南京冬季雾多发期边界层结构观测分析
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

1.南京信息工程大学 中国气象局大气物理与大气环境重点开放实验室,江苏 南京 210044;2.中国气象局 兰州干旱气象研究所,甘肃 兰州 730020;3.甘肃省干旱气候变化与减灾重点实验室,甘肃 兰州 730020;4.中国气象局 干旱气候变化与减灾重点开放实验室 甘肃 兰州 730020;5.陕西省人工影响天气中心,陕西 西安,710014


Observational research on boundary layer structure during high incidence period of winter fog in Nanjing
Author:
Affiliation:

Fund Project:

1.Key Laboratory of Atmospheric Physics & Environment,China Meteorological Administration,NUIST,Nanjing 210044,China;2.Key Laboratory of Arid Climatic Changing and Reducing Disaster of Gansu Province,China Meteorological Administration,Lanzhou 730020,China;3.Opening Key Laboratory of Arid Climatic Changing and Reducing Disaster, Lanzhou 730020, China;4.Lanzhou Institute of Arid Meteorology,China Meteorological Administration,Lanzhou 730020,China;5.Center of Weather Modification of Shaanxi Province,Xi’an 710014,China

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
  • |
  • 资源附件
    摘要:

    2006年冬季在南京北郊盘城利用系留气球探测系统、自动气象站等仪器对雾日和非雾日的边界层进行了监测,对比分析了两者的边界层结构。结果表明,非雾日主要为单层贴地逆温,并时常出现短时的双层结构,雾发展成熟时逆温则脱离地面。与非雾日相比,雾日平均雾顶之上温度日较差增大,雾顶之下则减小。平均风速的时间—高度分布在雾日和非雾日类似,在稳定性边界层中风速随高度出现一个或者两个极大值区。温度和比湿在非雾日没有显著的对应性,而在雾体内具有较好的对应关系,在雾顶升降过程中反相关。较强的逆温、较低的温度和较小的近地层风速是南京冬季成雾的背景条件。

    Abstract:

    An observation was carried out in the winter in 2006 at Pancheng,northern suburb of Nanjing,using tethered balloon system,automatic weather station and other instruments.The boundary layer structures on fog and fogfree days are analyzed and compared.Results show that on the fogfree days the temperature inversions are mainly singlelayer ones,sometimes with short duration doublelayer structures,while the fog mature stage inversions are free from the ground.Compared with the fogfree days,the temperature diurnal range above the average fog top on fog days is larger while the below one is smaller.The timeheight cross section of average wind speed on the fog days is similar to that on the fogfree days.In the stable boundary layer,the wind speed profiles have one or two maximum values.The average wind speed profiles on fog days are similar to those on the fogfree days.No remarkable relationship exists between the temperature and specific humidity profiles on the fogfree days.Differently,these two parameters have a good correspondence between each other in the fog body whereas they vary oppositely during the ascent and descent of the fog top.The stronger temperature inversion,lower temperature and smaller nearsurfacelayer wind speed are background for the winter fog formation in Nanjing.

    参考文献
    相似文献
    引证文献
引用本文

陆春松,牛生杰,岳平,岳治国,项磊,2011.南京冬季雾多发期边界层结构观测分析[J].大气科学学报,34(1):58-65. LU Chunsong, NIU Shengjie, YUE Ping, YUE Zhiguo, XIANG Lei,2011. Observational research on boundary layer structure during high incidence period of winter fog in Nanjing[J]. Trans Atmos Sci,34(1):58-65.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2010-06-12
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期:

地址:江苏南京宁六路219号南京信息工程大学    邮编:210044

联系电话:025-58731158    E-mail:xbbjb@nuist.edu.cn    QQ交流群号:344646895

大气科学学报 ® 2024 版权所有  技术支持:北京勤云科技发展有限公司