How can a moon have an ever-changing face?
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Imagine an inhabitated planet like ours with a moon of the same projected size in the sky. The moon has visible structures of colors or darker and lighter areas.
Every evening when the moon rises over the horizon, it's surface changed in at least 1/4 of the visible area. It didn't just rotate, no-one on this planet has ever seen the same image of the moon twice in their life.
How is it possible that the structure or pattern on the surface of a moon changes constantly while the planet is stable enough to support intelligent life?
Edit due to so many answers requiring an atmosphere to work: The moon can have an atmosphere, but the changing patterns must be on a planetary (or moony?) scale and look otherworldly. Simple clouds floating around are too similar to what the natives see every day on their home planet. Giant stoms like on Jupiter are ok, but they have the tendency to repeat their patterns.
science-based moons astronomy
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add a comment |
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Imagine an inhabitated planet like ours with a moon of the same projected size in the sky. The moon has visible structures of colors or darker and lighter areas.
Every evening when the moon rises over the horizon, it's surface changed in at least 1/4 of the visible area. It didn't just rotate, no-one on this planet has ever seen the same image of the moon twice in their life.
How is it possible that the structure or pattern on the surface of a moon changes constantly while the planet is stable enough to support intelligent life?
Edit due to so many answers requiring an atmosphere to work: The moon can have an atmosphere, but the changing patterns must be on a planetary (or moony?) scale and look otherworldly. Simple clouds floating around are too similar to what the natives see every day on their home planet. Giant stoms like on Jupiter are ok, but they have the tendency to repeat their patterns.
science-based moons astronomy
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago
add a comment |
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Imagine an inhabitated planet like ours with a moon of the same projected size in the sky. The moon has visible structures of colors or darker and lighter areas.
Every evening when the moon rises over the horizon, it's surface changed in at least 1/4 of the visible area. It didn't just rotate, no-one on this planet has ever seen the same image of the moon twice in their life.
How is it possible that the structure or pattern on the surface of a moon changes constantly while the planet is stable enough to support intelligent life?
Edit due to so many answers requiring an atmosphere to work: The moon can have an atmosphere, but the changing patterns must be on a planetary (or moony?) scale and look otherworldly. Simple clouds floating around are too similar to what the natives see every day on their home planet. Giant stoms like on Jupiter are ok, but they have the tendency to repeat their patterns.
science-based moons astronomy
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Imagine an inhabitated planet like ours with a moon of the same projected size in the sky. The moon has visible structures of colors or darker and lighter areas.
Every evening when the moon rises over the horizon, it's surface changed in at least 1/4 of the visible area. It didn't just rotate, no-one on this planet has ever seen the same image of the moon twice in their life.
How is it possible that the structure or pattern on the surface of a moon changes constantly while the planet is stable enough to support intelligent life?
Edit due to so many answers requiring an atmosphere to work: The moon can have an atmosphere, but the changing patterns must be on a planetary (or moony?) scale and look otherworldly. Simple clouds floating around are too similar to what the natives see every day on their home planet. Giant stoms like on Jupiter are ok, but they have the tendency to repeat their patterns.
science-based moons astronomy
science-based moons astronomy
edited 7 hours ago
Elmy
asked 10 hours ago
ElmyElmy
10.8k11850
10.8k11850
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago
add a comment |
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago
add a comment |
15 Answers
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active
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Make the Moon Bigger
Or, more accurately, more massive. You'd have to move its orbit out a bit to prevent more brutal tides on the planet, but make it massive enough to hold an atmosphere of its own. Make that atmosphere out of denser gases, ones that can be held with a more tenuous grip than our own, and, ideally, ones that can be coloured and have interesting fluid dynamics. Dinitrogen tetroxide, maybe.
With shifting cloud patterns (doubtless very lethal but very pretty), maybe from core heating, you get a relatively rapidly shifting lunar appearance without having to make the moon out of anything implausible.
Edit: Another option - if you're already allowing for an active core for additional heating (and an extra swirly atmosphere), you could also have volcanism. Nothing like a man in the moon with acne!
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It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
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– Mazura
9 hours ago
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You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
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– jdunlop
7 hours ago
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Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
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– Willk
7 hours ago
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How it could work
Water example
Your planet has a (water)ice surface. When the star doesn't shine upon the surface of the moon surface temperature falls below -10 °C (there is likely no pressure on the moon). But when it does shine temperature rises above -10 °C and it melts and the surface transforms, because of gravitational pulls. Other things effecting the surface would be:
Meteor impacts, solar winds, relative position to planet and sun.
Additional effects
Meteor impacts can form large mountain waves which take for months to get molten down while still changing their shape every day. They could also cause swirls and other uneven textures over the moon surface. Although these swirls would mostly be caused by solar winds. Another thing to consider is that the relative position between planet and sun will cause the overall flow direction to change, as would meteor impacts.
Alternatives
You could also use other elements with different melting points for scenarios where temperatures always exceed -10 °C or never exceed -10 °C. Examples:
Lower than -10 °C
- oxygen -218 °C
- chlorine -101 °C
- mercury -38 °C
Higher than -10 °C
- rubidium 39 °C
- sodium 97 °C
- tin 231 °C
Now these are just examples but I hope at least one of them can come to use.
This is my source(just type in the mentioned element and compare the result)
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Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
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– Shufflepants
8 hours ago
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@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
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– Soan
4 hours ago
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Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
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– B.fox
3 hours ago
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Unutterably Immense Aurora Borealis
Credit: nasa.gov -- Aurorae on Jupiter
If you don't already know, aurorae are electromagnetic spectacles caused by high-energy, solar-charged particles bombarding with an atmosphere. They come in many shapes, magnitudes, and colors. Here's how we'll construct your shape-shifting moon with them:
Multicolored Aurorae
Because you've now allowed for an atmosphere, we can actually design how our aurorae will appear. Atmospheric composition determines the color of the aurorae as those high-energy ions interact with the various gases involved. Atomic oxygen produces red, orange, or green light depending on the amount of energy it becomes excited by (generally green light at lower altitudes, more-so ruddy light at higher altitudes in Earth's specific atmosphere). At much lower altitudes, atomic oxygen (again, specific to Earth's atmosphere) becomes less common (atomic oxygen is produced when diatomic oxygen drifts into the upper stratosphere and is broken by UV radiation); nitrogen instead can be used and excited: nitrogen absorbing energy will produce blue light, while nitrogen losing energy (after having gained excess) will produce red light.
Aurorae manifest in curtains descending into the atmosphere, where atmospheric composition, descending into the atmosphere, changes as well. This results in regions where the colors mix: pink, a mixture of red and green light; and yellow, a mixture of green and red (greater intensity followed by lesser intensity).
We have a lot more colors to work with, however (keep in mind, lighter gases are likely to escape the atmosphere, so their concentrations will naturally be diminished [one should also factor in relative abundance under planetary formation conditions]): Helium, white to orange; Neon, red-orange; Argon, violet to a lavender blue; Water Vapor, dimmer pink or magenta; and Carbon Dioxide, blue-white to pink. Personally, I would select our basic, Earth-analog atmospheric concoction of Nitrogen and Oxygen, yet, with a greater proportion of Carbon Dioxide--much greater for the following reason:
Aurorae magnitude in relation to gravity, magnetosphere strength, and atmospheric mass
The magnetosphere of Earth is kind of weak. It manages to nudge only a small fraction of solar-charged particles to collide with the atmosphere. A stronger field will affect particle trajectories more, meaning more collisions with the atmosphere and more lights. Most of the particles flying off the Sun (besides neutrinos, I think) are electrons, which are negative in charge. If geomagnetic north sits at the north pole, then the aurorae will be stronger in the northern hemisphere, although, after some degree of intensity, this distinction may no longer matter as particles bombard most of the atmospheric surface pretty uniformly, in the sense of whether any particular region of atmosphere is exposed naked and non-bombarded. The south pole will attract the remaining positively-charged particles--protons and alpha particles--however, they are lesser in their abundances. Withal, the north pole would be "brighter," or more-so populated with aurorae than the south pole, however, ideally the aurorae will span the whole moon, just being brighter in those regions. Onward.
