Temporal and spatial variation relationship and influence factors on surface urban heat island and ozone pollution in the Yangtze River Delta, China

被引:132
|
作者
Wang, Yuanyuan [1 ,2 ]
Du, Hongyu [3 ,4 ]
Xu, Yanqing [5 ]
Lu, Debin [1 ,2 ]
Wang, Xiyuan [1 ,2 ]
Guo, Zhongyang [1 ,2 ]
机构
[1] East China Normal Univ, Minist Educ, Key Lab Geog Informat Sci, 500 Dongchuan Rd, Shanghai 200241, Peoples R China
[2] East China Normal Univ, Sch Geog Sci, Shanghai 200241, Peoples R China
[3] East China Normal Univ, Shanghai Key Lab Urban Ecol Proc & Ecorestorat, Shanghai 200241, Peoples R China
[4] East China Normal Univ, Dept Environm Sci, 500 Dongchuan Rd, Shanghai, Peoples R China
[5] Univ Toledo, Dept Geog & Planning, Toledo, OH 43606 USA
基金
中国国家自然科学基金;
关键词
Surface urban heat island; Ozone; NO2; Land surface parameters; AIR-POLLUTANTS; UNITED-STATES; SHANGHAI; O-3; CITY; PRECURSORS; PATTERNS; IMPACTS; CLIMATE; QUALITY;
D O I
10.1016/j.scitotenv.2018.03.050
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Urbanization has led to an obvious urban heat island (UHI) effect in the Yangtze River Delta (YRD), China. The ozone (O-3) pollution in the YRD is getting worse. The UHI effect is a key factor that affects the O-3 level. Understanding the influences of the UHI effect on O-3 concentrations is necessary for improving air quality. In this study, the temporal and spatial relationship between UM and O-3 in the YRD during 2015 was investigated. The influence factors of UHI effect and O-3 are both natural and artificial. Multi-source remote sensing data, which include land cover, land surface temperature (CST), Normalization Difference Vegetation Index (NDVI), and digital elevation model (DEM) data, were used to extract surface landscape elements. The results showed that: (1) the average hourly O-3 concentration was 61.83 mu g/m(3) (30.92 ppb), the highest value was 105.32 mu g/m(3) (52.66 ppb) at 15:00 and the O-3 peak was 82.50 mu g/m(3) (41.25 ppb) in September. The O-3 concentrations and temperature have a similar variation trend both in diurnal and monthly. The O-3 concentrations in coastal stations are higher than those inland. (2) The average daytime UHI intensity was 124 degrees C, and the daytime O-3 concentration was 80.66 mu g/m(3) (40.33 ppb). There is a positive relationship between UHI and O-3 in the YRD. The relationship in the central developed cities is higher than that in the northern and southern cities. (3) The related factors influencing UHI and O-3 include surface landscape, topography and population. The LST and NDVI are most important among these factors. (4) Due to various geographical backgrounds, the UHI intensities and O-3 concentrations show obvious spatial differences. This study provides a reference with which to better understand the relationship among UHI, O-3 and related factors. Furthermore, the issues of atmospheric and energy transmission in this region deserve further study. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:921 / 933
页数:13
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