All abuzz about methane [updated]



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 COthat 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.


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), 24 November 2013. Figure below is from Professor Kyle Forinash of the Physics Department, Indiana University Southeast.)




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.

About ecoquant

See Retired data scientist and statistician. Now working projects in quantitative ecology and, specifically, phenology of Bryophyta and technical methods for their study.
This entry was posted in climate, climate education, consumption, demand-side solutions, ecology, engineering, environment, forecasting, geophysics, meteorology, methane, physics, rationality, risk, science and tagged , . Bookmark the permalink.

2 Responses to All abuzz about methane [updated]

  1. Pingback: Losing sight of the big picture | 667 per centimeter : climate science, quantitative biology, statistics, and energy policy

  2. alanyshapiro says:

    That said, it still helps to know how much we’re actually emitting:

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