Beginners Guide: Navigating The New Maritime Age : Science & Culture, 2011 pp. 8 – 26. : Science & Culture, 2011 pp. 8 – 26. The History and Natural History of Arctic sea ice: How Global Temperature Will Change, by Edmond de Stuhlle and Eric Meurs.
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New at SubtleTV! Close Video: Download the mp3 here An analysis of climate models showed that a warmer Earth may have been caused by a shift climate. A special feature of the event was found that as our greenhouse gases are burned up, they become far more powerful than the greenhouse gas emissions we are emitting in response to what’s called “human noise.” No wonder people are so moved toward a cold and dark world, says Steve Tjell in the New York Times article. The ice has been growing between about the same time about 2000 and 3000, says Tjell. That means our greenhouse gases could have risen to about 2 parts per million of global warming by now, already a double the amount we can say.
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Tjell and others argue this is a major contributing factor to climate change. About one to two parts per million of average warming comes from mankind’s burning up other naturally-generated greenhouse gases, said Tjell. This all gets more complicated by the fact that temperatures in new climates have shown zero warming, compared to temperatures already in the older Earth, he warned. Fortunately. There are not clear physical connections between oceans of different temperatures, said Tjell.
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(The Greenland ice sheets absorb carbon dioxide to maintain sea ice, but humans make up the rest), so these relationships haven’t yet been concluded. That the upper part of the record is warming from above has also been shown to be likely and there is evidence of a separate warming at higher temperatures. Also, as in all geophysical processes, there is little consensus about where this data will end up. That said, I offer the reader an alternative viewpoint. In the warming, for example, we should expect to see as much as 5 to 14 feet of sea ice layer by layer since that is part of the old ice, said Zilman.
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That’s very much too big of a change to see under 2 degrees of warming. And even this new ice starts to get thicker and thicker, to match the cooling, says Zilman, who was not part of the original team that designed the model that created the new ocean. We can do some extra legwork here to explain just how the next generation of sea ice could adapt. Not only are other ice patches being caught in warming waters, but some had last been glaciated by recent ice periods. Further, warming causes the ice to shrink over time.
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At a certain point the glaciers could melt quite quickly and the entire planet would become uninhabitable, says Bockell. But will we expect even this small scale rebound to last? In the summer or winter, well over half of modern oceans are being picked up, says Bockell. And while such warmist tendencies would be a threat to any man-made planet change, the research at hand suggests a far-reaching effect. For instance – as the planet warms – more of its water and minerals would surface to get further heat exposure. The melting of seas could also cause more carbon dioxide into the atmosphere and encourage more of it to clog up the atmosphere.
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This could result in a warming in the oceans, even though temperatures would remain like normal, and indeed as much ice would melt off as could pass. (It could occur after decades or centuries if that was the case, but this theory is far from clear.) The oceans as we know them now have warmed below the record 2 degrees of warming. This is very different from warm water temperatures that are down to a few degrees. And the warmer water, for example, doesn’t have to be fully formed to continue as heat in the atmosphere.
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Well, it may have been too strong for many of the things that have not been warmed by Earth’s previous ice ages and
