All abuzz about methane [updated]

shakhov-2013-methane-release-smaller

 

RealClimate tours the methane landscape, that greenhouse gas of renown, as a result of a number of recent papers describing increased release rates. Methane should be considered in context, and the risk it poses to additional warming tempered with realization that:

  • While a physically powerful greenhouse gas, it does not have corresponding Earth blackbody radiation to absorb, and its absorption lines are narrow, at least compared to carbon dioxide and water (see chart below).
  • The rate of increase of methane, even with these findings, is relatively small.
  • It’s atmospheric lifetime (“residence time”, per ) is short, a 10 year lifetime, in contrast with carbon dioxide which has a 40% residence time of centuries, and a 20% atmospheric residence time of over 1000 years.
  • When methane decays in atmosphere, it decays into carbon dioxide. 

To quote Professor David Archer’s summary from an earlier RealClimate post:

Could methane be a point of no return?

Actually, releasing CO2 is a point of no return if anything is. The only way back to a natural climate in anything like our lifetimes would be to anthropogenically extract CO2 from the atmosphere. The CO2 that has been absorbed into the oceans would degas back to the atmosphere to some extent, so we’d have to clean that up too. And if hydrates or peats contributed some extra carbon into the mix, that would also have to be part of the bargain, like paying interest on a loan.

Conclusion

It’s the CO2, friend.

(Figure credit above is from N Shakhova, I. Semiletov, I. Leifer, V. Sergienko, A. Salyuk, D. Kosmach, D. Chernykh, C. Stubbs, D. Nicolsky, V. Tumskoy, Ö. Gustafsson, “Ebullition and storm-induced methane release from the East Siberian Arctic Shelf”, Nature Geoscience (2013) http://dx.doi.org/10.1038/ngeo2007, 24 November 2013. Figure below is from Professor Kyle Forinash of the Physics Department, Indiana University Southeast.)

GHGabsorption

 

 

Addendum, Saturday, 28th June 2014

Professor Ray Pierrehumbert has taken a close look at the option of reducing other greenhouse gases besides carbon dioxide in order to mitigate climate change. There is some suggestion that reducing these may have a significant impact, and doing so may not have the same political opposition that going after CO2 does. Nope. Quoting the above, but embellishing:

It’s STILL the CO2, friend.

Responses

  1. […] I’ve blogged about Methane before, quoting some of the same sources. Professor Pierrehumbert has a more detailed technical review article presenting the arguments why the focus should and must be Carbon Dioxide, as politically and economically difficult as that might seem (**). And he keeps trying to make that point. […]

  2. That said, it still helps to know how much we’re actually emitting: http://www.scientificamerican.com/article.cfm?id=us-methane-emissions-prove-higher&WT.mc_id=SA_DD_20131127

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About the author

Sophia Bennett is an art historian and freelance writer with a passion for exploring the intersections between nature, symbolism, and artistic expression. With a background in Renaissance and modern art, Sophia enjoys uncovering the hidden meanings behind iconic works and sharing her insights with art lovers of all levels. When she’s not visiting museums or researching the latest trends in contemporary art, you can find her hiking in the countryside, always chasing the next rainbow.