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Andrew Yee's Oct. 9th post on the Eddington Probe (could detect moons
of extrasolar planets) got me wondering... What would be the chances of a rich earthlike biosphere evolving on an earth-mass moon of an extrasolar jovian planet in orbit -within- the so- called "habitable zone" of its star? This is obviously a difficult question involving huge numbers of factors, but the first factor occurring to me as I read that post was...what would the climate or seasons be like, since that 'earth'-moon would have not only seasonal variations through the year (depending on orbital eccentricity etc., axial tilt etc.), but some variations due to its monthly changes in distance from its home star due to its lunar orbit about the jovian. Hmm..now that I think about it, such changes might not add up to much since they would generally only be a tiny fraction of the planet's average distance from its star. Gene |
#2
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![]() "Gene Partlow" wrote in message om... Andrew Yee's Oct. 9th post on the Eddington Probe (could detect moons of extrasolar planets) got me wondering... What would be the chances of a rich earthlike biosphere evolving on an earth-mass moon of an extrasolar jovian planet in orbit -within- the so- called "habitable zone" of its star? This is obviously a difficult question involving huge numbers of factors, but the first factor occurring to me as I read that post was...what would the climate or seasons be like, since that 'earth'-moon would have not only seasonal variations through the year (depending on orbital eccentricity etc., axial tilt etc.), but some variations due to its monthly changes in distance from its home star due to its lunar orbit about the jovian. Hmm..now that I think about it, such changes might not add up to much since they would generally only be a tiny fraction of the planet's average distance from its star. You are right, the latter would be an insignificant effect for a habitable jovian moon orbiting a planet in the habitable zone. The moon would also have to be (a) large enough to retain a significant atmosphere (i.e., a lot larger than Mars but maybe not requiring to be as large as Earth), (b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. -- Mike Dworetsky (Remove "pants" spamblock to send e-mail) |
#3
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"Mike Dworetsky" wrote in message news:
Hmm..now that I think about it, such changes might not add up to much since they would generally only be a tiny fraction of the planet's average distance from its star. You are right, the latter would be an insignificant effect for a habitable jovian moon orbiting a planet in the habitable zone. The moon would also have to be (a) large enough to retain a significant atmosphere (i.e., a lot larger than Mars but maybe not requiring to be as large as Earth), (b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), Yes...the Van Allen Belt problem. I was ignoring this just to focus on the possible monthly climate changes. While I know about as much about chaos theory as Curly, I yet wonder if something like the much abused butterfly effect might still apply due to the 'cumulative' effects of countless small lunar-cycle related weather perturbations...generating something out of proportion to the tiny individual excursions away from 'perfect' ellipticity. ?? Very hard to say. (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. Yes, these are good points and would seem to be necessary. A further qualm is the Jovian itself. Jovians seem to act as system-clearers acting on the inevitable comets and occasional asteroids. This role, due to their huge g-fields, might put the kibosh on stable biosphere evolution since our earth-size-moon might experience many more catastrophic collisions than did the earth itself as these objects are deflected briefly toward the Jovian primary. regards, Gene |
#4
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![]() "Gene Partlow" wrote in message om... "Mike Dworetsky" wrote in message news: Hmm..now that I think about it, such changes might not add up to much since they would generally only be a tiny fraction of the planet's average distance from its star. You are right, the latter would be an insignificant effect for a habitable jovian moon orbiting a planet in the habitable zone. The moon would also have to be (a) large enough to retain a significant atmosphere (i.e., a lot larger than Mars but maybe not requiring to be as large as Earth), (b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), Yes...the Van Allen Belt problem. I was ignoring this just to focus on the possible monthly climate changes. While I know about as much about chaos theory as Curly, I yet wonder if something like the much abused butterfly effect might still apply due to the 'cumulative' effects of countless small lunar-cycle related weather perturbations...generating something out of proportion to the tiny individual excursions away from 'perfect' ellipticity. ?? Very hard to say. (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. Yes, these are good points and would seem to be necessary. A further qualm is the Jovian itself. Jovians seem to act as system-clearers acting on the inevitable comets and occasional asteroids. This role, due to their huge g-fields, might put the kibosh on stable biosphere evolution since our earth-size-moon might experience many more catastrophic collisions than did the earth itself as these objects are deflected briefly toward the Jovian primary. The existence of asteroid belts, Kuiper Belts and Oort clouds is not inevitable in all systems, though probably likely. The craters on Callisto are mostly very ancient, so maybe a biosphere can exist after a few billion years. Every once in a while there may be an "evolution's helper" event. -- Mike Dworetsky (remove "pants" spamblock to send email) |
#5
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"Mike Dworetsky" wrote in message ...
