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So how
might orbital variations cause ice ages?
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One idea
is that since the ice sheets melt the most
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in the
summertime, the sunshine during this time
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of year
might be important for determining ice
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volume.
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But
exactly how orbital variability is translated into
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the huge
observed climate changes remains one
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of the
major unsolved problems of climate.
Any
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satisfactory
explanation will probably involve the
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dynamics
of the ice sheets themselves.
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