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通量-方差法估算沿海近地面层的湍流通量分析

徐安伦 吴晓庆 许利明 李多扬

徐安伦, 吴晓庆, 许利明, 李多扬. 通量-方差法估算沿海近地面层的湍流通量分析[J]. 热带气象学报, 2008, (6): 708-712.
引用本文: 徐安伦, 吴晓庆, 许利明, 李多扬. 通量-方差法估算沿海近地面层的湍流通量分析[J]. 热带气象学报, 2008, (6): 708-712.
XU An-lun, WU Xiao-qing, XU Li-ming, LI Duo-yang. ANALYSIS OF FLUX-VARIANCE METHOD IN ESTIMATION OF TURBULENT FLUX IN THE SURFACE LAYER OVER COASTAL AREA[J]. Journal of Tropical Meteorology, 2008, (6): 708-712.
Citation: XU An-lun, WU Xiao-qing, XU Li-ming, LI Duo-yang. ANALYSIS OF FLUX-VARIANCE METHOD IN ESTIMATION OF TURBULENT FLUX IN THE SURFACE LAYER OVER COASTAL AREA[J]. Journal of Tropical Meteorology, 2008, (6): 708-712.

通量-方差法估算沿海近地面层的湍流通量分析

基金项目: 中国科学院知识创新工程资助课题;国家自然科学基金资助项目(40475010)共同资助

ANALYSIS OF FLUX-VARIANCE METHOD IN ESTIMATION OF TURBULENT FLUX IN THE SURFACE LAYER OVER COASTAL AREA

  • 摘要: 利用通量-方差法,通过确定速度和温度归一化标准差与稳定度之间的变化关系,估算出东南沿海地区的湍流动量通量和感热通量。我们发现在中性条件下σT/T并不像Tillman等认为是常数,而是随稳定度参数按指数形式变化。与涡动协方差相关测量系统测量结果进行比较发现,通量-方差方法估算结果与测量值两者符合得较好,相关性高,动量通量的相关系数为0.87,而感热通量的为0.95。利用该方法估算沿海近地面层的湍流通量具有一定的代表性。

     

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出版历程
  • 收稿日期:  2007-06-21
  • 修回日期:  2008-01-21

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