Wind speed is the most influential meteorological factor in determining the dispersion of air pollutants because it determines the rate at which pollutants are transported away from their source.

Temperature affects the formation of photochemical smog by increasing the rate of chemical reactions that produce smog-forming pollutants.

Ozone is most likely to be exacerbated by high humidity because water vapor can react with ozone to form hydroxyl radicals, which are highly reactive and can lead to the formation of additional ozone.

Climate change leads to an increase in air pollution by increasing the frequency and intensity of heat waves, droughts, and wildfires, which can all lead to the formation of air pollutants.

Wind direction is the most important meteorological factor for forecasting the transport of air pollutants over long distances because it determines the path that pollutants will take.

Stable conditions lead to poor dispersion of air pollutants because they prevent the vertical mixing of pollutants, which can lead to the accumulation of pollutants near the ground.

Particulate matter is most likely to be exacerbated by low wind speeds because low wind speeds allow particles to accumulate in the air.

Climate change leads to an increase in the frequency and intensity of heat waves by increasing the amount of heat-trapping gases in the atmosphere.

Temperature is the most important meteorological factor for forecasting the formation of smog because high temperatures increase the rate of chemical reactions that produce smog-forming pollutants.

Clouds lead to poor dispersion of air pollutants because they can trap pollutants near the ground by preventing the vertical mixing of air.

Ozone is most likely to be exacerbated by high temperatures because high temperatures increase the rate of chemical reactions that produce ozone.

Climate change leads to an increase in the frequency and intensity of droughts by increasing the amount of evaporation from the land surface.

Wind speed is the most important meteorological factor for forecasting the transport of air pollutants over short distances because it determines the rate at which pollutants are transported away from their source.

Mountains lead to poor dispersion of air pollutants because they can block the flow of air, which can lead to the accumulation of pollutants in valleys.