Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China

This paper investigates the spatiotemporal variability of air stagnation in summer as well as its relation to summer ozone (O3) over the Yangtze River Delta (YRD) region of China. Air stagnation days (ASDs) in the YRD during the summers from 2001 to 2017 range from 9 to 54 days (9.2–58.4% of the ent...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Min Xie, Chenchao Zhan, Yangzhihao Zhan, Jie Shi, Yi Luo, Ming Zhang, Qian Liu, Fanhui Shen
Formato: article
Lenguaje:EN
Publicado: Frontiers Media S.A. 2021
Materias:
Acceso en línea:https://doaj.org/article/e4e17fa7ee0a4476a909e0819d02c940
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:e4e17fa7ee0a4476a909e0819d02c940
record_format dspace
spelling oai:doaj.org-article:e4e17fa7ee0a4476a909e0819d02c9402021-11-08T04:47:46ZSpatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China2296-665X10.3389/fenvs.2021.783524https://doaj.org/article/e4e17fa7ee0a4476a909e0819d02c9402021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fenvs.2021.783524/fullhttps://doaj.org/toc/2296-665XThis paper investigates the spatiotemporal variability of air stagnation in summer as well as its relation to summer ozone (O3) over the Yangtze River Delta (YRD) region of China. Air stagnation days (ASDs) in the YRD during the summers from 2001 to 2017 range from 9 to 54 days (9.2–58.4% of the entire summer days). With the empirical orthogonal function (EOF) analysis, the dominant weather systems affecting air stagnation in the YRD are illustrated. The first three EOFs explain 68.8, 11.3, and 7.1% of the total variance of ASDs, respectively. The first EOF represents the same phase of the entire YRD, which is attributed to the East Asian summer monsoon and mainly depends on the area and the intensity of the South China Sea subtropical high. The second EOF shows significant maritime-continental contrasts, which is related to stronger near-surface winds on sea. As for the third EOF, the air stagnation in the north and the south of the YRD has the opposite phase, with a dividing line along approximately 31°N. This spatial pattern depends on the area and the intensity of the northern hemisphere polar vortex that affects the meridional circulation. O3 is the typical air pollutant in hot seasons in the YRD. It is generally at a high pollution level in summer, and has a positive trend from 2013 to 2017. Air stagnation can affect O3 pollution levels in the YRD. In ASDs, there are usually weak wind, less precipitation, low relative humidity, high temperature, strong solar radiation and high surface pressure, which are favorable to the formation of O3. More O3 pollution episodes in 2013 than 2015 can be partly attributed to more ASDs in 2013. These results show that stagnant meteorological state can lead to the hazardous air quality, and provide valuable insight into the effect of air stagnation on the changes in surface O3 during hot months.Min XieChenchao ZhanYangzhihao ZhanJie ShiYi LuoMing ZhangMing ZhangQian LiuFanhui ShenFrontiers Media S.A.articleair qualityozoneair stagnationthe Yangtze River Delta regionpollution meteorological characteristicsEnvironmental sciencesGE1-350ENFrontiers in Environmental Science, Vol 9 (2021)
institution DOAJ
collection DOAJ
language EN
topic air quality
ozone
air stagnation
the Yangtze River Delta region
pollution meteorological characteristics
Environmental sciences
GE1-350
spellingShingle air quality
ozone
air stagnation
the Yangtze River Delta region
pollution meteorological characteristics
Environmental sciences
GE1-350
Min Xie
Chenchao Zhan
Yangzhihao Zhan
Jie Shi
Yi Luo
Ming Zhang
Ming Zhang
Qian Liu
Fanhui Shen
Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
description This paper investigates the spatiotemporal variability of air stagnation in summer as well as its relation to summer ozone (O3) over the Yangtze River Delta (YRD) region of China. Air stagnation days (ASDs) in the YRD during the summers from 2001 to 2017 range from 9 to 54 days (9.2–58.4% of the entire summer days). With the empirical orthogonal function (EOF) analysis, the dominant weather systems affecting air stagnation in the YRD are illustrated. The first three EOFs explain 68.8, 11.3, and 7.1% of the total variance of ASDs, respectively. The first EOF represents the same phase of the entire YRD, which is attributed to the East Asian summer monsoon and mainly depends on the area and the intensity of the South China Sea subtropical high. The second EOF shows significant maritime-continental contrasts, which is related to stronger near-surface winds on sea. As for the third EOF, the air stagnation in the north and the south of the YRD has the opposite phase, with a dividing line along approximately 31°N. This spatial pattern depends on the area and the intensity of the northern hemisphere polar vortex that affects the meridional circulation. O3 is the typical air pollutant in hot seasons in the YRD. It is generally at a high pollution level in summer, and has a positive trend from 2013 to 2017. Air stagnation can affect O3 pollution levels in the YRD. In ASDs, there are usually weak wind, less precipitation, low relative humidity, high temperature, strong solar radiation and high surface pressure, which are favorable to the formation of O3. More O3 pollution episodes in 2013 than 2015 can be partly attributed to more ASDs in 2013. These results show that stagnant meteorological state can lead to the hazardous air quality, and provide valuable insight into the effect of air stagnation on the changes in surface O3 during hot months.
format article
author Min Xie
Chenchao Zhan
Yangzhihao Zhan
Jie Shi
Yi Luo
Ming Zhang
Ming Zhang
Qian Liu
Fanhui Shen
author_facet Min Xie
Chenchao Zhan
Yangzhihao Zhan
Jie Shi
Yi Luo
Ming Zhang
Ming Zhang
Qian Liu
Fanhui Shen
author_sort Min Xie
title Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
title_short Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
title_full Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
title_fullStr Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
title_full_unstemmed Spatiotemporal Variability of Air Stagnation and its Relation to Summertime Ozone in the Yangtze River Delta of China
title_sort spatiotemporal variability of air stagnation and its relation to summertime ozone in the yangtze river delta of china
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/e4e17fa7ee0a4476a909e0819d02c940
work_keys_str_mv AT minxie spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT chenchaozhan spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT yangzhihaozhan spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT jieshi spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT yiluo spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT mingzhang spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT mingzhang spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT qianliu spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
AT fanhuishen spatiotemporalvariabilityofairstagnationanditsrelationtosummertimeozoneintheyangtzeriverdeltaofchina
_version_ 1718443049030254592