See below for reasonably convincing numerical treatment of the permafrost
runaway event. It claims to shows that, with political and technological
lag, we are likely to cross the tipping point and will be powerless to stop
runaway climate change without geoengineering

A
 ---------- Forwarded message ----------
From: "ClimateSight" <[email protected]>
Date: Oct 3, 2012 4:10 AM
Subject: [New post] Permafrost Projections
To: <[email protected]>

**
  climatesight posted: "During my summer at UVic, two PhD students at the
lab (Andrew MacDougall and Chris Avis) as well as my supervisor (Andrew
Weaver) wrote a paper modelling the permafrost carbon feedback, which was
recently published in Nature Geoscience. I read a draft ver"    Respond to
this post by replying above this line
      New post on *ClimateSight*
<http://climatesight.org/author/climatesight/>  Permafrost
Projections<http://climatesight.org/2012/10/02/permafrost-projections/>
by
climatesight <http://climatesight.org/author/climatesight/>

During my summer at UVic, two PhD students at the lab (Andrew MacDougall
and Chris Avis) as well as my supervisor (Andrew Weaver) wrote a paper
modelling the permafrost carbon feedback, which was recently published
in *Nature
Geoscience* <http://www.nature.com/ngeo/journal/v5/n10/full/ngeo1573.html>.
I read a draft version of this paper several months ago, and am very
excited to finally share it here.

Studying the permafrost carbon feedback is at once exciting (because it has
been left out of climate models for so long) and terrifying (because it has
the potential to be a real game-changer). There is about twice as much
carbon frozen into permafrost than there is floating around in the entire
atmosphere. As high CO2 levels cause the world to warm, some of the
permafrost will thaw and release this carbon as more CO2 - causing more
warming, and so on. Previous climate model simulations involving permafrost
have measured the CO2 released during thaw, but haven't actually applied it
to the atmosphere and allowed it to change the climate. This UVic study is
the first to close that feedback loop (in climate model speak we call this
"fully coupled").

The permafrost part of the land component was already in place - it was
developed for Chris's PhD thesis, and implemented in a previous
paper<http://www.nature.com/ngeo/journal/v4/n7/full/ngeo1160.html>.
It involves converting the existing single-layer soil model to a
multi-layer model where some layers can be frozen year-round. Also, instead
of the four 
RCP<http://www.nature.com/nclimate/journal/v1/n1/box/nclimate1058_BX1.html>scenarios,
the authors used DEPs (Diagnosed Emission Pathways): exactly the
same as RCPs, except that CO2 *emissions*, rather than concentrations, are
given to the model as input. This was necessary so that extra emissions
from permafrost thaw would be taken into account by concentration values
calculated at the time.

As a result, permafrost added an extra 44, 104, 185, and 279 ppm of CO2 to
the atmosphere for DEP 2.6, 4.5, 6.0, and 8.5 respectively. However, the
extra warming by 2100 was about the same for each DEP, with central
estimates around 0.25 °C. Interestingly, the logarithmic effect of CO2 on
climate (adding 10 ppm to the atmosphere causes more warming when the
background concentration is 300 ppm than when it is 400 ppm) managed to
cancel out the increasing amounts of permafrost thaw. By 2300, the central
estimates of extra warming were more variable, and ranged from 0.13 to 1.69
°C when full uncertainty ranges were taken into account. Altering climate
sensitivity (by means of an artificial feedback), in particular, had a
large effect.

As a result of the thawing permafrost, the land switched from a carbon sink
(net CO2 absorber) to a carbon source (net CO2 emitter) decades earlier
than it would have otherwise - before 2100 for every DEP. The ocean kept
absorbing carbon, but in some scenarios the carbon source of the land
outweighed the carbon sink of the ocean. That is, even without human
emissions, the land was emitting more CO2 than the ocean could soak up.
Concentrations kept climbing indefinitely, even if human emissions suddenly
dropped to zero. This is the part of the paper that made me want to hide
under my desk.

This scenario wasn't too hard to reach, either - if climate sensitivity was
greater than 3°C warming per doubling of CO2 (about a 50% chance, as 3°C is
the median estimate by scientists today), and people followed DEP 8.5 to at
least 2013 before stopping all emissions (a very intense scenario, but I
wouldn't underestimate our ability to dig up fossil fuels and burn them
really fast), permafrost thaw ensured that CO2 concentrations kept rising
on their own in a self-sustaining loop. The scenarios didn't run past 2300,
but I'm sure that if you left it long enough the ocean would eventually win
and CO2 would start to fall. The ocean always wins in the end, but things
can be pretty nasty until then.

As if that weren't enough, the paper goes on to list a whole bunch of
reasons why their values are likely underestimates. For example, they
assumed that all emissions from permafrost were  CO2, rather than the much
stronger CH4 which is easily produced in oxygen-depleted soil; the UVic
model is also known to underestimate Arctic amplification of climate change
(how much faster the Arctic warms than the rest of the planet). Most of the
uncertainties - and there are many - are in the direction we don't want,
suggesting that the problem will be worse than what we see in the model.

This paper went in my mental "oh shit" folder, because it made me realize
that we are starting to lose control over the climate system. No matter
what path we follow - even if we manage slightly negative emissions, i.e.
artificially removing CO2 from the atmosphere - this model suggests we've
got an extra 0.25°C in the pipeline due to permafrost. It doesn't sound
like much, but add that to the 0.8°C we've already seen, and take
technological inertia into account (it's simply not feasible to stop all
emissions 
overnight<http://climatesight.org/2012/05/30/modelling-the-apocalypse/>),
and we're coming perilously close to the big nonlinearity (i.e. tipping
point) that many argue is between 1.5 and 2°C. Take political inertia into
account (most governments are nowhere near even creating a plan to reduce
emissions), and we've long passed it.

Just because we're probably going to miss the the first tipping point,
though, doesn't mean we should throw up our hands and give up. 2°C is bad,
but 5°C is awful, and 10°C is unthinkable. The situation can *always* get
worse if we let it, and how irresponsible would it be if we did?
  *climatesight <http://climatesight.org/author/climatesight/>* | October
2, 2012 at 9:10 pm | Tags: arctic
<http://climatesight.org/?tag=arctic>, climate
change <http://climatesight.org/?tag=climate-change>, climate
models<http://climatesight.org/?tag=climate-models>,
education <http://climatesight.org/?tag=education>,
environment<http://climatesight.org/?tag=environment>,
global warming <http://climatesight.org/?tag=global-warming>,
permafrost<http://climatesight.org/?tag=permafrost>,
science <http://climatesight.org/?tag=science>,
UVic<http://climatesight.org/?tag=uvic>| Categories: Science
Lessons <http://climatesight.org/?cat=4183609> | URL: http://wp.me/puG7a-w9

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