Atmospheric Composition
The Earth's atmosphere is mostly
made up of nitrogen and oxygen. In fact, these two gases
contribute to about 99% of the total atmospheric composition.
The trace gases such as methane, carbon dioxide, and even
water vapor make up the remaining 1%. This last 1% contributes
heavily to the warming of our atmosphere, and this will
be discussed later on in the Greenhouse Gases section. In
this section though, one can find out about our atmospheric
composition and the layers of the atmosphere. Once finished
with this section, one should be able to differentiate between
the troposphere and the stratosphere, and one should be
able to list off the major constituents of our atmosphere.
To get started on the research, please click on one of the
links below and good luck!
1. Atmospheric
Composition
2. Layers
of the Atmosphere
Greenhouse Gases
When one hears someone talk about
the greenhouse effect, or global warming, it is often associated
with negativity. However, it is because of these processes
that there exists life on Earth. Examples of greenhouse
gases are carbon dioxide and methane. These gases are produced
naturally in our atmosphere and they help by raising Earth's
average temperature about 40 degrees. The occurs due to
a process called the greenhouse effect. Greenhouse gases
are floating around in the atmosphere, and when uv rays
from the Sun collide with these gas particles, most of the
uv is absorbed. This absorption traps the heat inside our
atmosphere, causing it to heat up! However, within the past
100 years, man has contributed to this heating-up process
by introducing more and more greenhouse gases into the atmosphere
via automobiles, factories, and other mechanical devices.
Thus, global warming is the concern that Earth's temperature
will continue to rise along with the numbers of these certain
gases in our atmosphere. Click on the links below to find
out more about these greenhouse gases.
1. The
Greenhouse Effect
2. NASA
Research: Greenhouse Gases
Atmospheric Aerosols
Aerosols are the miniscule particles floating
freely about the atmosphere at any given time. These can
be produced from volcanic eruptions, vehicular emissions,
or even wildfires. In fact, human activity accounts for
10% of the aerosols in the atmosphere. Because of our atmospheric
air currents, these particles have the ability of traveling
across the globe in a very short time, and remaining in
the atmosphere for months on end. The computer animation
below on Mt. Pinatubo's eruption in 1991 shows how dust
and ash, released in one spot on the globe, can affect the
entire Earth. In fact, in the months following the Mt. Pinatubo
eruption, the Earth's average temperature dropped by half
a degree! So, it can be seen that these aerosol particles
have an overall cooling effect on our climate. When the
uv radiation from the Sun enters the atmosphere, some is
reflected away from the Earth's surface by these free-floating
aerosols. Thus, less uv radiation actually hits the surface
of the Earth. Some scientists seem to believe that the aerosols
in the atmosphere could balance out the warming effects
caused by the increase in greenhouse gases.
-Mt.
Pinatubo animation-
1. What
are Aerosols?
2. Aerosols
and Climate
Intercontinental
Transport
One of the main focuses
of the INTEX mission will be to determine the chemical transport
on intercontinental scales. Evidence has shown that chemicals
from East-Asian countries have migrated over to the west
coast of the United States. As seen in the Mt. Pinatubo
demonstration video, our atmosphere is capable of circulating
matter around the globe in extremely short periods of time.
INTEX will strive to quantify this outflow of chemicals
from Asia to the United States, as well as from the United
States to Europe. The main concern is on those chemicals
that are particulary long-lived in the atmosphere. These
pose the greatest threat to long-term climate change, as
they can stay airborne for longer periods of time. Find
out more from the links below.
1. NOAA
Intercontinental Transport
2. Transport
of Nitrogen Oxide Pollution
K-6
Education | Sr High Education|
Games and Activities | Teacher
Resources | Ask a Scientist
| Outreach Home
Web
Creator: Stewart McIlvena
Website Administrator Dan Chirica
NASA Privacy Policy and Important Notices
Last modified on: June 18, 2003