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Global-warming potential

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Title: Global-warming potential  
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Subject: Global warming, Infrared spectroscopy, Climate forcing, Greenhouse gas emissions, Climate change acronyms
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Global-warming potential

Global-warming potential (GWP) is a relative measure of how much heat a greenhouse gas traps in the atmosphere. It compares the amount of heat trapped by a certain mass of the gas in question to the amount of heat trapped by a similar mass of carbon dioxide. A GWP is calculated over a specific time interval, commonly 20, 100 or 500 years. GWP is expressed as a factor of carbon dioxide (whose GWP is standardized to 1). In the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, methane has a lifetime of 12.4 years and with climate-carbon feedbacks a global warming potential of 86 over 20 years and 34 over 100 years in response to emissions. User related choices such as the time horizon can greatly affect the numerical values obtained for carbon dioxide equivalents. For a change in time horizon from 20 to 100 years, the GWP for methane decreases by a factor of approximately 3.[1] The substances subject to restrictions under the Kyoto protocol either are rapidly increasing their concentrations in Earth's atmosphere or have a large GWP.

The GWP depends on the following factors:

Thus, a high GWP correlates with a large infrared absorption and a long atmospheric lifetime. The dependence of GWP on the wavelength of absorption is more complicated. Even if a gas absorbs radiation efficiently at a certain wavelength, this may not affect its GWP much if the atmosphere already absorbs most radiation at that wavelength. A gas has the most effect if it absorbs in a "window" of wavelengths where the atmosphere is fairly transparent. The dependence of GWP as a function of wavelength has been found empirically and published as a graph.[2]

Because the GWP of a greenhouse gas depends directly on its infrared spectrum, the use of infrared spectroscopy to study greenhouse gases is centrally important in the effort to understand the impact of human activities on global climate change.


  • Calculating the global-warming potential 1
    • Use in Kyoto Protocol 1.1
  • Global Temperature change Potential (GTP) 2
  • Importance of time horizon 3
  • Values 4
  • See also 5
  • References 6
  • External links 7

Calculating the global-warming potential

Just as radiative forcing provides a simplified means of comparing the various factors that are believed to influence the climate system to one another, global-warming potentials (GWPs) are one type of simplified index based upon radiative properties that can be used to estimate the potential future impacts of emissions of different gases upon the climate system in a relative sense. GWP is based on a number of factors, including the radiative efficiency (infrared-absorbing ability) of each gas relative to that of carbon dioxide, as well as the decay rate of each gas (the amount removed from the atmosphere over a given number of years) relative to that of carbon dioxide.[3]

The radiative forcing capacity (RF) is the amount of energy per unit area, per unit time, absorbed by the greenhouse gas, that would otherwise be lost to space. It can be expressed by the formula:

RF = \sum_{n=1}^{100} Abs_i * F_i / (path length * density)

where the subscript i represents an interval of 10 inverse centimeters. Absi represents the integrated infrared absorbance of the sample in that interval, and Fi represents the RF for that interval.

The Intergovernmental Panel on Climate Change (IPCC) provides the generally accepted values for GWP, which changed slightly between 1996 and 2001. An exact definition of how GWP is calculated is to be found in the IPCC's 2001 Third Assessment Report. The GWP is defined as the ratio of the time-integrated radiative forcing from the instantaneous release of 1 kg of a trace substance relative to that of 1 kg of a reference gas:

GWP \left(x\right) = \frac{\int_0^{TH} a_x \cdot \left[x(t)\right] dt} {\int_0^{TH} a_r \cdot \left[r(t)\right] dt}

where TH is the time horizon over which the calculation is considered; ax is the radiative efficiency due to a unit increase in atmospheric abundance of the substance (i.e., Wm−2 kg−1) and [x(t)] is the time-dependent decay in abundance of the substance following an instantaneous release of it at time t=0. The denominator contains the corresponding quantities for the reference gas (i.e. CO2). The radiative efficiencies ax and ar are not necessarily constant over time. While the absorption of infrared radiation by many greenhouse gases varies linearly with their abundance, a few important ones display non-linear behaviour for current and likely future abundances (e.g., CO2, CH4, and N2O). For those gases, the relative radiative forcing will depend upon abundance and hence upon the future scenario adopted.

