Greenhouse Effect

Greenhouse gases have always been present in our atmosphere

Greenhouse gases are a group of atmospheric gases that naturally occur in our atmosphere, like water vapor, carbon dioxide, methane, and others. Nitrogen and oxygen by themselves make up 99% of all gases in earth’s atmosphere. Other gases are also present in very tiny amounts. Since the 1800s, we've known that some of those gases absorb and release energy. 

We call them greenhouse gases, and it's the changing amounts of those gases in the air that brings concern on their impact on climate.

The Natural Greenhouse Effect

As energy is given off by the earth, it is giving off long wavelengths of energy; most in the infrared category. A small range of these wavelengths can be absorbed by greenhouse gases. Once absorbed, the energy is given back off very quickly; however, the released energy goes off in all directions, like a tiny and much cooler sun.

  • Some goes back to earth’s surface to be given off again. 
  • If it goes in other directions, it may be absorbed by another greenhouse gas molecule. 
  • The overall effect of this is to slightly slow the release of energy to space, making the lower atmosphere slightly warmer than it would be if no greenhouse gases were present. 

Earths average temperature is about 57 degrees Fahrenheit. With no greenhouse gases, the earth's average temperature would be around 0 degrees F.

Human activity impacts the natural process, slowing the release and warming earth

There are many natural sources of these gases in the earth’s atmosphere and natural processes through which the earth’s surface and the atmosphere exchange these gases, like volcanic eruptions. But some greenhouse gases, like carbon dioxide, are also a byproduct of fossil fuel combustion. That means that when we drive our gas vehicles or use electricity derived from fossil fuel sources (coal, oil, etc.), we are contributing additional carbon dioxide, a greenhouse gas, to the atmosphere.  As a result of human activity, the atmospheric concentration of carbon dioxide has increased from the pre-industrial value of around 285 parts per million to the current concentration of around 425 ppm. 

The increased concentration of greenhouse gases in the atmosphere enhances the natural effect that was already there. As more greenhouse gases are present, it takes longer for the heat to escape. The earth near the surface becomes warmer as a result. It is a physical cause and the resulting effect.

At the global scale, near-surface air temperature has increased by more than 1°C (1.8°F) since the late 19th century. This may seem like a trivial amount of warming, but the impacts of 1°C are already widespread and cause a cascade effect beyond temperature. For example, warming also affects precipitation intensity (more extreme), changes in rain/snow distributions, and how long precipitation is on the surface before melting or evaporating. Increasing the temperature also leads to a loss of ice/snow on land and the expansion of ocean water, which are the largest contributors to the rise of global sea levels. 

Explaining the Greenhouse Effect

Most people have heard about the Greenhouse Effect, but many would not feel comfortable explaining the science behind it. This University of Illinois Extension webinar discusses, in simple terms, the basic scientific processes that make the greenhouse effect occur and will explain the natural...

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Energy and greenhouse gases

Energy sources such as coal, petroleum, and natural gas are all fossil fuels. They are located beneath the Earth's surface and emit significant amounts of carbon dioxide into the atmosphere when used as fuel. Carbon dioxide is a greenhouse gas that traps heat in our atmosphere, much like how a garden greenhouse retains heat. Greenhouse gases are necessary to keep the planet warm, but an excess of them can lead to continued heat-trapping and rising temperatures on Earth.

 These sources of energy are non-renewable.  Once they are consumed, we cannot use them again. In the U.S., about 88% of our energy comes from non-renewable sources. 

Renewable energy 

Renewable energy - biomass, wind, hydropower, solar, and geothermal - has great potential to reduce greenhouse gases, slow rising temperatures, and still support human energy needs. Utilizing available natural resources provides us with clean energy. These sources do not produce greenhouse gases, pollution, smoke, or clouds that would otherwise lead to reduced air quality.  

Two main renewable sources in Illinois are wind and solar. 

Wind turbines: The natural energy of moving air turns the turbine blades, and the generator converts the mechanical energy into electrical energy. Windmills should be established in a location with an average wind speed of at least 9 mph for a small turbine, and 13 mph for a utility-scale turbine. 

Solar energy: By using photovoltaic cells, photons in light hit the solar panel and knock electrons free. The electrons moving around create electricity, and the electric current flows through the inverter, changing it from direct current (DC) to alternating current (AC), which we can use on the grid or directly connected to your home.   

Blog: Renewable energy offers benefits for our future