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The Study for Spatial Structures and Time Development of Turbulence in the Atmospheric Boundary Layer

The Study for Spatial Structures and Time Development of Turbulence in the Atmospheric Boundary Layer
大气边界层湍流的空间结构和时间发展研究
批准号:
13640437
负责人:
HORIGUCHI Mitsuaki
金额:
$2.3万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2001
资助国家:
日本
项目状态:
已结题
起止时间:
2001 至 2002

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中文摘要
翻译
本文通过观测和数值试验研究了中性稳定度条件下湍流的空间结构和时间发展。首先,分析了柴崎市风场效应实验室和茂崎县观测站的观测资料。为了得到大风区域的平均模式,对测得的20m高空平均风向的风向分量进行了160秒连续小波变换。利用俄克拉荷马大学风暴分析预报中心开发的ARPS(高级区域预报系统)对大涡进行了数值模拟。在初始条件下,水平均匀场的风廓线在30m以下为对数线性风律,上方为Ekman螺线,位温廓线为近中性,最上层为逆温层,在该场上产生了随机位温扰动。积分时间为35040秒后,沿平均风向拉长的条纹状结构在近地表突出。7.5m高度的平均风向分量的小波方差在720m的空间尺度上最大。小波方差峰值附近的平均模式显示了从约150米的高度向下移动的高速区。平均风向为600米、垂直方向为240米的区域动量通量大于300米高度以下的其他区域。
英文摘要
In this study, the spatial structures and time development of turbulence was investigated using observations and numerical experiments for the neutral stability condition.At first, observed data at Shionomisaki Wind Effect Laboratory and Shigaraki MU Observatory was analyzed. To make an averaged pattern for the area of strong wind, continuous wavelet transform in the time scale of 160 seconds was applied to the wind component in mean wind direction measured at a height of 20 meters. The structures of the downward moving high-speed area and upward moving low-speed area ahead of it are shown.To execute numerical experiments, the ARPS (Advanced Regional Prediction System) developed by the CAPS (Center for Analysis and Prediction of Storms) at the University of Oklahoma was used for the large eddy simulation. For the initial condition, random potential temperature perturbation was induced on the horizontally homogeneous filed which has a wind profile with the log-linear wind law below the 30 meters and the Ekman spiral above it and an almost neutral potential temperature profile with uppermost inversion layer. After the integration time of 35040 sec., streaky structures elongated in mean wind direction are outstanding near the surface. Wavelet variance for the wind component in mean wind direction at a height of 7.5 meters is maximum at the spatial scale of 720 meters. Averaged pattern around the peak position for the wavelet variance shows the downward moving high-speed area from the height of about 150 meters. The area in length of 600 meters in mean wind direction and 240 meters in normal direction shows larger momentum flux than other areas below the height af 300 meters.
期刊论文(2)
专著(0)
科研奖励(0)
会议论文
堀口光章: "中立成層状態の大気境界層における組織的乱流構造"京都大学防災研究所年報. 第45号B. 347-355 (2002)
Mitsuaki Horiguchi:“中性分层下大气边界层的有组织湍流结构”京都大学防灾研究所年报第45 B. 347-355号(2002年)。
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通讯作者:
堀口光章: "中立成層状態の大気境界層における組織的乱流構造(第2報)"京都大学防災研究所年報. 第46号B(印刷中). (2003)
Mitsuaki Horiguchi:“中性分层下大气边界层的组织湍流结构(第二次报告)”京都大学防灾研究所年报第46 B号(出版中)。
DOI: --
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通讯作者:
Study for the occurrence and forecasting of strong wind disasters at the surface induced by the downward movement of the high-speed layer in the higher levels
  • 批准号:
    24651208
  • 项目类别:
    Grant-in-Aid for Challenging Exploratory Research
  • 资助金额:
    $2.58万
  • 财政年份:
    2012
  • 负责人:
    HORIGUCHI Mitsuaki
  • 依托单位:
国内基金
海外基金
流体湍流运动的相关数学分析
  • 批准号:
    10971174
  • 项目类别:
    面上项目
  • 资助金额:
    25.0万元
  • 批准年份:
    2009
  • 负责人:
    肖跃龙
  • 依托单位: