Patterns of COâ and radiocarbon across high northern latitudes during International Polar Year 2008
High-resolution in situ COâ measurements were conducted aboard the NASA DC-8 aircraft during the ARCTAS/POLARCAT field campaign, a component of the wider 2007â2008 International Polar Year activities. Data were recorded during large-scale surveys spanning the North American sub-Arctic to the North Pole from 0.04 to 12 km altitude in spring and summer of 2008. Influences on the observed COâ concentrations were investigated using coincident CO, black carbon, CHâCN, HCN, Oâ, C2Cl4, and ι â´COâ data, and the FLEXPART model. In spring, the COâ spatial distribution from 55°N to 90°N was largely determined by the long-range transport of air masses laden with Asian anthropogenic pollution intermingled with Eurasian fire emissions evidenced by the greater variability in the mid-to-upper troposphere. At the receptor site, the enhancement ratios of COâ to CO in pollution plumes ranged from 27 to 80 ppmv ppmv-1 with the highest anthropogenic content registered in plumes sampled poleward of 80°N. In summer, the COâ signal largely reflected emissions from lightning-ignited wildfires within the boreal forests of northern Saskatchewan juxtaposed with uptake by the terrestrial biosphere. Measurements within fresh fire plumes yielded COâ to CO emission ratios of 4 to 16 ppmv ppmv-1 and a mean COâ emission factor of 1698 ± 280 g kg-1 dry matter. From the ¹ â´C in COâ content of 48 whole air samples, mean spring (46.6 ± 4.4â°) and summer (51.5 ± 5â°) ι â´COâ values indicate a 5â° seasonal difference. Although the northern midlatitudes were identified as the emissions source regions for the majority of the spring samples, depleted ι â´COâ values were observed in <1% of the data set. Rather, ARCTAS ι â´COâ observations (54%) revealed predominately a pattern of positive disequilibrium (1-7â°) with respect to background regardless of season owing to both heterotrophic respiration and fire-induced combustion of biomass. Anomalously enriched ι â´COâ values (101-262â°) measured in emissions from Lake Athabasca and Eurasian fires speak to biomass burning as an increasingly important contributor to the mass excess in ι â´COâ observations in a warming Arctic, representing an additional source of uncertainty in the quantification of fossil fuel COâ.
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https://n2t.org/ark:/85065/d7mw2hn5
eng
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2016-01-01T00:00:00Z
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2011-07-16T00:00:00Z
Copyright 2011 American Geophysical Union.
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