Atmospheric Structure and Pollution Sources
The atmosphere is the thin layer of gas surrounding earth. Half of the
mass of the atmosphere is below a height of 5.5 km, 90% is below 16.5
km, and 99% is below 30 km.
This is what the atmosphere looks like viewed edge on from space. The
image is of a small cross-sectional area, note the small curvature
of the surface, yet the atmosphere is a small part of the whole. Looking
closely, you can see tall thunderstorm clouds silhouetted against an
orange layer of atmospheric gases backlit by the sun just below the
horizon. Above this layer is the clear blue of the stratosphere and
the blackness of space.
Space Shuttle Flight 6 on 4 April 1983.
The atmosphere is composed of 78.08% nitrogen and 20.95% oxygen with
small amounts of other gases: 0.93% argon, 0.038% carbon dioxide, 0.002%
neon, and yet smaller concentrations of helium, methane, krypton, and
hydrogen. Both nitrogen and oxygen exist in large quantities only because
of life on earth, especially life in the ocean.
It would seem that the composition of the atmosphere would be stratified
with different chemical composition at different heights. In fact, mixing
in the atmosphere causes the composition to be nearly uniform up to about
Ozone is a very important trace gas in the atmosphere.
It exits in two places:
- In the stratosphere at heights around 20-30 km. This is good ozone.
It protects all life on earth from dangerous solar ultraviolet radiation
- Close to the surface due to pollution. It is produced from nitrogen
oxides and volatile carbon-based compounds when there is intense solar
radiation (energy), above all in the spring and summer. This is bad
ozone. It causes respiratory illness; it damages plants; and it attacks
Remember "Good Up high, Bad Nearby"
Average ozone concentration in June (red line) and ozone pressure
(in nano bars, where one
bar is approximately atmospheric pressure at sea level) on 23 June
2006 (black line), as a function of height in kilometers above the
Swiss Payerne station. Click on image for a zoom.
From Swiss Federal Office of Meteorology and Climatology, ozone
Many other gases are found in trace amounts in the atmosphere.
Most are short lived pollutants. Most are local or regional in extent.
The space and time scales of trace gases in the atmosphere. The moderately
long-lived species contribute to regional and urban air pollution
and smog. The long-lived species contribute to the ozone hole and
The density and pressure of the atmosphere drop nearly
exponentially with height up to a height of 100 km. Temperature decreases
with height in the troposphere up to a height of 10-15 km, then it increases
with height in the stratosphere. The stratosphere is defined as that
region above the troposphere where temperature increases with height.
Because temperature increases with height, the layer is stable and stratified,
hence the name. The stratosphere is heated from above by the absorption
of solar ultraviolet radiation by ozone in the stratosphere.
Left: Density of the atmosphere as a
function of height. Click on the image for a zoom.
Michaelsen, University of California Santa Barbara.
Right: Temperature as a function
of height in the atmosphere measured by radiosondes at three cities.
Click on the image for a zoom. More plots are available from the
University of Wyoming's Department
of Meteorology. and from the University Center for Atmospheric
Research RAP Real-Time
From Don Collins, Texas A&M University.
If you look closely at the lower right corner of the temperature
plot, you will notice a small increase of temperature with height above
San Diego. This is called an inversion.
Inversion in the atmosphere above San Diego, red curve. The air at
a height of one kilometer is more than 5° C warmer than the air
at the surface. There is also a much weaker, and shallower inversion
Inversions strongly influence atmospheric pollution. Inversions
inhibit vertical convection, trapping pollutants close to the surface.
Strong, persistent, inversions over urban areas lead to much greater
concentrations of pollutants in the urban air.
- Limit vertical mixing. This traps pollutants close to the ground.
- Limit cloud formation. This leads to more sunlight, which drives
chemical reactions in the polluted air.
- Limits precipitation. This increases the lifetime of the pollutants
in the atmosphere.
Inversions are common along west coasts of continents. There winds blowing
toward the equator (purple arrow in figure below left) cause water at
the ocean's surface to move away from the coast (red arrow). The water
is replaced by colder water upwelled from deeper in the ocean (blue arrow).
The cold water cools the lower kilometer of the atmosphere, producing
the inversion. Strong inversions are common along the California coast.
They are responsible for the warm, dry, cool climate of Los angeles,
San Francisco, and San Diego. They are also responsible for smog commonly
found in these cities, especially Los Angeles. For more, read at Applications
of Ekman Theory.
Inversions also occur above inland lakes and rivers on days when the
water is cooler than the air, and winds are weak, and in valleys at night
when colder air drains off surrounding hills.
Right: Sea-surface temperature along
the US west coast on 16-18 July 2006 measured by the Advanced High
Resolution Radiometer AVHRR on the NOAA polar-orbiting, meteorological
satellites. The cold (blue) areas are upwelled water caused by north
winds offshore of the coast. Click on the image for a zoom with color
From NOAA CoastWatch.
Left: Schematic diagram showing equatorward
winds along the California coast (purple arrow) push water offshore
(red arrow), leading to upwelling of colder water along the coast (blue
arrow) shown in the figure on the right above. The cold water not only
influences the atmosphere, but it also carries nutrients that increase
the productivity of the area. Click on the image for a zoom.
From Bay Nature: A
Moveable Feast: The Ups and Downs of Coastal Upwelling. Drawing
by Fiona Morris.
Many processes contribute to atmospheric pollution and trace gases. Click
on image for a zoom.
