I don't know anything about methanotrophs.  I'll post this link here
http://www.google.com/url?sa=t&source=web&ct=res&cd=3&url=http%3A%2F%2Fmmbr.asm.org%2Fcgi%2Freprint%2F60%2F2%2F439.pdf&ei=YrKLSdCPDcH7tgfl882nBw&usg=AFQjCNGGbGLR6Fkk-fVrQSFAL19J44vYvw&sig2=fP6aqTs9vBrRuTi1KxcIAA
partly to remind myself to look at it again later.  Mass culture of
facultative methanotrophs sounds promising at first glance.

On Feb 5, 9:30 am, "John Nissen" <[email protected]> wrote:
> Dear Andrew,
>
> That is very unfair - a stab in the back.  
>
> 1.  I have given you several references to methane in the past, e.g. from 
> David Lawrence.  And there are plenty of references already in wikipedia, 
> e.g. here:http://en.wikipedia.org/wiki/Arctic_methane_release
> (I am sorry I can't help on the shoreline slumping.)
>
> 2.  I am trying to answer your basic question:  Is there REALLY a big and 
> immediate risk from the clathrate gun/permafrost?   You seemed to be arguing 
> only about the methane, without taking into account the Arctic sea ice albedo 
> effect.  
>
> 3.  The argument that the Arctic sea ice albedo effect is causing regional 
> runaway feedback is new to this list.  The argument that we should reverse 
> the Arctic sea ice retreat is also new - previously I had argued we simply 
> had to halt the retreat.
>
> 4.  These are common sense arguments.  If anybody can find some evidence to 
> dispute them, may they come forth.
>
> 5.  I have given my own conclusion repeatedly, because it bares repeating:
>
> If we do not act quickly with our SRM geoengineering, then thermal runaway 
> from methane (and also disasterous sea level rise) could become inevitable.  
>
> 6.  Your criticism is a stab in the back, because you seemed to be one of the 
> few people who accepted this conclusion, because of all the evidence I gave 
> you.
>
> Et tu, Brute.
>
> John.
>
>   ----- Original Message -----
>   From: Andrew Lockley
>   To: John Nissen
>
>   Cc: Geoengineering FIPC ; Prof John Shepherd ; John Gorman
>   Sent: Thursday, February 05, 2009 1:12 PM
>   Subject: Re: [geo] runaway arguments ripped to bits
>
>   John,
>   You've repeated these arguments on this list on numerous occasions.  
> However, you've failed to back them up with peer-reviewed science.
>
>   I've already emailed the list asking for scientific support for these very 
> ideas in the last 24hrs.  Specifically we need help with the alterations to 
> methane GWP, the decay rate of clathrates due to shoreline slumping in the 
> Arctic and calculations of the overall warming load arising from a methane 
> pulse.
>
>   I hope you can assist with the search for solid backing for your case and 
> not re-iterate oft-rehearsed arguments.
>
>   The relevant wiki is actually 
> athttp://en.wikipedia.org/wiki/Runaway_climate_change#Current_risk
>
>   A
>
>   2009/2/5 John Nissen <[email protected]>
>
>     The term "runaway" has an accepted meaning in the context of "thermal 
> runaway", and is characterised by positive feedback and resulting 
> acceleration in temperature change.  So the temperature rises more than 
> linearly, and may even rise exponentially or "explosively":
>    http://en.wikipedia.org/wiki/Thermal_runaway
>     Eventually the feedback peters out, and the temperature change becomes 
> linear again.  
>
>     This process is happening with the Arctic sea ice.  At present the albedo 
> feedback effect is causing an acceleration in temperature change in the polar 
> region - but this positive feedback will eventually peter out, when all the 
> ice and snow in the region has melted, including the Greenland ice sheet!  So 
> we are facing thermal runaway on a regional scale, affecting local climate 
> and ecosystem.  This will have a domino effect on methane release.
>
>     As the Arctic region warms, methane will invitably be released in larger 
> and larger quantities.  The speed of methane release depends critically on 
> the temperature above the frozen structure holding the methane.  For 
> permafrost on land, if the average surface temperature is maintained above 
> freezing, the permafrost will inevitably melt.  This is what is happening 
> over vast areas of Canada and Siberia, as the isotherms (lines of equal 
> temperature on a map) move northwards.
>
>     The methane itself provides feedback equally to both regional and global 
> warming, through its greenhouse effect.  The regional warming will increase 
> the rate of methane release.  Thus there could be thermal runaway on a global 
> scale and "we are toast", as Hansen puts it.
>
>     We have to find a way to quickly halt the Arctic regional warming.  I 
> maintain that the key to this is to halt and partially reverse the retreat of 
> the Arctic sea ice, by cooling the region.  And I maintain that the key to 
> cooling is use of solar radiation management (SRM) techniques - a combination 
> of stratospheric aerosols and marine cloud brightening.
