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首页> 外文期刊>Iranian Journal of Science and Technology >Controls on air pollution over a semi-enclosed basin, Tehran: A synoptic climatological approach
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Controls on air pollution over a semi-enclosed basin, Tehran: A synoptic climatological approach

机译:控制一个半封闭盆地德黑兰的空气污染:一种天气学方法

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In this study, a new array of meteorological elements and a synoptic climatologic classification to produce a baseline climate and to derive meteorological factors that are effective on air pollution in Tehran, which is located in a semi-enclosed basin was developed. The data set includes daily sea-level pressure and 500mb geopotential height fields from NCEP-NCAR and Tehran upper air sounding data at 00:00UTC for six months (July-December) of every year in the period 2001-2006. The classification is done through the principal component analysis (PCA) of data from the upper-air station. The results show that three meteorological factors are effective on variations of the Carbon Monoxide (CO) concentrations in the complicated terrain of Tehran basin. Thickness variations of different pressure layers (especially 850mb-700mb), Total totals index (TT) and surface wind speed are the most important dependent variables of these factors. Examination of the Carbon Monoxide (CO) pollution levels in Tehran, where emission sources are high shows that the synoptic classification identifies the patterns that are conducive to high pollution and those that are conducive to low pollutants build up in the basin. The synoptic climatology of events associated with five categories of CO concentrations show the role of synoptic forcings on decreasing CO concentrations. On the other hand, the role of high and thermal low pressure patterns in producing sever polluted episodes in the basin is also shown. These events occurred exclusively under special synoptic situations with high pressure developing on the airflow entrance of the basin and a thermal low pressure on the leeward side of the mountainous region. The coupled pressure system inducing horizontal pressure gradient produces a low level southerly cross wind toward the mountain barrier.
机译:在这项研究中,开发了一套新的气象要素和天气学气候分类,以产生基准气候并得出对半封闭盆地德黑兰的空气污染有效的气象因素。该数据集包括2001-2006年期间每年6个月(7月至12月)的NCEP-NCAR和德黑兰高空探测数据的每日海平面压力和500mb地势高度场。通过来自高空站的数据的主成分分析(PCA)进行分类。结果表明,三种气象因素对德黑兰盆地复杂地形中的一氧化碳浓度变化均有效。这些压力最重要的因变量是不同压力层(特别是850mb-700mb)的厚度变化,总指数(TT)和表面风速。对排放源较高的德黑兰的一氧化碳(CO)污染水平进行的调查表明,天气分类可以识别出有利于高污染的模式和有益于低污染的模式。与五种CO浓度相关的事件的天气气候学表明,天气强迫对降低CO浓度的作用。另一方面,还显示了高低压模式在盆地中产生严重污染事件中的作用。这些事件仅在特殊天气情况下发生,盆地的气流入口处形成高压,而山区的背风侧则形成热低压。产生水平压力梯度的耦合压力系统向山屏障产生低水平的南风。

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