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Stochastic Time-Inverted Lagrangian Transport model outputs quantify the influence of upwind surface fluxes on greenhouse gas concentrations measured at the NOAA Barrow Alaska Observatory. The dataset contains footprint fields for 12 selected years between 15 August and 15 October across a 30-year study period from 1982 to 2011. These results support retrospective analysis linking atmospheric composition changes to shifts in Arctic ecosystem structure and carbon cycling.
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