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Triton's atmosphere
ngunn
post Apr 14 2010, 11:13 AM
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Interesting news item:
http://www.spacedaily.com/reports/A_Summer...Triton_999.html
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pjam
post Apr 19 2010, 01:04 AM
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Thanks for posting the article link!
...There's also a recent UMSF discussion on Triton's atmosphere and aerobraking 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


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"We absolutely must leave room for doubt or there is no progress and there is no learning." -Richard P. Feynman
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Drkskywxlt
post Apr 20 2010, 12:21 AM
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QUOTE (pjam @ Apr 18 2010, 08:04 PM) *
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


From the article:
QUOTE
As Triton's southern hemisphere warms up, a thin layer of frozen nitrogen, methane, and carbon monoxide on Triton's surface sublimates into gas, thickening the icy atmosphere as the season progresses during Neptune's 165-year orbit around the Sun. A season on Triton lasts a little over 40 years, and Triton passed the southern summer solstice in 2000.

Based on the amount of gas measured, Lellouch and his colleagues estimate that Triton's atmospheric pressure may have risen by a factor of four compared to the measurements made by Voyager 2 in 1989, when it was still spring on the giant moon.


I can't imagine what mechanism would make the geysers seasonal on their own. More likely they're due to internal processes.
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Rob Pinnegar
post Apr 23 2010, 02:54 PM
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QUOTE (Drkskywxlt @ Apr 19 2010, 05:21 PM) *
I can't imagine what mechanism would make the geysers seasonal on their own. More likely they're due to internal processes.


That's certainly possible; however, I seem to remember reading at one time that they could also be due to solar heating.

It's been a long time since then, but I think 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?
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