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一次平流雾过程中湍流及能量输送特征研究

Study on Turbulent Structures and Energy Transfer during an AdvectiveFog Period

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【作者】 吴彬贵张宏升王兆宇朱好解以扬

【Author】 WU Bingui1),2) ZHANG Hongsheng1),3) WANG Zhaoyu2),ZHU Hao1),XIE Yiyang2)(1) Department of Atmospheric Science,School of Physics,Peking University,China Beijing 100871 ;2) Tianjin Meteorological Bureau,Tianjin 300074

【机构】 北京大学物理学院大气科学系天津市气象局

【摘要】 本文利用天津255米气象塔开展的大气边界层实验资料,分析了2006年2月一次平流雾过程湍流微结构及能量输送的演变特征,并结合冷锋过境、晴朗小风及轻雾等天气条件,讨论了雾过程中湍流动能特征。得到:雾中风速各风向能谱密度峰值频率偏于高频段,雾前和雾后风速能谱峰值频率偏向于低频段。与速度能谱相比较,雾形成前期,温度谱峰值频率的变化大于速度谱;雾消散期间,温度谱峰值频率比速度谱峰值频率更偏向于低频。雾过程中,平均动能较小,但湍流扰动活跃,湍流动量输送以垂直方向为主。平均动能和湍流动能在雾前出现异常跃升,这可能是平流雾的启动信号。

【Abstract】 Based on the observational tower data obtained during an atmospheric boundary layer experiment at Tianjin,the micro-structures of turbulence and characteristics of energy transfer during an advective fog process in February 2006 have been analyzed.Combined with cold front passage,clear and weak wind condition,and light fog,the characteristics of turbulent kinetic energy during the fog process are discussed.The results show that the peak frequencies of energy spectral density for all directions during the fog process are at the higher frequency part,while those preceding and after the fog are at the lower frequency part.Compared with the velocity spectra,the peak frequency change of temperature spectra is larger than that of velocity spectra before the fog formation.As the fog dissipates,the peak frequency of temperature spectra is lower than that of velocity spectra.During the fog,the mean kinetic energy shows a smaller value,while the turbulent disturbance is active,and the vertical turbulent momentum transfer is dominant.The abrupt rising of mean and turbulent kinetic energy before fog may be regarded as the starting signal of advective fog.

【基金】 国家自然科学基金资助项目40775013;天津市自然科学基金08JCYBJC10300;“十一五”国家科技支撑计划重点项目(2008BAC37B01,2008BAC37B05);财政部/科技部公益性行业(气象)科研专项GYHY200806007
  • 【会议录名称】 第27届中国气象学会年会大气物理学与大气环境分会场论文集
  • 【会议名称】第27届中国气象学会年会大气物理学与大气环境分会场
  • 【会议时间】2010-10-21
  • 【会议地点】中国北京
  • 【分类号】P426.4
  • 【主办单位】中国气象学会
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