Spatial and temporal variations of CO<sub>2</sub> mole fractions observed at Beijing, Xianghe, and Xinglong in North China

<p>Atmospheric <span class="inline-formula">CO<sub>2</sub></span> mole fractions are observed at Beijing (BJ), Xianghe (XH), and Xinglong (XL) in North China using Picarro G2301 cavity ring-down spectroscopy instruments. The measurement system is described com...

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Bibliographic Details
Main Authors: Y. Yang, M. Zhou, T. Wang, B. Yao, P. Han, D. Ji, W. Zhou, Y. Sun, G. Wang, P. Wang
Format: Article
Language:English
Published: Copernicus Publications 2021-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/21/11741/2021/acp-21-11741-2021.pdf
Description
Summary:<p>Atmospheric <span class="inline-formula">CO<sub>2</sub></span> mole fractions are observed at Beijing (BJ), Xianghe (XH), and Xinglong (XL) in North China using Picarro G2301 cavity ring-down spectroscopy instruments. The measurement system is described comprehensively for the first time. The geographical distances among these three sites are within 200 <span class="inline-formula">km</span>, but they have very different surrounding environments: BJ is inside the megacity; XH is in the suburban area; XL is in the countryside on a mountain. The mean and standard deviation of <span class="inline-formula">CO<sub>2</sub></span> mole fractions at BJ, XH, and XL between October 2018 and September 2019 are <span class="inline-formula">448.4±12.8</span>, <span class="inline-formula">436.0±9.2</span>, and <span class="inline-formula">420.6±8.2</span> <span class="inline-formula">ppm</span>, respectively. The seasonal variations of <span class="inline-formula">CO<sub>2</sub></span> at these three sites are similar, with a maximum in winter and a minimum in summer, which is dominated by the terrestrial ecosystem. However, the seasonal variations of <span class="inline-formula">CO<sub>2</sub></span> at BJ and XH are more affected by human activities as compared to XL. Using <span class="inline-formula">CO<sub>2</sub></span> at XL as the background, <span class="inline-formula">CO<sub>2</sub></span> enhancements are observed simultaneously at BJ and XH. The diurnal variations of <span class="inline-formula">CO<sub>2</sub></span> are driven by the boundary layer height, photosynthesis, and human activities at BJ, XH, and XL. We also compare the <span class="inline-formula">CO<sub>2</sub></span> measurements at BJ, XH, and XL with five urban sites in the USA, and it is found that the <span class="inline-formula">CO<sub>2</sub></span> mean concentration at BJ is the largest. Moreover, we address the impact of the wind on the <span class="inline-formula">CO<sub>2</sub></span> mole fractions at BJ and XL. This study provides an insight into the spatial and temporal variations of <span class="inline-formula">CO<sub>2</sub></span> mole fractions in North China.</p>
ISSN:1680-7316
1680-7324