A thicker, more massive atmosphere in tandem with a weaker gravitational pull is ideal for maximal aurorae activity. The weaker gravity will extend the atmosphere further from the moon's surface. The volumes of atmosphere where the solar-charged particles may interact will be extended under weaker gravity (the atmosphere will be taller).
To complete the picture
Our atmosphere may allow an observer to see the surface. Ideally, we want our aurorae to be consistent and it turns out that solar activity itself is pretty consistent and unvarying. If the surface is ever visible through the swathes of folding, shaping, shifting, entombing, iridescent ribbons, then we must make it indistinct. A volcanic past could achieve this.
Credit: earthscienceeducation.org -- Basalt Rock
A surface largely of basaltic and obsidian-like rock could probably accomplish this.
Non-repeating patterns
Now, aurorae typically follow magnetic field lines of the magnetosphere. Magnetosphere structures vary depending on a multitude of factors, such as the distance from the sun, the intensity of solar winds, among others. Magnetic geometry is not quite that simple, however. The Aurorae we should expect shouldn't fall into predictable routines, though, just to be safe, let's just offset it from its rotational axis and center of mass and make it do other weird stuff. Also, let's assume that our inhabited world also has a magnetosphere (a safe assumption?) of different, lesser strength and perhaps offset to another angle which isn't perpendicular to the equatorial (also a safe assumption that the moon orbits near the equatorial?). The planet's and the moon's magnetospheres will mesh and interact with one another, possibly in a chaotic fashion, which will certainly help the chaotic appearance of our moon's aurorae.
Credit: youtube.com -- Interacting magnetic dipoles
In essence, we are taking advantage of the dynamic state of our planet-moon system to mesh and twist the involved electromagnetic geometry as much as possible.
Conclusion
A small moon with a relatively thick atmosphere (perhaps the atmospheric mass of Earth's) perhaps comprised of oxygen, nitrogen, and carbon dioxide, with a basaltic surface of supremely dark, perhaps sooty-like rock and regolith, and an immense, offset, dislodged, and powerful magnetosphere responsible for chaotic bands of aurorae across its photosphere.
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Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
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– Elmy
6 hours ago
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@Elmy Oh! This'll surely make things a lot more interesting!
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– B.fox
5 hours ago
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Take Pluto as inspiration. From the wiki (all emphasis are mine):
Pluto's surface is composed of more than 98 percent solid nitrogen, with traces of methane and carbon monoxide. The face of Pluto oriented toward Charon contains more solid methane, whereas the opposite face contains more nitrogen and solid carbon monoxide. Distribution of volatile ices is thought to be season-dependent and influenced more by solar insolation and topography than subsurface processes.
(...)
Pluto's surface color has changed between 1994 and 2003: the northern polar region has brightened and the southern hemisphere has darkened. Pluto's overall redness has also increased substantially between 2000 and 2002. These rapid changes are probably related to seasonal condensation and sublimation of portions of Pluto's atmosphere (...)
Now this may seem to conflict with one of your requirements:
The moon does not have an atmosphere
But again, according to another page in Wikipedia:
The surface pressure of the atmosphere of Pluto, measured by New Horizons in 2015, is about 1 Pa (10 μbar), roughly 100,000 times less than Earth's atmospheric pressure.
Some satellites in LEO face similar atmospheric pressures and need reboosting every then. Bottom line being: that's what objects in space around us face. So for all practical purposes Pluto's surface is exposed to a vacuum. Standing naked on it wouldn't be much different from being naked on Earth's orbit.
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The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
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– Nuclear Wang
6 hours ago
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I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
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– Renan
6 hours ago
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Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
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– Elmy
6 hours ago
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@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
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– Renan
6 hours ago
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@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
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– alephzero
4 hours ago
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Naturally occurring Thermochromic chemicals.
Those of us old enough to remember the 1970s remember mood rings.
While such chemicals are unlikely as natural deposits, it is fairly easy to imagine that some flowering plants could incorporate such as a form of sexual attraction or such-like.
No earth-like plants exist without the benefit of atmosphere, but perhaps an different design of plant forms could exist in thin carbon-dioxide atmosphere that may be compatible with your story. A hard-vacuum is likely to make significant plant-like coverage impossible.
Any high-contrast vegetation that has a short lifespan would perhaps be sufficient, esp. competing forms with different reflectance characteristics.
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That solar system could be experiencing a phenomenon like the late heavy bombardment: the moon is constantly hit by meteorites, so that it is continuously shaped by these impacts.
The problem is that these meteorites must be very frequent (say in the order of the dozen of impacts in a day), but quite small - in the range of 10-20 meters - in order not to cause damage when they fall onto the main planet, burning in its atmosphere. In this case probably you should somehow justify the lack of bigger asteroids.
You could also point that the moon is of recent formation (maybe captured by the gravity of the planet), which implies its core is still active and gives origin to some vulcanic activity that shapes its surface (but in this case the changes would be slower and the surface of the moon wouldn't change a lot in the span of some days).
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Possibly there could be intelligence of some sort on the moon and their activities can make a big visual change in the appearance of large sections of the moon during short periods.
Possibly they are artists trying out various "paint" patterns to see which make the moon look best.
Perhaps they move countless millions of large vehicles of various colors around on the moon, arranging them in various patterns as part of some sort of "dance".
Maybe they are trying to send a message to the natives of the planet and thus making an ever changing series of patterns on the moon.
A century or so ago an astronomer believed that some tiny changes of color he observed on the moon were the results of vast hordes of insects moving around.
So possibly on your moon thick areas of vegetation spring up, changing the color of vast regions, and then vast wandering hordes of insects travel toward them, changing the face of the moon as they move. When the insects arrive at the forest or meadow or swamp their color mingles with the color of the plants and changes the color of the region as seen from the planet.
So the insects eat all the vegetation in the region, changing its color, and leave their wastes (containing many seeds) behind to fertilize the soil. The insects move on, searching for another area of vegetation, and the area is now a different color, barren of vegetation until the seeds sprout and start to grow. Eventually the plants become thick enough to change the color of the region back to vegetation colored, then the region retains that color until the same or a different horde of insects arrives to eat the vegetation.
Of course it seem rather doubtful that a planet small enough to be habitable would have a moon large enough to be habitable for at least some types of life. That would make them seem a lot more like a double planet than like a planet and its moon.
Of course the intelligent beings on the moon don't have to be living beings; they could be machines.
Or the two worlds could both be habitable planets orbiting their star if their orbits are a lot closer to each other than any planetary orbits in our solar system, so that when the planets pass closest to each other the natives of one can see surface features on the other. There is actually a known solar system where planets in the habitable zone of their star do sometimes orbit close enough for someone on one of them to see surface features on the other - TRAPPIST-1.
The distance between the orbits of TRAPPIST-1b and TRAPPIST-1c is only 1.6 times the distance between the Earth and the Moon. The planets should appear prominently in each other's skies, in some cases appearing several times larger than the Moon appears from Earth.[41] A year on the closest planet passes in only 1.5 Earth days, while the seventh planet's year passes in only 18.8 days.[38][34]
https://en.wikipedia.org/wiki/TRAPPIST-11
Or maybe the "planet" and "moon" are actually both moons that orbit a gas giant planet.
Your "planet" could actually be a giant, Earth sized habitable moon, and the "moon" would orbit closer to the gas giant. Sometimes your "planet" and the inner moon would be almost on opposite sides of the gas giant and the inner moon wouldn't look big enough for details to be visible. But at intervals, probably every few days, the inner moon would pass close to the outer habitable moon and the natives of the habitable moon could see details of the surface of the inner moon and note the changes (and only in the parts of the moon that were lit by their star) .
If the inner moon orbits close enough to the gas giant the tidal heating should make the inner moon hyper volcanic like Io, the innermost Galilean moon of Jupiter. Various volcanoes might erupt often, spewing out vast amounts of lava of various colors to constantly resurface the inner moon. So each time that details of the inner moon were visible the surface patterns would be at least slightly different.
The problem with this is that the clouds and weather patterns on the gas giant planet would be visible all the time and would also change, thus possibly distracting the natives of the habitable moon from the show on the inner moon.
