Snowball
Earth is an interesting hypothesis and shows us some things about the
climate
system of Earth - that it is a complex dynamic system with many
variables.
The more recent snowball Earth glaciations are thought to have happened
as
three or four glaciation events with the most recent, the Marinoan,
happening
about 650 million years ago. At the beginning of these glaciations the
CO2 was
relatively low for the time and the continents were distributed around
the
equator.
The mechanism which started the cooling periods is not known, but if
they are
cold enough the resulting ice can spread down to close to the equator.
As ice
has a higher albedo, about ~60% compared to the sea which reflects
about 6% of
incoming light, we get a "positive" feedback where cooling reflects
more of the suns energy away from the Earth causing more cooling. This
locked
the Earth into a frozen period for millions of years. This poses a
problem how
can the climate system unfreeze now most of the Sun's energy is
reflected away?
With much of the Earth frozen, CO2 will build up as there is very
little rock
weathering as it is all covered by ice and not much photosynthesis
either. By
the end of the snowball Earth period, CO2 may have risen to 12,000 ppm.
The
warming effect of the CO2 would have been weaker in this frozen state
then it
is now, because CO2 traps infrared radiation while most of the sun's
light was
being reflected in the visible part of the spectrum. This is why the
CO2 level
had to raise to such a high level to bring us out of this cold phase
even
though we are presently in a much warmer climate with less CO2. This
is
physics!