05-04
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaEnvironmental Research Letters (JOURNAL)
Identificadores de la revistaISSN: 1748-9326 • E-ISSN: 1748-9326
EditorialIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab8fd2
OpenAlexW3021706945
IdiomaEN
Citas recibidas1
Referencias citadas42

The past decade includes some of the most extensive boreal forest fires in the historical record. Warming temperatures, changing precipitation patterns, the desiccation of thick organic soil layers, and increased ignition from lightning all contribute to a combustive combination. Smoke aerosols travel thousands of kilometers, before blanketing the surfaces on which they fall, such as the Juneau Icefield. However, many aerosols found in smoke plumes 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

Aerosol · Atmospheric sciences · Biomass burning · Boreal · Climatology · Ecosystem · Fire regime · Geography · Ice field · Levoglucosan · Meteorology · Physical geography · Taiga · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Fire effects on ecosystems · Ecology · Forestry · Geology

  • High-latitude fire activity of recent decades derived from microscopic charcoal and black carbon in Greenland ice cores

    Open Access•Sandra O Brugger, Nathan J Chellman et al.•The Holocene•2022

  • Long-Term Fire Regime Estimated from Soil Charcoal in Coastal Temperate Rainforests

    Open Access•K Lertzman, Daniel G Gavin et al.•Conservation Ecology•2002

Obras citantes distintas1
Citas por año0,25
Intervalo de citas2022 - 2022 (1)
Velocidad de citaciónhistorical
Altamente citadoNo
Tipos de citaNeutras: 1
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