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Atmospheric Fossil Fuel CO2 Traced by Δ14C in Beijing and Xiamen, China: Temporal Variations, Inland/Coastal Differences and Influencing Factors
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Title

Atmospheric Fossil Fuel CO2Traced by Δ14C in Beijing and Xiamen, China: Temporal Variations, Inland/Coastal Differences and Influencing Factors

Authors

Niu, ZC; Zhou, WJ; Wu, SG; Cheng, P; Lu, XF; Xiong, XH; Du, H; Fu, YC; Wang, GH

Abstract

One year of atmospheric Δ14CO2were observed in 2014 in the inland city of Beijing and coastal city of Xiamen, China, to trace temporal CO2ffvariations and to determine the factors influencing them. The average CO2ffconcentrations at the sampling sites in Beijing and Xiamen were 39.7 +/- 36.1 ppm and 13.6 +/- 12.3 ppm, respectively. These contributed 75.2 +/- 14.6% and 59.1 +/- 26.8% to their respective annual ΔCO2offsets over background CO2concentrations. Significantly (p < 0.05) high CO2ffvalues were observed in winter in Beijing. We did not find any significant differences in CO2ffvalues between weekdays and weekends. Diurnal CO2ffvariations were plainly evident, with high values between midnight and 4:00, and during morning and afternoon rush hours. The sampling site in the inland city of Beijing displayed much higher CO2ffinputs and overall temporal variations than the site in the coastal city of Xiamen. The variations of CO2ffat both sites were controlled by a combination of emission sources, topography, and atmospheric dispersion. In particular, diurnal observations at the urban site in Beijing showed that CO2ffwas easily accumulated under the southeast wind conditions.

Corresponding author

Zhou Weijian

Volume

50

Issue

11

Page

5474-5480

Pub year

June, 2016

Publication name

Environmental Science & Technology

Details

http://pubs.acs.org/doi/abs/10.1021/acs.est.5b02591

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