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Study on an ozone episode in hot season in Hong Kong and transboundary air pollution over Pearl River Delta region of China

机译:香港炎热季节臭氧事件与中国珠三角地区越境空气污染的研究

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An ozone (O-3)episode that occurred in Hong Kong during 18-22 August 1999 was investigated. This episode lasted nearly 2 days with Typhoon Sam located at 500 km away from Hong Kong in the southeast. The maximum ground-level concentration of O-3 reached 334 mu g m(-3), which violated the Hong Kong Air Quality Objective for O-3 (240 mu g m(-3), 1 h). The visibility was reduced to 3.2 km and UV radiation was reduced by 50%. Investigations of local meteorological factors revealed that cloudless sky with high temperature and weak wind was responsible for the formation of O-3, which was trapped by sea-breeze circulations developed under stable atmospheric conditions. Backward trajectories indicated that transboundary transport induced by synoptic northwest wind due to the cyclone system played a critical role in this episode. It carried aged air mass of O-3 as well as its precursors from areas with heavy emissions. The PATH (Pollutants in the Atmosphere and their Transport over Hong Kong) model system was used to simulate the flow field and O-3 concentration. The computed results were basically consistent with field observations. Comparison with measurements showed that the model generally performed well in simulating flow structure over coastal complex terrain. The computed O-3 peaks at most stations were underestimated by 10%, which might be due to the uncertainty in NOx and VOC emission inventory in the study region. The H2O2/HNO3 ratio of 0.8-1.2 was identified to be the transition value for separating NOx- and VOC-sensitive regimes of O-3 chemistry. A process analysis further revealed the importance of horizontal transport in all physical and chemical evolution phases. Sensitivity study suggested that regional transport contributed to 60-90% of O-3 level at urban and rural areas of Hong Kong during the study period. (c) 2005 Elsevier Ltd. All rights reserved.
机译:调查了1999年8月18日至22日在香港发生的臭氧(O-3)事件。这集持续了将近2天,台风山姆位于距离香港500公里的东南方。 O-3的最高地面浓度达到334μg m(-3),这违反了香港对O-3的空气质量目标(240μg m(-3),1小时)。能见度降低到3.2 km,紫外线辐射降低50%。对当地气象因素的调查表明,高温和弱风的无云天空是O-3形成的原因,O-3被稳定的大气条件下形成的海风环流所困。向后的轨迹表明,由于旋风系统的影响,天气向西北风诱发的跨界运输在这一事件中起了关键作用。它携带着O-3的老化空气质量以及来自排放量大的地区的前体。 PATH(大气中的污染物及其在香港的运输)模型系统用于模拟流场和O-3浓度。计算结果与现场观察基本吻合。与测量结果的比较表明,该模型在模拟沿海复杂地形上的流动结构方面通常表现良好。在大多数站点计算出的O-3峰值被低估了10%,这可能是由于研究区域中NOx和VOC排放清单的不确定性所致。 H2O2 / HNO3比为0.8-1.2被确定为用于分离O-3化学物质的NOx和VOC敏感体系的转变值。过程分析进一步揭示了在所有物理和化学演化阶段中水平运输的重要性。敏感性研究表明,在研究期间,区域交通对香港城乡O-3水平的贡献率为60-90%。 (c)2005 Elsevier Ltd.保留所有权利。

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