The following information is provided by the British Antarctic  Society.
It squares with everything that I have seen on the same subject. 
Ice cores don't lie. They also totally demolish all conceivable
arguments made by "young earthers."
 
Relevant here is what the cores tell us about climate change. In the  past
there have, yes,  been massive changes in climate. All ( all )  however,
not counting gigantic asteroids and their effects, have been gradual,
with changes spread out over thousands of years.
 
What we are seeing now is unprecedented rapid atmospheric  deterioration.
The start of the process can be traced to the 19th century but takeoff  
begins
in about 1900 and has accelerated ever since.  Or has accelerated  until
very recently with implementation of environmental regulations in the
leading industrial nations since about 1980 or 1990. Data are still  fuzzy
about a "leveling off" but some slow down in increases seems  obvious
enough. This leaves us at crisis levels even if things are not as  dire
as environmental alarmists want us to believe.
 
The Left, unfortunately, seems to consist of 90 % alarmists.
 
However, the Right seems to consist of 90 % climate change deniers.
 
Which is worse ?  Take your pick.
 
Here are the basic facts that ice core evidence provides, with a 
short synopsis from the conclusion of the article to lead things  off,.
Anyone who insists that climate change is false has the  burden
of proof.  Where is the evidence that contravenes ice core data ? 
It is NOT "proof" to point out that some questionable researchers 
(alarmists) have cooked their books in other areas of study.
 
The question is ice-core specific.  What evidence exists that  in any way
contravenes ice core evidence ?  As far as I know there is no such 
counter evidence at all.  Therefore deniers necessarily argue on the  basis 
of ad hominem attacks or evasions or red herrings,
none of which is valid as science.
 
Anyway, the article recommends itself. And it is consistent with a  large
number of  other studies, including those from Scientific  American,
that are available on the Web.
 
Billy
 
-------------------------------------------------------------------
 
 
 
    *   Ice core. Cylinder of ice drilled out of an ice sheet or  glacier. 
Most ice core records come from Antarctica and Greenland. 
    *   Ice cores contain information about past temperature, and about 
many other  aspects of the environment. 
    *   Atmospheric carbon dioxide levels are now nearly 40% higher than 
before  the industrial revolution. This increase is due to fossil fuel usage 
and  deforestation. 
    *   The magnitude and rate of the recent increase are almost certainly  
unprecedented over the last 800,000 years. 
    *   Methane also shows a huge and unprecedented increase in 
concentration over  the last two centuries.

--------------------------------------------------------------
 
 
Ice cores and climate change
 
_Home_ (http://www.antarctica.ac.uk/)  » _BAS Research_ 
(http://www.antarctica.ac.uk/bas_research/index.php)  » _Science  Briefings_ 
(http://www.antarctica.ac.uk/bas_research/science_briefings.php)  » _Ice  cores 
and climate 
change_ 
(http://www.antarctica.ac.uk/bas_research/science_briefings/icecorebriefing.php)
  » 

 
Slices of ice core, drilled from the depths of the Earth’s ice  sheets 
reveal details of the planet’s past climate 
Introduction
Ice cores are cylinders of ice drilled out of an ice sheet or glacier. Most 
 ice core records come from Antarctica and Greenland, and the longest ice 
cores  extend to 3km in depth. The oldest continuous ice core records to date 
extend  123,000 years in Greenland and 800,000 years in Antarctica. Ice 
cores contain  information about past temperature, and about many other aspects 
of the  environment. Crucially, the ice encloses small bubbles of air that 
contain a  sample of the atmosphere — from these it is possible to measure 
directly the  past concentration of gases (including carbon dioxide and 
methane) in the  atmosphere. 
Greenhouse gases and the recent past_   
 
Fig 1: Measurements of CO2 from the Law Dome ice  core(1) fall onto the 
line of annual average atmospheric measurements  from South Pole(2)

_ 
(http://www.antarctica.ac.uk/press/journalists/resources/science/images/001.jpg)
 
