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Hi Andrew, You say: "I don't oppose John's argument, but the evidence on the severity of the problem is far from conclusive." I disagree. The methane presents a very real risk - because of the uncertainty on timing combined with the potential size of methane discharge - perhaps even enough to cause thermal runaway due to positive feedback, as is thought to have happened in the past [1]. Risk management involves identifying events and assessing them in terms of their likelihood and magnitude of impact [2]. Thus something with a small likelihood (such as rapid massive methane excursion) can have a high risk, if the magnitude of impact is sufficiently large (and you can't get much larger than thermal runaway). It is possible that much or most of the methane trapped in frozen structures has built up over hundreds of thousands of years. There is little sign of massive methane discharge in the ice record. In fact methane seems to track the temperature even better than CO2 [3]. But of course methane discharge is not the only high risk event - there is also the Greenland ice sheet disintegration. BTW, does anybody know the _immediate_ warming potential of methane, as opposed to the 20 year value (72), 100 years (25) or 500 years (7.6)? The lifetime is only 12 +/- 3 years. See [4]. Cheers, John [1] http://en.wikipedia.org/wiki/Clathrate_gun_hypothesis [2] http://en.wikipedia.org/wiki/Enterprise_risk_management [3] http://answers.yahoo.com/question/index?qid=20090329215018AAxqYFk [4] http://en.wikipedia.org/wiki/Greenhouse_gas --- Andrew Lockley wrote: At present the likely methane excursion is far from clear. Further, it is also unclear how quickly the total excursion will occur. The excursion rate is highly significant due to the short life of methane in the atmosphere. The methane ends up as CO2, in itself a major issue. However, the CO2's likely effect is nothing compared to the devastating temperature spike which may result from a sudden methane excursion. -- You received this message because you are subscribed to the Google Groups "geoengineering" group.To post to this group, send email to [email protected]. To unsubscribe from this group, send email to [email protected]. For more options, visit this group at http://groups.google.com/group/geoengineering?hl=. |
- [geo] Re: Rejected - a simple argument for SRM geoengin... jim woolridge
- Re: [geo] Re: Rejected - a simple argument for SRM... Andrew Lockley
- RE: [geo] Re: Rejected - a simple argument for... Eugene I. Gordon
- Re: [geo] Re: Rejected - a simple argument... Andrew Lockley
- Re: [geo] Re: Rejected - a simple argu... Sam Carana
- [geo] H2 in the atmosphere Oliver Wingenter
- [geo] Re: H2 in the atmospher... Sam Carana
- RE: [geo] Re: H2 in the atmos... Veli Albert Kallio
- Re: [geo] Re: H2 in the atmos... John Gorman
- RE: [geo] Re: H2 in the atmos... Veli Albert Kallio
- Re: [geo] Re: Rejected - a simple argument for... John Nissen
- Re: [geo] Re: Rejected - a simple argument... John Nissen
- Re: [geo] Re: Rejected - a simple argument... Sam Carana
- Re: [geo] Re: Rejected - a simple argument... Peter Read
- Re: [geo] Re: Rejected - a simple argu... Mike MacCracken
- RE: [geo] Re: Rejected - a simple... Eugene I. Gordon
- Re: [geo] Re: Rejected - a simple... John Nissen
- Re: [geo] Re: Rejected - a simple... Greg Rau
- Re: [geo] Re: Rejected - a si... Mike MacCracken
- Re: [geo] Re: Rejected - a si... Greg Rau
- RE: [geo] Re: Rejected - a si... David Keith