Possibly the moon in your story could suffer from tidal heating and constant resurfacing if it orbited a habitable planet in the right way. It would probably have to have an eccentric orbit which made it get noticeably farther and closer to the planet at various points in its orbit, and thus the patterns on its surface would only be visible when the moon was closer to the planet (and only in the parts of the moon that were lit by their star).
Possibly someone here can calculate if it is possible for a habitable planet to have a presumably recently captured moon with enough tidal heating to be constantly resurfacing itself.
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An alien race has covered the planet, or whatever percentage you see fit with a giant TV screen.
Maybe they double as solar panels somehow.
Now they can literally change any part of the visible surface at whim.
Just wait till they spam you with moon sized commericials... muhhahahahaha!
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Long ago an intelligent species found this moon and made plans to inhabit it. They created a network of tunnels all across the planet just below its surface. They planted the seeds of life and prepared to begin settling, but for some reason, they never did. So the moon was left, carved tunnels beneath its surface with the beginnings of life sprouting.
Fast forward a few thousand years to today, and the moon is buzzing with life--but that life all lives underground. A specific creature, the Mitter, has thrived on the underground flora and fauna. They are a fast moving species that is nomadic by nature, constantly moving to different places in different patterns every day.
However, when they move, they let off an abundance of benign chemicals that rise to the surface. These chemicals glow when in contact with the outside air--glowing a slightly different hue for each Mitter. With the abundance of the creatures and their unusual travel patterns, the planet appears to glow in ever changing shades and hues. Perhaps the Mitters' chemicals glow different colors depending on the time of season so the moon will go through phases of colors throughout the year?
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Oceans of nonlinear chemical oscillator compound!
Imagine that there`s an ocean on the moon that is filled to the brim with e.g. malonic acid and potassium bromate. That would yield literal chaotic color patterns floating both on its surface and all the way down to the seabed.
This is called the Belousov–Zhabotinsky reaction.
All weather changes, including the amount of sunlight absorbed, the surface waves, the underwater currents (well, technically it`s not water, but whatever), the winds, the evaporation, the volcanic activity — everything of the sort would add to the total randomness and uniqueness of the pattern.
Here`s a video of it oscillating in a Petri dish. And here`s another one.
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Here are some ideas, for a moon with a solid face:
- It could have really active plate tectonics moving the surface features around, which (as I understand it) would also imply a strong magnetic field and lots of volcanic activity.
- It could be very large, and the orbit of your planet could be just near-enough to an asteroid belt that whenever the moon moves toward the outer side of the orbit, it pulls asteroids into itself, actively rearranging the craters on its face
- If your planet is large, its moon could have a ring small of meteors around it, regularly falling into the moon (with no atmosphere to destroy them) and those could also rearrange the craters.
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A watery body, such as Enceladus (maybe Ceres as long as it has an icy core), orbits as a moon. This moon could have a very eccentric orbit, causing tidal forced to act upon it, causing cryo-volcanism. these cryovolcanos can cover the surface with various chemicals and minerals (water, salty brine, methane, ethane, or other organics) in an ever changing pattern.
The cracking and shifting of the fragile surface would also aid in the changing surface patterns.
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Arctic sea ice is constantly changing, although not on a daily timescale:
https://thumbs.gfycat.com/BothDismalEmperorpenguin.webp
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Your planet is tidally locked and it's moon is made of something with a low melting point.
This means that it's eternal twilight on the narrow band of habitable terrain on your planet, and that the day is marked by the ascent of the moon, which, continually melted by the sun and frozen by the planet's shadow, changes each day.
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The surface of the moon is covered in an exotic lifeform with an exceedingly rapid lifecycle. Colonies of this lifeform grow to cover large portions of the lunar surface in as little as 12 hours, competing for space with surrounding colonies, before rapidly crashing as soil fertility is depleted. No sooner has one colony collapsed, than another has begun its growth on another part of the moon's surface.
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15 Answers
15
active
oldest
votes
15 Answers
15
active
oldest
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$begingroup$
Make the Moon Bigger
Or, more accurately, more massive. You'd have to move its orbit out a bit to prevent more brutal tides on the planet, but make it massive enough to hold an atmosphere of its own. Make that atmosphere out of denser gases, ones that can be held with a more tenuous grip than our own, and, ideally, ones that can be coloured and have interesting fluid dynamics. Dinitrogen tetroxide, maybe.
With shifting cloud patterns (doubtless very lethal but very pretty), maybe from core heating, you get a relatively rapidly shifting lunar appearance without having to make the moon out of anything implausible.
Edit: Another option - if you're already allowing for an active core for additional heating (and an extra swirly atmosphere), you could also have volcanism. Nothing like a man in the moon with acne!
$endgroup$
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
add a comment |
$begingroup$
Make the Moon Bigger
Or, more accurately, more massive. You'd have to move its orbit out a bit to prevent more brutal tides on the planet, but make it massive enough to hold an atmosphere of its own. Make that atmosphere out of denser gases, ones that can be held with a more tenuous grip than our own, and, ideally, ones that can be coloured and have interesting fluid dynamics. Dinitrogen tetroxide, maybe.
With shifting cloud patterns (doubtless very lethal but very pretty), maybe from core heating, you get a relatively rapidly shifting lunar appearance without having to make the moon out of anything implausible.
Edit: Another option - if you're already allowing for an active core for additional heating (and an extra swirly atmosphere), you could also have volcanism. Nothing like a man in the moon with acne!
$endgroup$
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
add a comment |
$begingroup$
Make the Moon Bigger
Or, more accurately, more massive. You'd have to move its orbit out a bit to prevent more brutal tides on the planet, but make it massive enough to hold an atmosphere of its own. Make that atmosphere out of denser gases, ones that can be held with a more tenuous grip than our own, and, ideally, ones that can be coloured and have interesting fluid dynamics. Dinitrogen tetroxide, maybe.
With shifting cloud patterns (doubtless very lethal but very pretty), maybe from core heating, you get a relatively rapidly shifting lunar appearance without having to make the moon out of anything implausible.
Edit: Another option - if you're already allowing for an active core for additional heating (and an extra swirly atmosphere), you could also have volcanism. Nothing like a man in the moon with acne!
$endgroup$
Make the Moon Bigger
Or, more accurately, more massive. You'd have to move its orbit out a bit to prevent more brutal tides on the planet, but make it massive enough to hold an atmosphere of its own. Make that atmosphere out of denser gases, ones that can be held with a more tenuous grip than our own, and, ideally, ones that can be coloured and have interesting fluid dynamics. Dinitrogen tetroxide, maybe.
With shifting cloud patterns (doubtless very lethal but very pretty), maybe from core heating, you get a relatively rapidly shifting lunar appearance without having to make the moon out of anything implausible.
Edit: Another option - if you're already allowing for an active core for additional heating (and an extra swirly atmosphere), you could also have volcanism. Nothing like a man in the moon with acne!
edited 9 hours ago
answered 9 hours ago
jdunlopjdunlop
7,43311643
7,43311643
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
add a comment |
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
It has to be big enough to hold an atmosphere otherwise it will have frozen to death long ago. You can't have geological activity on a body without an atmosphere that isn't being tidally heated - and live on it (can't live on Io) +1
$endgroup$
– Mazura
9 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
You're not required to live on it; the OP's specs are just that it have a changing face. Definitely wouldn't want to live on Titan, either!
$endgroup$
– jdunlop
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
$begingroup$
Check out Jupiter's swirly atmosphere! cnn.com/2018/01/08/weather/jupiter-nasa-photos-juno-trnd/…
$endgroup$
– Willk
7 hours ago
add a comment |
$begingroup$
How it could work
Water example
Your planet has a (water)ice surface. When the star doesn't shine upon the surface of the moon surface temperature falls below -10 °C (there is likely no pressure on the moon). But when it does shine temperature rises above -10 °C and it melts and the surface transforms, because of gravitational pulls. Other things effecting the surface would be:
Meteor impacts, solar winds, relative position to planet and sun.
Additional effects
Meteor impacts can form large mountain waves which take for months to get molten down while still changing their shape every day. They could also cause swirls and other uneven textures over the moon surface. Although these swirls would mostly be caused by solar winds. Another thing to consider is that the relative position between planet and sun will cause the overall flow direction to change, as would meteor impacts.
