Abstract
Cities have multiple fugitive emission sources of methane (CH4) and policies adopted by China on replacing coal with natural gas in recent years can cause fine spatial heterogeneities at the range of kilometers within a city and also contribute to the CH4 inventory. In this study, a mobile observatory was used to monitor the real-time CH4 concentrations at fine spatial and temporal resolutions in Beijing, the most important pilot city of energy transition. Results showed that: several point sources, such as a liquefied natural gas (LNG) power plant which has not been included in the Chinese national greenhouse gas inventory yet, can be identified; the ratio “fingerprints” (CH4:CO2) for an LNG carrier, LNG filling station, and LNG power plant show a shape of “L”; for city observations, the distribution of CH4 concentration, in the range of 1940–2370 ppbv, had small variations while that in the rural area had a much higher concentration gradient; significant correlations between CO2 and CH4 concentrations were found in the rural area but in the urban area there were no such significant correlations; a shape of “L” of CH4:CO2 ratios is obtained in the urban area in wintertime and it is assigned to fugitive emissions from LNG sources. This mobile measurement methodology is capable of monitoring point and non-point CH4 sources in Beijing and the observation results could improve the CH4 inventory and inform relevant policy-making on emission reduction in China.
Highlights
Methane (CH4 ) contributes ~17% of the radiative forcing by the long-lived greenhouse gases (GHG) [1], with global warming potential (GWP) more than 25 times greater than that of CO2 at a 100-yr time horizon [2]
A mobile observatory was applied to real-time monitor the CH4 concentration of point and
A mobile observatory was applied to real-time monitor the CH4 concentration of point and non-point sources in Beijing
Summary
Methane (CH4 ) contributes ~17% of the radiative forcing by the long-lived greenhouse gases (GHG) [1], with global warming potential (GWP) more than 25 times greater than that of CO2 at a 100-yr time horizon [2]. Its mean annual increase rate witnessed no growth during 1999–2006 but has been increasing again since 2007 [1,3]. Increased emission from anthropogenic sources at mid-latitudes of the northern hemisphere has been considered as one possible main contributor of the recent increase [1,3], while some estimates indicated that China is the world’s largest anthropogenic emitter of CH4 [4]. It is essential to quantify the anthropogenic sources of CH4 emissions in China and further evaluate their contributions. Atmosphere 2019, 10, 554 important anthropogenic sources of CH4 [5].
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