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2021
DOI: 10.1016/j.atmosres.2021.105735
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Effect of springtime thermal forcing over Tibetan Plateau on summertime ozone in Central China during the period 1950–2019

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Cited by 9 publications
(3 citation statements)
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“…[ 68 ] Seasonal differences in urban ozone concentrations are mainly influenced by temperature, and we observe that peaks in O 3 concentrations occur during the summer months when temperatures are higher, due to the favorable conditions for O 3 formation provided by intense solar radiation and rising temperatures. [ 69 ] This effect is particularly pronounced in the cities of northern, eastern, and northeastern China. This finding aligns with the results of the He et al.…”
Section: Discussionmentioning
confidence: 99%
“…[ 68 ] Seasonal differences in urban ozone concentrations are mainly influenced by temperature, and we observe that peaks in O 3 concentrations occur during the summer months when temperatures are higher, due to the favorable conditions for O 3 formation provided by intense solar radiation and rising temperatures. [ 69 ] This effect is particularly pronounced in the cities of northern, eastern, and northeastern China. This finding aligns with the results of the He et al.…”
Section: Discussionmentioning
confidence: 99%
“…Ma et al (2021b) [ 55 ] illustrated that the increase in volatile organic compounds (VOCs) along with depletions in NO 2 and CO significantly boosted the ozone photochemical production in North China plain. Wang et al (2021) [ 56 ] showed that the annual summertime ozone over Central China was significantly correlated with the springtime thermal forcing, indicated by total atmospheric energy over Tibetan Plateau in an interdecadal timescale. During the COVID-19 lockdown period, the results of Yin et al (2021) [ 57 ] suggest that conventional emission reduction of NO x could not be sufficient to reduce surface O 3 concentration, and ozone pollution needs to be controlled by a variety of pollutants in central China.…”
Section: Discussionmentioning
confidence: 99%
“…2CSAm, influencing the middle troposphere over each sub-region of CEC, is situated further south and west compared to 2CSAl, which affects the lower 345 troposphere. Notably, 2CSAm1, positioned at 50°-90° E, 25°-45° N, originates over the Tibetan Plateau, influenced by the South Asian High modulated by the heat source over the plateau (Wang et al, 2021). This source exerts the most substantial impact on LP, followed by the sub-regions NC, NE, EC, and CC.…”
Section: Csas For Dsi 340mentioning
confidence: 99%