Alternatives
You could also use other elements with different melting points for scenarios where temperatures always exceed -10 °C or never exceed -10 °C. Examples:
Lower than -10 °C
- oxygen -218 °C
- chlorine -101 °C
- mercury -38 °C
Higher than -10 °C
- rubidium 39 °C
- sodium 97 °C
- tin 231 °C
Now these are just examples but I hope at least one of them can come to use.
This is my source(just type in the mentioned element and compare the result)
$endgroup$
3
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
add a comment |
$begingroup$
How it could work
Water example
Your planet has a (water)ice surface. When the star doesn't shine upon the surface of the moon surface temperature falls below -10 °C (there is likely no pressure on the moon). But when it does shine temperature rises above -10 °C and it melts and the surface transforms, because of gravitational pulls. Other things effecting the surface would be:
Meteor impacts, solar winds, relative position to planet and sun.
Additional effects
Meteor impacts can form large mountain waves which take for months to get molten down while still changing their shape every day. They could also cause swirls and other uneven textures over the moon surface. Although these swirls would mostly be caused by solar winds. Another thing to consider is that the relative position between planet and sun will cause the overall flow direction to change, as would meteor impacts.
Alternatives
You could also use other elements with different melting points for scenarios where temperatures always exceed -10 °C or never exceed -10 °C. Examples:
Lower than -10 °C
- oxygen -218 °C
- chlorine -101 °C
- mercury -38 °C
Higher than -10 °C
- rubidium 39 °C
- sodium 97 °C
- tin 231 °C
Now these are just examples but I hope at least one of them can come to use.
This is my source(just type in the mentioned element and compare the result)
$endgroup$
3
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
add a comment |
$begingroup$
How it could work
Water example
Your planet has a (water)ice surface. When the star doesn't shine upon the surface of the moon surface temperature falls below -10 °C (there is likely no pressure on the moon). But when it does shine temperature rises above -10 °C and it melts and the surface transforms, because of gravitational pulls. Other things effecting the surface would be:
Meteor impacts, solar winds, relative position to planet and sun.
Additional effects
Meteor impacts can form large mountain waves which take for months to get molten down while still changing their shape every day. They could also cause swirls and other uneven textures over the moon surface. Although these swirls would mostly be caused by solar winds. Another thing to consider is that the relative position between planet and sun will cause the overall flow direction to change, as would meteor impacts.
Alternatives
You could also use other elements with different melting points for scenarios where temperatures always exceed -10 °C or never exceed -10 °C. Examples:
Lower than -10 °C
- oxygen -218 °C
- chlorine -101 °C
- mercury -38 °C
Higher than -10 °C
- rubidium 39 °C
- sodium 97 °C
- tin 231 °C
Now these are just examples but I hope at least one of them can come to use.
This is my source(just type in the mentioned element and compare the result)
$endgroup$
How it could work
Water example
Your planet has a (water)ice surface. When the star doesn't shine upon the surface of the moon surface temperature falls below -10 °C (there is likely no pressure on the moon). But when it does shine temperature rises above -10 °C and it melts and the surface transforms, because of gravitational pulls. Other things effecting the surface would be:
Meteor impacts, solar winds, relative position to planet and sun.
Additional effects
Meteor impacts can form large mountain waves which take for months to get molten down while still changing their shape every day. They could also cause swirls and other uneven textures over the moon surface. Although these swirls would mostly be caused by solar winds. Another thing to consider is that the relative position between planet and sun will cause the overall flow direction to change, as would meteor impacts.
Alternatives
You could also use other elements with different melting points for scenarios where temperatures always exceed -10 °C or never exceed -10 °C. Examples:
Lower than -10 °C
- oxygen -218 °C
- chlorine -101 °C
- mercury -38 °C
Higher than -10 °C
- rubidium 39 °C
- sodium 97 °C
- tin 231 °C
Now these are just examples but I hope at least one of them can come to use.
This is my source(just type in the mentioned element and compare the result)
edited 4 hours ago
answered 9 hours ago
SoanSoan
1,711216
1,711216
3
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
add a comment |
3
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
3
3
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
Not sure this will get what the OP wants. Melting and refreezing will almost certainly occur in the same places each day. It might change a bit from season to season, but each day will look pretty much like yesterday and each season will look pretty much the same as the same season last year. Definitely not the 1/4 of it is completely different from yesterday every day.
$endgroup$
– Shufflepants
8 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
@Shufflepants that's not the case because solar winds and other factors hugely effect the flow of molten substances. Other factors are impacts of meteors, current position in the orbit relative to the planet and the sun.
$endgroup$
– Soan
4 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
$begingroup$
Reshaping a celestial body's surface requires a lot of energy in and of itself; solar winds are nearly intangible and will likely not fuel such processes--consider the interplanetary medium. Ices in a vacuum and exposed to hard sunlight will convert to a gas and eventually form an atmosphere. The sheer energy required to alter a landscape continuously is astronomically great.
$endgroup$
– B.fox
3 hours ago
add a comment |
$begingroup$
Unutterably Immense Aurora Borealis
Credit: nasa.gov -- Aurorae on Jupiter
If you don't already know, aurorae are electromagnetic spectacles caused by high-energy, solar-charged particles bombarding with an atmosphere. They come in many shapes, magnitudes, and colors. Here's how we'll construct your shape-shifting moon with them:
Multicolored Aurorae
Because you've now allowed for an atmosphere, we can actually design how our aurorae will appear. Atmospheric composition determines the color of the aurorae as those high-energy ions interact with the various gases involved. Atomic oxygen produces red, orange, or green light depending on the amount of energy it becomes excited by (generally green light at lower altitudes, more-so ruddy light at higher altitudes in Earth's specific atmosphere). At much lower altitudes, atomic oxygen (again, specific to Earth's atmosphere) becomes less common (atomic oxygen is produced when diatomic oxygen drifts into the upper stratosphere and is broken by UV radiation); nitrogen instead can be used and excited: nitrogen absorbing energy will produce blue light, while nitrogen losing energy (after having gained excess) will produce red light.
Aurorae manifest in curtains descending into the atmosphere, where atmospheric composition, descending into the atmosphere, changes as well. This results in regions where the colors mix: pink, a mixture of red and green light; and yellow, a mixture of green and red (greater intensity followed by lesser intensity).
We have a lot more colors to work with, however (keep in mind, lighter gases are likely to escape the atmosphere, so their concentrations will naturally be diminished [one should also factor in relative abundance under planetary formation conditions]): Helium, white to orange; Neon, red-orange; Argon, violet to a lavender blue; Water Vapor, dimmer pink or magenta; and Carbon Dioxide, blue-white to pink. Personally, I would select our basic, Earth-analog atmospheric concoction of Nitrogen and Oxygen, yet, with a greater proportion of Carbon Dioxide--much greater for the following reason:
Aurorae magnitude in relation to gravity, magnetosphere strength, and atmospheric mass
The magnetosphere of Earth is kind of weak. It manages to nudge only a small fraction of solar-charged particles to collide with the atmosphere. A stronger field will affect particle trajectories more, meaning more collisions with the atmosphere and more lights. Most of the particles flying off the Sun (besides neutrinos, I think) are electrons, which are negative in charge. If geomagnetic north sits at the north pole, then the aurorae will be stronger in the northern hemisphere, although, after some degree of intensity, this distinction may no longer matter as particles bombard most of the atmospheric surface pretty uniformly, in the sense of whether any particular region of atmosphere is exposed naked and non-bombarded. The south pole will attract the remaining positively-charged particles--protons and alpha particles--however, they are lesser in their abundances. Withal, the north pole would be "brighter," or more-so populated with aurorae than the south pole, however, ideally the aurorae will span the whole moon, just being brighter in those regions. Onward.
A thicker, more massive atmosphere in tandem with a weaker gravitational pull is ideal for maximal aurorae activity. The weaker gravity will extend the atmosphere further from the moon's surface. The volumes of atmosphere where the solar-charged particles may interact will be extended under weaker gravity (the atmosphere will be taller).
To complete the picture
Our atmosphere may allow an observer to see the surface. Ideally, we want our aurorae to be consistent and it turns out that solar activity itself is pretty consistent and unvarying. If the surface is ever visible through the swathes of folding, shaping, shifting, entombing, iridescent ribbons, then we must make it indistinct. A volcanic past could achieve this.
