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For decades, radiocarbon has been the gold standard for separating fossil and non-fossil CO2 (ffCO2) contributions in ambient atmospheric CO2. Although continuous 14CO2 measurements are promising, they are still unavailable with sufficient precision for atmospheric applications. Therefore, ongoing attempts are to use alternative continuously measurable proxies to quantify fossil CO2 admixture at a high temporal resolution. Proxies such as CO or NOx have the advantage of being observed by remote sensing as well. The ICOS Central Radiocarbon Laboratory was conducting an intensive research campaign on ffCO2 proxies for two and a half years at its urban pilot station in Heidelberg, Germany. The campaign aimed to investigate the potential and synergies of the three different ffCO2 proxies: CO, NOx and APO. All proxies have been observed continuously, and more than 400 flask samples have been collected and analysed for 14CO2. This study examines and compares proxy-specific properties resulting in first order from their different atmospheric lifetimes. In addition, we quantify variabilities in the proxy/ffCO2 ratio and deduce uncertainties of proxy-based ffCO2 estimates.
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