The other problem with 100-year GWPs is that they tend to hide all that can
be done with the short-lived species (black carbon, methane, ozone
precursors), so what we really need to do is to use both 20 and 500+ year
GWPs. Use of 100-year GWPs covers up both of the important tails.

Mike


On 11/20/09 2:49 PM, "Greg Rau" <[email protected]> wrote:

> Thanks, David.  I agree. Failure to appreciate long term effects and ocean
> acidification impacts, together with questionable/opaque discounting schemes
> has I believe resulted in CO2 mitigation being greatly undervalued by the
> economists and this is significantly undermining policy and political will.
> Regards,
> Greg  
> 
>> Greg
>>  
>> GWP's by design ignore all climate impacts beyond 100 years.
>>  
>> This has real consequences as it makes methane look relatively more important
>> that it should be, and it also overweight's the beneficial impacts of biomass
>> sequestration in some calculations.
>>  
>> While some traditional economists may assume that discounting allows them to
>> ignore any impact beyond 100 years, this GWP formula has long been a point of
>> contention as most of us do value the future of the planet beyond 100 years.
>>  
>> Adopting a 100 year analysis horizon, as the IPCC generally does, takes our
>> eye off the long term consequences of dumping fossil carbon in the
>> atmosphere. The risk of sea level rise look much less serious if one only
>> looks a century out.
>>  
>> Scientific understanding about the long term impacts of fossil emissions is
>> decades old (see Jim Kasting's old papers for example), popular realization
>> of these facts is long overdue.
>>  
>> Cheers,
>> David
>>  
>>  
>> 
>> From: Greg Rau [mailto:[email protected]]
>> Sent: November 16, 2009 1:23 PM
>> To: [email protected]; [email protected]
>> Subject: Re: [geo] Re: Rejected - a simple argument for SRM geoengineering
>>  
>> In light of recent modeling results on the lifetime of CO2 in the atmosphere,
>> I am concerned that the current time-integrated (not instantaneous) GWP
>> estimate for CO2 has been underestimated and hence GWP's of other gases (esp
>> short-lived gases) relative to CO2 have been overestimated.  E.g., Eby et
>> al., 2009:
>> http://*ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F2008J
>> CLI2554.1
>> show that 20-30% of excess emissions of CO2 and 60-70% of the subsequent
>> CO2-caused surface air temp anomally exists 10,000 years after emission.
>> Isn't this (or is this?) a far larger total time-integrated GW effect than a
>> mass equivalent emission of CH4?  Experts please set me straight.
>> Thanks,
>> Greg 
>>  
>>> Agreed, one has to consider a time period, so assume one takes a day that
>>> when injected there is no decay over this period-so it might as well be a
>>> second of time one takes-so virtually instantaneous. And I'll assume
>>> linearity on methane absorption and logarithmic for CO2.
>>> 
>>> So, for methane, humans have caused an increase of roughly 1000 ppb which
>>> converts to about 3 GtCH4, and this causes a forcing of about 0.5 W/m**2 (at
>>> the tropopause) per IPCC.
>>> 
>>> For CO2, we know that a doubling (so we'll say from 300 to 600 ppm so we are
>>> in the range of interest) causes a forcing of about 3.6 W/m**2 (at the
>>> tropopause). So, 300 ppm of CO2 in the atmosphere is roughly 600 GtC or 2200
>>> GtCO2 (and global warming potential is done for CO2, I believe.
>>> 
>>> So, if we take the ratio of forcing to mass for CH4 divided by the ratio of
>>> forcing to mass for CO2, we get a rough estimate of the instantaneous GWP,
>>> so
>>> 
>>> [0.5/3]/[3.6/2200] equals roughly 100
>>> 
>>> for the ratio at t=0 (so allowing for no decay) of the radiative forcing
>>> caused by a unit mass of CH4 added to the atmosphere to a unit mass of CO2
>>> added to the atmosphere.
>>> 
>>> Not exact, but plausible.
>>> 
>>> Mike
>>> 
>>> 
>>> 
>>> 
>>> On 11/16/09 3:42 AM, "Peter Read" <[email protected]> wrote:
>>> John, Andrew
>>> Re "BTW, does anybody know the _immediate_ warming potential of methane?"
