JiscMail Logo
Email discussion lists for the UK Education and Research communities

Help for CRISIS-FORUM Archives


CRISIS-FORUM Archives

CRISIS-FORUM Archives


CRISIS-FORUM@JISCMAIL.AC.UK


View:

Message:

[

First

|

Previous

|

Next

|

Last

]

By Topic:

[

First

|

Previous

|

Next

|

Last

]

By Author:

[

First

|

Previous

|

Next

|

Last

]

Font:

Proportional Font

LISTSERV Archives

LISTSERV Archives

CRISIS-FORUM Home

CRISIS-FORUM Home

CRISIS-FORUM  February 2013

CRISIS-FORUM February 2013

Options

Subscribe or Unsubscribe

Subscribe or Unsubscribe

Log In

Log In

Get Password

Get Password

Subject:

Re: Major methane release is almost inevitable - New Scientist

From:

Peter Carter <[log in to unmask]>

Reply-To:

Peter Carter <[log in to unmask]>

Date:

Fri, 22 Feb 2013 23:08:00 -0800

Content-Type:

multipart/mixed

Parts/Attachments:

Parts/Attachments

text/plain (171 lines) , Zero C 1.5C planet emergency response.png (171 lines)

The fuse to the Arctic methane time bomb has been burning a long time, and 
without drastic emergency intervention the future is committed to planetary 
catastrophe. This latest research proves are right out of time.

The Arctic methane time bomb is warming peatlands, thawing permafrost and 
melting sea floor frozen solid methane hydrate.
Thawing permafrost generates its own heat so reaches a stage where the 
thawing is self increasing irreversible.

This Arctic methane is at least three times all atmospheric carbon.

There is a way out, but we have to act now or there won’t be- for today's 
young generation.

Our commitment is way over 1.5C.
1.5C is also the end of the coral reefs.

The ocean heat lag alone commits us to 1.4C by 2100.

Our unavoidable commitment to more warming is at least 2.4C  (published).
(Ramanathan Feng 2008 PNAS On Avoiding Dangerous Anthropogenic Interference 
with the Climate System)  ... even the most aggressive CO2 mitigation steps 
as envisioned now can only limit further additions to the committed warming, 
but not reduce the already committed GHGs warming of 2.4°C.

The Ramanathan  commitment is from the ocean heat lag (more than doubles 
todays warming)  and unmasking of air pollution aerosol cooling.

The warming incurred by the time it will take to stabilize atmospheric GHGs 
and the added warming from terrestrial carbon (excludes Arctic carbon) 
feedback warming has to be added to that to get the total committed warming, 
which is at least 3C.

Robert Watson has stated we are committed to 3C may be up to 5C.
The World Back says we are rapidly committing ourselves to 4C.

Today’s combined national UN filed emissions reduction pledges commit us the 
4.4C by 2100, and nations have not acted on these pledges (Climate 
Interactive)

An emergency response now can get us below 1.5C

1) rapidly stabilize Arctic albedo snow and ice cooling and thereby Arctic 
methane by regional Arctic cooling
This also prevents American food producing regions being ruined by drought.

2) zero carbon emissions mitigation on a rapid emergency basis. That is 
total conversion off all fossil fuels to 100% clean energy.

Zero carbon takes care of most black carbon but there is further black 
carbon mitigation from other sources of soot like biomass burning and open 
cook stoves. As black carbon is second only to soot in global warming this 
can drop the warming 0.5C.
Zero carbon also takes care of most ground level ozone- another much smaller 
added drop of warming.

Zero carbon decarbonization could be done within 20 years by a total 
conversion off all fossil fuel energy and a halt to deforestation.

Once virtual zero carbon  is reached (we cannot achieve actual zero) 
atmospheric CO2 concentration is stabilized.

3) World afforestation would remove and store some carbon out of the 
atmosphere so achieving zero carbon – for many decades at least
4) Biochar would sink carbon for a couple of centuries.
5) Remove CO2 directly from the air (doable in theory) would maintain 
negative carbon in order to drop atmospheric CO2 below 350 ppm.

It will take a hundred years for atmospheric CO2 to get below 350, but if we 
act now we may leave a legacy of a sustainable future.
If we fail to act now our legacy is a short dark age and no future.

The only hope is to convince people of the planetary Arctic warming 
emergency- we have to acknowledge how bad this is and then act for our 
survival.

Peter C


-----Original Message----- 
From: Oliver Tickell
Sent: Friday, February 22, 2013 5:56 AM
To: [log in to unmask]
Subject: Major methane release is almost inevitable - New Scientist

Abstract link
http://m.sciencemag.org/content/early/2013/02/20/science.1228729.abstract?sid=d26b1542-62e0-4aa0-9239-a82abda2d1ad

Major methane release is almost inevitable

19:00 21 February 2013 by Michael Marshall

We are on the cusp of a tipping point in the climate. If the global
climate warms another few tenths of a degree, a large expanse of the
Siberian permafrost will start to melt uncontrollably. The result: a
significant amount of extra greenhouse gases released into the
atmosphere, and a threat – ironically – to the infrastructure that
carries natural gas from Russia to Europe.The Arctic is warming faster
than the rest of the planet, and climatologists have long warned that
this will cause positive feedbacks that will speed up climate change
further. The region is home to enormous stores of organic carbon, mostly
in the form of permafrost soils and icy clathrates that trap methane – a
powerful greenhouse gas that could escape into the atmosphere.The
Siberian permafrost is a particular danger. A large region called the
Yedoma could undergo runaway decomposition once it starts to melt,
because microbes in the soil would eat the carbon and produce heat,
melting more soil and releasing ever more greenhouse gases. In short,
the melting of Yedoma is a tipping point: once it starts, there may be
no stopping it.For the first time, we have an indication of when this
could start happening. Anton Vaks of the University of Oxford in the UK
and colleagues have reconstructed the history of the Siberian permafrost
going back 500,000 years. We already know how global temperatures have
risen and fallen as ice sheets have advanced and retreated, so Vaks's
team's record of changing permafrost gives an indication of how
sensitive it is to changing temperatures.

