http://www.skepticalscience.com/print.php?n=1785
No alternative to atmospheric CO2 draw-down

This article suggests that the current atmospheric CO2 level is already 
triggering amplifying feedbacks from the Earth system and therefore, in 
themselves, efforts at reduction in atmospheric CO2-emission are no longer 
sufficient to prevent further global warming. For this reason, along with sharp 
reductions in carbon emissions, efforts need to be undertaken in an attempt to 
reduce atmospheric CO2 levels from their current level of near-400 ppm to well 
below 350 ppm. NASA-applied outer space-shade technology may buy time for such 
planetary defense effort.

The scale and rate of modern climate change have been greatly underestimated. 
The release to date of a total of over 560 billion ton of carbon through 
emissions from  industrial and transport sources, land clearing and fires, has 
raised CO2 levels from about 280 parts per million (ppm) in pre-industrial 
periods to 397-400 ppm and near 470 ppm CO2-equivalent (a value which includes 
the CO2-equivalent effect of methane), reaching a current CO2 growth rate of 
about 2 ppm per year<http://www.globalcarbonproject.org/>

[http://www.skepticalscience.com/pics/glikson_figure1.gif]

Figure 1: Part A. Mean CO2 level from ice cores, Mouna Loa observatory and 
marine sites; Part B (inset). Climate forcing 1880 - 
2003<http://pubs.giss.nasa.gov/abs/ha06510a.html>. Aerosol forcing includes all 
aerosol effects, including indirect effects on clouds and snow albedo. GHGs 
include ozone (O3) and stratospheric H2O, in addition to well-mixed greenhouse 
gases.

[http://www.skepticalscience.com/pics/glikson_figure2.gif]

Figure 2: Relations between CO2 rise rates and mean global temperature rise 
rates during warming periods<http://cci.anu.edu.au/files/download/?id=4951>, 
including the Paleocene-Eocene Thermal Maximum, Oligocene, Miocene, glacial 
terminations, Dansgaard-Oeschger cycles and the post-1750 period.

These developments are shifting the Earth's climate toward Pliocene-like (5.2 - 
2.6 million years-ago; mean global temperatures of +2-3oC above pre-industrial 
temperatures) and possibly toward mid-Miocene-like (approximately 16 million 
years-ago; mean global temperatures +4oC above pre-industrial 
temperatures<http://www.nature.com/ngeo/journal/v4/n7/fig_tab/ngeo1186_ft.html>)
 conditions within a few centuries--a geological blink of an eye.

The current CO2 level generates amplifying feedbacks, including the reduced 
capacity of warming water to absorb CO2 from the atmosphere, CO2 released from 
fires, droughts, loss of vegetation cover, disintegration of methane released 
from bogs, permafrost and methane-bearing ice particles and methane-water 
molecules.

With CO2 atmospheric residence times in the order of thousands to tens of 
thousands 
years<http://www.pnas.org/content/early/2009/01/28/0812721106.abstract>, 
protracted reduction in emissions, either flowing from human decision or due to 
reduced economic activity in an environmentally stressed world, may no longer 
be sufficient to arrest the feedbacks.

Four of the large mass extinction of species events in the history of Earth 
(end-Devonian, Permian-Triassic, end-Triassic, K-T boundary) have been 
associated with rapid perturbations of the carbon, oxygen and sulphur cycles, 
on which the biosphere depends, at rates to which species could not 
adapt<http://theconversation.edu.au/is-another-mass-extinction-event-on-the-way-5397>.

Since the 18th century, and in particular since about 1975, the Earth system 
has been shifting away from Holocene (approximately 10,000 years to the 
pre-industrial time) conditions, which allowed agriculture, previously hindered 
by instabilities in the climate and by extreme weather events. The shift is 
most clearly manifested by the loss of polar 
ice<http://www.agu.org/pubs/crossref/2011/2011GL046583.shtml>. Sea level rises 
have been accelerating, with a total of more than 20 cm since 1880 and about 6 
cm since 
1990<http://www.eea.europa.eu/data-and-maps/indicators/sea-level-rise-1/assessment>.

