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A Simple Dispersion Model of Ground Level Ultrafine Particle Concentrations Downwind of a Major Airport

机译:大型机场顺风方向地面超细颗粒浓度的简单扩散模型

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Introduction: Recent studies have observed a broad footprint of increased ultrafine particle number concentrations up to and possibly beyond 10 km downwind of major airports. Here we compare mobile monitoring measurements downwind of LAX with predictions from a set of relatively simple plume dispersion models. Methods: Mobile monitoring of ultrafine particle number concentrations took place on six days during daytime hours along seven N-S transects ranging from 2 to 9 km downwind of LAX. Background concentrations were first derived using the values obtained by applying a moving boxcar filter to the observations. Cross-wind integrated concentrations (ClCs) of estimated ultrafine particle background concentrations were then computed each sampling day for each transect. ANCOVA was used to compare observations with dispersion model predictions with a random effect of sampling day. The Aermod dispersion model was run separately with hourly average wind data averaged from LAX one minute ASOS data. The source configuration was either a volume-line source to represent the descent path emissions, a surface area source to represent ground level sources at the airport, or a surface trapezoidal area representing cross-wind, ground level transport of the aircraft vortices generated near the ground during descent. The volume-line source geometry was tilted to represent the descent path of the aircraft at a 3 degree inclination. This tilted source was then lowered uniformly by 300 m (descent 300) to represent the effect of transport from descending vortices, resulting in a part of this source being placed at ground level near the airport. Results: Comparison of predicted versus observed ClCs using ANCOVA indicate that either of the ground-level area source models performed better (adjusted R~2 was 0.57 and 0.58 for the trapezoid and the airport area source models, respectively) than the volume line source model (adjusted R~2 = 0.39). In two variable ANCOVA models (line and area source predictions), only the area source term was significant. Conclusions: Two different ground level area source models performed moderately well in predicting background-adjusted, cross-wind integrated concentrations obtained from a mobile monitoring platform at distances up to 9 km downwind of LAX. A descending volume line source model had less skill.
机译:简介:最近的研究发现,在主要机场的下风处,超细颗粒物的浓度增加到甚至可能超过10 km时,都会产生很大的影响。在这里,我们将LAX顺风方向的移动监测测量结果与一组相对简单的羽流弥散模型的预测结果进行了比较。方法:在白天的六天内,沿着LAX顺风2至9 km范围内的7个N-S横断面,对超细颗粒数浓度进行了移动监测。首先使用通过将移动棚车滤镜应用于观测值而获得的值得出背景浓度。然后在每个采样日的每个采样日计算估计的超细颗粒背景浓度的横风积分浓度(ClCs)。 ANCOVA用于比较观察结果与色散模型预测以及采样日的随机影响。 Aermod弥散模型是分别运行的,每小时平均风速数据是根据LAX一分钟ASOS数据求出的平均值。源配置可以是代表下降路径排放量的体积线源,代表机场的地平面源的表面积源,也可以是代表在飞机场附近产生的飞机涡流的侧风,地平面传输的表面梯形区域。下降时接地。将体积线源几何形状倾斜以代表飞机3度倾斜的下降路径。然后将该倾斜的源均匀降低300 m(下降300),以表示来自下降涡流的传输效果,从而导致该源的一部分放置在机场附近的地面上。结果:使用ANCOVA进行的预测ClCl和观察到的ClC的比较表明,两种地面面积源模型的效果都比体积线源模型更好(梯形和机场区域源模型的调整后R〜2分别为0.57和0.58) (调整后的R〜2 = 0.39)。在两个可变的ANCOVA模型(线和面源预测)中,只有面源项才有意义。结论:两种不同的地面面积源模型在预测从LAX顺风9公里处的移动监测平台获得的背景调整后的侧风积分浓度方面表现中等。降序线源模型的技能较低。

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