Even as a layman I can't understand why scientists everywhere aren’t
hollering their heads off – perhaps it is because after studying and
observing global warming proceed at a snails pace for decades, they
have been lulled into a calm?

Methane levels in 2011 are 1.8 ppm, an atmospheric total of ~3.5 Gt C.
As of 2009 methane fluxes in the ESAS are adding 3.5 Gt C to the
atmosphere [1]. If i’m not mistaken, that has just doubled the
atmospheric methane burden in a year, and tripled as of 2011. I don’t
know how much of that gets oxidized. Releases of up to 50 Gt of
hydrate is possible at any time [2]. Mixing time for methane is about
a year, but major releases in the Arctic would take 15-40 years to
spread to the South Pole [3]. Is the long mix time a good or bad
thing? Would 3.5 Gt C be considered a major release? Methane focusing
heating in the Arctic just speeds the whole melting process up. Once
the heat pulse starts penetrating hydrate sediments, top-down cooling
won't stop the process either [3].

James Hansen predicts 2012 will be the hottest year on record. I don’t
see how methane release can go anywhere but up. With the number of
recent earthquakes, could even greater releases be occurring
unnoticed? I think the precautionary principle means we should be
treating this as an emergency and have geoengineering capacity on
standby.

[1] 
http://symposium.serdp-estcp.org/content/download/8914/107496/version/1/file/1A_Shakhova_Final.pdf

[2] http://www.cosis.net/abstracts/EGU2008/01526/EGU2008-A-01526.pdf

[3] 
http://groups.google.com/group/geoengineering/attach/b9fcdd6ead8da6f3/Methane+Blowout+Events.pdf?part=4

[4] http://climateprogress.org/2011/04/11/extreme-warming-temperature-map/


On Apr 16, 2:51 pm, John Nissen <[email protected]> wrote:
> Hi Alvia,
>
> I said: "we are now in a desperate situation calling for emergency action".
>
> You dispute this.  Thanks for your honest opinion about the gravity, or
> otherwise, of the situation as you see it.  But isn't your opinion
> rather wishful thinking?
>
<snip>

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