Credit: earthscienceeducation.org -- Basalt Rock
A surface largely of basaltic and obsidian-like rock could probably accomplish this.
Non-repeating patterns
Now, aurorae typically follow magnetic field lines of the magnetosphere. Magnetosphere structures vary depending on a multitude of factors, such as the distance from the sun, the intensity of solar winds, among others. Magnetic geometry is not quite that simple, however. The Aurorae we should expect shouldn't fall into predictable routines, though, just to be safe, let's just offset it from its rotational axis and center of mass and make it do other weird stuff. Also, let's assume that our inhabited world also has a magnetosphere (a safe assumption?) of different, lesser strength and perhaps offset to another angle which isn't perpendicular to the equatorial (also a safe assumption that the moon orbits near the equatorial?). The planet's and the moon's magnetospheres will mesh and interact with one another, possibly in a chaotic fashion, which will certainly help the chaotic appearance of our moon's aurorae.
Credit: youtube.com -- Interacting magnetic dipoles
In essence, we are taking advantage of the dynamic state of our planet-moon system to mesh and twist the involved electromagnetic geometry as much as possible.
Conclusion
A small moon with a relatively thick atmosphere (perhaps the atmospheric mass of Earth's) perhaps comprised of oxygen, nitrogen, and carbon dioxide, with a basaltic surface of supremely dark, perhaps sooty-like rock and regolith, and an immense, offset, dislodged, and powerful magnetosphere responsible for chaotic bands of aurorae across its photosphere.
$endgroup$
$begingroup$
Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@Elmy Oh! This'll surely make things a lot more interesting!
$endgroup$
– B.fox
5 hours ago
add a comment |
$begingroup$
Unutterably Immense Aurora Borealis
Credit: nasa.gov -- Aurorae on Jupiter
If you don't already know, aurorae are electromagnetic spectacles caused by high-energy, solar-charged particles bombarding with an atmosphere. They come in many shapes, magnitudes, and colors. Here's how we'll construct your shape-shifting moon with them:
Multicolored Aurorae
Because you've now allowed for an atmosphere, we can actually design how our aurorae will appear. Atmospheric composition determines the color of the aurorae as those high-energy ions interact with the various gases involved. Atomic oxygen produces red, orange, or green light depending on the amount of energy it becomes excited by (generally green light at lower altitudes, more-so ruddy light at higher altitudes in Earth's specific atmosphere). At much lower altitudes, atomic oxygen (again, specific to Earth's atmosphere) becomes less common (atomic oxygen is produced when diatomic oxygen drifts into the upper stratosphere and is broken by UV radiation); nitrogen instead can be used and excited: nitrogen absorbing energy will produce blue light, while nitrogen losing energy (after having gained excess) will produce red light.
Aurorae manifest in curtains descending into the atmosphere, where atmospheric composition, descending into the atmosphere, changes as well. This results in regions where the colors mix: pink, a mixture of red and green light; and yellow, a mixture of green and red (greater intensity followed by lesser intensity).
We have a lot more colors to work with, however (keep in mind, lighter gases are likely to escape the atmosphere, so their concentrations will naturally be diminished [one should also factor in relative abundance under planetary formation conditions]): Helium, white to orange; Neon, red-orange; Argon, violet to a lavender blue; Water Vapor, dimmer pink or magenta; and Carbon Dioxide, blue-white to pink. Personally, I would select our basic, Earth-analog atmospheric concoction of Nitrogen and Oxygen, yet, with a greater proportion of Carbon Dioxide--much greater for the following reason:
Aurorae magnitude in relation to gravity, magnetosphere strength, and atmospheric mass
The magnetosphere of Earth is kind of weak. It manages to nudge only a small fraction of solar-charged particles to collide with the atmosphere. A stronger field will affect particle trajectories more, meaning more collisions with the atmosphere and more lights. Most of the particles flying off the Sun (besides neutrinos, I think) are electrons, which are negative in charge. If geomagnetic north sits at the north pole, then the aurorae will be stronger in the northern hemisphere, although, after some degree of intensity, this distinction may no longer matter as particles bombard most of the atmospheric surface pretty uniformly, in the sense of whether any particular region of atmosphere is exposed naked and non-bombarded. The south pole will attract the remaining positively-charged particles--protons and alpha particles--however, they are lesser in their abundances. Withal, the north pole would be "brighter," or more-so populated with aurorae than the south pole, however, ideally the aurorae will span the whole moon, just being brighter in those regions. Onward.
A thicker, more massive atmosphere in tandem with a weaker gravitational pull is ideal for maximal aurorae activity. The weaker gravity will extend the atmosphere further from the moon's surface. The volumes of atmosphere where the solar-charged particles may interact will be extended under weaker gravity (the atmosphere will be taller).
To complete the picture
Our atmosphere may allow an observer to see the surface. Ideally, we want our aurorae to be consistent and it turns out that solar activity itself is pretty consistent and unvarying. If the surface is ever visible through the swathes of folding, shaping, shifting, entombing, iridescent ribbons, then we must make it indistinct. A volcanic past could achieve this.
Credit: earthscienceeducation.org -- Basalt Rock
A surface largely of basaltic and obsidian-like rock could probably accomplish this.
Non-repeating patterns
Now, aurorae typically follow magnetic field lines of the magnetosphere. Magnetosphere structures vary depending on a multitude of factors, such as the distance from the sun, the intensity of solar winds, among others. Magnetic geometry is not quite that simple, however. The Aurorae we should expect shouldn't fall into predictable routines, though, just to be safe, let's just offset it from its rotational axis and center of mass and make it do other weird stuff. Also, let's assume that our inhabited world also has a magnetosphere (a safe assumption?) of different, lesser strength and perhaps offset to another angle which isn't perpendicular to the equatorial (also a safe assumption that the moon orbits near the equatorial?). The planet's and the moon's magnetospheres will mesh and interact with one another, possibly in a chaotic fashion, which will certainly help the chaotic appearance of our moon's aurorae.
Credit: youtube.com -- Interacting magnetic dipoles
In essence, we are taking advantage of the dynamic state of our planet-moon system to mesh and twist the involved electromagnetic geometry as much as possible.
Conclusion
A small moon with a relatively thick atmosphere (perhaps the atmospheric mass of Earth's) perhaps comprised of oxygen, nitrogen, and carbon dioxide, with a basaltic surface of supremely dark, perhaps sooty-like rock and regolith, and an immense, offset, dislodged, and powerful magnetosphere responsible for chaotic bands of aurorae across its photosphere.
$endgroup$
$begingroup$
Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@Elmy Oh! This'll surely make things a lot more interesting!
$endgroup$
– B.fox
5 hours ago
add a comment |
$begingroup$
Unutterably Immense Aurora Borealis
Credit: nasa.gov -- Aurorae on Jupiter
If you don't already know, aurorae are electromagnetic spectacles caused by high-energy, solar-charged particles bombarding with an atmosphere. They come in many shapes, magnitudes, and colors. Here's how we'll construct your shape-shifting moon with them:
Multicolored Aurorae
Because you've now allowed for an atmosphere, we can actually design how our aurorae will appear. Atmospheric composition determines the color of the aurorae as those high-energy ions interact with the various gases involved. Atomic oxygen produces red, orange, or green light depending on the amount of energy it becomes excited by (generally green light at lower altitudes, more-so ruddy light at higher altitudes in Earth's specific atmosphere). At much lower altitudes, atomic oxygen (again, specific to Earth's atmosphere) becomes less common (atomic oxygen is produced when diatomic oxygen drifts into the upper stratosphere and is broken by UV radiation); nitrogen instead can be used and excited: nitrogen absorbing energy will produce blue light, while nitrogen losing energy (after having gained excess) will produce red light.
Aurorae manifest in curtains descending into the atmosphere, where atmospheric composition, descending into the atmosphere, changes as well. This results in regions where the colors mix: pink, a mixture of red and green light; and yellow, a mixture of green and red (greater intensity followed by lesser intensity).