For temperature rise of 2.3oC, to which the climate is committed if sulphur 
aerosol emission discontinues<http://pubs.giss.nasa.gov/abs/ha06510a.html> (see 
Figure 1), sea levels would reach Pliocene-like levels of 25 meters plus or 
minus 12 meters, with lag effects due to ice sheet hysteresis (system inertia).

With global atmospheric CO2-equivalent (a value which includes the effect of 
methane) above 470 ppm, just under the upper stability limit of the Antarctic 
ice sheet<http://www.columbia.edu/~jeh1/2008/TargetCO2_20080407.pdf>, with 
current rate of CO2 emissions from fossil fuel combustion, cement production, 
land clearing and fires of ~9.7 billion ton of carbon in 
2010<http://www.science.org.au/natcoms/nc-ess/documents/GEsymposium.pdf>, 
global civilization faces the following alternatives:

  1.  With carbon reserves sufficient to raise atmospheric CO2 levels to above 
1000 ppm<http://www.columbia.edu/~jeh1/mailings/.../20120130_CowardsPart2.pdf>, 
continuing business-as-usual emissions can only result in advanced melting of 
the polar ice sheets, a corresponding rise of sea levels on the scale of meters 
to tens of meters, on a time scale of decades to centuries, and high to extreme 
continental temperatures rendering agriculture and human habitat over large 
regions 
unlikely<http://www.ccrc.unsw.edu.au/staff/profiles/sherwood/wetbulb.html>.
  2.  With atmospheric CO2 at about 400 ppm, abrupt decrease in carbon 
emissions may no longer be sufficient to prevent current feedbacks (melting of 
ice, methane release from permafrost, fires). Attempts to stabilize the climate 
require global efforts at CO2 draw-down, using a range of methods, including 
global reforestation, extensive biochar application, chemical CO2 sequestration 
(using sodium hydroxide, serpentine and new innovations) as well as burial of 
CO2<http://www.science.org.au/natcoms/nc-ess/documents/GEsymposium.pdf>.

As indicated in Table 1, the use of short-term solar radiation shields such as 
sulphur aerosols cannot be regarded as more than a band aid, with severe 
deleterious consequences in terms of ocean acidification and retardation of the 
monsoon and of precipitation over large parts of the Earth.

[http://www.skepticalscience.com/pics/glikson_table1.gif]

By contrast, retardation of solar radiation through space sunshade 
technology<http://www.sciencedaily.com/releases/2006/11/061104090409.htm> may 
allow time for CO2 draw-down. Unlike sulphur dioxide injections this will not 
have ocean acidification effects - an effort requiring a planetary defense 
project by NASA.

Dissemination of ocean iron 
filings<http://newswatch.nationalgeographic.com/2012/10/18/iron-fertilization-savior-to-climate-change-or-ocean-dumping/>
 aimed at increasing fertilization by plankton and algal blooms, or temperature 
exchange through vertical ocean pipe 
systems<http://www.realclimate.org/index.php/archives/2007/04/ocean-cooling-not/>,
 are unlikely to constitute effective means of transporting CO2 to relatively 
safe water depths.

By contrast to these methods, CO2 sequestration through fast track 
reforestation, soil carbon, biochar and possible chemical methods such as 
"sodium 
trees"<http://www.realclimate.org/index.php/archives/2007/04/ocean-cooling-not/>
 and serpentine (combining Ca and Mg with 
CO2<http://onlinelibrary.wiley.com/doi/10.1002/cjce.5450810373/abstract>) may 
be effective, provided these are applied on a global scale

Such efforts will require an effective planetary defense effort on the scale 
currently expended on military spending (totaling more than $20 trillion since 
WWII).

It is likely that a species which decoded the basic laws of nature, split the 
atom, placed a man on the moon and ventured into outer space should also be 
able to develop the methodology for fast sequestration of atmospheric CO2. The 
alternative, in terms of global heating, sea level rise, extreme weather 
events, and the destruction of the world's food sources is unthinkable.

Good planets are hard to come by.

Posted by Andrew Glikson on Thursday, 14 February, 2013

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