Particulates in urban areas are greater than rural
Higher carbon monoxide
Higher sulphur dioxide
Where do atmospheric pollutants come from?
Vehicle exhausts
Burning - wood, coal, rubbish etc
Construction, mining and quarrying
Plants generate coarse particulates e.g. pollen, mould spores
Carbon monoxide from vehicles
Road vehicles engines perform combustion but when insuffienct oxygen supply, carbon monoxide forms > highest concentration of carbon monoxide on busy roads (90%)
Also a switch to coal
Sulphur dioxide:
Produced from coal power stations and oil refineries > cause haze and acid rain, coughing, chest problems
The increased haze affects lichens photosynthesis and chlorophyll
Poor urban air quality impacts:
Respiratoryproblems e.g. asthma
Increases haze - sulphur dioxide
Increase carbondioxide > enhance greenhouse effect and global warming
Increaed particulates in the atmopshere attack building facades - weathering
Photochemcaloxidants cause eye irritations and headaches
Photochemical smog: Ozone and PAN (Peroxyacetyl Nitrate)
Photochermical smog is a mixture of pollutants that are formed when nitrogen oxides and volatileorganiccompounds (VOC) react to ultraviolet light from the sun > creates a brown haze above cities
Road transport produced 50% of nitrogen oxides
Causes asthma and lung inflammation and accerlerated weathering
More common in warm, sunnier ctieis as these areas suffer from temperature inversionfog (layer of warm air trapped below dense cooler air) > keeps pollutants at surface level
Particulate matter (PM's)
Produced from powerstations, vehicle exhausts, dust and ash and pollen
Damage lungs and airways
Ella-AdooKissiDebrah:
The first person in the world to have air pollution listed on her death sentence
High levels of PM's 2.5's and nitrogren dioxide and pollution from wood burning stoves > developed asthma > admitted to hospital 27 times > died from asthma attack
Trapping air pollution: Temperature inversions and development of photochemical smog:
Extended periods of highpressure (anticyclonic conditions) in winter - calm and clear
Solarradiation reaches ground and warms it up
Night > lack of cloudcover means ground loses heatrapidly and air in contact with ground becomes colder
Coolerairsinks in lower areas e.g. valleys, basins > condensation > fog forms
Warmairrises > acts as lid > trap colder air and fog closer to ground
Trapping air pollution: Temperature inversions and development of photochemical smog
6. Air pollution also trapped > layer close to ground becomes more polluted