Since all GWP calculations are a comparison to CO2 which is non-linear, all GWP values are affected. Assuming otherwise as is done above will lead to lower GWPs for other gases than a more detailed approach would. Clarifying this, while increasing CO2 has less and less effect on radiative absorption as ppm concentrations rise, more powerful greenhouse gases like methane and nitrous oxide have different thermal absorption frequencys to CO2 that are not filled up (saturated) as much as CO2, so rising ppms of these gases are far more significant.

Use in Kyoto Protocol

Under the Kyoto Protocol, the Conference of the Parties decided (decision 2/CP.3) that the values of GWP calculated for the IPCC Second Assessment Report are to be used for converting the various greenhouse gas emissions into comparable CO2 equivalents when computing overall sources and sinks.[4]

Global Temperature change Potential (GTP)

The Global Temperature change Potential is another way to quantify the ratio change from a substance relative to that of CO2, in global mean surface temperature, used for a specific time span.[5]

Importance of time horizon

Note that a substance's GWP depends on the timespan over which the potential is calculated. A gas which is quickly removed from the atmosphere may initially have a large effect but for longer time periods as it has been removed becomes less important. Thus methane has a potential of 34 over 100 years but 86 over 20 years; conversely sulfur hexafluoride has a GWP of 22,800 over 100 years but 16,300 over 20 years (IPCC TAR). The GWP value depends on how the gas concentration decays over time in the atmosphere. This is often not precisely known and hence the values should not be considered exact. For this reason when quoting a GWP it is important to give a reference to the calculation.

The GWP for a mixture of gases can not be determined from the GWP of the constituent gases by any form of simple linear addition.

Commonly, a time horizon of 100 years is used by regulators (e.g., the California Air Resources Board).


Carbon dioxide has a GWP of exactly 1 (since it is the baseline unit to which all other greenhouse gases are compared).

GWP values and lifetimes from 2013 IPCC AR5 p714
(with climate-carbon feedbacks) [6]
Lifetime (years) GWP time horizon
20 years
100 years
Methane 12.4 86 34
HFC-134a (hydrofluorocarbon) 13.4 3790 1550
CFC-11 (chlorofluorocarbon) 45.0 7020 5350
Nitrous oxide (N2O) 121.0 268 298
Carbon tetrafluoride (CF4) 50000 4950 7350
GWP values and lifetimes from 2007 IPCC AR4 p212 [7]
(2001 IPCC TAR [8] in parentheses)
Lifetime (years) GWP time horizon
20 years
100 years
500 years
Methane 12         (12) 72         (62) 25         (23) 7.6       (7)
Nitrous oxide 114       (114) 289       (275) 298       (296) 153       (156)
HFC-23 (hydrofluorocarbon) 270       (260) 12,000   (9400) 14,800   (12,000) 12,200   (10,000)
HFC-134a (hydrofluorocarbon) 14         (13.8) 3,830     (3,300) 1,430     (1,300) 435       (400)
Sulfur hexafluoride 3200     (3,200) 16,300   (15,100) 22,800   (22,200) 32,600   (32,400)

Although water vapour has a significant influence with regard to absorbing infrared radiation (which is the green house effect; see greenhouse gas), its GWP is not calculated. Its concentration in the atmosphere mainly depends on air temperature. There is no possibility to directly influence atmospheric water vapour concentration.

The values given in the table assume the same mass of compound is released. This must not be confused with chemical reactions in which masses change from reactants to products. For instance, burning methane to carbon dioxide would indeed reduce the global warming impact, but by a smaller factor than the one given in the table because the mass of methane burning is lesser than the mass of carbon dioxide released (ratio 1:2.75).[9] If you started with 1 tonne of methane which has a GWP of 25, after combustion you have 2.75 tonnes of CO2, each tonne of which has a GWP of 1. The effect of this burning is to reduce the Global warming effect of the gas released in the ratio 25:2.75 or by about 9. Similarly, for each tonne of methane burned to CO2, the release of tonne CO2 equivalent is reduced by 25 – 2.75 = 22.25.

