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Effects from downbursts on overhead lines. Meteorological thunderstorm study-climatological, meteorological and CFD analysis

机译:突降对架空线的影响。气象雷暴研究-气候,气象和CFD分析

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In February and March 2008 cyclone "Emma" crossed some countries of central Europe and caused severe damages. In very local areas thunderstorms with downbursts were embedded in "Emma" and led to collapses of overhead lines. Downbursts are downward winds with high velocity within a thunderstorm concerning a relative small area. They occur seldom but can have severe effects and are responsible for various local damages on buildings, forests and infrastructure as e.g. overhead lines. In many cases in history, such damages were not brought into connection with downbursts. The Cigre reports 350 and 410 deal with localized high intensity winds. They state that".. .more research is needed to study the interaction of localized winds with supports..." The question arose if the terrain triggered wind speed-up effects. Another question was which wind forces and directions occurred during these events. To investigate the influences of high wind speeds on damaged overhead lines, a pilot study was carried out. Three dimensional wind fields where computed and analyzed regarding to speed-up effects. This paper presents the investigations, climatological aspects as well as CFD case studies (Computational Fluid Dynamics) and shows the amplification factors for the wind speed. The method which was developed in the project can be used for any other region to simulate tendencies of wind speed-up, regardless if they come from downbursts or not. It helps to a better understanding of the reason for wind induced failures.
机译:2008年2月和2008年3月,“艾玛”(Emma)飓风越过中欧一些国家,造成了严重破坏。在非常局部的地区,“ Emma”内埋有雷暴和暴风雨,导致架空线倒塌。暴发是雷暴天气中相对较小区域的高速下行风。它们很少发生,但可能造成严重影响,并造成建筑物,森林和基础设施等各种局部损坏,例如架空线。在历史上的许多情况下,此类破坏与爆发无关。 Cigre报告350和410涉及局部高强度风。他们指出:“……需要更多的研究来研究局部风与支撑的相互作用……”如果地形引发风速增加效应,就会出现问题。另一个问题是在这些事件中发生了哪些风力和风向。为了调查高风速对受损架空线的影响,进行了一项初步研究。计算和分析关于加速效果的三维风场。本文介绍了调查,气候方面以及CFD案例研究(计算流体动力学),并显示了风速的放大因子。该项目中开发的方法可用于任何其他区域,以模拟风速上升趋势,而不论其是否来自暴风雨。它有助于更​​好地了解风致故障的原因。

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