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tropical insolation was actually reduced, as was winter insolation at higher northern latitudes. That makes these natural past changes in radiative forcing very different from those associated with modern greenhouse increases which are positive during both seasons, in both hemispheres, and in the tropics as well as high latitudes. Let’s start out with a look at the longest timescale changes that are documented in the geological record. We’re talking hundreds of millions of year timescales. While the records are imperfect at best, we do have a rough idea from very old sedimentary Amazing roses are red foxes are clever i like your butt let me touch it forever coffee mug records as to the broad-scale changes in global temperatures and in atmospheric CO2 over these timescales. On these very long timescales, the changes in atmospheric CO2 are related to geologic processes such as plate tectonics, which govern the outgassing of CO2 from Earth’s interior by volcanoes, and the slow changes in Earth’s continental configuration and relief, which influence natural processes such as chemical and physical weathering that take CO2 out of the atmosphere. What about the number of Atlantic TCs, including the hyperactive 2005 season with its 28 named
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