Atmospheric chemistry and aerosols
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Temples emit PM 2.5 with elevated metal concentrations and stable Pb isotope ratios, especially during major events and higher visitor numbers, impacting air quality.
Deep convection over the Loess Plateau significantly enhances ozone pollution, with column ozone in the residual layer doubling during pollution episodes.
Wildfire-specific PM 2.5 increases are linked to 10-16% higher cardiopulmonary hospitalization risks, surpassing non-wildfire PM 2.5 effects in 20 US states.
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Atmospheric methane lifetime during the Last Glacial Maximum was reduced to 7.8 years, 20% shorter than today, due to dust-mediated chlorine chemistry.
Brake wear particles exhibit an exceptionally high SO2 oxidation rate, with uptake coefficients up to 2.87 × 10^-5, vastly surpassing mineral dust and soot under dark conditions.
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