Atmospheric Sounding Station El Arenosillo, National Institute of Aerospace Technology (INTA), Crta. Huelva - Matalascañas, km 33, 21130, Mazagón, Huelva, Spain.
Environ Sci Pollut Res Int. 2010 Feb;17(2):355-68. doi: 10.1007/s11356-008-0098-9. Epub 2009 Jan 20.
Photochemical ozone pollution of the lower troposphere (LT) is a very complex process involving meteorological, topographic emissions and chemical parameters. Ozone is considered the most important air pollutant in rural, suburban and industrial areas of many sites in the world since it strongly affects human health, vegetation and forest ecosystems, and its increase during the last decades has been significant. In addition, ozone is a greenhouse gas that contributes to climate change. For these reasons, it is necessary to carry out investigations that determine the behaviour of ozone at different locations. The aim of this work is to understand the levels and temporal variations of surface ozone in an industrial-urban region of the Southwest Iberian Peninsula.
The study is based on ozone hourly data recorded during a 6-year period, 2000 to 2005 at four stations and meteorological data from a coastal station. The stations used were El Arenosillo and Cartaya--both coastal stations, Huelva--an urban site and Valverde--an inland station 50 km away from the coastline. The general characteristics of the ozone series, seasonal and daily ozone cycles as well as number of exceedances of the threshold established in the European Ozone Directive have been calculated and analysed.
Analysis of the meteorological data shows that winter-autumn seasons are governed by the movement of synoptic weather systems; however, in the spring-summer seasons, both synoptic and mesoescale conditions exist. Average hourly ozone concentrations range from 78.5 +/- 0.1 microg m(-3) at Valverde to 57.8 +/- 0.2 microg m(-3) at Huelva. Ozone concentrations present a seasonal variability with higher values in summer months, while in wintertime, lower values are recorded. A seasonal daily evolution has also been found with minimum levels around 08:00 UTC, which occurs approximately 1-1.5 h after sunrise, whereas the maximum is reached at about 16:00 UTC. Furthermore, during summer, the maximum value at El Arenosillo and Valverde stations remains very uniformed until 20:00 UTC. These levels could be due to the photochemical production in situ and also to the horizontal and vertical ozone transport at El Arenosillo from the reservoir layers in the sea and in the case of Valverde, the horizontal transport, thanks to the marine breeze. Finally, the data have been evaluated relative to the thresholds defined in the European Ozone Directive. The threshold to protect human health has been exceeded during the spring and summer months mainly at El Arenosillo and Valverde. The vegetation threshold has also been frequently exceeded, ranging from 131 days at Cartaya up to 266 days at Valverde.
The results in the seasonal and daily variations demonstrate that El Arenosillo and Valverde stations show higher ozone concentrations than Cartaya and Huelva during the spring and summer months. Under meteorological conditions characterized by land-sea breeze circulation, the daytime sea breeze transports the emissions from urban and industrial sources in the SW further inland. Under this condition, the area located downwind to the NE is affected very easily by high ozone concentrations, which is the case for the Valverde station. Nevertheless, according to this circulation model, the El Arenosillo station located at the coast SE from these sources is not directly affected by their emissions. The ozone concentrations observed at El Arenosillo can be explained by the ozone residual layer over the sea, similar to other coastal sites in the Mediterranean basin.
The temporal variations of the ozone concentrations have been studied at four measurement sites in the southwest of the Iberian Peninsula. The results obtained point out that industrial and urban emissions combined with specific meteorological conditions in spring and summer cause high ozone levels which exceed the recommended threshold limits and could affect the vegetation and human health in this area.
This work is the first investigation related to surface ozone in this region; therefore, the results obtained may be a useful tool to air quality managers and policy-makers to apply possible air control strategies towards a reduction of ozone exceedances and the impact on human health and vegetation. Due to the levels, variability and underlying boundary layer dynamics, it is necessary to extend this research in this geographical area with the purpose of improving the understanding of photochemical air pollution in the Western Mediterranean Basin and in the south of the Iberian Peninsula.
低层大气(LT)的光化学臭氧污染是一个非常复杂的过程,涉及气象、地形排放和化学参数。由于臭氧强烈影响人类健康、植被和森林生态系统,并且在过去几十年中其浓度显著增加,因此在世界上许多地区的农村、郊区和工业区,臭氧被认为是最重要的空气污染物。此外,臭氧是一种温室气体,会导致气候变化。出于这些原因,有必要开展调查,以确定不同地点的臭氧行为。本工作的目的是了解伊比利亚半岛西南部一个工业城市地区的地表臭氧的水平和时间变化。
本研究基于 2000 年至 2005 年在四个站点记录的臭氧每小时数据以及沿海站点的气象数据。使用的站点是埃尔阿伦索罗(El Arenosillo)和卡塔亚(Cartaya)——均为沿海站点,韦尔瓦(Huelva)——城市站点,以及距离海岸线 50 公里的瓦尔韦德(Valverde)——内陆站点。计算并分析了臭氧序列的一般特征、季节性和每日臭氧循环以及超过欧洲臭氧指令中规定的阈值的次数。
气象数据分析表明,冬-秋季受天气系统运动的影响;然而,在春-夏季,既存在天气系统又存在中尺度条件。平均每小时臭氧浓度范围从瓦尔韦德的 78.5+/-0.1µg m(-3)到韦尔瓦的 57.8+/-0.2µg m(-3)。臭氧浓度具有季节性变化,夏季月份浓度较高,而冬季月份浓度较低。还发现了季节性每日变化,最低水平约在协调世界时 08:00 左右,大约在日出后 1-1.5 小时发生,而最大值则在协调世界时 16:00 左右达到。此外,在夏季,埃尔阿伦索罗和瓦尔韦德两个站点的最大值一直保持到协调世界时 20:00 左右,这一水平可能是由于光化学原位产生以及埃尔阿伦索罗的臭氧水平在海面上的储层层中的水平和垂直输送,以及瓦尔韦德的水平输送,这要归功于海洋微风。最后,根据欧洲臭氧指令中定义的阈值对数据进行了评估。在春季和夏季,主要在埃尔阿伦索罗和瓦尔韦德,超过了保护人类健康的阈值。植被阈值也经常超过,从卡塔亚的 131 天到瓦尔韦德的 266 天。
季节性和每日变化的结果表明,在春季和夏季,埃尔阿伦索罗和瓦尔韦德两个站点的臭氧浓度高于卡塔亚和韦尔瓦。在海陆风环流气象条件下,白天的海风将城市和工业源的排放物输送到西南内陆更远的地方。在这种情况下,下风方向的地区很容易受到高臭氧浓度的影响,瓦尔韦德就是这种情况。然而,根据这种环流模式,位于这些源下风方向的埃尔阿伦索罗站不会直接受到它们排放物的影响。在埃尔阿伦索罗观察到的臭氧浓度可以通过海上的臭氧残留层来解释,类似于地中海盆地的其他沿海站点。
在伊比利亚半岛西南部的四个测量站点研究了臭氧浓度的时间变化。所得结果表明,春季和夏季的工业和城市排放物与特定的气象条件相结合,导致臭氧水平升高,超过了建议的阈值限制,并可能影响该地区的植被和人类健康。
这是该地区首次与地表臭氧有关的研究;因此,所获得的结果可能是空气质量管理者和决策者的有用工具,可以采取可能的空气控制策略,以减少臭氧超标,并减少对人类健康和植被的影响。由于水平、可变性和潜在的边界层动力学,有必要在该地理区域扩展这项研究,以提高对西地中海盆地和伊比利亚半岛南部光化学空气污染的理解。