We have a lot more colors to work with, however (keep in mind, lighter gases are likely to escape the atmosphere, so their concentrations will naturally be diminished [one should also factor in relative abundance under planetary formation conditions]): Helium, white to orange; Neon, red-orange; Argon, violet to a lavender blue; Water Vapor, dimmer pink or magenta; and Carbon Dioxide, blue-white to pink. Personally, I would select our basic, Earth-analog atmospheric concoction of Nitrogen and Oxygen, yet, with a greater proportion of Carbon Dioxide--much greater for the following reason:
Aurorae magnitude in relation to gravity, magnetosphere strength, and atmospheric mass
The magnetosphere of Earth is kind of weak. It manages to nudge only a small fraction of solar-charged particles to collide with the atmosphere. A stronger field will affect particle trajectories more, meaning more collisions with the atmosphere and more lights. Most of the particles flying off the Sun (besides neutrinos, I think) are electrons, which are negative in charge. If geomagnetic north sits at the north pole, then the aurorae will be stronger in the northern hemisphere, although, after some degree of intensity, this distinction may no longer matter as particles bombard most of the atmospheric surface pretty uniformly, in the sense of whether any particular region of atmosphere is exposed naked and non-bombarded. The south pole will attract the remaining positively-charged particles--protons and alpha particles--however, they are lesser in their abundances. Withal, the north pole would be "brighter," or more-so populated with aurorae than the south pole, however, ideally the aurorae will span the whole moon, just being brighter in those regions. Onward.
A thicker, more massive atmosphere in tandem with a weaker gravitational pull is ideal for maximal aurorae activity. The weaker gravity will extend the atmosphere further from the moon's surface. The volumes of atmosphere where the solar-charged particles may interact will be extended under weaker gravity (the atmosphere will be taller).
To complete the picture
Our atmosphere may allow an observer to see the surface. Ideally, we want our aurorae to be consistent and it turns out that solar activity itself is pretty consistent and unvarying. If the surface is ever visible through the swathes of folding, shaping, shifting, entombing, iridescent ribbons, then we must make it indistinct. A volcanic past could achieve this.
Credit: earthscienceeducation.org -- Basalt Rock
A surface largely of basaltic and obsidian-like rock could probably accomplish this.
Non-repeating patterns
Now, aurorae typically follow magnetic field lines of the magnetosphere. Magnetosphere structures vary depending on a multitude of factors, such as the distance from the sun, the intensity of solar winds, among others. Magnetic geometry is not quite that simple, however. The Aurorae we should expect shouldn't fall into predictable routines, though, just to be safe, let's just offset it from its rotational axis and center of mass and make it do other weird stuff. Also, let's assume that our inhabited world also has a magnetosphere (a safe assumption?) of different, lesser strength and perhaps offset to another angle which isn't perpendicular to the equatorial (also a safe assumption that the moon orbits near the equatorial?). The planet's and the moon's magnetospheres will mesh and interact with one another, possibly in a chaotic fashion, which will certainly help the chaotic appearance of our moon's aurorae.
Credit: youtube.com -- Interacting magnetic dipoles
In essence, we are taking advantage of the dynamic state of our planet-moon system to mesh and twist the involved electromagnetic geometry as much as possible.
Conclusion
A small moon with a relatively thick atmosphere (perhaps the atmospheric mass of Earth's) perhaps comprised of oxygen, nitrogen, and carbon dioxide, with a basaltic surface of supremely dark, perhaps sooty-like rock and regolith, and an immense, offset, dislodged, and powerful magnetosphere responsible for chaotic bands of aurorae across its photosphere.
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Unutterably Immense Aurora Borealis
Credit: nasa.gov -- Aurorae on Jupiter
If you don't already know, aurorae are electromagnetic spectacles caused by high-energy, solar-charged particles bombarding with an atmosphere. They come in many shapes, magnitudes, and colors. Here's how we'll construct your shape-shifting moon with them:
Multicolored Aurorae
Because you've now allowed for an atmosphere, we can actually design how our aurorae will appear. Atmospheric composition determines the color of the aurorae as those high-energy ions interact with the various gases involved. Atomic oxygen produces red, orange, or green light depending on the amount of energy it becomes excited by (generally green light at lower altitudes, more-so ruddy light at higher altitudes in Earth's specific atmosphere). At much lower altitudes, atomic oxygen (again, specific to Earth's atmosphere) becomes less common (atomic oxygen is produced when diatomic oxygen drifts into the upper stratosphere and is broken by UV radiation); nitrogen instead can be used and excited: nitrogen absorbing energy will produce blue light, while nitrogen losing energy (after having gained excess) will produce red light.
Aurorae manifest in curtains descending into the atmosphere, where atmospheric composition, descending into the atmosphere, changes as well. This results in regions where the colors mix: pink, a mixture of red and green light; and yellow, a mixture of green and red (greater intensity followed by lesser intensity).
We have a lot more colors to work with, however (keep in mind, lighter gases are likely to escape the atmosphere, so their concentrations will naturally be diminished [one should also factor in relative abundance under planetary formation conditions]): Helium, white to orange; Neon, red-orange; Argon, violet to a lavender blue; Water Vapor, dimmer pink or magenta; and Carbon Dioxide, blue-white to pink. Personally, I would select our basic, Earth-analog atmospheric concoction of Nitrogen and Oxygen, yet, with a greater proportion of Carbon Dioxide--much greater for the following reason:
Aurorae magnitude in relation to gravity, magnetosphere strength, and atmospheric mass
The magnetosphere of Earth is kind of weak. It manages to nudge only a small fraction of solar-charged particles to collide with the atmosphere. A stronger field will affect particle trajectories more, meaning more collisions with the atmosphere and more lights. Most of the particles flying off the Sun (besides neutrinos, I think) are electrons, which are negative in charge. If geomagnetic north sits at the north pole, then the aurorae will be stronger in the northern hemisphere, although, after some degree of intensity, this distinction may no longer matter as particles bombard most of the atmospheric surface pretty uniformly, in the sense of whether any particular region of atmosphere is exposed naked and non-bombarded. The south pole will attract the remaining positively-charged particles--protons and alpha particles--however, they are lesser in their abundances. Withal, the north pole would be "brighter," or more-so populated with aurorae than the south pole, however, ideally the aurorae will span the whole moon, just being brighter in those regions. Onward.
A thicker, more massive atmosphere in tandem with a weaker gravitational pull is ideal for maximal aurorae activity. The weaker gravity will extend the atmosphere further from the moon's surface. The volumes of atmosphere where the solar-charged particles may interact will be extended under weaker gravity (the atmosphere will be taller).
To complete the picture
Our atmosphere may allow an observer to see the surface. Ideally, we want our aurorae to be consistent and it turns out that solar activity itself is pretty consistent and unvarying. If the surface is ever visible through the swathes of folding, shaping, shifting, entombing, iridescent ribbons, then we must make it indistinct. A volcanic past could achieve this.
Credit: earthscienceeducation.org -- Basalt Rock
A surface largely of basaltic and obsidian-like rock could probably accomplish this.
Non-repeating patterns
Now, aurorae typically follow magnetic field lines of the magnetosphere. Magnetosphere structures vary depending on a multitude of factors, such as the distance from the sun, the intensity of solar winds, among others. Magnetic geometry is not quite that simple, however. The Aurorae we should expect shouldn't fall into predictable routines, though, just to be safe, let's just offset it from its rotational axis and center of mass and make it do other weird stuff. Also, let's assume that our inhabited world also has a magnetosphere (a safe assumption?) of different, lesser strength and perhaps offset to another angle which isn't perpendicular to the equatorial (also a safe assumption that the moon orbits near the equatorial?). The planet's and the moon's magnetospheres will mesh and interact with one another, possibly in a chaotic fashion, which will certainly help the chaotic appearance of our moon's aurorae.
Credit: youtube.com -- Interacting magnetic dipoles
In essence, we are taking advantage of the dynamic state of our planet-moon system to mesh and twist the involved electromagnetic geometry as much as possible.
Conclusion
A small moon with a relatively thick atmosphere (perhaps the atmospheric mass of Earth's) perhaps comprised of oxygen, nitrogen, and carbon dioxide, with a basaltic surface of supremely dark, perhaps sooty-like rock and regolith, and an immense, offset, dislodged, and powerful magnetosphere responsible for chaotic bands of aurorae across its photosphere.
edited 3 hours ago
answered 7 hours ago
B.foxB.fox
1,0181316
1,0181316
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Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
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– Elmy
6 hours ago
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@Elmy Oh! This'll surely make things a lot more interesting!
