The gray smog pictured above is stuck between two layers of air. The bottom layer is more dense than the top layer, so there is no mixing between the two layers. In winter, an inversion traps all of the pollutants that are emitted into the air over a region.
The two types of air pollutants are primary pollutants, which enter the atmosphere directly, and secondary pollutants, which form from a chemical reaction.
Some primary pollutants are natural, such as volcanic ash. Dust is natural but exacerbated by human activities; for example, when the ground is torn up for agriculture or development. Most primary pollutants are the result of human activities, the direct emissions from vehicles and smokestacks. Primary pollutants include:
High CO2 levels are found in major metropolitan areas and along the major interstate highways.
Particulates from a brush fire give the sky a strange glow in Arizona.
Any city can have photochemical smog, but it is most common in sunny, dry locations. A rise in the number of vehicles in cities worldwide has increased photochemical smog. Nitrogen oxides, ozone, and several other compounds are some of the components of this type of air pollution.
Photochemical smog forms when car exhaust is exposed to sunlight. Nitrogen oxide is created by gas combustion in cars and then into the air (Figure below). In the presence of sunshine, the NO2 splits and releases an oxygen ion (O). The O then combines with an oxygen molecule (O2) to form ozone (O3). This reaction can also go in reverse: Nitric oxide (NO) removes an oxygen atom from ozone to make it O2. The direction the reaction goes depends on how much NO2 and NO there is. If NO2 is three times more abundant than NO, ozone will be produced. If nitric oxide levels are high, ozone will not be created.
The brown color of the air behind the Golden Gate Bridge is typical of California cities, because of nitrogen oxides.
Ozone is one of the major secondary pollutants. It is created by a chemical reaction that takes place in exhaust and in the presence of sunlight. The gas is acrid-smelling and whitish. Warm, dry cities surrounded by mountains, such as Los Angeles, Phoenix, and Denver, are especially prone to photochemical smog. Photochemical smog peaks at midday on the hottest days of summer. Ozone is also a greenhouse gas.
Use this resource to answer the questions that follow.
| Color | Highlighted Text | Notes | |
|---|---|---|---|
| Please Sign In to create your own Highlights / Notes | |||
| Image | Reference | Attributions |
|---|---|---|
| Credit: Image copyright Mattia Terrando, 2014 Source: http://www.shutterstock.com License: Used under license from Shutterstock.com | ||
| Credit: Courtesy of Jesse Allen and Robert Simmon, NASA Source: http://earthobservatory.nasa.gov/IOTD/view.php?id=8903 License: Public Domain | ||
| Credit: Miles Orchinik Source: CK-12 Foundation License: CC BY-NC 3.0 | ||
| Credit: Bluerock123 Source: https://pixabay.com/photos/sf-san-francisco-golden-gate-golden-3549164/ License: Pixabay License |
Your search did not match anything in .