Dear Andrew,

We need to read the explanation of Runaway Greenhouse Efffect in Wayne
1st ed pg. 49. I will dictate into an email soon.

Sincerley,

Oliver Wingenter

On Feb 2, 4:50 pm, Andrew Lockley <[email protected]> wrote:
> I have an alternative theory as to why we don't see too many instances
> of runaway climate change from the 'clathrate gun' effect, or from
> permafrost.
>
> Methane has a very short life in the atmosphere, but is a potent
> greenhouse gas.  If the rate of warming is low, a little methane is
> released, which quickly degrades to CO2 which has little short term
> effect and can then disappear into sinks.  As warming continues, more
> methane is released, but never fast enough to make a significant
> difference to the climate before it degrades again to CO2.
>
> HOWEVER:
>
> In AGW, the temperature is rising very fast.  This has the potential
> to make methane belch out from soils and seas very quickly.  This
> speed is of the essence, as large quantities of methane will be enough
> to influence future methane release to create a runaway event.
>
> The process is like pull starting a chainsaw.  A little tug gets you
> the odd cough. Tug hard, the the chainsaw motor gets started and runs
> on its own.
>
> Now, pretty please with sugar on top, can someone tell me what the
> proper, scientific, not-to-be-argued with name for that process is?
> The people on wikipedia really don't like 'runaway climate change' -
> as apparently 'proper' climate scientists don't use that term.
> Citations much appreciated, thankyou!!
>
> A
>
> 2009/2/2 Alvia Gaskill <[email protected]>:
>
> > Not enough CO2 in the atmosphere.
>
> > ----- Original Message -----
> > From: Andrew Revkin
> > To: [email protected] ; [email protected]
> > Cc: [email protected] ; Tom Wigley ; Andrew Lockley ; geoengineering ;
> > Prof John Shepherd ; Tim Lenton ; David Lawrence
> > Sent: Monday, February 02, 2009 3:29 PM
> > Subject: [geo] runaway climate change
> > Who on this list knows why the Arctic warming ~ 8,000 years ago (quite
> > protracted and significantly warmer than today) did not lead to "runaway"
> > warming?
> >  Presumably something kicked in the other direction?
> > I'm pursuing a clearer picture of lessons from the Holocene and the Eemian
> > (the previous interglacial) related to feedbacks and whether there are, or
> > are not, one-way doors in the climate system. Leads eagerly pursued. ..
> > Andy
> > At 5:29 PM +0530 2/2/09, Govindasamy bala wrote:
>
> > Runaway feedback means running its course completely. It is feedback
> > specific.
>
> > A good example is the presumed water vapor feedback on Venus.
> > Apparently, earth and venus started with similar amount of h2o.
> > Because Venus started with much higher surface temperature, the evolution of
> > temperature and water vapor never intercepted the phase line of vapor and
> > liquid. The climate warmed until all the water got evaporated. Basically,
> > there was no sink for vapor which precipitation. On earth, this is not going
> > to happen because we got the precipitation sink on earth...how lucky we are.
>
> > But I guess we do have runaway ice-albedo feedback on earth. we could get
> > ice-free planet or snowball earth........
>
> > Cheers.
> > Bala
>
> > On Mon, Feb 2, 2009 at 5:03 PM, Eugene I. Gordon <[email protected]>
> > wrote:
>
> > I guess it is not going to end.
>
> > A runaway train meets only #2 and even that has to be qualified because the
> > train eventually runs out of (fossil?) fuel or track. Certainly climate has
> > run away a half dozen times in 540 million years but always hits a limit
> > which seems to be 24C except when an asteroid hits. It eventually turns
> > around after remaining at the limit temperature for many millions of years.
> > We have been in a runaway mode for the last 18,000 years but with some
> > superimposed small wiggles in temperature. Without geoengineering the
> > temperature will certainly get to the 24 C limit.
>
> > I think runaway is appropriate for the current situation even if there may
> > be better suited terms.
>
> > -----Original Message-----
> > From: [email protected]
>
> > [mailto:[email protected]] On Behalf Of John Nissen
> > Sent: Monday, February 02, 2009 6:08 AM
> > To: Tom Wigley; Andrew Lockley
> > Cc: geoengineering; Prof John Shepherd; Tim Lenton; David Lawrence
> > Subject: [geo] Re: runaway climate change
>
> > Dear Tom,
>
> > The concept of "runaway" has certain connotations:
>
> > 1.  Significant in resultant effect
> > 2.  Uncontrollable
> > 3.  Exponential initial behaviour - characteristised by acceleration of
> > process 4.  No obvious limit 5.  Irreversible 6.  Rapid.
>
> > These can all be applied to climate change:
>
> > 1.  "Significant" could be over 5 degrees global warming, sufficient for a
> > mass extinction event.  Or it could be applied to several metres of sea
> > level rise.
> > 2.  "Uncontrollable" could be where anthropogenic greenhouse gas emissions
> > reduction would not have a significant effect on the rate of climate change.
> > 3.  Exponential behaviour could be caused by a "tipping" of some part of the