Direct and continuous measurements of carbon dioxide (CO2) in the  
atmosphere extend back only to the 1950s. Ice core measurements allow us to  
extend 
this way back into the past. In an Antarctic core (Law Dome) with a very  
high snowfall rate, it has been possible to measure concentrations in air from 
 as recently as the 1980s that is already enclosed in bubbles within the 
ice.  Comparison with measurements made at South Pole station show that the 
ice core  acts as a faithful recorder of atmospheric concentrations (see Fig. 
1), although  we do have to be cautious, as artefacts can arise at sites 
with high  concentrations of other impurities. 
Antarctic ice cores show us that the concentration of CO2 was  stable over 
the last millennium until the early 19th century. It then started to  rise, 
and its concentration is now nearly 40% higher than it was before the  
industrial revolution (see Fig. 2). Other measurements (e.g. isotopic data)  
confirm that the increase must be due to emissions of CO2 from fossil  fuel 
usage and deforestation. Measurements from older ice cores (discussed  below) 
confirm that both the magnitude and rate of the recent increase are  almost 
certainly unprecedented over the last 800,000 years. _ 
 
Fig 2: CO2 and CH4 over the last 1,000  years(1-4)

_ 
(http://www.antarctica.ac.uk/press/journalists/resources/science/images/002.jpg)
 The fastest large natural increase measured  in older ice cores is 
around 20ppmv (parts per million by volume) in 1000 years  (a rate seen 
during Earth’s emergence from the last ice age around 12,000 years  ago). CO2 
concentration increased by the same amount, 20ppmv, in the  last 11 years! 
Methane (CH4), another important greenhouse gas, also  shows a huge and 
unprecedented increase in concentration over the last two  centuries. Its 
concentration is now much more than double its pre-industrial  level. This is 
mainly 
due to the increase in emissions from sources such as rice  fields, ruminant 
animals and landfills, that comes on top of natural emissions  from wetlands 
and other sources.  
Natural climate changes: glacial-interglacial cycles  
 
(http://www.antarctica.ac.uk/images/image.php?id=53616c7465645f5f4ef4aac34eb4d219edd0574838ac612ba5d2209cc449fcbe)
  
A slice of ice core containing tiny bubbles of ancient  air.


By measuring the ratios of different water isotopes in polar ice cores, we  
can determine how temperature in Antarctica and Greenland has changed in 
the  past. The oldest ice core we have was drilled by the European Project for 
Ice  Coring in Antarctica (EPICA) from Dome C on the Antarctic plateau. It 
extends  back 800,000 years and shows a succession of long cold ‘glacial’ 
periods,  interspersed roughly every 100,000 years by warm ‘interglacial’ 
periods (of  which the last 11,000 years is the most recent). This succession 
of events is  well-known from other records, and the coldest periods in 
Antarctica are the  times when we had ice ages. Ice sheets extended over North 
America as far south  as Wisconsin, and over Britain to south of The Wash. 
The role of greenhouse gases in glacial-interglacial cycles
_  
Fig 3: Ice core data from the EPICA Dome C (Antarctica)  ice core: 
deuterium ( D) is a proxy for local temperature; CO2 from  the ice core air(5,6)

_ 
(http://www.antarctica.ac.uk/press/journalists/resources/science/images/003.jpg)
 From the air in our oldest  Antarctic ice core, we can see that CO2 
changed in a remarkably  similar way to Antarctic climate, with low 
concentrations during cold times, and  high concentrations during warm periods 
(see 
Fig. 3). This is entirely  consistent with the idea that temperature and CO2 
are intimately  linked, and each acts to amplify changes in the other (what 
we call a positive  feedback).It is believed that the warmings out of 
glacial periods are paced by  changes in Earth’s orbit around the Sun, but the 
tiny changes in climate this  should cause are amplified, mainly by the 
resulting increase in CO2,  and by the retreat of sea ice and ice sheets (which 
leads to less sunlight being  reflected away). Looking at the warming out of 
the last glacial period in  detail, we can see how remarkably closely 
Antarctic temperature and  CO2 tracked each other. _ 
 
Fig 4: Close-up of deuterium (temperature proxy) and  CO2 from the EPICA 
Dome C ice core over the warming from the last  glacial period.(7)

