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Turbulence variance characteristics in the unstable atmospheric boundary layer above flat pine forest.

机译:平松林上空大气边界层湍流变化特征

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摘要

Variances of the velocity components and scalars are important as indicators of the turbulence intensity. They also can be utilized to estimate surface fluxes in several types of "variance methods", and the estimated fluxes can be regional values if the variances from which they are calculated are regionally representative measurements. On these motivations, variances measured by an aircraft in the unstable ABL over a flat pine forest during HAPEX-Mobilhy were analyzed within the context of the similarity scaling arguments.; The variances of temperature and vertical velocity within the atmospheric surface layer were found to follow closely the Monin-Obukhov similarity theory, and to yield reasonable estimates of the surface sensible heat fluxes when they are used in variance methods. This gives a validation to the variance methods with aircraft measurements. On the other hand, the specific humidity variances were influenced by the surface heterogeneity and clearly fail to obey MOS. A simple analysis based on the similarity law for free convection produced a comprehensible and quantitative picture regarding the effect of the surface flux heterogeneity on the statistical moments, and revealed that variances of the active and passive scalars become dissimilar because of their different roles in turbulence. The analysis also indicated that the mean quantities are also affected by the heterogeneity but to a less extent than the variances.; The temperature variances in the mixed layer (ML) were examined by using a generalized top-down bottom-up diffusion model with some combinations of velocity scales and inversion flux models. The results showed that the surface shear stress exerts considerable influence on the lower ML. Also with the temperature and vertical velocity variances ML variance methods were tested, and their feasibility was investigated.; Finally, the variances in the ML were analyzed in terms of the local similarity concept; the results confirmed the original hypothesis by Panofsky and McCormick that the local scaling in terms of the local buoyancy flux defines the lower bound of the moments.
机译:速度分量和标量的方差作为湍流强度的指标很重要。在几种类型的“方差方法”中,也可以利用它们来估计表面通量,如果从中计算出的通量是区域代表性的测量值,则估计的通量可以是区域值。基于这些动机,在相似缩放参数的背景下,分析了飞机在HAPEX-Mobilhy期间在平坦的松树林中的不稳定ABL中测得的方差。发现大气表层内温度和垂直速度的变化密切遵循Monin-Obukhov相似性理论,并且在将它们用于变化方法时可以对表面感热通量做出合理的估计。这可以验证飞机测量的方差方法。另一方面,比湿度变化受表面异质性的影响,显然不能服从MOS。对自由对流基于相似律的简单分析产生了关于表面通量非均质性对统计矩的影响的可理解的定量图像,并揭示了由于它们在湍流中的不同作用,主动和被动标量的方差变得不同。分析还表明,平均量也受异质性的影响,但程度小于方差。通过使用广义的自上而下的自底向上的扩散模型以及速度标度和反演通量模型的某些组合来检查混合层(ML)中的温度变化。结果表明,表面剪切应力对较低的ML有很大影响。还对温度和垂直速度方差进行了ML方差检验,并研究了其可行性。最后,根据局部相似性概念分析了机器学习的方差。结果证实了Panofsky和McCormick的原始假设,即根据局部浮力通量确定的局部比例确定了矩的下界。

著录项

  • 作者

    Asanuma, Jun.;

  • 作者单位

    Cornell University.;

  • 授予单位 Cornell University.;
  • 学科 Physics Atmospheric Science.
  • 学位 Ph.D.
  • 年度 1996
  • 页码 215 p.
  • 总页数 215
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
  • 关键词

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