首页> 外文会议>Conference on agricultural and forest meteorology >AN OBJECTIVE ASSESSMENT OF THE CONNECTION BETWEEN METEOROLOGICAL ELEMENTS AND THE CONCENTRATIONS OF THE MAIN AIR POLLUTANTS AT SZEGED, HUNGARY
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AN OBJECTIVE ASSESSMENT OF THE CONNECTION BETWEEN METEOROLOGICAL ELEMENTS AND THE CONCENTRATIONS OF THE MAIN AIR POLLUTANTS AT SZEGED, HUNGARY

机译:客观评估气象元素与匈牙利塞格德主要空气污染物浓度的关系

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According to the results, four factors both for the winter and summer months can be considered as main contributors to the formation of weather and air pollution conditions at Szeged. Wind speed is an important parameter in diluting concentrations of air pollutants both in winter and summer. High wind speed is accompanied with good ventilation conditions and, consequently, with low concentration levels of primary pollutants and vice versa (Horvath et al., 2001). 63 concentrations seem to be inversely proportional to the concentrations of primary pollutants. The ozone parameters have the basic loadings in Factor 4 both for the winter and summer months. The loading of NO_2/NO ratio (in parenthesis) in Factor 4 is relatively high both for the winter and summer months. In winter, this loading indicates that only a part of the variation of O_3 is controlled by the irradiance. As a consequence of the direct proportion between the NO_2/NO ratio and the ozone parameters, higher NO_2 concentration implies higher ozone concentration and vice versa. In summer, changes of O_3 concentrations are mostly controlled by primary pollutants and not by the total amount of irradiance, which varies very little from day to day. In addition, the mean daily value of this secondary pollutant is inversely proportional to the mean daily values of the primary ones. This behaviour of O_3 can be explained by the fact that O_3 depends on the ratio of NO_2/NO. Namely, high value of this ratio implies high O_3 concentrations. It is revealed that temperature is controlled by the irradiance in summer, while this is not the case in winter, when temperature depends mainly on thermal characteristics of air masses affecting the Carpathian Basin.
机译:根据结果​​,冬季和夏季的四个因素可以被视为塞格德天气和空气污染条件的主要贡献者。风速是冬季和夏季稀释空气污染物浓度的重要参数。高风速伴随着良好的通风条件,因此,低浓度的主要污染物,反之亦然(Horvath等,2001)。 63浓度似乎与原发性污染物的浓度成反比。臭氧参数为冬季和夏季的因子4中的基本负载。因子4中的NO_2 / NO比(在括号中)的负载相对较高,冬季和夏季均相对较高。在冬季,该负载表明O_3的只有一部分由辐照度控制。由于NO_2 / NO比和臭氧参数之间的直接比例,较高的NO_2浓度意味着更高的臭氧浓度,反之亦然。在夏季,O_3浓度的变化主要由初级污染物控制,而不是通过辐照度的总量,从日常到一天中不等。此外,该二级污染物的平均每日值与主要污染物的平均日值成反比。 O_3的这种行为可以通过O_3取决于NO_2 / NO的比率来解释。即,该比率的高值意味着高O_3浓度。据透露,夏季,温度受到辐照度,而冬季则不是这种情况,当温度主要取决于影响喀尔巴阡山脉的空气肿块的热特性。

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