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There is now a CONTENT FREEZE for Mercury while we switch to a new platform. It began on Friday, March 10 at 6pm and will end on Wednesday, March 15 at noon. No new content can be created during this time, but all material in the system as of the beginning of the freeze will be migrated to the new platform, including users and groups. Functionally the new site is identical to the old one. webteam@gatech.edu
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How many Snowballs out there?
Planetary climates are complex systems that include a multitude of stabilizing (negative) and destabilizing (positive) feedback loops. One of them, the ice-albedo feedback, is possibly causing multiple stable states in Earth’s climate, with the alternation between ice-covered conditions (the most extreme being the so-called Snowball) and warm states. Here, we adopt the view of climate as a dynamical system, strip down its complexity using a simple one-dimensional Energy Balance Model called ESTM and explore the conditions leading to bistability in the climate of Earth-like planets, briefly recalling the potential role of stochastic resonance.
We shall then consider the effects of the ice-albedo feedback for a wide range of orbital and planetary parameters such as distance from the star, ellipticity, obliquity and atmospheric pressure. Other mechanisms for bistability will be mentioned, such as the vegetation-albedo and vegetation-moisture feedbacks, and the crucial role of atmospheric composition. Implications on planetary habitability will finally be considered.