Interesting news item:
http://www.spacedaily.com/reports/A_Summer_Sky_Of_Methane_And_Carbon_Monoxide_Lights_Up_Triton_999.html
Thanks for posting the article link!
...There's also a recent UMSF discussion on http://www.unmannedspaceflight.com/index.php?showtopic=3768 where this 40 year seasonal variability in atm pressure might play into plans for aerobraking a spacecraft!
I wonder what the mechanism is for seasonal growth of atmosphere -is it mostly from sublimation or is there a major role for the geysers?
-pjam
That's right- in that case they would be quite similar to the "arachnoid" features seen on the subliming Martian polar cap.
The problem is that we have almost no data on the Triton plumes- just a handful of very low resolution images and some poorly-constrained models. My money is on the plumes being essentially meteorological (in the broad sense of including seasonal frost phenomena) rather than geological. I'm not yet ready to include Triton with Earth, Io, and Enceladus in the club of worlds proven to be currently geologically active.
John
"the basic idea was that some sunlight could be getting through the top layer of ice, and warming the nitrogen beneath it. Phil, do you remember this one?"
Yes, Rob - it was called a solid-state greenhouse, I think, though that term has been used for other places like Europa as well. I agree with John that it's premature to call Triton geologically active, though it's clearly been active in the not too distant past. It looks quite a bit older than Europa, but not as old as Ganymede (recognizing the limitations of our imaging coverage). But it's quite active in an atmosphere-surface-solar heating sense - there of course it's far ahead of Europa. Winds, plumes, frosts etc. Truly a fascinating place. Gotta go back!
Phil
Interesting distinctions emerging: geologically "exoactive" vs. "endoactive" worlds. Io is manifestly exoactive, so when discussing Triton aren't we talking about differences in magnitude of activity rather than anything else?
Seems as if endoactivity requires a body of a certain size. Earth & probably Venus are currently endoactive, Mars once was, might still be at very low levels. Io, Enceladus & Triton are exoactive, maybe Pluto will prove to be as well (solar heating + tidal effects from Charon?); Titan might be either a borderline or hybrid case.
I agree these categories trigger interesting trains of thought. I suspect though the primary distinction for most planetary scientists would be between activity arising from an internal heat source, however generated, and processes driven by sunlight. True, tidal heating comes from outside, but in the widest sense so does the radioactivity from heavy atoms produced in a supernova. So I think there are two separate questions to ask of any candidate world:
When and how did/do you acquire the energy that drives your active processes?
What materials are involved in the activity and over what range of temperatures?
If we're lucky, New Horizons will find analogous plumes on Pluto and will give us much better data on them than Voyager could do at Triton. Though it's more likely that Pluto will come up with its own quite different but equally bizarre phenomena to amaze us.
John
Yeah...if there's anything like a consistent truism in planetary exploration it's that if we expect A, admit that B is possible, what we actually find is X...
And then of course we find A somewhere else entirely. It's been said that all hypothesized solar system phenomena turn out to be real, just not necessarily on the worlds where they were first proposed. Thus we find Percival Lowell's canals on Europa, not Mars; Transient Lunar Phenomena on Io, not our own moon; lakes of exotic liquid on Titan, not Triton; high-albedo volcanic plains on Mercury, not our Moon, and so on.
John
We'll probably discover the Sirens on Ceres then.
Who?
--Bill
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