| GEO 125
Physical Geography
Composition of the Atmosphere
Uniform gases (also known as constant or nonvariable gases
because their amount in the modern atmosphere is fixed)
- Nitrogen (79% of all atmospheric gas molecules)
- Oxygen (20% of all atmospheric gas molecules)
- Other minor uniform gases include argon, helium, krypton
The Uniform gases play no role in affecting weather and
climate but are of extreme importance to the completion of natural cycles that sustain
life on the earth
Variable gases (also known as the nonconstant or nonuniform
gases because their amounts fluctuate over time and space) are derived from both natural
sources and are also present in the atmosphere as the result of pollution. They modify
both weather and climate and can impact human health and cause property damage
- Water vapor (measured as humidity; a key component in the
hydrologic cycle; and directly impacts humans in terms of sensible heat)
- Carbon monoxide (natural sources include volcanic eruptions,
associated with mobile sources of pollution; and number one atmospheric pollutant by
weight)
- Carbon dioxide (natural sources associated with volcanic
eruptions, decay of plants, and forest fires; as a pollutant associated with generation of
electricity, disposal of solid wastes by burning, and other industrial processes; carbon
dioxide is the major greenhouse gas and controls world temperatures
- Sulfur dioxide (naturally associated with volcanic eruptions
and wildfires in coniferous forests; as a pollutant is is associated with the burning of
fossil fuels; as a pollutant it causes the greatest impact on human health and is a key
contributor to acid rain)
- Nitrogen oxides (naturally associated with volcanic
eruptions; as a pollutant it is associated with certain industrial processes and as an
output from mobile sources of pollution; a prime component of photochemical smog)
- Ozone (a form of oxygen, can be formed by lightning or other
intense electrical discharges into the atmosphere or as a by-product from the emissions of
mobile sources of pollution; near the ground surface ozone is considered to be a primary
pollutant and is a prime component of photochemical smog)
- Chloroflurocarbons (CFCs) (manmade chemical that is used for
many purposes including, enters the atmosphere from several small sources, chemically
inert but will react with ultraviolet light, leading chemical associated with ozone
depletion; CFSs are also considered to be a greenhouse gas)
Particulate matter in the atmosphere (also known as
suspended solids) can be derived from both natural sources or associated with ar
pollution.
- Natural sources of particulate matter include the eruption of
composite volcanoes, forest fires, dust storms, ocean spray; plants, and meteor impacts
- Sources of particulate matter associate with atmospheric
pollution include heavy industry, burning (solid waste disposal, agricultural burning; or
home heating), exotic vegetation oil fires, and as result of nuclear winter
Importance of particulate matter in the atmosphere
- High amounts input into the atmosphere by volcanic eruptions
can cause short term cooling
- The hydrologic cycle could not be completed without
particulate matter in the atmosphere to act as condensation nuclei
- Increased levels of particulate matter in the atmosphere,
associated with either natural sources or as a result of pollution, have been associated
with increased levels of precipitation
- Scattering of light in the atmosphere by particulate matter
causes sky to be blue and sunrises and sunsets to be red or orange
- As a pollutant, particulate matter is the second most
important pollutant to impact human health
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