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A model for calculating the vertical distribution of the atmospheric electric potential in the exchange layer in a maritime clean atmosphere

机译:海洋清洁大气中交换层中大气电势垂直分布的计算模型

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A theoretical model is developed for calculating the vertical distribution of atmospheric electric potential in exchange layer of maritime clean atmosphere. The transport of space charge in electrode layer acts as a convective generator in this model and plays a major role in determining potential distribution in vertical. Eddy diffusion is the main mechanism responsible for the distribution of space charge in vertical. Our results show that potential at a particular level increases with increase in the strength of eddy diffusion under similar conditions. A method is suggested to estimate columnar resistance, the ionospheric potential and the vertical atmospheric electric potential distribution in exchange layer from measurements of total air-earth current density and surface electric field made over oceans. The results are validated and found to be in very good agreement with the previous aircraft measurements. Different parameters involved in the proposed methodology can be determined either theoretically, as in the present work, or experimentally using the near surface atmospheric electrical measurements or using some other surface-based measurement technique such as LIDAR. A graphical relationship between the atmospheric eddy diffusion coefficient and height of exchange layer obtained from atmospheric electrical approach, is reported.
机译:建立了计算海洋清洁大气交换层大气电位垂直分布的理论模型。在此模型中,空间电荷在电极层中的传输充当对流生成器,并在确定垂直方向的电势分布中起主要作用。涡流扩散是负责垂直空间电荷分布的主要机制。我们的结果表明,在类似条件下,特定水平的电势会随着涡流扩散强度的增加而增加。建议使用一种方法,通过测量海洋上的总地电流密度和表面电场,估算交换层中的柱状电阻,电离层电势和垂直大气电势分布。结果经过验证,与先前的飞机测量结果非常吻合。可以在理论上(如本工作中)确定所提出方法中涉及的不同参数,也可以使用近地表大气电学测量或使用其他基于表面的测量技术(例如LIDAR)进行实验确定。报告了大气涡流扩散系数和通过大气电学方法获得的交换层高度之间的图形关系。

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