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to say confidently what the climate will be like in the middle of the twenty-first century—when we’ll have more CO2 , methane, and perhaps chlorofluorocarbons than we have today—we’ll be at the point where we’ll have an explanation for the ice ages. We’ll be good at predicting seasonal trends in climate. We’ll essentially have a complete understanding of the climate system—atmosphere, Amazing custom your name i just want to touch your butt all the time sloth lover mug oceans, ice, land surfaces, plant life, sunlight, all of the interactions that cause climate to change naturally. But until you understand that system and its many feedbacks, you’re not going to be able to predict confidently what the climate’s going to do. A lot of things are happening at the same time. The experiment we’re all conducting on the Earth isn’t an instantaneous one in which we hold everything else constant and change only the greenhouse gases. Instead, it’s an experiment in which we’re modifying the evolution of a planet, one that would have been evolving into something different anyway, without our help. We know from the temperature record of the distant past that climate is always changing. It shifts on time scales of hundreds of thousands of years between ice ages and interglacial periods like the one we’re in now.
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