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Climate Change:
High Global Warming Potential Gases

What are the high GWP gases and where are they used?

The high global warming potential (GWP) gases include hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and sulfur hexafluoride (SF6). HFCs and PFCs are used as substitutes for the ozone-depleting chemicals that are now restricted under the Montreal Protocol of 1987. These gases are used in a wide range of manufacturing plants and consumer products such as:

  • Automobile air conditioners
  • Refrigerators
  • Propellants in certain consumer aerosol products, for example: aerosol paint, personal care products, tire inflators, party spray (foam strings), air horns
  • Spray foam insulation and other foams
  • Fire extinguishing
  • Tennis balls
  • Electric power transmission

Emissions of these chemicals are a result of human activities. They are released as a result of their direct use or unintentionally as an industrial byproduct.

2010 Greenhouse Gas Emissions
Source: US EPA 2012 Greenhouse Gas Inventory Report

High GWP gases make up a small portion of the total US greenhouse gas emissions. They are, however, very potent and long lived.

Number of Years Certain High GWP Gases Remain in the Atmosphere
Source: US EPA High GWP Gases and Climate Change, 2011

These gases are very stable in the atmosphere. They can remain there for many years. Therefore, concentrations and impacts of these gases in the atmosphere will increase as long as emissions of these gases continue.

Why be concerned about high global warming potential GWP gases?

Certain gases trap heat in the atmosphere and, as a result, have the potential to contribute to climate change by raising the temperature in the atmosphere. Carbon dioxide (CO2) is the best -known and most common global-warming gas. It has been assigned a “global warming potential” of 1. Other greenhouse gases are assigned a GWP relative to CO2. The chart below shows the assigned GWP of a few important greenhouse gases.

Global Warming Potentials Relative to CO2
Source: IPCC Fourth Assessment Report, Working Group I: The Physical Science Basis TS2.5 Net Global Radiative Forcing, Global Warming Potentials and Patterns of Forcing, 2007

Some gases have the potential to trap a much greater amount of heat in the atmosphere than CO2 does.  For example, PFC-116 can trap 12200 times more heat in the atmosphere than CO2 over a 100-year period. This means that relatively small amounts of these gases in the atmosphere have large impacts.

In 2007, the Minnesota Legislature passed into law the Next Generation Energy Act. The law specifies the development of a comprehensive plan to reduce Minnesota’s emissions of greenhouse gases.

A high GWP gas reporting statute was passed in May 2008 as part of the Energy Omnibus bill (Minn. Stat. § 216H.11).

High GWP Reporting Requirements

As a result of Minn. Stat. § 216H.11, Minnesota is taking a number of steps, including collecting information about certain high GWP gases and their uses.

For further information, contact Anne Claflin at 651-757-2277.

Where can I find more information about high GWP gases or climate change?

Last modified on June 11, 2013 15:42