Generalized Milankovitch Cycles and Longterm Climatic Habitability
David S. Spiegel (1), Sean N. Raymond (2), Courtney D. Dressing (1),, Caleb A. Scharf (3), Jonathan L. Mitchell (4) ((1) Princeton University, (2), Universite de Bordeaux, (3) Columbia University, (4) UCLA)

TL;DR
This paper explores how Milankovitch-like orbital variations can influence the climate stability and habitability of exoplanets, especially in relation to snowball states and the effects of giant planets on orbital eccentricity.
Contribution
It introduces a simple algorithm for modeling ice melt on frozen planets and analyzes how giant planets can induce eccentricity oscillations affecting habitability.
Findings
Eccentricity oscillations can melt snowball planets.
Giant planets can cause extreme eccentricity variations.
Long-term habitability depends on planetary system architecture.
Abstract
Although the Earth's orbit is never far from circular, terrestrial planets around other stars might experience substantial changes in eccentricity that could lead to climate changes, including possible "phase transitions" such as the snowball transition (or its opposite). There is evidence that Earth has gone through at least one globally frozen, "snowball" state in the last billion years, which it is thought to have exited after several million years because global ice-cover shut off the carbonate-silicate cycle, thereby allowing greenhouse gases to build up to sufficient concentration to melt the ice. Due to the positive feedback caused by the high albedo of snow and ice, susceptibility to falling into snowball states might be a generic feature of water-rich planets with the capacity to host life. This paper has two main thrusts. First, we revisit one-dimensional energy balance…
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