Physical Society Colloquium
How the physics of clouds affects Snowball Earth and
the runaway greenhouse
Geophysical Sciences University of Chicago
The physics of clouds has a huge impact on the climate of a planet. On Earth,
if the clouds forgot that part of their job is to reflect solar energy, we
would suffer a runaway greenhouse and end up like Venus. If instead clouds
forgot that part of their job is to absorb infrared radiation emitted by
the surface and contribute to the greenhouse effect, we would enter global
glaciation. Although they are very important for climate, clouds are very
difficult to model and represent the largest source of uncertainty in climate
modeling. This results both from insufficient resolution to resolve cloud-scale
circulation and incomplete understanding of cloud microphysics. Cloud
simulation is therefore the main reason our current models aren't better,
and is a critical area to attack if we want to create generalized models that
could be easily applied to different planets (the clouds might not be water
clouds in this case). In this talk I will discuss how we can use the models
we have to gain insight into cloud behavior in climates vastly different from
modern Earth. The two examples I will focus on are the Snowball Earth episodes
that occurred 600-800 million years ago and the runaway greenhouse of tidally
locked super-Earths at the inner edge of the habitable zone of M-stars.
Friday, April 11th 2014, 15:30
Ernest Rutherford Physics Building, Keys Auditorium (room 112)
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