The global warming potential of perfluorotributylamine (PFTBA) over a 100 year time horizon has been estimated to be approximately 7100.[10] It has been used by the electrical industry since the mid-20th century for electronic testing and as a heat transfer agent.[11] PFTBA has the highest radiative efficiency (relative effectiveness of greenhouse gases to restrict long-wave radiation from escaping back into space[12]) of any molecule detected in the atmosphere to date.[13] The researchers found an average of 0.18 parts per trillion of PFTBA in Toronto air samples, whereas carbon dioxide exists around 400 parts per million.[14]

See also


  1. ^ "Climate Change 2013: The Physical Science Basis". IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Ch.8, p. 711-714, Table 8.7.. 2013. Retrieved 2014-02-13. 
  2. ^ Matthew Elrod, "Greenhouse Warming Potential Model." Based on Elrod, M. J. (1999). "Greenhouse Warming Potentials from the Infrared Spectroscopy of Atmospheric Gases". Journal of Chemical Education 76 (12): 1702.  
  3. ^ "Glossary: Global warming potential (GWP)". U.S. Energy Information Administration. Retrieved 2011-04-26. An index used to compare the relative radiative forcing of different gases without directly calculating the changes in atmospheric concentrations. GWPs are calculated as the ratio of the radiative forcing that would result from the emission of one kilogram of a greenhouse gas to that from the emission of one kilogram of carbon dioxide over a fixed period of time, such as 100 years. 
  4. ^ Conference of the Parties (25 March 1998). "Methodological issues related to the Kyoto Protocol". Report of the Conference of the Parties on its third session, held at Kyoto from 1 to 11 December 1997 Addendum Part Two: Action taken by the Conference of the Parties at its third session.  
  5. ^ "IPCC AR5 - Anthropogenic and Natural Radiative Forcing (Chapter 8 / page 663)". 2013. 
  6. ^ Myhre, G., D. Shindell, F.-M. Bréon, W. Collins, J. Fuglestvedt, J. Huang, D. Koch, J.-F. Lamarque, D. Lee, B. Mendoza, T. Nakajima, A. Robock, G. Stephens, T. Takemura and H. Zhang (2013) "Anthropogenic and Natural Radiative Forcing". In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.). Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Anthropogenic and Natural Radiative Forcing
  7. ^ Forster, P., V. Ramaswamy, P. Artaxo, T. Berntsen, R. Betts, D.W. Fahey, J. Haywood, J. Lean, D.C. Lowe, G. Myhre, J. Nganga, R. Prinn, G. Raga, M. Schulz and R. Van Dorland (2007) "Changes in Atmospheric Constituents and in Radiative Forcing". In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M.Tignor and H.L. Miller (eds.). Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
  8. ^ "6.12.2 Direct GWPs" in IPCC Third Assessment Report – Climate Change 2001. GRID-Arendal (2003)
  9. ^ This is so, because of the reaction formula: CH4 + 2O2 → CO2 + 2 H2O. As mentioned in the article, the oxygen and water is not considered for GWP purposes, and one molecule of methane (molar mass = 16.04 g mol−1) will yield one molecule of carbon dioxide (molar mass = 44.01 g mol−1. This give a mass ratio of 2.74. (44.01/16.04≈2.74).
  10. ^ Hong, Angela C.; Cora J. Young; Michael D. Hurley; Timothy J. Wallington; Scott A. Mabury (28 November 2013). "Perfluorotributylamine: A novel long-lived greenhouse gas". Geophysical Research Letters 40 (22): 6010–6015.  
  11. ^ New Greenhouse Gas Discovered, PFTBA Has Higher Global Warming Impact Than CO2. (2013-12-10). Retrieved on 2014-04-23.
  12. ^ Radiative efficiency definition of Radiative efficiency in the Free Online Encyclopedia. Retrieved on 2014-04-23.
  13. ^ Newly discovered greenhouse gas '7,000 times more powerful than CO2' | Environment. 10 December 2013.
  14. ^ New greenhouse gas discovered by U of T chemists | Toronto Star. (2013-12-11). Retrieved on 2014-04-23.

External links

  • 2007 IPCC Fourth Assessment Report (AR4) by Working Group 1 (WG1) and Chapter 2 of that report (Changes in Atmospheric Constituents and in Radiative Forcing) which contains GWP information.
  • 2001 IPCC Third Assessment Report (TAR) page on Global-Warming Potentials and Direct GWP.
  • List of Global Warming Potentials and Atmospheric Lifetimes from the U.S. EPA
  • O as a greenhouse gas2An overview of the role of H from RealClimate
  • e explained2GWP and the different meanings of CO
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