EGU2020-5391
https://doi.org/10.5194/egusphere-egu2020-5391
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Multiple level of CO2 fluxes over Beijing megacity with eddy covariance method

Yang Liu1 and Huizhi Liu2
Yang Liu and Huizhi Liu
  • 1Institute of Atmospheric physics, Laboratory of atmospheric boundary layer physics and atmospheric chemistry, China (164784502@qq.com)
  • 2Institute of Atmospheric physics, Laboratory of atmospheric boundary layer physics and atmospheric chemistry, China (ly0801@mail.iap.ac.cn)

Based on the CO2 fluxes measured with eddy covariance method from 2008 to 2012 at 47, 140 and 280m in Beijing 325m meteorological tower, we have investigated the exchange process of CO2 flux between atmosphere and the urban surface in Beijing megacity. Because of the total vehicle control from 2011, the increasing rate of annual total CO2 flux at 140m from 2008~2010 is 7.8% while from 2010~2012 is 2.3%. The average annual total CO2 flux during the 5 year measurement is largest at 140m (6.41kg C m-2 yr-1) while at 47 (5.78 kg C m-2 yr-1) and 280m (3.99 kg C m-2 yr-1) are much smaller. The measured fluxes were highly dependent on the prevailing wind direction. The CO2 fluxes at weekends are nearly the same as at weekdays because of the traffic restriction rule during Mon to Fri. Total vehicle numbers and population are main controlling factors of annual total CO2 fluxes in Beijing. The CO2 fluxes at three layers all present positive correlation with road fraction in the footprint area. The R-squares are respectively 0.69, 0.57 and 0.54 at 47, 140 and 280m. The decreasing fraction of vegetation will cause the increasing of annual total CO2 flux and there is a exponential relationship between them. The annual total CO2 flux is larger when the population density is higher.

How to cite: Liu, Y. and Liu, H.: Multiple level of CO2 fluxes over Beijing megacity with eddy covariance method, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5391, https://doi.org/10.5194/egusphere-egu2020-5391, 2020