![]() ![]() In 2014, CO 2 accounted for about 80.9% of all U.S. Greenhouse Gas Emissions and Sinks: 1990–2014.Ĭarbon dioxide (CO 2) is the primary greenhouse gas emitted through human activities. Note: All emission estimates are from the Inventory of U.S. Gases with a higher GWP absorb more energy, per pound, than gases with a lower GWP, and thus contribute more to warming Earth. Some gases are more effective than others at making the planet warmer and "thickening the Earth's blanket."įor each greenhouse gas, a Global Warming Potential (GWP) has been calculated to reflect how long it remains in the atmosphere, on average, and how strongly it absorbs energy. How strongly do they impact global temperatures? All of these gases remain in the atmosphere long enough to become well mixed, meaning that the amount that is measured in the atmosphere is roughly the same all over the world, regardless of the source of the emissions. To learn more about the increasing concentrations of greenhouse gases in the atmosphere, visit the Causes of Climate Change and the Climate Change Indicators: Atmospheric Concentrations of Greenhouse Gases pages.Įach of these gases can remain in the atmosphere for different amounts of time, ranging from a few years to thousands of years. One part per million is equivalent to one drop of water diluted into about 13 gallons of liquid (roughly the fuel tank of a compact car). Greenhouse gas concentrations are measured in parts per million, parts per billion, and even parts per trillion. Larger emissions of greenhouse gases lead to higher concentrations in the atmosphere. How much of these gases are in the atmosphere?Ĭoncentration, or abundance, is the amount of a particular gas in the air. These gases are typically emitted in smaller quantities, but because they are potent greenhouse gases, they are sometimes referred to as High Global Warming Potential gases ("High GWP gases").Įach gas's effect on climate change depends on three main factors: Fluorinated gases are sometimes used as substitutes for stratospheric ozone-depleting substances (e.g., chlorofluorocarbons, hydrochlorofluorocarbons, and halons). Fluorinated gases: Hydrofluorocarbons, perfluorocarbons, sulfur hexafluoride, and nitrogen trifluoride are synthetic, powerful greenhouse gases that are emitted from a variety of industrial processes. ![]()
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