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Aug - Nov
00
A Cold Wind Blows
A Listserver Discussion
Lynn Perkins asked a question on the listserver about the plumes seen on
Triton by Voyager. With the focus this issue being on Triton, Garry
Harwood's reply was quite timely.
"Wind is the most likely explanation for the plume
distortions you refer to. As I understand it Triton has polar caps
that might change with the seasons (although there's some speculation
about this) and the southern hemisphere was some ways into spring when
Voyager 2 flew past. What may be happening is that frost that has
formed during winter vaporizes during spring, increasing the local
atmospheric pressure. This tends to transport vapor away from that
region to the opposite colder hemisphere as the 165-year long Tritonian
'year' progresses, so as one cap shrinks its cousin on the opposite pole
might grow and vice versa. It's this migration of vapor from one
hemisphere to the other that is believed to be the source of Triton's 10
meters per sec or so wind.
"As to why the plume rises to a particular height where it
appears to be sheared off, if I recall correctly this is likely due to a
combination of the force with which the material is erupted (if we're
talking geysers) and buoyancy. The material in the plume is probably
somewhat warmer than the surrounding atmosphere, and at a certain height
the temperature of the atmosphere reverses - so the plume stops
rising. That's where the wind comes in and shears the plume off in
that right-angled pattern, taking the material downwind and causing the
streaks."

"The Surface of Triton"
By Don Dixon
Here Fellow member Don shows us a view of
Triton's surface with Neptune hanging in the sky. From Don's great
web site.
 Copyright © 2000 International Association of Astronomical
Artists
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