Stalagmite record

But there is no direct record of how the permafrost has changed, so Vaks
had to find an indirect method. His team visited six caves that run
along a south-north line, with the two southernmost ones being under the
Gobi desert. Further north, three caves sit beneath a landscape of
sporadic patches of permafrost, and the northernmost cave is right at
the edge of Siberia's continuous permafrost zone.The team focused on the
500,000-year history of stalagmites and similar rock formations in the
caves. "Stalagmites only grow when water flows into caves," Vaks says.
"It cannot happen when the soil is frozen." The team used radiometric
dating to determine how old the stalagmites were. By building up a
record of when they grew, Vaks could figure out when the ground above
the caves was frozen and when it wasn't.As expected, in most of the
caves, stalagmites formed during every warm interglacial period as the
patchy permafrost melted overhead.But it took a particularly warm
interglacial, from 424,000 and 374,000 years ago, for the stalagmites in
the northernmost cave to grow – suggesting the continuous permafrost
overhead melted just once in the last 500,000 years.At the time, global
temperatures were 1.5 °C warmer than they have been in the last 10,000
years. In other words, today's permafrost is likely to become vulnerable
when we hit 1.5 °C of global warming, says Vaks."Up until this point, we
didn't have direct evidence of how this happened in past warming
periods," says Ted Schuur of the University of Florida in Gainesville.It
will be very hard to stop the permafrost degrading as a warming of
1.5 °C is not far off. Between 1850 and 2005, global temperatures rose
0.8 °C, according to the 2007 report of the Intergovernmental Panel on
Climate Change. Even if humanity stopped emitting greenhouse gases
tomorrow, temperatures would rise another 0.2 °C over the next 20 years.
That would leave a window of 0.5 °C – but in fact our emissions are
increasing. What's more, new fossil fuel power stations commit us to
several decades of emissions.

Soggy permafrost

What are the consequences? The greatest concern, says Tim Lenton of the
University of Exeter in the UK, is the regional landscape. Buildings and
infrastructure are often built on hard permafrost, and will start
subsiding. "Ice roads won't exist any more."The increasingly soggy
permafrost will also threaten the pipelines that transport Russian gas
to Europe. "The maintenance and upkeep of that infrastructure is going
to cost a lot more," says Schuur.As for the methane that could be
released into the atmosphere, Schuur estimates that emissions will be
equivalent to between 160 and 290 billion tonnes of carbon dioxide.That
sounds like a lot, but is little compared to the vast amount humans are
likely to emit, says Lenton. "The signal's going to be swamped by fossil
fuel [emissions]."He says the dangers of the permafrost greenhouse gases
have been overhyped, particularly as much of the methane will
be converted to carbon dioxide by microbes in the soil, leading to a
slower warming effect.Schurr agrees with Lenton that the methane
emissions are "not a runaway effect but an additional source that is not
accounted in current climate models".Journal reference: Science, DOI:
10.1126/science.1228729 

Top of Message | Previous Page | Permalink

JiscMail Tools


RSS Feeds and Sharing


Advanced Options


Archives

April 2024
September 2022
May 2018
January 2018
September 2016
May 2016
February 2016
January 2016
December 2015
September 2015
August 2015
May 2015
March 2015
December 2014
November 2014
October 2014
September 2014
July 2014
June 2014
May 2014
March 2014
February 2014
January 2014
December 2013
November 2013
October 2013
September 2013
August 2013
July 2013
June 2013
May 2013
April 2013
March 2013
February 2013
January 2013
December 2012
November 2012
October 2012
September 2012
August 2012
July 2012
June 2012
May 2012
April 2012
March 2012
February 2012
January 2012
December 2011
November 2011
October 2011
September 2011
August 2011
July 2011
June 2011
May 2011
April 2011
March 2011
February 2011
January 2011
December 2010
November 2010
October 2010
September 2010
August 2010
July 2010
June 2010
May 2010
April 2010
March 2010
February 2010
January 2010
December 2009
November 2009
October 2009
September 2009
August 2009
July 2009
June 2009
May 2009
April 2009
March 2009
February 2009
January 2009
December 2008
November 2008
October 2008
September 2008
August 2008
July 2008
June 2008
May 2008
April 2008
March 2008
February 2008
January 2008
December 2007
November 2007
October 2007
September 2007
August 2007
July 2007
June 2007
May 2007
April 2007
March 2007
February 2007
January 2007
December 2006
November 2006
October 2006
September 2006
August 2006
July 2006
June 2006
May 2006
April 2006
March 2006
February 2006
January 2006
December 2005
November 2005
October 2005
September 2005
August 2005
July 2005
June 2005
May 2005
April 2005
March 2005
February 2005
January 2005
December 2004
November 2004
October 2004
July 2004


JiscMail is a Jisc service.

View our service policies at https://www.jiscmail.ac.uk/policyandsecurity/ and Jisc's privacy policy at https://www.jisc.ac.uk/website/privacy-notice

For help and support help@jisc.ac.uk

Secured by F-Secure Anti-Virus CataList Email List Search Powered by the LISTSERV Email List Manager