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天气形势对华北平原夏季臭氧污染的影响。

The impact of synoptic patterns on summertime ozone pollution in the North China Plain.

机构信息

Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, China.

Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, China.

出版信息

Sci Total Environ. 2020 Sep 15;735:139559. doi: 10.1016/j.scitotenv.2020.139559. Epub 2020 May 19.

Abstract

Surface ozone pollution is a challenging environmental issue in most parts of China. In particular, the North China Plain (NCP) region suffers from the severest ozone pollution throughout the country. In addition to the emission of precursors, ozone concentration is closely related to meteorological conditions resulting from regional atmospheric circulation. In this study, we investigate the relationship between synoptic patterns and summertime ozone pollution in the NCP using the objective principal component analysis in T-mode (T-PCA) classification method. Four dominant synoptic patterns are identified during the summers of 2014-2018. The heaviest ozone pollution is found to be associated with a high pressure anomaly over the Northwest Pacific and a distinct low pressure center in Northeast China. The southwesterly wind surrounding the low pressure center brings dry, warm air from inland South China, resulting in a high temperature, low humidity environment in the NCP, which favors the chemical formation of surface ozone. Locally, this type is associated with a moderate planetary boundary layer height (PBLH) of ~860 m and a stronger warm anomaly within the boundary layer than the upper level. We also notice a non-linear relationship between surface ozone concentration and the PBLH, i.e., ozone concentration first increases with PBLH till ~0.9 km, and then remains stable. This initial increase may relate to enhanced mixing with upper levels where ozone concentration is typically higher than that near the surface. However, when PBLH further increases, this downward mixing effect is balanced with the stronger upward turbulent mixing so that surface ozone shows little change. The synoptic patterns identified here, however, is unlikely responsible for the observed increasing trend in ozone concentration over the NCP region. Our study sheds light on the meteorological contribution to surface ozone pollution in North China and provides a reference for the pollution control and prediction.

摘要

在中国大部分地区,地表臭氧污染是一个具有挑战性的环境问题。特别是华北平原(NCP)地区是全国臭氧污染最严重的地区。除了前体物的排放外,臭氧浓度还与区域大气环流产生的气象条件密切相关。本研究采用 T 模式(T-PCA)主成分分析分类法,探讨了 NCP 地区天气型与夏季臭氧污染的关系。在 2014-2018 年的夏季,共识别出四种主要的天气型。研究发现,臭氧污染最严重时与西北太平洋上空的高压异常和东北地区明显的低压中心有关。低压中心周围的西南风从中国南部内陆带来干燥、温暖的空气,导致 NCP 地区出现高温、低湿度的环境,有利于地表臭氧的化学形成。在局部地区,这种类型与中高约 860m 的行星边界层高度(PBLH)和边界层内比上层更强的暖异常有关。我们还注意到地表臭氧浓度与 PBLH 之间存在非线性关系,即臭氧浓度先随 PBLH 增加至约 0.9km,然后保持稳定。这种初始增加可能与与高层的增强混合有关,因为臭氧浓度通常高于地表附近的浓度。然而,当 PBLH 进一步增加时,这种向下混合效应与更强的向上湍流混合相平衡,导致地表臭氧几乎没有变化。然而,这里识别的天气型不太可能是造成 NCP 地区臭氧浓度观测到的增加趋势的原因。本研究揭示了气象因素对华北地区地表臭氧污染的贡献,为污染控制和预测提供了参考。

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