>>> Someone will correct me no doubt but my understanding is that warming is a
>>> rate process measured in W/m^2
>>> So "instantaneous" [[== "immediate"?]] warming is an incorrect concept
>>> Unless it continues for a second, a week, a year, 25 years, for whatever, no
>>> warming takes place.
>>> So it is necessary to multiply by a duration to get joules/m^2
>>> It's how many joules get into the low albedo meltwater on top of Greenland's
>>> ice that decides how much gets melted each year to fall down crevasses and
>>> lubricate the eventual collapse of large areas of ice into the oceans.
>>> Meaning that the integral [[roughly]] under the CO2 level curve is what
>>> matters [multiplied by the warming potential over that period]  when it
>>> comes to measuring threats of Greenland's collapse
>>> So the key issue is duration - how long elevated greenhouse gas levels last
>>> and how to get them down.
>>> Think that's right
>>> Peter
>>> 
>>> ----- Original Message -----
>>>  
>>> From:  John Nissen <mailto:[email protected] 
>>> <mailto:[email protected]>
>>> >   
>>>  
>>> To: [email protected]
>>>  
>>>> Cc: geoengineering <mailto:[email protected]
>>>> <mailto:[email protected]> >
>>>>  
>>>> Sent: Monday, November 16, 2009 6:18  PM
>>>>  
>>>> Subject: Re: [geo] Re: Rejected - a  simple argument for SRM geoengineering
>>>>  
>>>> 
>>>> 
>>>> 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
>>>> <http://**en.wikipedia.org/wiki/Clathrate_gun_hypothesis>
>>>> 
>>>> [2]  http://**en.wikipedia.org/wiki/Enterprise_risk_management
>>>> <http://**en.wikipedia.org/wiki/Enterprise_risk_management>
>>>> 
>>>> [3] http://**answers.yahoo.com/question/index?qid=20090329215018AAxqYFk
>>>> <http://**answers.yahoo.com/question/index?qid=20090329215018AAxqYFk>
>>>> 
>>>> [4] http://**en.wikipedia.org/wiki/Greenhouse_gas
>>>> <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.
>>>> 
>>>>  
>>>> I don't oppose John's argument, but the evidence on the severity of the
>>>> problem is far from conclusive.  We need much more research into:
>>>>  
>>>> 1)  The methane reservoir in clathrates and permafrost
>>>>  
>>>> 2) The size of potential methane sources currently frozen as organic
>>>> detritus
>>>>  
>>>> 3) The likely changes to the GWP of methane in future atmospheres, as  the
>>>> levels of hydroxyl radicals etc. shift over time and as a direct result  of
>>>> methane excursion.  Recent research on this asks more questions than  it
>>>> answers.
>>>>  
>>>> 
>>>>  
>>>> My personal feeling is that the range of likely outcomes is from a
>>>> significant amplification of AGW, right up to a 'Great Dying' sized
>>>> mass-extinction event when we come within a sneeze of sterilising the
>>>> entire  planet.  I'd be tempted to bet on the latter, but I wouldn't be
>>>> around  to collect the winnings, so I'll keep my wallet in my pocket.
>>>>  
>>>> 
>>>>  
>>>> My suggestions is that geoengineers look at ways to clean up the  methane
>>>> from the atmosphere, and then lock down the resulting carbon.   My guess is
>>>> we've got about 50 years to do this, but virtually no time  at all if the
>>>> methane can't be dealt with once it's in the atmosphere.  Therefore, I'd
>>>> support John out of precautionary principle-based  reasoning.
>>>>  
>>>> 
>>>>  
>>>> A
>>>> 
>>>>  
>>>> 2009/11/15 jim woolridge <[email protected]>
>>>>  
>>>> Nice one, John; the train of argument is clear (of  limpid clarity, in
>>>> fact!)  The problem is that the people and  institutions addressed are
>>>> in the business of politics, the art of the  possible, rather than in
>>>> the business of logical evaluation.  They  hear what you are saying and
>>>> must see the validity of it. But  politically what is true and what is
>>>> doable do not always coincide, as  we all know from as many examples as
>>>> one cares to ennumerate.
