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Long-Term Dynamics of Ozone in Surface Atmosphere at Remote Mountain, Rural and Urban Sites of South-East Siberia, Russia

机译:俄罗斯西伯利亚东南部偏远山区,农村和城市地区地表大气中臭氧的长期动态

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Long-term monitoring of near-ground ozone concentration was performed in the remote mountain area as well as at rural and urban sites of South-East Siberia. Ozone concentrations at all three sites had similar seasonal dynamics with its maximum in spring and minimum in autumn. Such seasonal trends were characteristic of many areas of the Northern Hemisphere. Diurnal fluctuations of ozone concentrations were caused by photochemical generation of ozone at daytime and its partial depletion at night. Diurnal fluctuations were maximal in spring and summer and minimal in December and January in accordance with solar radiation intensity. At the urban site, mean ozone concentrations were significantly lower (about 2 times) than those in the rural and background areas. This was likely attributed to the increased consumption of ozone for oxidation of air pollutants in the urbanized area. A tendency to the decrease of mean annual ozone concentrations was recorded during long-term observations at the mountain site Mondy.
机译:在偏远山区以及西伯利亚东南部的农村和城市地区进行了近地臭氧浓度的长期监测。这三个地点的臭氧浓度具有相似的季节动态,春季最大,秋季最小。这种季节性趋势是北半球许多地区的特征。臭氧浓度的昼夜波动是由白天光化学产生的臭氧和夜间臭氧的部分消耗引起的。根据太阳辐射强度,春季和夏季的日波动最大,12月和1月的日波动最小。在城市地区,平均臭氧浓度明显低于农村和背景地区(约2倍)。这可能归因于城市化区域中用于氧化空气污染物的臭氧消耗量增加。在山地Mondy的长期观测期间,记录了平均年臭氧浓度下降的趋势。

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