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Individual Particle Based Description of Atmospheric Dispersion: a Dynamical Systems Approach

机译:基于个体粒子的大气扩散描述:动态系统方法

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摘要

We argue that a proper treatment of material dispersion should be based on individual particle tracking using realistic size and density. The effect of turbulent diffusion and the scavenging of particles by precipitation are shown to be treatable as stochastic perturbations of the deterministic Newtonian equation of motion. This approach enables one to investigate the chaotic aspects of particle dispersion by means of dynamical systems concepts. Topologi-cal entropy is shown to be in this context the growth rate of material lines, which can be considered to provide a novel characterization of the state of the atmosphere. The deposition process is found to be well characterizable by the escape rate (being a measure of the strength of the exponential decay of the number of particles not yet reached the surface), which might depend on local turbulence and rain intensity. The variability of the dispersion process due to the difference between different meteorological forecasts within an ensemble forecast are also illustrated. Examples are taken from volcanic eruptions and the Fukushima accident.
机译:我们认为对材料分散的正确处理应基于使用实际大小和密度的单个粒子跟踪。湍流扩散和沉淀物清除颗粒的影响被证明可以作为确定性牛顿运动方程的随机扰动来对待。这种方法使人们能够借助动力学系统概念研究粒子分散的混沌方面。在这种情况下,拓扑学熵被证明是物质线的增长率,可以认为它提供了大气状态的新颖表征。发现沉积过程可以通过逃逸速率(作为尚未到达表面的颗粒数量的指数衰减强度的度量)很好地表征,该逃逸速率可能取决于局部湍流和降雨强度。还说明了由于整体预报内不同气象预报之间的差异导致的分散过程的可变性。以火山喷发和福岛事故为例。

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  • 来源
    《The Fluid Dynamics of Climate》|2013年|95-119|共25页
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  • 作者

    Timea Haszpra; Tamas Tel;

  • 作者单位

    MTA-ELTE Theoretical Physics Research Group, Pazmany P. s. 1/A, H-1117 Budapest, Hungary;

    MTA-ELTE Theoretical Physics Research Group, Pazmany P. s. 1/A, H-1117 Budapest, Hungary,Department of Theoretical Physics, Eoetvoes Lorand University, Pazmany P. s. 1/A, H-1117 Budapest, Hungary;

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