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– B.fox
5 hours ago
add a comment |
$begingroup$
Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@Elmy Oh! This'll surely make things a lot more interesting!
$endgroup$
– B.fox
5 hours ago
$begingroup$
Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
Thanks for your answer, it sounds really interesting. Please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@Elmy Oh! This'll surely make things a lot more interesting!
$endgroup$
– B.fox
5 hours ago
$begingroup$
@Elmy Oh! This'll surely make things a lot more interesting!
$endgroup$
– B.fox
5 hours ago
add a comment |
$begingroup$
Take Pluto as inspiration. From the wiki (all emphasis are mine):
Pluto's surface is composed of more than 98 percent solid nitrogen, with traces of methane and carbon monoxide. The face of Pluto oriented toward Charon contains more solid methane, whereas the opposite face contains more nitrogen and solid carbon monoxide. Distribution of volatile ices is thought to be season-dependent and influenced more by solar insolation and topography than subsurface processes.
(...)
Pluto's surface color has changed between 1994 and 2003: the northern polar region has brightened and the southern hemisphere has darkened. Pluto's overall redness has also increased substantially between 2000 and 2002. These rapid changes are probably related to seasonal condensation and sublimation of portions of Pluto's atmosphere (...)
Now this may seem to conflict with one of your requirements:
The moon does not have an atmosphere
But again, according to another page in Wikipedia:
The surface pressure of the atmosphere of Pluto, measured by New Horizons in 2015, is about 1 Pa (10 μbar), roughly 100,000 times less than Earth's atmospheric pressure.
Some satellites in LEO face similar atmospheric pressures and need reboosting every then. Bottom line being: that's what objects in space around us face. So for all practical purposes Pluto's surface is exposed to a vacuum. Standing naked on it wouldn't be much different from being naked on Earth's orbit.
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The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
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– Nuclear Wang
6 hours ago
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I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
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– Renan
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
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– Elmy
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
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– Renan
6 hours ago
1
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
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– alephzero
4 hours ago
add a comment |
$begingroup$
Take Pluto as inspiration. From the wiki (all emphasis are mine):
Pluto's surface is composed of more than 98 percent solid nitrogen, with traces of methane and carbon monoxide. The face of Pluto oriented toward Charon contains more solid methane, whereas the opposite face contains more nitrogen and solid carbon monoxide. Distribution of volatile ices is thought to be season-dependent and influenced more by solar insolation and topography than subsurface processes.
(...)
Pluto's surface color has changed between 1994 and 2003: the northern polar region has brightened and the southern hemisphere has darkened. Pluto's overall redness has also increased substantially between 2000 and 2002. These rapid changes are probably related to seasonal condensation and sublimation of portions of Pluto's atmosphere (...)
Now this may seem to conflict with one of your requirements:
The moon does not have an atmosphere
But again, according to another page in Wikipedia:
The surface pressure of the atmosphere of Pluto, measured by New Horizons in 2015, is about 1 Pa (10 μbar), roughly 100,000 times less than Earth's atmospheric pressure.
Some satellites in LEO face similar atmospheric pressures and need reboosting every then. Bottom line being: that's what objects in space around us face. So for all practical purposes Pluto's surface is exposed to a vacuum. Standing naked on it wouldn't be much different from being naked on Earth's orbit.
$endgroup$
$begingroup$
The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
$endgroup$
– Nuclear Wang
6 hours ago
$begingroup$
I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
$endgroup$
– Renan
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
$endgroup$
– Renan
6 hours ago
1
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
$endgroup$
– alephzero
4 hours ago
add a comment |
$begingroup$
Take Pluto as inspiration. From the wiki (all emphasis are mine):
Pluto's surface is composed of more than 98 percent solid nitrogen, with traces of methane and carbon monoxide. The face of Pluto oriented toward Charon contains more solid methane, whereas the opposite face contains more nitrogen and solid carbon monoxide. Distribution of volatile ices is thought to be season-dependent and influenced more by solar insolation and topography than subsurface processes.
(...)
Pluto's surface color has changed between 1994 and 2003: the northern polar region has brightened and the southern hemisphere has darkened. Pluto's overall redness has also increased substantially between 2000 and 2002. These rapid changes are probably related to seasonal condensation and sublimation of portions of Pluto's atmosphere (...)
Now this may seem to conflict with one of your requirements:
The moon does not have an atmosphere
But again, according to another page in Wikipedia:
The surface pressure of the atmosphere of Pluto, measured by New Horizons in 2015, is about 1 Pa (10 μbar), roughly 100,000 times less than Earth's atmospheric pressure.
Some satellites in LEO face similar atmospheric pressures and need reboosting every then. Bottom line being: that's what objects in space around us face. So for all practical purposes Pluto's surface is exposed to a vacuum. Standing naked on it wouldn't be much different from being naked on Earth's orbit.
$endgroup$
Take Pluto as inspiration. From the wiki (all emphasis are mine):
Pluto's surface is composed of more than 98 percent solid nitrogen, with traces of methane and carbon monoxide. The face of Pluto oriented toward Charon contains more solid methane, whereas the opposite face contains more nitrogen and solid carbon monoxide. Distribution of volatile ices is thought to be season-dependent and influenced more by solar insolation and topography than subsurface processes.
(...)
Pluto's surface color has changed between 1994 and 2003: the northern polar region has brightened and the southern hemisphere has darkened. Pluto's overall redness has also increased substantially between 2000 and 2002. These rapid changes are probably related to seasonal condensation and sublimation of portions of Pluto's atmosphere (...)
Now this may seem to conflict with one of your requirements:
The moon does not have an atmosphere
But again, according to another page in Wikipedia:
The surface pressure of the atmosphere of Pluto, measured by New Horizons in 2015, is about 1 Pa (10 μbar), roughly 100,000 times less than Earth's atmospheric pressure.
Some satellites in LEO face similar atmospheric pressures and need reboosting every then. Bottom line being: that's what objects in space around us face. So for all practical purposes Pluto's surface is exposed to a vacuum. Standing naked on it wouldn't be much different from being naked on Earth's orbit.
answered 9 hours ago
RenanRenan
45.7k11106230
45.7k11106230
$begingroup$
The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
$endgroup$
– Nuclear Wang
6 hours ago
$begingroup$
I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
$endgroup$
– Renan
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
$endgroup$
– Renan
6 hours ago
1
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
$endgroup$
– alephzero
4 hours ago
add a comment |
$begingroup$
The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
$endgroup$
– Nuclear Wang
6 hours ago
$begingroup$
I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
$endgroup$
– Renan
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
$endgroup$
– Renan
6 hours ago
1
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
$endgroup$
– alephzero
4 hours ago
$begingroup$
The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
$endgroup$
– Nuclear Wang
6 hours ago
$begingroup$
The changes you describe are seasonal in nature, and wouldn't give a changing appearance on the order of days.
$endgroup$
– Nuclear Wang
6 hours ago
$begingroup$
I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
$endgroup$
– Renan
6 hours ago
$begingroup$
I said use Pluto as an inspiration. It is very far from the Sun, so the temperature differences between its day and night are smaller than our Moon's. At our distance from the Sun the changes could happen daily.
$endgroup$
– Renan
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
Thanks for your answer. It sounds really intetesting, but could this kind of condensation occur in such a magnitude that it changes the look of the moon on a daily basis? Also please note that I edited the question to allow an atmosphere.
$endgroup$
– Elmy
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
$endgroup$
– Renan
6 hours ago
$begingroup$
@elmy yes. The (non-water) ices on the moon will not melt completely, but will become slush that slowly ane constantly moves as the Moon's own terminator line terminator line moves over its surface.
$endgroup$
– Renan
6 hours ago
1
1
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
$endgroup$
– alephzero
4 hours ago
$begingroup$
@Elmy Yes it could. We don't know what the climate is like where you live, but in in the UK on winter mornings the ground is often covered overnight with white frost which melts within a few hours after sunrise.
$endgroup$
– alephzero
4 hours ago
add a comment |
$begingroup$
Naturally occurring Thermochromic chemicals.
Those of us old enough to remember the 1970s remember mood rings.
