研究报告

  • 孙冉,王鸿宇,马骁骏,陈勇航,赵兵科,秦艳,张华,叶文.上海一次典型雾霾过程中不同天气现象的气溶胶光学特性及转化机制[J].环境科学学报,2017,37(3):814-823

  • 上海一次典型雾霾过程中不同天气现象的气溶胶光学特性及转化机制
  • Aerosol optical properties and formation mechanism of a typical air pollution episode in Shanghai during different weather condition periods
  • 基金项目:国家自然科学基金(No.41575002,40975012);上海市气象与健康重点实验室开放基金;上海市大气颗粒物污染防治重点实验室开放课题
  • 作者
  • 单位
  • 孙冉
  • 东华大学环境科学与工程学院, 上海 201620
  • 王鸿宇
  • 东华大学环境科学与工程学院, 上海 201620
  • 马骁骏
  • 东华大学环境科学与工程学院, 上海 201620
  • 陈勇航
  • 东华大学环境科学与工程学院, 上海 201620
  • 赵兵科
  • 中国气象局上海台风研究所, 上海 200030
  • 秦艳
  • 东华大学环境科学与工程学院, 上海 201620
  • 张华
  • 中国气象局国家气象中心, 北京 100081
  • 叶文
  • 东华大学环境科学与工程学院, 上海 201620
  • 摘要:以上海市2013年冬季一次持续雾霾过程为例,根据能见度和相对湿度的地面观测资料将雾霾过程划分为干霾、湿霾、雾3种不同天气现象,对不同天气现象的气溶胶光学特性垂直分布特征进行了研究,并初步分析不同天气现象的转化机制.结果表明,3种不同天气现象的发生顺序为湿霾→干霾→湿霾及湿霾→雾→干霾→湿霾,相对湿度对能见度的影响最大,温度次之,再次是风速,而PM2.5对能见度的影响最小.CALIPSO(Cloud Aerosol Lidar and Infrared Pathfinder Satellite Observation)探测期间,存在2~3 km明显气溶胶层,且不同天气现象的气溶胶层厚度不同(雾 > 湿霾 > 干霾);雾霾发生期间,1.0 km以下高度气溶胶消光能力最大;在干霾、湿霾到雾的转化过程中,球形、大粒径气溶胶增多,非球形、小粒径气溶胶减少.
  • Abstract:This study examined the vertical distribution of aerosol optical properties in different weather conditions of a pollution episode in Shanghai in the winter of 2013 and preliminarily analyzed the cause of pollution episode. Three types of weather conditions (dry haze, wet haze and fog) were classified based on ground-level observation of visibility and relative humidity. Results showed that the dominant sequences of the three weather conditions were wet haze→dry haze→wet haze and wet haze→fog→dry haze→wet haze. Relative humidity has the most significant relationship with visibility deterioration, followed by temperature, wind speed, and PM2.5 mass concentration. During the period of CALIPSO detection, an obvious aerosol layer around 2~3 km above ground existed, and the thickness is different in different weather conditions (fog > wet haze > dry haze). During pollution episode, the largest aerosol extinction was found below 1.0 km. In the transition process from dry haze, wet haze to fog, spherical and large grain size aerosols increased while non-spherical and small size aerosols reduced.

  • 摘要点击次数: 1765 全文下载次数: 2599