4.2 Article

Spatial and temporal variation of haze in China from 1961 to 2012

期刊

JOURNAL OF ENVIRONMENTAL SCIENCES
卷 46, 期 -, 页码 134-146

出版社

SCIENCE PRESS
DOI: 10.1016/j.jes.2015.12.033

关键词

China; Haze; Spatial distribution; Interannual trend; Meteorological factors; Anthropogenic activities

资金

  1. CMA's special Funds for climate change [CCSF201439]
  2. CMA's special Funds for key technology [CMAGJ2015M79]
  3. MEP's Special Funds for Research on Public Welfares [201409002]

向作者/读者索取更多资源

The purpose of this study is to analyze the climatic characteristics and long-term spatial and temporal variations of haze occurrence in China. The impact factors of haze trends are also discussed. Meteorological data from 1961 to 2012 and daily PM10 concentrations from 2003 to 2012 were employed in this study. The results indicate that the annual-average hazy days at all stations have been increasing rapidly from 4 days in 1961 to 18 days in 2012. The maximum number of haze days occur in winter (41.1%) while the minimum occur in summer (10.4%). During 1961-2012, the high occurrence areas of haze shifted from central to south and east regions of China. The Beijing-Tianjin-Hebei (ling-Jin-Ji) region, Shanxi, Shaanxi, and Henan Province are the high occurrence areas for haze, while the Yangtze River Delta (YRD) and the Pearl River Delta (PRD) have become regions with high haze occurrences in the last 25 years. Temperature and pressure are positively correlated with the number of haze days. However, wind, relative humidity, precipitation, and sunshine duration are negatively correlated with the number of haze days. The key meteorological factors affecting the formation and dissipation of haze vary for high and low altitudes, and are closely related to anthropogenic activities. In recent years, anthropogenic activities have played a more important role in haze occurrences compared with meteorological factors. (C) 2016 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.

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