>
>     If we do not act quickly with our SRM geoengineering, then thermal 
> runaway from methane (and also disasterous sea level rise) could become 
> inevitable.  
>
>     Cheers from Chiswick,
>
>     John
>
>     P.S.  Note that geoengineering to reduce atmospheric CO2.
>
>     ----- Original Message -----
>     From: "Andrew Lockley" <[email protected]>
>     To: "Geoengineering FIPC" <[email protected]>
>     Sent: Thursday, February 05, 2009 2:28 AM
>     Subject: [geo] runaway arguments ripped to bits
>
>     > After getting thoroughly shouted at, I realised I needed to improve my
>     > 'runaway' arguments.
>
>     > My current skeleton is below.  However, it's currently missing a few
>     > crucial bones which now need replacing.  I need citations for the
>     > following:
>
>     > 1)  A clathrate gun effect that shows rapid release?  Buffett and
>     > Archer, and Archer alone, show a slow release, although from a large
>     > reservoir.
>     > 2) A calculation of the eventual warming that may result from methane
>     > release from permafrost/clathrates.
>     > 3) A study showing the impacts of such a level of warming on human
>     > civilisation/survival.
>     > 4) What happens to methane sinks under conditions of bulk outgassing?
>     > Do they fail and massively increase the global warming potential of
>     > methane?
>
>     > We've discussed all these issues before, but I think it's now time to
>     > get any available research on the issue into the open.  Is there
>     > REALLY a big and immediate risk from the clathrate gun/permafrost?
>
>     > A
>
>     >http://en.wikipedia.org/wiki/Effects_of_global_warming#Abrupt_climate...
>
>     > The scientific consensus in the [[IPCC Fourth Assessment Report]] is
>     > that "Anthropogenic warming could lead to some effects that are abrupt
>     > or irreversible, depending upon the rate and magnitude of the climate
>     > change."
>
>     > The phenomenon of [[Arctic shrinkage]] is leading some scientists to
>     > fear that a runaway climate change event may be
>     > 
> imminent<ref>http://www.guardian.co.uk/environment/2006/oct/18/bookextracts.books</ref>,
>     > and may even have
>     > started<ref>http://www.terranature.org/environmentalCrisis.htm</ref>.
>     > There is an [[albedo]] effect, as white ice is replaced by dark ocean.
>     > Rapid [[Arctic shrinkage]] is occurring, with 2007 being the lowest
>     > ever recorded area and 2008 being possibly the lowest ever recorded
>     > 
> volume.<ref>http://nsidc.org/news/press/20081002_seaice_pressrelease.html</ref>
>     > This will induce or accelerate other [[positive feedback]] mechanisms,
>     > such as [[Arctic methane release]] from melting [[permafrost]] and
>     > [[clathrates]]. Lawrence et al(2008) suggests that a rapid melting of
>     > the sea ice may up a feedback loop that rapidly melts arctic
>     > 
> permafrost.<ref>http://www.ucar.edu/news/releases/2008/permafrost.jsp</ref><ref>{{Citation
>     > | year=2008 | title=Accelerated Arctic land warming and permafrost
>     > degradation during rapid sea ice loss | first=David M. | last=Lawrence
>     > | first2=Andrew G. | last2=Slater | first3=Robert A. | last3=Tomas |
>     > first4=Marika M. | last4=Holland | first5=Clara | last5=Deser |
>     > journal=[[Geophysical Research Letters]] | volume=35 | issue=11 |
>     > doi=10.1029/2008GL033985 |
>     > 
> url=http://www.cgd.ucar.edu/ccr/dlawren/publications/lawrence.grl.submit....}}</ref>
>
>     > Estimates of the size of the total carbon reservoir in Arctic
>     > [[permafrost]] and [[clathrates]] vary widely.  It is suggested that
>     > at least 900 gigatonnes of carbon in permafrost exists
>     > 
> worldwide.<ref>http://www.terranature.org/methaneSiberia.htm</ref>{{fact}}.
>     > Further, there are believed to be around and another 400 gigatonnes
>     > of carbon in methane clathrates in permafrost regions
>     > alone.<ref>http://www.springerlink.com/content/r4w867922g607w2j/</ref>.
>     > Should this estimate of volume be correct or at least too low, and if
>     > clathrates are omitted from the analysis completely, then 900
>     > gigatonnes of carbon may potentially be released as methane as a
>     > result of human activity.  [[Methane]] is a potent [[greenhouse gas]]
>     > with a higher [[global warming potential]] than [[CO2]].  A release on
>     > this scale will create [[catastrophic climate change]].
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