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Simulation of CO2 variations at Chinese background atmospheric monitoring stations between 2000 and 2009: Applying a CarbonTracker model
Authors:YanLi Cheng  XingQin Aa  FangHua Yun  LingXi Zhou  LiXin Liu  ShuangXi Fang  Lin Xu
Institution:1. Key Laboratory for Atmospheric Chemistry of China Meteorological Administration, Research Institute of Atmospheric Composition of Chinese Academy of Meteorological Sciences, Beijing, 100081, China
2. School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing, 210044, China
Abstract:We carried out a downscaling treatment over China using the CarbonTracker numerical model, which was applied using double grid nesting technology (3° × 2° over the whole globe, 1° × 1° over China), simulating and analyzing atmospheric CO2 concentrations over 10 recent years (2000–2009). The simulation results agreed very well with observed data from four background atmospheric monitoring stations in China (The periods for which the simulation results and observed values be compared were January 2000 to December 2009 for the WLG station and June 2006 to December 2009 for the SDZ, LFS, and LAN stations), giving correlation coefficients of >0.7. The high-resolution simulation data correlated slightly better than the low resolution simulation data with the observed data for three of the regions’ atmospheric background stations. Further analysis of the annual, seasonal CO2 concentration variations at the background stations showed that the CO2 concentration increased each year over the study period, with an average annual increase of more than 5%, and annual increases of more than 7% at the Shangdianzi and Lin’an stations. Seasonal CO2 variations were greater at the Longfengshan station than at the Shangdianzi or Lin’an stations. However, the CO2 concentrations were higher at the Shangdianzi and Lin’an stations because they are greatly affected by human activities in the Jingjinji and Changjiang Delta economic zones. Spatial distribution in CO2 concentrations and fluxes were higher in eastern than in western China.
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