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大气边界层湍流的动力非平稳性的验证
引用本文:李敏,蒋维楣,李昕,浦一芬.大气边界层湍流的动力非平稳性的验证[J].地球物理学报,2005,48(3):493-500.
作者姓名:李敏  蒋维楣  李昕  浦一芬
作者单位:南京大学大气科学系,南京,210093;中国科学院大气物理研究所大气边界层与大气化学国家重点实验室,北京,100029;北京市环境保护局,北京,100044;中国科学院大气物理研究所大气边界层与大气化学国家重点实验室,北京,100029
基金项目:国家自然科学基金项目 (4 0 3 3 3 0 2 7和 40 2 0 5 0 0 3 )资助
摘    要:首次用验证时间序列中是否存在动力非平稳性的一种简单图示方法——space time index法来分析大气边界层湍流的动力平稳性特征.本文以取自淮河流域和威斯康星森林下垫面条件下的三维高精度风速和温度、湿度湍流脉动资料对大气边界层湍流的平稳性特征进行了分析.结果表明space time index方法能有效地检验大气边界层湍流信号中是否存在动力平稳性.另外,均匀下垫面条件(水稻田)及复杂下垫面条件(森林)下的大气边界层湍流信号中几乎都存在动力非平稳性,大气湍流动力学非平稳性可能是边界层湍流信号相当普遍具有的一种特性.大气边界层湍流中的间歇性和相干结构使得其非平稳性图形的特征不同于一般时间序列非平稳性图形的“V”型特征;森林下垫面条件下的湍流信号比相对均匀下垫面(水稻田)下的湍流信号更有组织性,相干结构更强.

关 键 词:Space  time-index  非平稳性  大气边界层湍流  间歇性  相干结构
文章编号:0001-5733(2005)03-0493-08
收稿时间:2003-10-20
修稿时间:2004-12-28

A test of the dynamical nonstationarity in atmospheric boundary layer turbulence
LI Min,JIANG Wei-mei,LI Xin,PU Yi-fen.A test of the dynamical nonstationarity in atmospheric boundary layer turbulence[J].Chinese Journal of Geophysics,2005,48(3):493-500.
Authors:LI Min  JIANG Wei-mei  LI Xin  PU Yi-fen
Institution:1.Department of Atmospheric Sciences, Nanjing University, Nanjing 210093, China2 LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 3 Beijing Municipal Environmental Protection Bureau, Beijing 100044, China
Abstract:A graphical method, named space time-index plots for testing dynamical nonstationarity in general time series is addressed. In this method, the graph is V-shaped due to nonstationarity. The method is used to test dynamical nonstationarity in atmospheric boundary layer turbulence. The high resolution temperature, humidity and three components of wind speed under various land surface obtained from HUBEX(Study of Energy and Water Cycle Over Huaihe River Basin) and PFRD (Park Falls Ranger District of the Chequamegon National Forest, about 15km east of Park Falls, Wisconsin, U.S.A.) are analyzed. The results show that the space time-index plots method can test whether dynamical nonstationarity exists in atmospheric boundary layer turbulence signal. There is almost few dynamical stationarity in atmospheric boundary layer turbulence signal both under rice from HUBEX and under forest from PFRD. Dynamical nonstationarity is likely one common property of atmospheric boundary layer turbulence signal. The intermittency and coherent structures in atmospheric boundary layer turbulence lead to some differences in the nonstationarity graph shape between atmospheric boundary layer turbulence and general time series. The results show that the turbulence signal over forest from PFRD is dominated by more distinct coherent structures and intermittency than that over rice from HUBEX.
Keywords:Space time-index plots  Nonstationarity  Atmospheric boundary layer turbulence  
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