Air pollution and topography in Tehran

IF 0.5 Q3 GEOGRAPHY
Faezeh Afarideh, Mohammad Hossein Ramasht, Graham Mortyn
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引用次数: 0

Abstract

Tehran is one of the most polluted cities in the world with 48 days of air pollution exceeding the admissible threshold (AQI > 150) for 3 months of the 15 years studied. This period coincides with the time when Tehran’s inversion reaches its maximum stability. The purpose of this study was to determine the height of air pollution in Tehran in the days when pollution exceeds the permissible limit. Continuing to study the pressure and temperature conditions of these days, we then considered the geographical and topographic conditions, and finally identified the best of these cells for potential theoretical air turbulence. The results of this study, based on the Harmonic Analysis method and based on Tehran temperature and pressure data over a 15-year period (2003–2017), show that the highest elevation of Tehran inversion does not exceed 1800 m on polluted days. Only within 6 days of those beyond the admissible threshold, temperature and pressure cells with the highest Newtonian mass are formed. The center of these cells formed with a compressive difference of 32 mg in November, 7 mg in January, 11 mg in December, and temperature difference of 1.1° in November, 4.4° in January, and 1.9° in December. Generally, we considered the formed cells by the temperature and pressure difference and the gradient between them, as well as the difference in height between the cells and their location. This information, combined with the local winds causing the differences in temperature and pressure, allows us to elucidate conditions for creating air turbulence in Tehran and mitigating the amount and degree of air pollution.
德黑兰的空气污染和地形
德黑兰是世界上污染最严重的城市之一,有48天的空气污染超过了可接受的阈值(AQI >在15年的研究中,有3个月是150美元。这一时期与德黑兰逆温达到最大稳定性的时间相吻合。本研究的目的是确定在污染超过允许限度的日子里德黑兰空气污染的高度。继续研究这些天的压力和温度条件,然后我们考虑了地理和地形条件,最后确定了这些潜在的理论空气湍流的最佳单元。本研究基于调和分析方法,基于德黑兰15年(2003-2017年)的温度和压力数据,结果表明,污染日德黑兰逆温最高海拔不超过1800 m。只有在超过允许阈值的6天内,才会形成具有最高牛顿质量的温度和压力细胞。11月、1月、12月的气压差分别为32 mg、7 mg、11 mg; 11月、1月、12月的温差分别为1.1°、4.4°、1.9°。一般来说,我们考虑的是形成的细胞的温度和压力差和它们之间的梯度,以及细胞之间的高度差和它们的位置。这些信息,结合当地风造成的温度和压力差异,使我们能够阐明在德黑兰产生空气湍流的条件,并减轻空气污染的数量和程度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
AUC Geographica
AUC Geographica GEOGRAPHY-
CiteScore
1.20
自引率
0.00%
发文量
11
审稿时长
20 weeks
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