From US Strategic Plan for the Climate Change Science Program, Final
Report July 2003: Chapter
3 Atmospheric Composition.
The important sources of atmospheric pollution on a global or regional
- Automobiles. According to the U.S.
Environmental Protection Agency (EPA), driving a car is the single
most polluting thing that most of us do. Motor vehicles emit millions
of tons of pollutants into the air each year. In many urban areas,
motor vehicles are the single largest contributor to ground-level ozone,
a major component of smog.
The primary pollutants produced by automobiles are:
- Hydrocarbons. They come from the evaporation of fuel, especially
on hot days, leaking fluids, and during refueling at gas stations.
- Nitrogen oxides. Produced by high heat during the burning of
- Carbon monoxide. Produced by the incomplete burning of fuel.
Modern automobiles pollute much less than older models thanks to
emission controls including catalytic converters. But the number
of cars is so large, and they are driven so much, they are still
major sources of pollution.
- Urban activity. The world's population
is concentrated more and more in mega cities, with five urban areas
having more than 20 million people: Tokyo, Japan (34,997,000); Mexico
City (22,800,000); Seoul, South Korea (22,300,000); New York (21,900,000);
and São Paulo, Brazil (20,200,000). Urban air pollution is now
common in all large cities, worse on some days, better on others, but
Pollution in Mexico City by Pierre
Madl of Salzburg University Sound and Video Studio.
It is caused not only by emissions from cars, trucks, buses and lawnmowers
(operating a lawn mower for one hour produces as much pollution as
driving a car 100 miles), but also by fumes from drying paint, charcoal
fires (grills), and dry cleaners.
A huge traffic jam backs up the streets in Bangkok. High population
density in large urban areas leads to air pollution. Click on image
for a zoom.
Urban activity leads to photochemical smog in many areas such as Los
Angeles, Houston, Mexico City, and London, the archetype of a smoggy
city (The term smog was coined by Dr. Henry Antoine Des Voeux in 1905,
when he combined the words smoke and fog).
In London, the smoke came from the burning of coal to heat thousands
of houses. The London smog began in the middle ages, and extreme smog
events led to periodic attempts to reduce air pollution. The great
smog of 5-9 December 1952 killed more than 4,700 people during the
event, and led to an additional 8,000 deaths in the year following
the event. During the event, visibility was reduced to 20 m over an
area of 20 by 40 km (Boubel et al, 1994) and deaths reached 900 per
day. To ensure that such an event would never happen again, parliament
passed the UK Clean Air Act of 1956.
Photochemical smog is formed when sunlight acts on volatile carbon-based
molecules and nitrous oxides trapped below inversions above cities.
The sunlight powers chemical reaction that form harmful pollutants
such as tropospheric ozone, aldehydes, and peroxyacyl nitrates (PAN).
Here is an outline of some important chemical reactions leading to
The high temperature in automobile and diesel engines converts nitrogen
gas to nitrous oxide.
N2 + O2 -----> 2 NO (nitric oxide)
In the atmosphere, nitric oxide is converted to nitrogen dioxide NO2,
a brown gas which gives smog its characteristic color.
2 NO + O2 ------> 2 NO2
When nitrogen dioxide concentrations are high, sunlight leads to the
formation of ozone.
NO2 + sunlight ----------> NO + O
O + O2 ---------> O3.
NO2 + O2 + hydrocarbons + sunlight ----------> CH3CO-OO-NO2 (peroxyacetylnitrate).
Los Angeles smog on 29 January 2004. The top of the inversion layer
is easily seen against the backdrop of distant mountains. Hilltops
above the layer are visible at great distances, urban areas below the
layer are obscured. Click on image for a zoom.
Photo by Alan
Clements, Middlesbrough, England.
This is what the smog in Los Angeles looks like from the ground, a
thick brown or slightly orange haze with a strong smell of ozone. In
this scene, the inversion is below the top of the highest buildings.
The exhaust from more than a million cars driven in the morning rush
hour is trapped below this level. Click on image for a zoom.
From Larvalbug article Choking
- Agricultural burning
Crop burning, Alberta Canada. Click on image for a zoom.
Centre, Government of Alberta, Canada.
- Forest fires.
Wildfires and smoke on 23 October 2007 in southern California. The
fires burned 800 square miles, and area almost 2/3 the size of Rhode
Island. The smoke from the fires is clearly visible over the Pacific
ocean on the left of the image. Red spots mark the location of the
fires. Click on image for zoom.
From NASA California
Wildfires. Other similar images are at the NOAA site: Operational
Significant Event Imagery.
NOAA issues daily Fire
Products, including a map showing all forest fires in North America,
and information of Fire
- Industrial activity
Smelters, steel mills, oil refineries and chemical plants, paper mills,
manufacturing plants, and power plants, especially coal-fired plants
are the major sources. But even relatively clean industries such
as semiconductor fabrication plants, which make computer chips, also
contribute. Many of the worst polluters were in the format Soviet
Union. Fortunately, industrial emissions are being greatly reduced
as nations become richer.
V.I. Lenin Steel mill, Magnitogorsk, 1991. From Monroe
Gallery of Photography, photographed by Shepard Sherbell.
- Dust storms. Strong winds blowing across
desert regions lift dust high into the troposphere. The higher-level
winds then carry dust great distances. The Sahara, the Aral
Sea, and Mongolia are
Dust blown from the Sahara across the Atlantic on 24 July 2005. Dust
is colored yellow-brown in the image.
From NOAA Dust
Storm site. NASA has a catalog of images of dust
23 December, 2008