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Turbulent characteristics of saltation and uncertainty of saltation model parameters

机译:盐化的湍流特征和盐化模型参数的不确定性

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It is widely recognised that saltation is a turbulent process, similar to other transport processes in the atmospheric boundary layer. Due to a lack of high-frequency observations, the statistic behaviour of saltation is so far not well understood. In this study, we use the data from the Japan–Australia Dust Experiment (JADE) to investigate the turbulent characteristics of saltation by analysing the probability density function, energy spectrum and intermittency of saltation fluxes. Threshold friction velocity, usub*t/sub, and saltation coefficient, csub0/sub, are two important parameters in saltation models often assumed to be deterministic. As saltation is turbulent in nature, we argue that it is more reasonable to consider them as parameters obeying certain probability distributions. We estimate these distributions using the JADE data. The factors contributing to the stochasticity of usub*t/sub and csub0/sub are examined.
机译:众所周知,盐化是一个湍流过程,类似于大气边界层中的其他传输过程。由于缺乏高频观测,到目前为止对盐析的统计行为还不甚了解。在这项研究中,我们使用来自日本-澳大利亚粉尘实验(JADE)的数据,通过分析概率密度函数,能谱和盐通量的间歇性来研究盐化的湍流特征。阈值摩擦速度u * t 和盐分系数c 0 是通常被认为是确定性的盐分模型中的两个重要参数。由于盐分在本质上是湍流的,因此我们认为将它们视为服从某些概率分布的参数更为合理。我们使用JADE数据估算这些分布。研究了影响u * t 和c 0 随机性的因素。

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