2018
DOI: 10.1088/1748-9326/aabf65
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Quantifying the variability of potential black carbon transport from cropland burning in Russia driven by atmospheric blocking events

Abstract: The deposition of short-lived aerosols and pollutants on snow above the Arctic Circle transported from northern mid-latitudes have amplified the short term warming in the Arctic region. Specifically, black carbon has received a great deal of attention due to its absorptive efficiency and its fairly complex influence on the climate. Cropland burning in Russia is a large contributor to the black carbon emissions deposited directly onto the snow in the Arctic region during the spring when the impact on the snow/i… Show more

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Cited by 13 publications
(7 citation statements)
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“…Shorter fire return intervals combined with climate change-induced drought will reduce the resiliency of evergreen and broadleaf species to re-seed and/or establish after wildfires, leading to expansion of grassland ecosystems in what is now Northern Canadian forests . Increased grass-dominated landscapes would create a new fire regime of frequent but low severity fires, with the likelihood of SLCF transport to the Arctic most likely in the spring months of March through May (Hall and Loboda, 2018).…”
Section: Climate Change Will Increase Number Of Non-forest Firesmentioning
confidence: 99%
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“…Shorter fire return intervals combined with climate change-induced drought will reduce the resiliency of evergreen and broadleaf species to re-seed and/or establish after wildfires, leading to expansion of grassland ecosystems in what is now Northern Canadian forests . Increased grass-dominated landscapes would create a new fire regime of frequent but low severity fires, with the likelihood of SLCF transport to the Arctic most likely in the spring months of March through May (Hall and Loboda, 2018).…”
Section: Climate Change Will Increase Number Of Non-forest Firesmentioning
confidence: 99%
“…For example, the timing of fires in agricultural landscapes, boreal forest fires, and the Arctic tundra occur during the early spring to early summer months (i.e., March through May for 50° N and May and June for 60° N and 65° as seen in Suppl. to the Arctic is possible and critical for the cryosphere (Hall and Loboda, 2018) and air pollution (Law and Stohl, 2007), both from long-range (Thomas et al, 2017) and local sources of BC deposition (Evangeliou et al, 2019). For example, BC transport is possible as early as March into mid-May for agricultural landscapes of eastern Europe (Hall and Loboda, 2017) and peatlands, grasslands, and forests in North America (Qi and Wang, 2019), with fires grasslands, forests, and agricultural lands most common in southern Siberia (Kukavskaya et al, 2016) and the Russian Far East (Hayasaka et al, 2020) during the spring months of March, April, and May.…”
Section: Non-fire Anthropogenic Versus Fire Emissionsmentioning
confidence: 99%
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“…Her notable works include the development of new algorithms for determining burned area and carbon cycle products in satellite sensor imagery [34] and assessing fire risk in Russia [243]. Her recent works have included efforts to assess black carbon emissions from cropland burning in Russia, with impacts on the Arctic [244,245].…”
Section: Approachmentioning
confidence: 99%
“…Her notable works include the development of new algorithms for determining burned area and carbon-cycle products in satellite sensor imagery [200], and assessing fire risk in Russia [412]. Her recent works include efforts to assess black carbon emissions from cropland burning in Russia, with impacts on the Arctic [413,414].…”
Section: Kendra Mclauchlan Is a Professor At Kansas State University mentioning
confidence: 99%