Carbon and carbon dioxide

Carbon
Carbon (C) is a chemical element that is found in many forms as an energy source for building things such as:
our bodies (18% of a person) – in our DNA, muscles, bones and more
the atmosphere – as CO₂
rocks, soils and the Earth’s crust
fossil fuels – for example, petrol and diesel
oceans
animals
plants
buildings
the atmosphere.
In the atmosphere, carbon can be found as carbon dioxide (CO2), carbon monoxide (CO) and methane (CH4).
Carbon dioxide
Carbon dioxide, also called CO2 (pronounced see-oh-two), is the most important of the greenhouse gases as it is emitted in large quantities and has a long-lasting influence.
CO2 stays in the atmosphere for thousands of years (also known as the atmospheric lifetime). This is one of the reasons why it builds up in the atmosphere and why we must reduce emissions.
Other greenhouse gases have shorter lifetimes or much smaller concentrations in the atmosphere. For example, 0.04% of the atmosphere is CO2, while methane accounts for 0.00003%. Even such small quantities are enough to trap lots of heat.
Carbon dioxide in the atmosphere is part of the carbon cycle. Carbon moves around the Earth between these different forms through the carbon cycle. The carbon cycle is the movement of carbon in the form of CO2 into and out of the atmosphere.
Global warming potential
Global warming potential (GWP) is a way to compare how much heat a greenhouse gas can trap in the atmosphere over a period of time. It helps us compare the different greenhouse gases.
Related articles
Related activities
Related media
Carbon cycle – interactive
SLH and the carbon cycle – webinar
Useful links
How carbon affects nearly everything on Earth – including our future – video by Smithsonian’s National Museum of Natural History
The carbon cycle is key to understanding climate change – video, The Economist
Overview of greenhouse gases – resource, US Environmental Protection Agency
The greenhouse effect – video, US Environmental Protection Agency