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Pollutant Dispersion in a Developing Valley Cold-Air Pool

机译:正在发展的山谷冷空气池中的污染物扩散

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摘要

Pollutants are trapped and accumulate within cold-air pools, thereby affecting air quality. A numerical model is used to quantify the role of cold-air-pooling processes in the dispersion of air pollution in a developing region of enhanced cooling within an Alpine valley under decoupled stable conditions. Results indicate that the negatively buoyant downslope flows transport and mix pollutants into the valley to depths that depend on the temperature deficit of the flow and the ambient temperature structure inside the valley. Along the slopes, pollutants are generally entrained above the region of enhanced cooling and detrained within the region of enhanced cooling largely above the ground-based inversion layer. The ability of the region of enhanced cooling to dilute pollutants is quantified. The analysis shows that the downslope flows fill the valley with air from above, which is then largely trapped within the region of enhanced cooling and that dilution depends on where the pollutants are emitted with respect to the positions of the top of the ground-based inversion layer and region of enhanced cooling, and on the slope wind speeds. Over the lower part of the slopes, the concentrations averaged across the region of enhanced cooling are proportional to the slope wind speeds where the pollutants are emitted, and diminish as the region of enhanced cooling deepens. Pollutants emitted within the ground-based inversion layer are largely trapped there. Pollutants emitted farther up the slopes detrain within the region of enhanced cooling above the ground-based inversion layer, although some fraction, increasing with distance from the top of the slopes, penetrates into the ground-based inversion layer.
机译:污染物被捕获并积聚在冷空气池中,从而影响空气质量。一个数值模型被用来量化在解耦的稳定条件下,冷空气循环过程在空气污染扩散中在高山山谷内增强冷却的发展区域中的作用。结果表明,负浮力的下坡流将污染物输送并混合到山谷中,深度取决于气流的温度不足和山谷内部的环境温度结构。沿着斜坡,污染物通常被夹带在增强冷却的区域上方,而在较大冷却的区域内则被带走,这些区域主要在地基反演层上方。量化增强冷却区域稀释污染物的能力。分析表明,下坡流从上方充满了山谷的空气,然后大部分被困在增强冷却的区域内,稀释程度取决于污染物的排放位置(相对于地面反演顶部的位置)层和区域增强的冷却作用,以及坡度上的风速。在斜坡的下部,整个强化冷却区域的平均浓度与污染物排放的斜坡风速成正比,并随着强化冷却区域的加深而减小。地面反演层内排放的污染物大部分被困在那里。尽管在距地面顶部反演层上方的距离随距离增加而增加的某些部分渗透到地面基础反演层中,但在斜坡上方散发的污染物却在增强冷却的区域内减退。

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