浮尘,沙源,后向轨迹," /> 浮尘,沙源,后向轨迹,"/>  Floating dust,Sand source,Backward trajectory,"/> 2011年长春市一次持续浮尘天气成因分析
主办单位：中国气象局沈阳大气环境研究所
国际刊号：ISSN 1673-503X
国内刊号：CN 21-1531/P
气象与环境学报

气象与环境学报 ›› 2013, Vol. 29 ›› Issue (6): 24-30.doi:

• 论　文 • 上一篇    下一篇

2011年长春市一次持续浮尘天气成因分析

马梁臣1刘海峰1 王宁2 李杭玥3   

  1. 1.长春市气象局，吉林 长春 130051；2.吉林省气象服务中心， 吉林 长春 130062；3.南京信息工程大学，江苏 南京 210044
  • 出版日期:2013-12-31 发布日期:2013-12-31

1. Changchun Meteorological Service, Changchun 130051, China; 2.Nanjing University of Information Science &Technology, Nanjing 210044, China

MA Liang-chen1 LIU Hai-feng1 WANG Ning2 LI Hang-yue3   

  1. 1. Changchun Meteorological Service, Changchun 130051, China; 2.Nanjing University of Information Science &Technology, Nanjing 210044, China
  • Online:2013-12-31 Published:2013-12-31

PDF (PC)

400

被引次数

4

摘要： 利用气象探测资料和环境监测数据,采用统计分析、环流演变分析、物理量诊断以及后向轨迹法分析了长春市浮尘发生气候特征和2011年5月12日长春市出现的一次持续时间较长、污染程度较重的浮尘天气过程。结果表明：长春地区浮尘天气整体上呈波动性减少趋势，3—5月是主要发生时期；本次浮尘天气过程沙源来自蒙古国中部和内蒙古中东部，并随高空急流的输送影响东北地区，本地沙源没有补充；高空急流明显、地面风速较小、温度露点差较大、内蒙古东部辽宁省北部存在弱风区、整层大气稳定是该区域未出现沙尘暴而出现浮尘的主要原因。

关键词: font-family: 宋体, mso-bidi-font-family: 'Times New Roman', mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, 浮尘')">mso-bidi-language: AR-SA">浮尘, 沙源, 后向轨迹

Abstract: Based on the meteorological and environmental data, a continuous floating dust pollution event on May 12, 2011 in Changchun was analyzed by methods of a climate statistics, a circulation evolution, a physical diagnosis and a back trajectory analysis. The results show that the annual dust day is in a fluctuant decreasing trend in Changchun. The dust weather mainly occurs during March to May. The sand source is originated from the central Mongolia and mid-eastern of Inner Mongolia, and the dust is transported to northeast China with upper jet stream. There is no local sand source in this process. It is a continuous floating dust process rather than a sandstorm because of obviously upper jet stream, smaller surface wind speed, larger temperature dew point difference, weak wind areas in the eastern Inner Mongolia and northern Liaoning province and stable atmosphere in the whole layer.

Key words: font-family: "Times New Roman", mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, mso-bidi-language: AR-SA,  Floating dust')">mso-fareast-font-family: 宋体"> Floating dust, font-family: "Times New Roman", mso-ansi-language: EN, mso-fareast-language: ZH-CN, mso-bidi-language: AR-SA, Sand source')">mso-fareast-font-family: 宋体">Sand source, font-family: "Times New Roman", mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, mso-bidi-language: AR-SA, Backward trajectory')">mso-fareast-font-family: 宋体">Backward trajectory