Tropospheric ozone is formed when nitrogen oxides (NOx) and volatile organic compounds released from burning fossil fuels react with oxygen in the presence of sunlight. This causes eye and skin irritation and breathing problems in humans. In large cities, ozone levels are lower due to reactions with NO from vehicles forming photochemical smog.
Photochemical smog forms in cities with low wind and stable atmospheric conditions. It is a mixture of ozone, NOx and VOCs produced when these pollutants react in sunlight. Summer smog is worse in sunny areas and winter smog occurs in inversion layers trapping pollution. Smog levels may be higher surrounding city centers where polluted air drifts.