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Modelling concentrations of volcanic ash encountered by aircraft in past eruptions

机译:模拟飞机在过去喷发中遇到的火山灰浓度

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Prolonged disruption to aviation during the April—May 2010 eruption of Eyjafjallajokull, Iceland resulted in pressure to predict volcanic ash plume concentrations for the purpose of allowing aircraft to fly in regions with low ash contamination. Over the past few decades there have been a number of incidents where aircraft have encountered volcanic ash resulting in damage to the aircraft and loss of power to engines. Understanding the volcanic ash concentrations that these aircraft have encountered provides important input to determining a safe concentration limit. Aircraft encounters with six volcanic eruption plumes have been studied and ash concentrations predicted using the atmospheric dispersion model NAME. The eruptions considered are Galunggung 1982, Soputan 1985, Redoubt 1989, Pinatubo 1991, Hekla 2000 and Manam 2006. Uncertainties in the eruption source details (start time, stop time and eruption height) and in the aircraft encounter location and flight path are found to be major limitations in some cases. Errors in the driving meteorological data (which is often coarse in resolution for historic studies) and the lack of eruption plume dynamics (e.g. umbrella cloud representation) results in further uncertainties in the predicted ash concentrations. In most of the case studies, the dispersion modelling shows the presence of ash at the aircraft encounter location. Maximum ash concentrations in the vicinity of the aircraft are predicted to be at least 4000 μg m~(-3) although confidence in the estimated concentrations is low and uncertainties of orders of magnitude are shown to be possible.
机译:在2010年4月至2010年5月冰岛埃亚菲亚德拉霍库尔火山喷发中,航空业受到长期干扰,这导致预测火山灰羽流浓度的压力很大,目的是使飞机在低灰分污染地区飞行。在过去的几十年中,飞机发生火山灰事故,造成飞机损坏和发动机动力损失。了解这些飞机遇到的火山灰浓度为确定安全浓度限值提供了重要信息。已经研究了飞机遇到六个火山喷发羽流的情况,并使用大气弥散模型NAME预测了灰分浓度。所考虑的喷发是加隆贡1982年,索普坦1985年,重生1989年,皮纳图博1991年,海克拉2000年和马纳姆2006年。发现喷发源细节(开始时间,停止时间和喷发高度)以及飞机相遇地点和飞行路线的不确定性在某些情况下是主要限制。驾驶气象数据的错误(对于历史研究而言,分辨率通常较差)以及喷发羽流动力学的缺乏(例如伞云表示)会导致预计的灰分浓度进一步不确定。在大多数案例研究中,色散模型显示了飞机相遇位置处存在灰烬。尽管估计浓度的可信度很低,并且显示出可能存在数量级的不确定性,但预计飞机附近的最大烟灰浓度至少为4000μgm〜(-3)。

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