We often hear about the "greenhouse effect" in the negative context of global warming -- it's why the glaciers are melting and climate patterns are undergoing dangerous shifts. But the greenhouse effect is not actually a bad thing in itself -- it's a crucial and positive part of Earth's energy balance. It's what allows Earth to stay warm enough for life to survive. Without it, Earth would feel something like Mars.
The process gets its name from the greenhouses that stay nice and warm for growing plants. This is basically the same process that keeps Earth nice and warm for sustaining life. One example of the greenhouse effect that most of us experience in everyday life is the warming of a car's interior when the vehicle is left out in the sun.
You've probably noticed that your car is always much hotter inside than the outside temperature if it's been sitting there for a while. The sun's rays enter through your car's windows. Some of the heat from the sun is absorbed by the seats, the dashboard and the carpeting and floor mats. When those objects release this heat, it doesn't all get out through the windows. Some is reflected back in -- the heat radiated by the seats is a different wavelength than the light of the sun that made it through the windows in the first place, and the window glass won't let as much of that wavelength through. So a certain amount of energy is going in, and less energy is going out. The result is a gradual increase in the temperature inside your car.
Earth's greenhouse effect keeps the planet much warmer than surrounding space. In this article, we'll find out how that happens and see what's involved in maintaining Earth's energy balance. We'll also see what has happened to throw that balance out of whack.
Using the car-in-the-sun example, we can look at Earth's atmosphere as a giant, spherical car window.
When the sun's rays hit the Earth's atmosphere and the surface of the Earth, approximately 70 percent of the energy stays on the planet, absorbed by land, oceans, plants and other things. The other 30 percent is reflected into space by clouds, snow fields and other reflective surfaces [source: NASA]. But even the 70 percent that gets through doesn't stay on Earth forever (otherwise the Earth would become a blazing fireball). The things around the planet that absorb the sun's heat eventually radiate a portion of that heat (radiation) back out at a different wavelength, like your car seats and dashboard do.
This absorption-radiation process keeps the Earth in radiative equilibrium: The sun's radiation continually strikes the Earth, warming it; the warm Earth emits some of that radiation back into space, cooling itself. The more solar radiation the Earth absorbs, the more radiation it releases.
Some of that released radiation makes it into space, and the rest of it ends up getting reflected back down to Earth when it hits certain things in the atmosphere, such as carbon dioxide, methane gas and water vapor -- the car windows. The heat that doesn't make it out through Earth's atmosphere keeps the planet warmer than it is in outer space, because more energy is coming in through the atmosphere than is going out. This is the greenhouse effect that keeps the Earth warm.
If there were no greenhouse effect on Earth, it would probably look a lot like Mars. Mars doesn't have a thick enough atmosphere to reflect much heat back to the planet, so it gets very cold there.
So the greenhouse effect is actually a good thing. And as with most good things, moderation is key. The reason we often associate the greenhouse effect with environmental damage is that since the Industrial Revolution, the greenhouse effect has fallen out of balance: Earth's atmosphere is trapping too much heat.
Trapping Too Much Heat
Scientists estimate that without an atmosphere, the surface of the Earth would be about 54 degrees Fahrenheit (30 degrees Celsius) cooler than it is now [source: NASA]. That would bring it to about 5 degrees F (-15 degrees C); for comparison, the surface of Mars comes in around -9.4 degrees F (-23 degrees C) [source: Elert].
In other words, without Earth's atmosphere and the greenhouse effect it provides, we'd be up a creek. But it turns out that an overactive greenhouse effect can result a similarly devastating outcome. With too many heat-absorbing greenhouse gases in the atmosphere, too much radiation gets trapped, causing the Earth to warm beyond its ideal temperature.
Basically, Earth is not able to expel enough heat to keep itself cool, resulting in what's become known as "global warming." It's the greenhouse effect gone wild.
The problem is mostly the increased concentration of carbon dioxide (CO2) in the atmosphere. CO2 (in addition to water vapor) is the most substantial greenhouse gas.
In Earth's natural state, CO2 levels are kept in balance mostly by the activity of plant life. But as humans started burning more and more CO2-releasing fossil fuels, levels have shifted out of balance. We're emitting too much CO2 for the plants to handle (especially with the added effects of deforestation). Before the Industrial Revolution in the late 1700s, the concentration of CO2 in the atmosphere was about 280 parts per million (ppm). In the mid-1900s, that number was 300 ppm, and at the start of the 21st century, we have levels around 360 ppm [source: NASA].
This increase has led to a 1.8 degrees F (1 degree C) increase in Earth's temperature -- which may not seem like a lot until you realize that scientists predict dire, irreversible global effects at a 2 degrees C temperature increase, including melting ice sheets, rising sea levels and accompanying flooding, extreme climate patterns and widespread destruction of wildlife habitat [source: Times].
In agreements like the Kyoto Protocol, the world has begun to take action to try to curb this increased greenhouse effect. It remains to be seen whether these efforts will succeed in averting disaster or will prove to be too little too late.
For more information on the greenhouse effect, global warming and related topics, look over the links on the next page.
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More Great Links
- Global Warming. NASA Earth Observatory.http://earthobservatory.nasa.gov/Experiments/PlanetEarthScience/GlobalWarming/GW.php
- Greenhouse Effect. HyperPhysics.http://hyperphysics.phy-astr.gsu.edu/hbase/thermo/grnhse.html
- Pearce, Fred. "Instant Expert: Climate Change." New Scientist. Sept. 1, 2006.http://www.newscientist.com/article/dn9903-instant-expert-climate-change.html