Effects of urban land expansion on the regional meteorology and air quality of eastern China

被引:68
|
作者
Tao, W. [1 ]
Liu, J. [1 ]
Ban-Weiss, G. A. [2 ]
Hauglustaine, D. A. [3 ]
Zhang, L. [4 ]
Zhang, Q. [5 ]
Cheng, Y. [6 ]
Yu, Y. [7 ]
Tao, S. [1 ]
机构
[1] Peking Univ, Lab Earth Surface Proc, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Univ So Calif, Sonny Astani Dept Civil & Environm Engn, Los Angeles, CA 90089 USA
[3] CEA CNRS UVSQ, Lab Sci Climat & Environm, UMR8212, Gif Sur Yvette, France
[4] Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Lab Climate & Ocean Atmosphere Sci, Beijing 100871, Peoples R China
[5] Tsinghua Univ, Ctr Earth Syst Sci, Beijing 100084, Peoples R China
[6] Chinese Acad Meteorol Sci, Beijing, Peoples R China
[7] Nanjing Municipal Environm Monitoring Ctr, Nanjing 210013, Jiangsu, Peoples R China
基金
中国国家自然科学基金;
关键词
YANGTZE-RIVER DELTA; OZONE FORMATION; HEAT-ISLAND; DRY DEPOSITION; CANOPY MODEL; WRF MODEL; CLIMATE; SURFACE; PARAMETERIZATION; POLLUTION;
D O I
10.5194/acp-15-8597-2015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Rapid urbanization throughout eastern China is imposing an irreversible effect on local climate and air quality. In this paper, we examine the response of a range of meteorological and air quality indicators to urbanization. Our study uses the Weather Research and Forecasting model coupled with chemistry (WRF/Chem) to simulate the climate and air quality impacts of four hypothetical urbanization scenarios with fixed surface pollutant emissions during the month of July from 2008 to 2012. An improved integrated process rate (IPR) analysis scheme is implemented in WRF/Chem to investigate the mechanisms behind the forcing-response relationship at the process level. For all years, as urban land area expands, concentrations of CO, elemental carbon (EC), and particulate matter with aerodynamic diameter less than 2.5 microns (PM2.5) tend to decrease near the surface (below similar to 500 m), but increase at higher altitudes (1-3 km), resulting in a reduced vertical concentration gradient. On the other hand, the O-3 burden, averaged over all newly urbanized grid cells, consistently increases from the surface to a height of about 4 km. Sensitivity tests show that the responses of pollutant concentrations to the spatial extent of urbanization are nearly linear near the surface, but nonlinear at higher altitudes. Over eastern China, each 10% increase in nearby urban land coverage on average leads to a decrease of approximately 2% in surface concentrations for CO, EC, and PM2.5, while for O-3 an increase of about 1% is simulated. At 800 hPa, pollutants' concentrations tend to increase even more rapidly with an increase in nearby urban land coverage. This indicates that as large tracts of new urban land emerge, the influence of urban expansion on meteorology and air pollution would be significantly amplified. IPR analysis reveals the contribution of individual atmospheric processes to pollutants' concentration changes. It indicates that, for primary pollutants, the enhanced sink (source) caused by turbulent mixing and vertical advection in the lower (upper) atmosphere could be a key factor in changes to simulated vertical profiles. The evolution of secondary pollutants is further influenced by the upward relocation of precursors that impact gas-phase chemistry for O-3 and aerosol processes for PM2.5. Our study indicates that dense urbanization has a moderate dilution effect on surface primary airborne contaminants, but may intensify severe haze and ozone pollution if local emissions are not well controlled.
引用
收藏
页码:8597 / 8614
页数:18
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