[Coral-List] La Nina and global warming
David M. Lawrence
dave at fuzzo.com
Tue Nov 16 18:06:00 EST 2010
Some [arguably biased] highlights from the Geological Society of London
statement:
What are the grounds for concern?
* Evidence from the geological record is consistent with the physics
that shows that adding large amounts of carbon dioxide to the atmosphere
warms the world and may lead to: higher sea levels and flooding of
low-lying coasts; greatly changed patterns of rainfall2; increased
acidity of the oceans 3,4,5,6; and decreased oxygen levels in seawater7,8,9.
* There is now widespread concern that the Earth’s climate will warm
further, not only because of the lingering effects of the added carbon
already in the system, but also because of further additions as human
population continues to grow. Life on Earth has survived large climate
changes in the past, but extinctions and major redistribution of species
have been associated with many of them. When the human population was
small and nomadic, a rise in sea level of a few metres would have had
very little effect on Homo sapiens. With the current and growing global
population, much of which is concentrated in coastal cities, such a rise
in sea level would have a drastic effect on our complex society,
especially if the climate were to change as suddenly as it has at times
in the past. Equally, it seems likely that as warming continues some
areas may experience less precipitation leading to drought. With both
rising seas and increasing drought, pressure for human migration could
result on a large scale.
What is the Greenhouse Effect?
* The Greenhouse Effect arises because certain gases (the so-called
greenhouse gases) in the atmosphere absorb the long wavelength infrared
radiation emitted by the Earth’s surface and re-radiate it, so warming
the atmosphere. This natural effect keeps our atmosphere some 30ºC
warmer than it would be without those gases. Increasing the
concentration of such gases will increase the effect (i.e. warm the
atmosphere more)19.
Has sudden climate change occurred before?
* Yes. About 55 million years ago, at the end of the Paleocene, there
was a sudden warming event in which temperatures rose by about 6ºC
globally and by 10-20ºC at the poles22. Carbon isotopic data show that
this warming event (called by some the Paleocene-Eocene Thermal Maximum,
or PETM) was accompanied by a major release of 1500-2000 billion tonnes
or more of carbon into the ocean and atmosphere. This injection of
carbon may have come mainly from the breakdown of methane hydrates
beneath the deep sea floor10, perhaps triggered by volcanic activity
superimposed on an underlying gradual global warming trend that peaked
some 50 million years ago in the early Eocene. CO2 levels were already
high at the time, but the additional CO2 injected into the atmosphere
and ocean made the ocean even warmer, less well oxygenated and more
acidic, and was accompanied by the extinction of many species on the
deep sea floor. Similar sudden warming events are known from the more
distant past, for example at around 120 and 183 million years ago23,24.
In all of these events it took the Earth’s climate around 100,000 years
or more to recover, showing that a CO2 release of such magnitude may
affect the Earth’s climate for that length of time25.
How did levels of CO2 in the atmosphere change during the ice age?
* The atmosphere of the past 800,000 years can be sampled from air
bubbles trapped in Antarctic ice cores. The concentrations of CO2 and
other gases in these bubbles follow closely the pattern of rising and
falling temperature between glacial and interglacial periods. For
example CO2 levels varied from an average of 180 ppm (parts per million)
in glacial maxima to around 280 ppm during interglacials. During
warmings from glacial to interglacial, temperature and CO2 rose together
for several thousand years, although the best estimate from the end of
the last glacial is that the temperature probably started to rise a few
centuries before the CO2 showed any reaction. Palaeoclimatologists think
that initial warming driven by changes in the Earth’s orbit and axial
tilt eventually caused CO2 to be released from the warming ocean and
thus, via positive feedback, to reinforce the temperature rise already
in train28. Additional positive feedback reinforcing the temperature
rise would have come from increased water vapour evaporated from the
warmer ocean, water being another greenhouse gas, along with a decrease
in sea ice, and eventually in the size of the northern hemisphere ice
sheets, resulting in less reflection of solar energy back into space.
[DML: Note that this excerpt addresses Gene's point about warming
preceding CO2 increases.]
How has carbon dioxide in the atmosphere changed in recent times?
* Atmospheric CO2 is currently at a level of 390 ppm. It has increased
by one third in the last 200 years33. One half of that increase has
happened in the last 30 years. This level and rate of increase are
unprecedented when compared with the range of CO2 in air bubbles locked
in the ice cores (170-300 ppm). There is some evidence that the rate of
increase in CO2 in the atmosphere during the abrupt global warming 183
million years ago (Early Jurassic), and perhaps also 55 million years
ago (the PETM), was broadly similar to today’s rate34.
