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The
radiative energy budget of the Earth is a balance between the
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absorption
of incoming SW (mainly visible) solar radiation and
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outgoing
LW (IR) thermal radiation.
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The
huge complexity of the physical processes that control these energy
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fluxes
means that we cannot presently model or predict many aspects of
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climate
and how it will change with adequate accuracy.
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Many
problems, e.g. :
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+Greenhouse warming vs. natural
variability?
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+How well balanced?
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+Role of clouds in equilibrium and in
feedback?….
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