Mapping urban methane (CH4) emissions

Mapping CH4 in urban areas is still challenging because emissions are often diffuse. A new study https://doi.org/10.1016/j.atmosenv.2024.120743 finds evidence of urban superemitters that can substantially incrase emissions.

Methane fluxes increased significantly with decreasing temperature and showed a negligible weekend to weekday effect. CH4 emissions were dominated by natural gas consumption in the residential, commercial and public sectors in Innsbruck. The average methane to CO2 flux was 0.2%. For the building sector this translates to a 100 y GWP adjusted value of 12% relative to CO2, Likely emission sources of methane are building vents and chimneys at roof top levels. Generally, post-metre emissions from gas furnaces consist of time-varying and constant factors. These include leaking valves and fittings, and incomplete combustion of natural gas appliances during ignition or usage. The study shows that time-varying fluxes due to malfunctioning devices and/or leaks can persist for months, increasing area weighted fluxes by up to a factor of 2. Eddy covariance observations above the urban canopy are uniquely suited to constrain the total methane flux, because measurements at street level could miss a large fraction of the post-meter emissions from building vents and chimneys in an urban area. Assessments of street level observations therefore likely yield a lower limit of urban methane emissions. 

Flux footprint weighted CH4 fluxes of the highest 5% plotted on top of a georeferenced areal image during November 2021 to June 2022. The blue dot represents the location of the IAO. The red dots are visually obtained chimneys and rooftop vents from an aerial photo around the emission hotspot

 

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