- Index
- Background and Basics
- Climate Variability
- Climate Change

Greenhouse gases are gases that absorb energy emitted from the earth and radiate it back into the atmosphere. If there are too many greenhouse gases, the earth could become too warm. If greenhouse gases dramatically decrease, the earth may be too cool for human activities, such as farming, planting, and harvesting, to occur.
Why do I care? A certain amount of greenhouse gases is essential to life on earth. However, human activities are affecting the levels of these gases in the atmosphere, which are in turn affecting the climate we have adapted to.
| Figure A: Carbon Dioxide, a Greenhouse Gas Which Absorbs and Emits Infrared Radiation |
| http://www.windows.ucar.edu/earth/climate/images/carbon.gif |
Greenhouse gases are the gases that absorb long-wave energy and emit it back into our atmosphere. They are responsible for keeping the earth warm enough to live on. Most of these gases are present in the atmosphere naturally. However, anthropogenic (manmade) processes are dramatically increasing the concentration of these gases. This is one of the main reasons we think our earth is experiencing warming and climate changes.
Concentrations of greenhouse gases are commonly given in percentages as well as mixing ratios of gases to total air volume, such as ppt, ppb, and ppm. The percentages are the percentage of the atmosphere made up by these gases. Since the percentages are very small, most of the time concentrations are referred to in parts per trillion (ppt), parts per billion (ppb) or parts per million (ppm). This means that for every trillion, billion or million molecules, the number given is the amount of molecules that are composed of that gas per trillion air molecules, etc. For example, as of 2009, our atmosphere currently contains a CO2 concentration of 385ppm; for every million molecules, about 385 of them are carbon dioxide.
In the linked pages, you should also keep in mind that a fossil fuel is any hydrogen and carbon rich substance that was created by the decomposition of prehistoric plants and animals that can be burned to produce heat or energy. This includes coal, petroleum, and natural gas products.
Want to learn more? Carbon Dioxide, Methane, Nitrous Oxide, Ozone, Water Vapor, Halocarbons, Ozone Layer
Activity: Ground-level Ozone: Your Vehicle (You will be re-directed to a pdf version of an activity shared by the owners of the site.)
Description: This activity will assist students in understanding the role of vehicles on greenhouse gas levels. Students will use their vehicle or their parent's vehicle to calculate the emissions levels for nitrogen oxides and hydrocarbons and compare the values to a hybrid vehicle.
All modules using this activity: Greenhouse Gases, Ozone Layer, Causes of Climate Change
Activity: Human Activity and Climate Change (You will be re-directed to the UCAR website to an activity shared by the owners of the site.)
Description: This activity focuses on the increase in greenhouse gas emissions associated with human activity. Students will observe changes in greenhouse gases through graphs and will also calculate their contribution to greenhouse gas levels.
All modules using this activity: Greenhouse Gases
Activity: Trees and Carbon (You will be re-directed to a pdf version of an activity shared by the owners of the site.)
Description: This activity will assist students in understanding the importance of forests on the carbon dioxide level and the amount of carbon that the trees are able to store.
All modules using this activity: Greenhouse Effect, Greenhouse Gases, Global Warming vs. Climate Change
Activity: What is a Greenhouse? (You will be re-directed to the UCAR website to an activity shared by the owners of the site.)
Description: This activity focuses on how a greenhouse retains heat. Students will build a greenhouse model to explain this process.
All modules using this activity: Longwave & Shortwave Radiation, Greenhouse Effect, Greenhouse Gases, Ozone, Nitrous Oxide, Carbon Dioxide, Methane, Water Vapor, Halocarbons
Last modified date: Monday, June 25, 2012 - 12:38pm