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Nuclear power was not available back then. We are discussing the situation today, not in 1800.RogueOne said:1.) Yes that probably is very hard to quantify, considering the life expectancy increases that the human race has enjoyed due to the industrial revolution (made possible by coal)
How exactly is that relevant here? I answered a question that is relevant, because I though that is more interesting.RogueOne said:2.) Thats a different question than what was asked. The correct answer is that if we halved the amount of atmospheric CO2 that we have right now, all of the crops as we know them would stop growing.
Water vapor is the largest contribution to the greenhouse effect, but the fraction of water vapor coming from humans is completely negligible. The fraction of atmospheric CO2 coming from humans is large - because CO2 stays in the atmosphere for a long time.RogueOne said:3.) Given that the water vapor has a lifetime of several days, but is released every day, How do we know that the water vapor is irrelevant as a greenhouse gas? Are there any potential benefits of the water vapor release? What negative aspects is the increase in water vapor capable of on local/global levels?
That won't happen for about a billion years. See all the history where plants survived many glacial cycles without problems.RogueOne said:Lets say temperature decreased in a few thousand years, as we leave this interglacial period, and slowed the carbonate silicate cycle to the point at which plant life was receiving insufficient CO2.
And if you think this would be an issue and we should care about it, then we should stop burning fossil fuels immediately - to save them for later.