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q |
Small variations in received insolation do occur in connection with
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Earth’s eccentric orbit about the Sun, but these appear only as
changes
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in the total energy received by the entire Earth, not as seasonal
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variations.
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q |
Compared to the changes in seasonal insolation of 10% or more that
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occur at the tilt and precession cycles, these annual eccentricity
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changes are smaller by a factor of 50 or more.
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