Smog

Smog, or smoke fog, is a type of intense <a href="/facts/Air_pollution/zmk9Dy7S">air pollution</a>. The word "smog" was coined in the early 20th century, and is a <a href="/facts/Portmanteau/d124JEbz">portmanteau</a> of the words <a href="/facts/Smoke/KRJaumoC">smoke</a> and <a href="/facts/Fog/mrIdyIc7">fog</a> to refer to smoky fog due to its opacity, and odour. The word was then intended to refer to what was sometimes known as <a href="/facts/Pea_soup_fog/jT0GBLEs">pea soup fog</a>, a familiar and serious problem in <a href="/facts/London/KozCCsy9">London</a> from the 19th century to the mid-20th century, where it was commonly known as a London particular or London fog. This kind of visible air pollution is composed of <a href="/facts/Nitrogen_oxide/ved7hE6X">nitrogen oxides</a>, <a href="/facts/Sulfur_oxide/KuLlKlbC">sulfur oxide</a>, <a href="/facts/Ozone/o0E5gn2p">ozone</a>, smoke and other <a href="/facts/Particulate_matter/RleGr5E6">particulates</a>. Man-made smog is derived from coal combustion emissions, vehicular emissions, industrial emissions, forest and agricultural fires and photochemical reactions of these emissions.
Smog is often categorized as being either <a href="/facts/Summer_smog/5FYzS8sT">summer smog</a> or winter smog. Summer smog is primarily associated with the photochemical formation of ozone. During the summer season when the temperatures are warmer and there is more sunlight present, photochemical smog is the dominant type of smog formation. During the winter months when the temperatures are colder, and <a href="/facts/Inversion_(meteorology)/GXdVvy7I">atmospheric inversions</a> are common, there is an increase in coal and other fossil fuel usage to heat homes and buildings. These combustion emissions, together with the lack of pollutant <a href="/facts/Atmospheric_dispersion_modeling/dCX1tDCy">dispersion</a> under inversions, characterize winter smog formation. Smog formation in general relies on both primary and secondary pollutants. Primary pollutants are emitted directly from a source, such as emissions of <a href="/facts/Sulfur_dioxide/jDK1fIDs">sulfur dioxide</a> from coal combustion. Secondary pollutants, such as ozone, are formed when primary pollutants undergo chemical reactions in the atmosphere.
Photochemical smog, as found for example in Los Angeles, is a type of air pollution derived from <a href="/facts/Vehicular_emission/2vrAgltu">vehicular emission</a> from <a href="/facts/Internal_combustion_engine/Ju4BXzj0">internal combustion engines</a> and industrial fumes. These pollutants react in the atmosphere with sunlight to form secondary pollutants that also combine with the primary emissions to form <a href="/facts/Photochemical_smog/5FYzS8sT">photochemical smog</a>. In certain other cities, such as Delhi, smog severity is often aggravated by <a href="/facts/Stubble_burning/vaBNF4Ng">stubble burning</a> in neighboring agricultural areas since the 1980s. The atmospheric pollution levels of <a href="/facts/Los_Angeles/pyXpYEX9">Los Angeles</a>, <a href="/facts/Beijing/Bg4puFBv">Beijing</a>, <a href="/facts/Delhi/Xa6CKgnf">Delhi</a>, <a href="/facts/Lahore/cjHrUPaD">Lahore</a>, <a href="/facts/Mexico_City/gEnGxDEd">Mexico City</a>, <a href="/facts/Tehran/S8dmdwyG">Tehran</a> and other cities are often increased by an inversion that traps pollution close to the ground. The developing smog is <a href="/facts/Toxic/qa96rs60">toxic</a> to humans and can cause severe sickness, a shortened life span, or immature death.

Smog open-in-new

Smog