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q |
The 23,000-year cycle of
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precissional change
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dominants the insolation
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changes at low and middle
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latitudes.
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q |
The 41,000-year cycle of
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tilt change dominants the
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insolation changes at higher
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latitudes.
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q |
Eccentricity changes (the
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1000,000 or 413,000-year
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cycles) is not a significant
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influence on seasonal
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insolation chanes.
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