When was CO2 last at today’s level, and what was the world like then?
* The most recent estimates35 suggest that at times between 5.2 and 2.6
million years ago (during the Pliocene), the carbon dioxide
concentrations in the atmosphere reached between 330 and 400 ppm. During
those periods, global temperatures were 2-3°C higher than now, and sea
levels were higher than now by 10 – 25 metres, implying that global ice
volume was much less than today36. There were large fluctuations in ice
cover on Greenland and West Antarctica during the Pliocene, and during
the warm intervals those areas were probably largely free of
ice37,38,39. Some ice may also have been lost from parts of East
Antarctica during the warm intervals40. Coniferous forests replaced
tundra in the high latitudes of the Northern Hemisphere41, and the
Arctic Ocean may have been seasonally free of sea-ice42.
In conclusion - what does the geological record tell us about the
potential effect of continued emissions of CO2?
* Over at least the last 200 million years the fossil and sedimentary
record shows that the Earth has undergone many fluctuations in climate,
from warmer than the present climate to much colder, on many different
timescales. Several warming events can be associated with increases in
the ‘greenhouse gas’ CO2. There is evidence for sudden major injections
of carbon to the atmosphere occurring at 55, 120 and 183 million years
ago, perhaps from the sudden breakdown of methane hydrates beneath the
seabed. At those times the associated warming would have increased the
evaporation of water vapour from the ocean, making CO2 the trigger
rather than the sole agent for change. During the Ice Age of the past
two and a half million years or so, periodic warming of the Earth
through changes in its position in relation to the sun also heated the
oceans, releasing both CO2 and water vapour, which amplified the ongoing
warming into warm interglacial periods. That process was magnified by
the melting of sea ice and land ice, darkening the Earth’s surface and
reducing the reflection of the Sun’s energy back into space.
* While these past climatic changes can be related to geological events,
it is not possible to relate the Earth’s warming since 1970 to anything
recognisable as having a geological cause (such as volcanic activity,
continental displacement, or changes in the energy received from the
sun)43. This recent warming is accompanied by an increase in CO2 and a
decrease in Arctic sea ice, both of which – based on physical theory and
geological analogues - would be expected to warm the climate44.
* In the coming centuries, continued emissions of carbon from burning
oil, gas and coal at close to or higher than today’s levels, and from
related human activities, could increase the total to close to the
amounts added during the 55 million year warming event – some 1500 to
2000 billion tonnes. Further contributions from ‘natural’ sources
(wetlands, tundra, methane hydrates, etc.) may come as the Earth
warms22. The geological evidence from the 55 million year event and from
earlier warming episodes suggests that such an addition is likely to
raise average global temperatures by at least 5-6ºC, and possibly more,
and that recovery of the Earth’s climate in the absence of any
mitigation measures could take 100,000 years or more. Numerical models
of the climate system support such an interpretation44. In the light of
the evidence presented here it is reasonable to conclude that emitting
further large amounts of CO2 into the atmosphere over time is likely to
be unwise, uncomfortable though that fact may be.
Dave
On 11/16/2010 2:36 PM, Eugene Shinn wrote:
> Dear Listers, Good to see the neurons are firing on all cylinders.
> The Geological Society of London statement
> http://www.geolsoc.org.uk/gsl/views/policy_statements/climatechange
> is well done. It pretty much says what I have been trying to say. I
> was a little concerned that they did not put more emphasis on water
> vapor as the greatest green house gas or methane and others. But then
> the IPCC said little as well. Why are we all so stuck on Co2? Plants
> love it!
> Also, there was no mention that ice cores show warming occurred
> before Co2 peaked by at least 400 years. Shouldn't it be the other
> way around? I would like to suggest a new book by Robert Carter a
> well-respected Australian geologist/paleontologist. The title is,
> "Climate: The Counter Consensus.:
> The book is technical but easy reading and is not strident like so
> many anti AGW/IPCC publications. He even discusses corals and ocean
> acidification oops! I meant alkalinity shift, which he clearly
> explains. There is a lot about sea level rise and fall and how it
> depends on where you are. His major point is the IPCC is all about
> "projections" (their words) not predictions as the mass media and
> warming enthusiasts call it. Gene
>
--
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David M. Lawrence | Home: (804) 559-9786
7471 Brook Way Court | Fax: (804) 559-9787
Mechanicsville, VA 23111 | Email: dave at fuzzo.com
USA | http: http://fuzzo.com
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