2.5: air pollution
air and the atmosphere
- atmosphere: a sea of air that surrounds the earth
- divided into several layers, separated from each other by abrupt changes in temperature due to differences in absorption of solar energy
layers of the atmosphere
- troposphere
- lowest layer, contains 75% of the mass of earth’s air
- extends 10km/6mi up from sea level at the equator
- temperature declines with altitude and then abruptly rises when entering the tropopause
- tropopause: the boundary between the troposphere and upper layers
- air composition
- 78% nitrogen, 21% oxygen, 1% other eg. permanent gases and variable gases
- stratosphere
- second layer, extends from 10-50km/6-30mi above earth’s surface
- air is very calm
- temperature increases with altitude until another reversal in the stratopause
- stratopause: the boundary between the stratosphere and upper layers
- air composition
- similar to troposphere with two exceptions:
- less water vapor
- 1000x more ozone (O3)
- ozone in troposphere = bad, in stratosphere = good
air pollution
- air pollution: the presence of chemicals in the air in quantities and durations that are harmful to the environment and human health
- some pollutants are natural
- natural fires
- terpenes (from forests)
- pollen (allergen)
- dust (from volcanos)
types of pollutants
- primary pollutants: harmful substances emitted directly in that form
- may react with one another or with a basic air component to become secondary pollutants
- conventional pollutants + pollutant criteria
- the EPA sets the National Ambient Air Quality Standards (NAAQS) which limits six major pollutants
- particulate matter (PM)
- classified based on diameter
- PM10: 10 micrometers or smaller
- PM2.5: 2.5 micrometers or smaller
- comes from wildfires, industrial activities, motor vehicles, cooking, and fuel burning
- particles can enter the lungs, and the smallest can enter the bloodstream
- this can cause heart attacks, strokes, and negatively impact children’s nervous systems
- associated with ~80,000 deaths in the US
- ozone (ground level)
- nitrogen oxides (NOx)
- sulfur oxides (SOx)
- carbon monoxide (CO)
- lead
smog
- “smog” = fusion of words “smoke” and “fog”
- two types
- industrial smog
- photochemical smog
industrial smog
- important until the mid-1900’s in industrial cities (eg. London, Donora, Pittsburg, Chicago)
- now, rarely a problem in MDCs but still a problem in China, India, Eastern Europe
- caused by large amounts of heavy oil and coal burnt in homes for heat and in industrial work
- generally worse in winter
- releases sulfur oxides (SOx) and particulate matter
- appears grey in color
the great smog
- took place in London in December 1952
- unusually cold → more coal burnt
- visibility fell to ~12 inches
- 100,000+ people treated for respiratory problems
- caused 3,000-4,000 extra deaths
- extra death: a death caused by smog above the normal rates which are attributed to the abnormal smog conditions
- mainly of cardiac and respiratory ailments
- asthma
- disease which negatively effects lungs
- more common among people alive/born during the great smog
- US equivalent: Donora, PA, October 1948
photochemical smog
- more pressing current problem in more developed countries
- composed of a mixture of primary and secondary pollutants
- formed when primary pollutants interact under the effect of sunlight and give origin to a mixture of 100 chemicals dominated by ozone
- worse in summer
- primary pollutants involved and their sources
- nitrogen oxides (NOx) mainly from vehicles
- volatile organic compounds (VOCs) from vehicles, gas stations, dry cleaners, print shops, vegetation
- appears orange in color
ozone
- stratospheric → good
- ground level → bad
- very irritating for the respiratory system
thermal inversions
- thermal inversion: a process which occurs when a layer of cold air temporarily trapped near the ground by a warmer, upper layer
- pollutants do not get dispersed during thermal inversions
- warm air is less dense than cold air
- normal conditions
- during the day, sun warms up the air near the surface, which expands and rises, carrying low-lying pollutants higher
- under normal conditions, there is a constant movement of air
- sometimes a layer of cold air is trapped beneath a warmer, less dense error
- warm air prevents ascending air currents and the dispersion of pollutants
- common in valleys and urban areas
urban heat islands
- structures eg. buildings, roads, and other infrastructure absorb and re-emit the sun’s heat more than natural landscapes such as forests and water bodies
- urban areas become islands of higher temperature relative to outlying areas
- result in thermal inversions and more thunderstorms
- dust domes: pollutants including soot trapped in urban air through thermal inversions
case study: mexico city
- megacity with over 22 million people in the metro area
- more people, more industry, more cars
- located at a high altitude → solar radiation is intense
- surrounded by mountains, air can be stagnant with winter thermal invasions
- deforestation and construction have exposed soil to wind erosion