the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The monitoring network of greenhouse gas (CO2, CH4) in the Paris' region
Abstract. There is a growing interest for the study of greenhouse gas emissions over urban areas. In this context, a network for measuring greenhouse gas concentrations was set up in Paris in 2015. Since then, seven stations located in and around Paris and equipped with cavity ring-down spectrometers (CRDS) have been monitoring gas concentrations of different species (CO2, CH4, CO) on a continuous basis. Procedures for maintenance, calibration, data processing have been adapted to ensure that the network is operational, providing good quality data in near-real time (NRT) and with high availability. The CO2 and CH4 concentrations show a growth rate of the baseline (linear trend of the averaged concentrations over the Paris region) concentrations (+2.34 ppm CO2/year and +11.1 ppb CH4/year) between 2015 and 2022 consistent with that observed at remote observatories such as Jungfraujoch (Switzerland). The amplitude of the CO2 seasonal cycle is around 20 ppm (i.e. around 5 %) while that of CH4 is 40 ppb (i.e. around 2 %). The concentration gradients calculated as the differences between up- and down-wind concentrations, can be used to infer the emissions for long lived species. We use the measurements from the 100 m Saclay tower, outside of Paris, as a regional background during suitable wind direction conditions. The largest differences with these background measurements are observed in the two stations that are located within Paris (JUS and CDS), with urban offset up to ~ 50 ppm CO2 and ~ 100 ppb CH4 in winter and ~ 10 ppm CO2 and ~ 50 ppb CH4 in summer. In winter, the co-variability of CO and CO2 hourly measurements (correlation coefficient r ~ 0.9 in all stations) indicates that the concentration variability is driven by anthropogenic emissions. Conversely, in summer, lower correlations between these two gases concentration (r ~ 0.3 in peri-urban stations and r ~ 0.6 at CDS and JUS) shows the more dominant role of vegetation fluxes.
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