Methane global warming potential

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SUMMARY

Methane (CH4) exhibits a higher Global Warming Potential (GWP) than carbon dioxide (CO2) over a 100-year period due to its ability to absorb more long-wave radiation on a molecule-per-molecule basis. Key studies, including Prather et al. (2001) and Ramaswamy et al. (2001), identify four indirect radiative effects of CH4 emissions, which enhance its atmospheric lifetime despite its shorter lifespan of approximately 12 years. The unique chemical bonds of methane contribute to its significant impact on climate change, particularly in less saturated parts of the infrared spectrum.

PREREQUISITES
  • Understanding of Global Warming Potential (GWP)
  • Familiarity with infrared radiation absorption
  • Knowledge of atmospheric chemistry, specifically methane and carbon dioxide
  • Awareness of the indirect radiative effects of greenhouse gases
NEXT STEPS
  • Research the indirect radiative effects of methane emissions as outlined in Prather et al. (2001) and Ramaswamy et al. (2001)
  • Study the infrared absorption characteristics of greenhouse gases, focusing on methane and carbon dioxide
  • Examine the role of hydroxyl (OH) concentration in methane's atmospheric lifetime
  • Explore the implications of methane's GWP in climate policy and mitigation strategies
USEFUL FOR

Climate scientists, environmental policy makers, and anyone involved in greenhouse gas emissions research will benefit from understanding the complexities of methane's impact on global warming.

Charles123
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I understand that CH4 absorbs more long-wave radiation, on a molecule-per-molecule basis, than CO2. I also understand that "four indirect radiative effects of CH4 emissions have been identified (see Prather et al., 2001; Ramaswamy et al., 2001). Methane enhances its own lifetime through changes in the OH concentration: it leads to changes in tropospheric ozone, enhances stratospheric water vapour levels, and produces CO2" (http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch2s2-10-3.html). All this combined leads to CH4 being defined as having a higher Global Warming Potential than CO2 over 100 years, even with a much lower atmospheric lifetime (around 12 years).
Looking only to the fact that methane absorbs more long-wave radiation, this has to do with the characteristics of the two molecules (methane and carbon dioxide), particularly its chemical bounds. But, looking at the absorptivity of both molecules at different frequencies and the of Earth emitted long wave radiation intensity also at different frequencies is quite difficult to see this. Check the figures in the following links for example:
http://www.meteor.iastate.edu/gccourse/forcing/images/image7.gif
http://www.theresilientearth.com/?q=content/why-i-am-global-warming-skeptic
Although the second figure does not show methane, N2O could indicate approximately the methane behavior.
Can you please help me understand why this figures apparently don’t show what I said in the first paragraph?
Thank you
Best regards
 
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I believe the main reason methane is such a threat is that the parts of the IR spectrum it blocks are not nearly as saturated, so a small increase in gas has a large effect. See e.g. http://zebu.uoregon.edu/2004/es399/lec02.html
 
This is one of our banned topics.

Zz.
 

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