>>>> 
>>>> We  have to keep hammering away at the arguments, to the point at  which
>>>> they are generally understood and accepted, and also keep  on
>>>> politicking in the sure and certain hope that eventually  the
>>>> acceptance of the arguments and the cowardice/caution/horse  sense/
>>>> opportunistic careerism of the politicos will achieve the right  kind
>>>> of intersection.  In the next year or so (& wouldn't it  be a great
>>>> help to have the environmental NGOs on board.)
>>>>  
>>>>  
>>>> 
>>>> On Nov 12, 10:51 pm, John Nissen <[email protected]> wrote:
>>>>> > It is  incredible. It is so obvious.
>>>>> >
>>>>> > 1. Global warming is driven  largely by atmospheric CO2 according to the
>>>>> > concentration above  its pre-industrial level; and
>>>>> >
>>>>> > 2. After emissions are  stopped it could take millenia for the
>>>>> > concentration to fall back  to that level, because the effective
>>>>> lifetime
>>>>>> > of some of that  excess CO2 is many thousands of years.
>>>>>> >
>>>>>> > Therefore:
>>>>>> >  3.  Drastic emissions reduction, even to zero overnight, cannot and
>>>>>> will
>>>>>> > not stop the Arctic continuing to warm for  decades.
>>>>>> >
>>>>>> > Therefore:
>>>>>> > 4. The Arctic sea ice will  continue to retreat, accelerating the
>>>>>> warming
>>>>>> > due to the albedo  effect.
>>>>>> >
>>>>>> > Therefore:
>>>>>> > 5.  The permafrost will  continue to thaw releasing increasing
>>>>>> quantities
>>>>>> > of methane, a  potent greenhouse gas, potentially adding many degrees
>>>>>> to
>>>>>> > global  warming; and
>>>>>> >
>>>>>> > 6.  The Greenland ice sheet will become  increasingly unstable,
>>>>>> > potentially contributing to an eventual sea  level rise of 7 metres.
>>>>>> >
>>>>>> > Therefore:
>>>>>> > 7.  To  avoid these two catastrophes, we need to cool the Arctic
>>>>>> quickly
>>>>>> >  enough to save the Arctic sea ice; and
>>>>>> >
>>>>>> > 8.  Probably  the only feasible way to do this is through solar
>>>>>> radiation
>>>>>> >  management (SRM) geoengineering.
>>>>>> >
>>>>>> > 9.  SRM is not a  last resort, it is needed now to cool the Arctic.
>>>>>> >
>>>>>> > It is  incredible that people do not seem to follow this train of logic
-
>>>>>> >  it is so obvious.
>>>>>> >
>>>>>> > Yet when I challenged a panel of  geoengineering experts to refute this
>>>>>> > argument, the response was  that geoengineering (even just to cool the
>>>>>> > Arctic) was too  dangerous - not that the argument was false! [1]
>>>>>> >
>>>>>> > So we  continue to hear politicians and their advisers claiming that
>>>>>> >  emissions reduction alone can be sufficient to keep the planet safe.
>>>>>> [2]
>>>>>> >
>>>>>> > And we continue to hear geoengineering experts saying  that
>>>>>> > geoengineering should only be used as a last resort.  [3]
>>>>>> >
>>>>>> > How can this mindset be changed quickly, to avoid  leaving
>>>>>> geoengineering
>>>>>> > too late?
>>>>>> >
>>>>>> >  John
>>>>>> >
>>>>>> > P.S. Apologies to those who have heard this all  before and accept the
>>>>>> > logic as self-evident.
>>>>>> >
>>>>>> > [1]   This challenge was put to the panel at the launch of the  Royal
>>>>>> > Society geoengineering report, on September 1st, with  response from
>>>>>> the
>>>>>> > team leader and panel chairman, Professor John  Shepherd.
>>>>>> >
>>>>>> > [2]  For example at the geoengineering  hearing at the House of
>>>>>> Commons,
>>>>>> > November 2008.
>>>>>> >
>>>>>> >  [3] For example at the congressional hearing on geoengineering,
>>>>>> November
>>>>>> > 2009.
>>>>> 
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