The first paper quoted in this thread seems to suggest that any significant global water coverage would help to stabilize a planet's climate.
I would expect that if a planet that were close to its star had more severe seasonal variations than a planet farther away, it would be more attributable to being in a steeper temperature gradient than the atmosphere adapting to the changes.
Imagine a pot of water, if you crank the temperature up, then down, then up in rapid succession, the water doesn't have much time to react to the changes in temperature, so the temperature would oscillate less than if you were to walk away and do something else in-between adjusting the temperature. But of course the temperature the planet is does not scale linearly with the distance to the star, so more extreme seasons (I would assume) would be expected for a closer in planet than a farther out planet.
Maybe geological lag (I'm sure there's a real term for that) would help to keep the year roughly stable. Recall that Pluto's atmosphere has gotten denser since it passed through perihelion. Even as Pluto gets farther from the sun, its atmosphere thickens. Maybe for some planets, eccentricity-related effects are damped out by other processes, in addition to the "thermal inertia" provided by ocean cover.
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