Classification of ozone pollution and analysis of meteorological factors in the Yangtze River Delta

IF 4.2 3区 地球科学 Q1 COMPUTER SCIENCE, INFORMATION SYSTEMS Big Earth Data Pub Date : 2023-01-05 DOI:10.1080/20964471.2022.2157093
Yufen Cao, Yuanhao Qu, Jinghui Ma
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Abstract

ABSTRACT Serious regional ozone (O3) pollution often plagues the Yangtze River Delta (YRD). The formation mechanism of these regional pollution events, including the meteorological and emission factors leading to these pollution events and how to affect the distribution of O3, still needs further research and exploration. In this study, we first define the standard of O3 regional pollution in the YRD, and then select 248 regional pollution cases from 2015 to 2020 according to the defined standard. For the pollution cases in pollution months (May and June), PCT (principal component analysis in T-mode) classification method is used to classify the ozone concentration distribution in YRD area. The regional distribution of the O3 concentrations in the YRD is divided into five types, and the overall type (Type 1) accounts for 15%, which is related to the control of YRD area by high-pressure center. Under the control of high pressure, the weather is sunny with the high temperature, and this weather condition is favorable for ozone generation and intercity transmission, causing extensive pollution. The double center type (Type 2) accounts for 8%. This type of YRD is controlled by the front of the high pressure (the high-pressure center is located in North China), and the weather in the middle and north is conducive to the generation and transmission of O3. Inland type (Type 3) accounts for 24%. The main body of this type of high pressure is located in Mongolia. The easterly wind in YRD area is conducive to the inland transmission of O3 precursors. The northern coastal type (Type 4) accounts for 44%. This type of YRD area is mainly controlled by the weak pressure field. The weather in the northern coastal area is sunny and the solar radiation for a long time is conducive to the formation of O3. The southern coastal type (Type 5) accounts for 10%, the solar radiation is strong in the southern region mainly under the influence of the post-offshore high pressure. This study provides new insights into the relationship between O3 pollution distribution types and atmospheric circulation in YRD area, and reveals the difference of potential meteorological impacts of different O3 pollution distribution types.
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长江三角洲臭氧污染分类及气象因子分析
摘要:严重的区域性臭氧(O3)污染经常困扰长三角地区。这些区域污染事件的形成机制,包括导致这些污染事件的气象和排放因素,以及如何影响O3的分布,还需要进一步的研究和探索。在本研究中,我们首先定义了长三角区域的O3污染标准,然后根据定义的标准选取2015 - 2020年248个区域污染案例。对于污染月份(5月和6月)的污染案例,采用PCT (t型主成分分析)分类方法对长三角地区臭氧浓度分布进行分类。长三角地区O3浓度的区域分布可分为5种类型,整体类型(1型)占15%,与高压中心对长三角地区的控制有关。在高压控制下,天气晴朗,气温较高,这种天气条件有利于臭氧的产生和城际传输,造成大面积污染。双中心型(2型)占8%。该型长三角受高压锋面控制(高压中心位于华北),中北部的天气有利于O3的产生和输送。内陆型(3型)占24%。这类高压的主体位于蒙古境内。长三角地区的东风有利于O3前体向内陆传播。北部沿海型(第4型)占44%。这种类型的长三角区域主要受弱压力场控制。北部沿海地区天气晴朗,长期的太阳辐射有利于O3的形成。南部沿海型(5型)占10%,南部地区太阳辐射强,主要受近海后高压影响。本研究对长三角地区O3污染分布类型与大气环流的关系提供了新的认识,揭示了不同O3污染分布类型对潜在气象影响的差异。
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来源期刊
Big Earth Data
Big Earth Data Earth and Planetary Sciences-Computers in Earth Sciences
CiteScore
7.40
自引率
10.00%
发文量
60
审稿时长
10 weeks
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