中大機構典藏-NCU Institutional Repository-提供博碩士論文、考古題、期刊論文、研究計畫等下載:Item 987654321/26335
English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 80990/80990 (100%)
造訪人次 : 41667895      線上人數 : 1554
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋


    請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/26335


    題名: LOW-WAVE-NUMBER SPECTRAL CHARACTERISTICS OF VELOCITY AND TEMPERATURE IN THE ATMOSPHERIC SURFACE-LAYER
    作者: KATUL,GG;CHU,CR;PARLANGE,MB;ALBERTSON,JD;ORTENBURGER,TA
    貢獻者: 土木工程研究所
    關鍵詞: TURBULENT BOUNDARY-LAYERS;WALL TURBULENCE;GRADIENT
    日期: 1995
    上傳時間: 2010-06-29 17:11:03 (UTC+8)
    出版者: 中央大學
    摘要: The structure df atmospheric surface layer turbulence low wavenumbers was analyzed using 56 Hz triaxial velocity and temperature measurements above a uniform dry lake bed, A key feature of this experiment was the, small roughness length of the surface that resulted in a small roughness Reynolds number. Under near-neutral atmospheric stability conditions, a -1 power law was observed in both measured velocity and temperature spectra which is consistent with previously proposed dimensional analysis for rough and smooth turbulent boundary layer flows. The wavenumber at which the -1 power law terminates and the -5/3 power law commences was derived as a function of the Kolmgorov and von Karman constants, Good agreement between the predicted and the measured transition. wavenumber from -1 to -5/3, was holed for fully rough-flow conditions. However, this was ndt the case fdr other roughness conditions. The similarity theory constants for the neutral case were determined and they compared favorably with other laboratory and field studies. For unstable atmospheric conditions, directional dimensional analysis was used to predict the slopes of the power spectra of temperature and velocity. It was demonstrated that for moderately unstable conditions, the temperature and vertical velocity power spectra exhibited a -1 power law, but the longitudinal velocity exhibited a -2 power law. The agreement between predicted and measured power laws was within experimental errors. Some differences between the constants determined from this experiment and other experiments are also discussed.
    關聯: JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
    顯示於類別:[土木工程研究所] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML473檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明