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Simulation of sea-land breezes and a discussion of their implications on the transport of air pollution during a multi-day ozone episode in the Pearl River Delta of China

机译:珠江三角洲多日臭氧事件中海风的模拟及其对空气污染传输的影响的讨论

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Sea-land breezes (SLBs) play an important role in transporting air pollution from urban areas on the coast. In this study, a meso-scale model MM5 was used to simulate SLBs and to understand the transport of pollution during a prolonged ozone episode observed in Hong Kong in September 2001. With the designed settings, the model performed very well in the simulation of SLBs. The simulated surface winds and the planetary boundary layer (PBL) heights are presented to contrast the characteristics of dispersion and transport on pre-episode and episode days. The diurnal variations in horizontal and vertical winds on an episode day are then presented to illustrate the evolution of SLBs. The results indicate that on episode days the onset of sea breezes (SBs) was delayed to noontime due to offshore synoptic winds, while on pre-episode days the SBs had already penetrated deep inland by early afternoon. The simulation shows that SBs propagated in both onshore and offshore directions in the afternoon, leading to the formation of nocturnal regional-scale SBs. The maximum distance for the inland penetration of an SB front (SBF) was about 60-80 km, in contrast to 120-150 km for offshore propagation. With the aid of high-resolution trajectories, the main meteorological factors contributing to the occurrence of the observed ozone episode are discussed. It is believed that the offshore synoptic wind, the delayed SBs, as well as the low mixing height contributed to the daytime transport of pollution and high ozone on the coast. The trajectory analysis also indicates important contributions from regional sources of emission.
机译:海陆风(SLB)在从沿海城市地区输送空气污染中起着重要作用。在这项研究中,使用中尺度模型MM5来模拟SLB,并了解在2001年9月香港发生的长时间臭氧事件中污染物的迁移。在设计设置的基础上,该模型在SLB的模拟中表现非常好。提出了模拟的表面风和行星边界层(PBL)的高度,以对比前期和发作日的弥散和输运特征。然后介绍一个发作日水平和垂直风的日变化,以说明SLB的演变。结果表明,在海浪发生的日子里,由于近海天气刮风,海风的发生被推迟到中午,而在大风爆发之前,海风已经在午后时分穿透了深内陆。模拟表明,SB在下午沿陆上和海上方向传播,导致形成了夜间区域规模的SB。 SB前沿(SBF)向内陆穿透的最大距离约为60-80 km,相比之下,近海传播的最大距离为120-150 km。借助高分辨率轨迹,讨论了导致观测到的臭氧事件发生的主要气象因素。据认为,近海天气,SB的延迟以及低混合高度是造成海岸上白天污染物和高臭氧排放的原因。轨迹分析还表明了区域排放源的重要贡献。

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