> > climate system, such as Arctic sea ice or methane release, where there is
> > strong positive feedback.
> > 4.  There would be no obvious final equilibrium temperature - mainly because
> > of the difficulty of modelling positive feedback and its behaviour over
> > time.
> > 5.  It would be extremely difficult or impossible to reverse processes such
> > as methane release or Greenland ice sheet disintegration, although it is
> > conceivable to halt these processes or even reverse their effects
> > (presumably through geoengineering).
> > 6.  "Rapid" could be anything from one season to 3000 years, on a geological
> > timescale.
>
> > Therefore I think that "runaway" captures the semantics that we require for
>
> > the climate change that would result from, for example, a massive methane
> > release, triggered by Arctic sea ice disappearance.  Can you think of a
> > better word to capture the six characteristics above, especially as
> > applicable to climate change?
>
> > Cheers,
>
> > John
>
> > ----- Original Message -----
> > From: "Tom Wigley" <[email protected]>
> > To: "Andrew Lockley" <[email protected]>
> > Cc: <[email protected]>; "geoengineering"
> > <[email protected]>; "Prof John Shepherd"
> > <[email protected]>; "Tim Lenton" <[email protected]>; "David Lawrence"
> > <[email protected]>
> > Sent: Monday, February 02, 2009 3:43 AM
> > Subject: Re: [geo] Re: runaway climate change
>
> >> Andrew,
>
> >> Poor analogy. running does not equal running away.
>
> >> More importantly, just because a term has been misused in the
> >> past does not mean we should perpetuate its misuse (or use).
> >> If the word is to be used at all (and, as a practicing scientist,
> >> I never have or will), one should start off by saying that the
> >> word runaway is open to misinterpretation, that it does not
> >> mean running off to infinity, and that it's real meaning is ...
> >> etc. etc. Then talk about irreversible changes (with the caveat
> >> that even these are probably not irreversible), positive
> >> feedbacks (which also have limits), etc.
>
> >> Tom.
>
> >> +++++++++++++++++++++++====
>
> >> Andrew Lockley wrote:
> >>> For better or worse, the term is now in general use in scientific,
> >>> industrial, environmental and general media.  (See
> >>>http://en.wikipedia.org/wiki/Runaway_climate_changefor refs.)
>
> >>> I don't agree with Tom about 'to infinity and beyond'.  I run as a
> >>> hobby, and I've never run to infinity (or beyond).  I think most
> >>> people realise that runaway doesn't mean run-for-ever.
>
> >>> However, a general definition would be very useful.
>
> >>> A
>
> >>> 2009/2/2  <[email protected]>:
> >>>> Dear All,
>
> >>>> I've said this before, but here goes again.
>
> >>>> If one sticks to dictionary definitions of words (which I
> >>>> think is wise) then there is no such thing as "runaway"
> >>>> climate change. Strictly, using the words of Buzz Lightyear,
> >>>> "runaway" must mean "to infinity and beyond".
>
> >>>> Further, the word "runaway" is loaded and should be eschewed
> >>>> in the climate context.
>
> >>>> The confusion here is that what some people are calling
> >>>> "runaway" climate change is really better referred to as
> >>>> "irreversible" climate change. For instance, the sudden release
> >>>> of a large amount of CH4 would possibly cause large warming
> >>>> that would put the globe in a new state that was much warmer
> >>>> than present. But the climate (or global-mean temperature) would
> >>>> *not* runaway -- it would eventually stabilize. Even this change
> >>>> would not strictly be irreversible, as the excess CH4 would
> >>>> slowly be oxidized (more slowly than today because of the well
> >>>> known positive feedback of CH4 on its own lifetime due to OH loss),
> >>>> but a lot of the excess CH4 would slowly disappear and be replaced
> >>>> by CO2 that has less forcing. This CO2 would, of course, stay
> >>>> around for a long time.
>
> >>>> If anyone is interested, this case can easily be run with MAGICC,
> >>>> but some minor tweaks are needed to get the CH4 to CO2 flux right.
> >>>> Conceptually trivial.
>
> >>>> So, please, please try not to cry wolf with these loaded and sadly
> >>>> oft-misused words.
>
> >>>> Tom.
>
> >>>> ++++++++++++++++++++++++++++
>
> >>>>> Andrew,
>
> >>>>> 1.  I think the concept of runaway climate change is kosher.  See this
> >>>>> quote
> >>>>> from
> >>>>>http://www.meridian.org.uk/_PDFs/FeedbackDynamics.pdf
>
> >>>>> "The possibility of a tipping point in the earth system as a whole
> >>>>> which
> >>>>> prevents the recovery of stable equilibrium and leads to a process of
> >>>>> runaway climate change, is now the critical research agenday, requiring
>
> >>>>> the
> >>>>> concerntration of global resources in a "Manhattan Project" style
> >>>>> engagement.  All other work on impact assessment, mitigation and
> >>>>> adaptration
> >>>>> depends on the outcome of thie overarching issue"
>
> >>>>> I would prefer to have "runaway global warming", because that's what we
> >>>>> are
> >>>>> really talking
>
> ...
>
> read more »
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