_ 
(http://www.antarctica.ac.uk/press/journalists/resources/science/images/004.jpg)
 It is often said that the  temperature ‘leads’ the CO2 during the 
warming out of a glacial  period. On the most recent records, there is a hint 
that the temperature started  to rise slightly (at most a few tenths of a 
degree) before the CO2,  as expected if changes in Earth’s orbit cause an 
initial small warming. But for  most of the 6,000-year long ‘transition’, 
Antarctic temperature and  CO2 rose together, consistent with the role of CO2 
as 
an  important amplifier of climate change (see Fig. 4). In our modern era, 
of  course, it is human emissions of CO2 that are expected to kick-start  
the sequence of events. We see no examples in the ice core record of a major  
increase in CO2 that was not accompanied by an increase in  temperature. 
Methane concentration also tracks the glacial-interglacial changes,  probably 
because there were less wetlands in the colder, drier glacial periods.  
Abrupt climate changes
The climate changes described above were huge, but relatively gradual.  
However, ice cores have provided us with evidence that abrupt changes are also  
possible. During the last glacial period, Greenland experienced a sequence 
of  very fast warmings (see Fig. 5). _ 
 
Fig 5: Oxygen isotope ratio (temperature proxy) from the  NorthGRIP 
(Greenland) ice core showing a sequence of rapid temperature  jumps.(8)

_ 
(http://www.antarctica.ac.uk/press/journalists/resources/science/images/005.jpg)
 The temperature increased by more than 10°C  within 40 years. Other 
records show us that major changes in atmospheric  circulation and climate 
were experienced all around the northern hemisphere.  Antarctica and the 
Southern Ocean experienced a different pattern, consistent  with the idea that 
these rapid jumps were caused by sudden changes in the  transport of heat in 
the ocean. At this time, there was a huge ice sheet (the  Laurentide) over 
northern North America. Freshwater delivered from the ice sheet  to the North 
Atlantic was able periodically to disrupt the overturning of the  ocean, 
causing the transport of tropical heat to the north to reduce and then  
suddenly increase again. While this mechanism cannot occur in the same way in  
today’s world, it does show us that, at least regionally, the climate is 
capable  of extraordinary changes within a human lifetime: rapid switches we 
certainly  want to avoid experiencing.  
Summary
Ice cores provide direct information about how greenhouse gas 
concentrations  have changed in the past, and they also provide direct evidence 
that the 
climate  can change abruptly under some circumstances. However, they provide 
no direct  analogue for the future because the ice core era contains no 
periods with  concentrations of CO2 comparable to those of the next century. 
Factfile
    *   Ice core. Cylinder of ice drilled out of an ice sheet or  glacier. 
Most ice core records come from Antarctica and Greenland. 
    *   Ice cores contain information about past temperature, and about 
many other  aspects of the environment. 
    *   Atmospheric carbon dioxide levels are now nearly 40% higher than 
before  the industrial revolution. This increase is due to fossil fuel usage 
and  deforestation. 
    *   The magnitude and rate of the recent increase are almost certainly  
unprecedented over the last 800,000 years. 
    *   Methane also shows a huge and unprecedented increase in 
concentration over  the last two centuries.
Data sources
    1.  MacFarling Meure, C., and others: Law Dome CO2, CH4  and N2O ice 
core records extended to 2,000 years BP, Geophys. Res. Lett., 33, L14810, 
doi:10.1029/2006GL026152,  2006 
    2.  Atmospheric data supplied by NOAA/ESRL 
    3.  Friedli, H., and others: Ice core record of the 13C/12C ratio of  
atmospheric CO2 in the past two centuries, Nature, 324, 237–238, 1986 
    4.  Siegenthaler, U., and others: Supporting evidence from the EPICA 
Dronning  Maud Land ice core for atmospheric CO2 changes during the past  
millennium, Tellus Ser. B-Chem. Phys.  Meteorol., 57, 51–57, 2005 
    5.  Jouzel, J., and others: Orbital and millennial Antarctic climate  
variability over the last 800,000 years, Science, 317, 793–796, 2007 
    6.  Lüthi, D., and others: High-resolution carbon dioxide concentration 
record  650,000–800,000 years before present, Nature, 453, 379–382, 2008 
    7.  Monnin, E., and others: Atmospheric CO2 concentrations over the 
last  glacial termination, Science, 291, 112–114, 2001 with data converted to 
the age  scale of Parrenin, F., and others: The EDC3 chronology for the EPICA 
Dome C  ice core, Climate of the Past, 3, 485–497, 2007 
    8.  North Greenland Ice Core Project Members: High-resolution record of 
 Northern Hemisphere climate extending into the last interglacial period, 
Nature, 431, 147–151,  2004

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