Detrimental health effects of smog
Smog is a type of air pollution that results from the combination of smoke and fog or the reaction of sunlight with unburned hydrocarbons from vehicles. It poses significant health risks, contributing to respiratory issues, cardiovascular diseases, and even fatalities during severe episodes. Historical instances, such as the Meuse Valley incident in 1930 and the London fog of 1952, highlight the acute health impacts of smog, which can lead to widespread illness and increased mortality rates, particularly among vulnerable populations like the elderly and those with pre-existing health conditions.
Another form known as photochemical smog arises from automobile emissions reacting with sunlight, producing harmful compounds including ozone, which can irritate the eyes, lungs, and exacerbate asthma. Current research indicates that nearly 120 million Americans are exposed to unhealthy air quality due to smog and soot, with a disproportionate impact on communities of color. Efforts to reduce chemical pollutants have led to legislative changes in some areas, aiming to improve air quality and protect public health. However, challenges remain, particularly in regions like California, where wildfires have intensified air pollution issues.
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Detrimental health effects of smog
DEFINITION: Air pollution resulting from the combination of smoke with fog or from sunlight acting on unburned hydrocarbons emitted from automobiles
Severe smog episodes have been responsible for many deaths and widespread illness in cities around the world. Growing recognition of the detrimental health effects of smog have led many governments to pass laws designed to reduce chemical pollutants in the air.
Originally a blend of the words “smoke” and “fog,” the term “smog” was coined to describe the severe air that results when from factories combines with fog during a temperature inversion. As one ascends upward from Earth’s surface, the air temperature drops by about 3 degrees Celsius (5.5 degrees Fahrenheit) every 300 meters (1,000 feet). Temperature inversions occur when this normal condition is reversed so that a blanket of warm air is sandwiched between two cooler layers. A restricts the normal rise of surface air to the cooler upper layers, in effect placing a lid over a region. When the air above a city cannot rise, the air currents that carry pollutants away from their sources stagnate, causing pollution levels to increase drastically. A combination of severe air pollution, prolonged temperature inversion, and moisture-laden air may result in what has been termed “killer fog.”

Killer Fogs
Several acute episodes of killer fog occurred during the twentieth century. One was in the Meuse Valley of Belgium. During the first week of December 1930, a thick fog and stagnant air from a temperature inversion concentrated pollutants spewing forth from a variety of factories in this heavily industrialized river valley. After three days of such abnormal conditions, thousands of residents became ill with nausea, shortness of breath, and coughing. Approximately sixty people died, primarily elderly people and persons with chronic heart and lung diseases. The detrimental effects on health were later attributed to sulfur oxide gases emitted by combusting fossil fuels; the gases were concentrated to lethal levels by the abnormal weather. The presence of soot, combined with moisture from the fog, exacerbated the effect.
A second episode occurred in Donora, Pennsylvania, during the last week of October 1948. Donora is situated in a highly industrialized river valley south of Pittsburgh. A five-day temperature inversion with fog concentrated the gaseous effluents from steel mills with the sulfur oxides released by burning fossil fuels. Severe respiratory tract infections began to occur, especially in the elderly, and 50 percent of the became ill. Twenty people died, a tenfold increase in the normal death rate.
A third major episode occurred in London, England, in early December 1952. At that time, many residents burned soft coal in open grates to heat their homes. When a strong temperature inversion and fog enveloped the city for five consecutive days, Londoners began complaining of respiratory ailments. By the time the inversion had lifted, four thousand excess deaths had been recorded. In this case, it was not only the elderly who were affected—deaths occurred in all age categories. During the next decade, London experienced two additional episodes: one in 1956, which claimed the lives of one thousand people, and one in 1962, which caused seven hundred deaths. The decline in rates resulted from the restriction of the use of soft coal, with its high sulfur content, as a source of fuel. Sulfur oxide compounds are responsible for causing lung problems during such episodes; therefore, the term “killer fog” has come to be replaced by the more accurate “sulfurous smog.”
Photochemical Smog
Photochemical smog, first noticed in the Los Angeles basin in the late 1940s, has been an increasingly serious problem in cities around the world. Moisture is not part of the equation in this type of air pollution, and smoke-belching factories dumping tons of sulfur oxide compounds into the atmosphere are not required. Rather, results when unburned hydrocarbon fuel, emitted in automobile exhaust, is acted upon by sunlight. The Los Angeles basin, hemmed in by mountains to the east and ocean to the west, has a high of automotive traffic and plenty of sunshine. Varying driving conditions mean that gasoline is never completely consumed by automobile engines; instead, it is often changed into other highly reactive substances. Sunlight acts as an energy that changes these compounds into the variety of powerful oxidizing agents that constitute photochemical smog. This type of smog has a faint bluish-brown tint and typically contains several powerful eye irritants. The chemical reactions also produce aldehydes, a class of chemical best typified by an unpleasant odor.
The complicated chemistry of photochemical smog also produces ozone, which is extremely reactive; it damages plants and irritates human lungs. Because ozone production is stimulated by sunlight and high temperatures, it becomes a particularly pernicious problem during the summer, especially during morning rush hours. Under temperature inversion conditions, the ozone created in photochemical smog can increase to dangerous levels. Ozone is highly toxic. It irritates the eyes, causes chest irritation and coughing, exacerbates asthma, and damages the lungs.
Photochemical smog and ozone are now common ingredients in urban air. Although acute episodes of ozone-induced mortality are rare, concerns have grown about the detrimental long-term consequences of the brief but repetitive exposures to ozone consistently inflicted on commuters. A 2022 report by the American Lung Association (ALA) found that nearly 120 million Americans are still exposed to unhealthy air caused by smog and soot. The organization also found that people of color are nearly four times as likely to live in polluted places than White people. People of color account for 54 percent of those living in regions with poor air quality, even though they make up only 40 percent of the general population.
Ten of the eleven most polluted counties are in California, where frequent wildfires are reversing the improvements made on air quality. These California regions include Fresno, San Bernardino, Los Angeles, and Tulare. In Pennsylvania, Pittsburgh and Lancaster were the two worst places for soot, referred to as PM2.5. States that were on the ALA's dirtiest air list that have cut emissions include New Jersey, New York, and Ohio.
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