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Kali74
reply to post by Krakatoa
Has it been 125,000 years since year 0 AD?
Kali74
reply to post by Krakatoa
Has it been 125,000 years since year 0 AD?
When Mt. Pinatubo erupted in the 90's it raised the annual temperature about 3 degrees for around 4 years or so.
Many warmers don't take into account the earth's ability to absorb damage or correct things out of the normal. The things that were causing warming 20 years ago are already gone.
Kali74
reply to post by Tinkerpeach
When Mt. Pinatubo erupted in the 90's it raised the annual temperature about 3 degrees for around 4 years or so.
Actually the Mt. Pinatubo eruption lowered global temperatures by .02 to .05 C over 3 years or so. Volcanic eruptions tend to put Sulphur Dioxide into the atmosphere which reflects sunlight.
Many warmers don't take into account the earth's ability to absorb damage or correct things out of the normal. The things that were causing warming 20 years ago are already gone.
According to who?
Ahh yes that was my mistake. My point was however that nature can and often does have far greater impact on the environment than humans do.
Many people point to the increase in carbon emissions since the industrial revolution as the reason for our current global warming and do not realize that the effects from pollutants put out in 1930 are no longer in the system today. There is no cumulative effect that lasts for decades.
we still need to determine how much of the warming can be directly related to human activity as opposed to natural.
Kali74
reply to post by bloodreviara
In my opinion, no, it's not too early to make determinations. For the past 450,000 years the trend was roughly 10k years warming, 90k years cooling. That trend very obviously broke at the industrial age. Could it be coincidence? Could there be some unknown factor? I highly doubt it. One thing, and only one thing was very different at the end of the 19th century.edit on 25-9-2013 by Kali74 because: (no reason given)
So, if we have halted the natural cooling trend (in your opinion), then haven't we, in effect, delayed a coming ice-age?
Do you have the data for these from the Vostock core samples to make a comparative graph?
Kali74
reply to post by Tinkerpeach
Isotopes are the Key
How can we distinguish between the different sources and sinks of carbon dioxide? Carbon dioxide, or CO2, contains the key piece of information within the carbon atoms themselves. Although it may seem that a carbon atom is just the same as every other carbon atom out there (perhaps they appear to all be clones of each other–where each looks and acts exactly the same), this is not the case.
In fact there are three isotopes of carbon atoms - all three react the same way in chemical reactions–the only chemical difference between them is that they have slightly different masses. The heaviest is carbon-14 (which, in the scientific world, is written as 14C), followed by carbon-13 (13C), and the lightest, most common carbon-12 (12C). Different carbon reservoirs “like” different isotopes, so the relative proportion of the three isotopes is different in each reservoir - each has its own, identifying, isotopic fingerprint. By examining the isotopic mixture in the atmosphere, and knowing the isotopic fingerprint of each reservoir, atmospheric scientists can determine how much carbon dioxide is coming and going from each reservoir, making isotopes an ideal tracer of sources and sinks of carbon dioxide.
NOAA