Abstract

Abstract. To investigate temporal variability of methane (CH4) fluxes in an urban environment, air–surface exchange fluxes of CH4 were continuously measured using eddy covariance techniques at a city-centre site in Łódź, Poland, from July 2013 to August 2015. In the immediate vicinity of the measurement site, potential methane sources include vehicle traffic, dense sewerage infrastructure and natural gas networks. Sensible and latent heat fluxes have also been measured since 2000 and carbon dioxide fluxes since 2007 at this site. Upward CH4 fluxes dominated during the measurement period, indicating that the city centre is a net source of CH4 to the troposphere. The highest monthly fluxes were observed in winter (2.0 to 2.7 g m−2 month−1) and the lowest in summer (0.8 to 1.0 g m−2 month−1). Fluxes on working days were around 6 % higher than on weekends. The cumulative flux indicates that the city centre emitted a net quantity of nearly 18 g m−2 of CH4 in 2014. Stable values of the FCO2∕ FCH4 ratio in months (minimum 2.41 × 10−3, maximum 5.3 × 10−3) and the lack of a clear annual course suggest comparable magnitude of both fluxes.

Highlights

  • The temporal and spatial variability of greenhouse gas fluxes in the atmosphere is currently one of the most widely discussed climatological problems in the scientific community

  • The effect of the combustion of natural gas is mainly water vapour and carbon dioxide

  • The combustion of fossil fuels is, predominantly incomplete and is an important factor causing anthropogenic methane emissions. This happens in the case of combustion of both natural gas and hydrocarbons contained in petrol and other fuels (Nam et al, 2004; Nakagawa et al, 2005; Wennberg et al, 2012)

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Summary

Introduction

The temporal and spatial variability of greenhouse gas fluxes in the atmosphere is currently one of the most widely discussed climatological problems in the scientific community. An increase in the concentration of methane contributes to an enhancement of the greenhouse effect (Ciais et al, 2013) Emissions of this gas into the atmosphere should be carefully monitored. The combustion of fossil fuels is, predominantly incomplete and is an important factor causing anthropogenic methane emissions. This happens in the case of combustion of both natural gas and hydrocarbons contained in petrol and other fuels (Nam et al, 2004; Nakagawa et al, 2005; Wennberg et al, 2012).

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