(b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), Or its own magnetic field, one of the Jupiter moons has its own. Would Earth's present magnetic field protect us if Earth was to replace Ganymede or Callisto, or Europa for that matter ? (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. So, perhaps better be in Europa's orbit than Callisto's ? Regards Carsten Nielsen Denmark |
#6
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"Mike Dworetsky" :
The existence of asteroid belts, Kuiper Belts and Oort clouds is not inevitable in all systems, though probably likely. The craters on Callisto are mostly very ancient, so maybe a biosphere can exist after a few billion years. Every once in a while there may be an "evolution's helper" event. On the otherhand having ringside seats to watch a ShoeMaker event would do wonder to get people to keep a eye on the skies. Earl Colby Pottinger -- I make public email sent to me! Hydrogen Peroxide Rockets, OpenBeos, SerialTransfer 3.0, RAMDISK, BoatBuilding, DIY TabletPC. What happened to the time? http://webhome.idirect.com/~earlcp |
#7
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"Mike Dworetsky" wrote in message ...
"Gene Partlow" wrote in message om... Andrew Yee's Oct. 9th post on the Eddington Probe (could detect moons of extrasolar planets) got me wondering... What would be the chances of a rich earthlike biosphere evolving on an earth-mass moon of an extrasolar jovian planet in orbit -within- the so- called "habitable zone" of its star? This is obviously a difficult question involving huge numbers of factors, but the first factor occurring to me as I read that post was...what would the climate or seasons be like, since that 'earth'-moon would have not only seasonal variations through the year (depending on orbital eccentricity etc., axial tilt etc.), but some variations due to its monthly changes in distance from its home star due to its lunar orbit about the jovian. Hmm..now that I think about it, such changes might not add up to much since they would generally only be a tiny fraction of the planet's average distance from its star. You are right, the latter would be an insignificant effect for a habitable jovian moon orbiting a planet in the habitable zone. The moon would also have to be (a) large enough to retain a significant atmosphere (i.e., a lot larger than Mars but maybe not requiring to be as large as Earth), (b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. Deep-sea volcanos emit different substances: http://www.pmel.noaa.gov/vents/chemi...ges/vents2.gif Perhaps, the medium, into which a volcano erupts, shapes the biosphere. For example, methane is a large component of both the "black smokers" and Titan. John Curtis |
#8
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![]() "Carsten Nielsen" wrote in message om... "Mike Dworetsky" wrote in message ... (b) far enough from the primary not to be badly affected by magnetic fields of the primary (in the case of Jupiter this could be a problem unless the atmosphere is protective), Or its own magnetic field, one of the Jupiter moons has its own. Would Earth's present magnetic field protect us if Earth was to replace Ganymede or Callisto, or Europa for that matter ? Earth's magnetic field undergoes reversals, and during these the "protective" effect is much reduced. Jupiter's magnetic field is much stronger than Earth's, even at large distances from the planet. The main thing that has to be protected against is charged particles and solar wind. Jupiter has a lot of charged particles in its field. (c) not affected by internal tidal heating effects such as those that cause Io to be volcanic. The last of these could be avoided if the large moon is the only large natural satellite and has a circular orbit, or is orbiting a long way out, like Callisto. Maybe one would want just enough internal tidal heating to generate volcanic activity leading to outgassing of CO2, SO2, S2, NO2, NO, and H2O, so that a breathable atmosphere could eventually evolve. So, perhaps better be in Europa's orbit than Callisto's ? Possibly. If the body is large enough and made of the right materials, like Earth, it will have volcanism all by itself, so it could be at a much larger distance. -- Mike Dworetsky (Remove "pants" spamblock to send e-mail) |
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