While such chemicals are unlikely as natural deposits, it is fairly easy to imagine that some flowering plants could incorporate such as a form of sexual attraction or such-like.
No earth-like plants exist without the benefit of atmosphere, but perhaps an different design of plant forms could exist in thin carbon-dioxide atmosphere that may be compatible with your story. A hard-vacuum is likely to make significant plant-like coverage impossible.
Any high-contrast vegetation that has a short lifespan would perhaps be sufficient, esp. competing forms with different reflectance characteristics.
$endgroup$
add a comment |
$begingroup$
Naturally occurring Thermochromic chemicals.
Those of us old enough to remember the 1970s remember mood rings.
While such chemicals are unlikely as natural deposits, it is fairly easy to imagine that some flowering plants could incorporate such as a form of sexual attraction or such-like.
No earth-like plants exist without the benefit of atmosphere, but perhaps an different design of plant forms could exist in thin carbon-dioxide atmosphere that may be compatible with your story. A hard-vacuum is likely to make significant plant-like coverage impossible.
Any high-contrast vegetation that has a short lifespan would perhaps be sufficient, esp. competing forms with different reflectance characteristics.
$endgroup$
add a comment |
$begingroup$
Naturally occurring Thermochromic chemicals.
Those of us old enough to remember the 1970s remember mood rings.
While such chemicals are unlikely as natural deposits, it is fairly easy to imagine that some flowering plants could incorporate such as a form of sexual attraction or such-like.
No earth-like plants exist without the benefit of atmosphere, but perhaps an different design of plant forms could exist in thin carbon-dioxide atmosphere that may be compatible with your story. A hard-vacuum is likely to make significant plant-like coverage impossible.
Any high-contrast vegetation that has a short lifespan would perhaps be sufficient, esp. competing forms with different reflectance characteristics.
$endgroup$
Naturally occurring Thermochromic chemicals.
Those of us old enough to remember the 1970s remember mood rings.
While such chemicals are unlikely as natural deposits, it is fairly easy to imagine that some flowering plants could incorporate such as a form of sexual attraction or such-like.
No earth-like plants exist without the benefit of atmosphere, but perhaps an different design of plant forms could exist in thin carbon-dioxide atmosphere that may be compatible with your story. A hard-vacuum is likely to make significant plant-like coverage impossible.
Any high-contrast vegetation that has a short lifespan would perhaps be sufficient, esp. competing forms with different reflectance characteristics.
answered 9 hours ago
Gary WalkerGary Walker
14.8k22754
14.8k22754
add a comment |
add a comment |
$begingroup$
That solar system could be experiencing a phenomenon like the late heavy bombardment: the moon is constantly hit by meteorites, so that it is continuously shaped by these impacts.
The problem is that these meteorites must be very frequent (say in the order of the dozen of impacts in a day), but quite small - in the range of 10-20 meters - in order not to cause damage when they fall onto the main planet, burning in its atmosphere. In this case probably you should somehow justify the lack of bigger asteroids.
You could also point that the moon is of recent formation (maybe captured by the gravity of the planet), which implies its core is still active and gives origin to some vulcanic activity that shapes its surface (but in this case the changes would be slower and the surface of the moon wouldn't change a lot in the span of some days).
$endgroup$
add a comment |
$begingroup$
That solar system could be experiencing a phenomenon like the late heavy bombardment: the moon is constantly hit by meteorites, so that it is continuously shaped by these impacts.
The problem is that these meteorites must be very frequent (say in the order of the dozen of impacts in a day), but quite small - in the range of 10-20 meters - in order not to cause damage when they fall onto the main planet, burning in its atmosphere. In this case probably you should somehow justify the lack of bigger asteroids.
You could also point that the moon is of recent formation (maybe captured by the gravity of the planet), which implies its core is still active and gives origin to some vulcanic activity that shapes its surface (but in this case the changes would be slower and the surface of the moon wouldn't change a lot in the span of some days).
$endgroup$
add a comment |
$begingroup$
That solar system could be experiencing a phenomenon like the late heavy bombardment: the moon is constantly hit by meteorites, so that it is continuously shaped by these impacts.
The problem is that these meteorites must be very frequent (say in the order of the dozen of impacts in a day), but quite small - in the range of 10-20 meters - in order not to cause damage when they fall onto the main planet, burning in its atmosphere. In this case probably you should somehow justify the lack of bigger asteroids.
You could also point that the moon is of recent formation (maybe captured by the gravity of the planet), which implies its core is still active and gives origin to some vulcanic activity that shapes its surface (but in this case the changes would be slower and the surface of the moon wouldn't change a lot in the span of some days).
$endgroup$
That solar system could be experiencing a phenomenon like the late heavy bombardment: the moon is constantly hit by meteorites, so that it is continuously shaped by these impacts.
The problem is that these meteorites must be very frequent (say in the order of the dozen of impacts in a day), but quite small - in the range of 10-20 meters - in order not to cause damage when they fall onto the main planet, burning in its atmosphere. In this case probably you should somehow justify the lack of bigger asteroids.
You could also point that the moon is of recent formation (maybe captured by the gravity of the planet), which implies its core is still active and gives origin to some vulcanic activity that shapes its surface (but in this case the changes would be slower and the surface of the moon wouldn't change a lot in the span of some days).
answered 9 hours ago
McTroopersMcTroopers
2213
2213
add a comment |
add a comment |
$begingroup$
Possibly there could be intelligence of some sort on the moon and their activities can make a big visual change in the appearance of large sections of the moon during short periods.
Possibly they are artists trying out various "paint" patterns to see which make the moon look best.
Perhaps they move countless millions of large vehicles of various colors around on the moon, arranging them in various patterns as part of some sort of "dance".
Maybe they are trying to send a message to the natives of the planet and thus making an ever changing series of patterns on the moon.
A century or so ago an astronomer believed that some tiny changes of color he observed on the moon were the results of vast hordes of insects moving around.
So possibly on your moon thick areas of vegetation spring up, changing the color of vast regions, and then vast wandering hordes of insects travel toward them, changing the face of the moon as they move. When the insects arrive at the forest or meadow or swamp their color mingles with the color of the plants and changes the color of the region as seen from the planet.
So the insects eat all the vegetation in the region, changing its color, and leave their wastes (containing many seeds) behind to fertilize the soil. The insects move on, searching for another area of vegetation, and the area is now a different color, barren of vegetation until the seeds sprout and start to grow. Eventually the plants become thick enough to change the color of the region back to vegetation colored, then the region retains that color until the same or a different horde of insects arrives to eat the vegetation.
Of course it seem rather doubtful that a planet small enough to be habitable would have a moon large enough to be habitable for at least some types of life. That would make them seem a lot more like a double planet than like a planet and its moon.
Of course the intelligent beings on the moon don't have to be living beings; they could be machines.
Or the two worlds could both be habitable planets orbiting their star if their orbits are a lot closer to each other than any planetary orbits in our solar system, so that when the planets pass closest to each other the natives of one can see surface features on the other. There is actually a known solar system where planets in the habitable zone of their star do sometimes orbit close enough for someone on one of them to see surface features on the other - TRAPPIST-1.
The distance between the orbits of TRAPPIST-1b and TRAPPIST-1c is only 1.6 times the distance between the Earth and the Moon. The planets should appear prominently in each other's skies, in some cases appearing several times larger than the Moon appears from Earth.[41] A year on the closest planet passes in only 1.5 Earth days, while the seventh planet's year passes in only 18.8 days.[38][34]
https://en.wikipedia.org/wiki/TRAPPIST-11
Or maybe the "planet" and "moon" are actually both moons that orbit a gas giant planet.
Your "planet" could actually be a giant, Earth sized habitable moon, and the "moon" would orbit closer to the gas giant. Sometimes your "planet" and the inner moon would be almost on opposite sides of the gas giant and the inner moon wouldn't look big enough for details to be visible. But at intervals, probably every few days, the inner moon would pass close to the outer habitable moon and the natives of the habitable moon could see details of the surface of the inner moon and note the changes (and only in the parts of the moon that were lit by their star) .
If the inner moon orbits close enough to the gas giant the tidal heating should make the inner moon hyper volcanic like Io, the innermost Galilean moon of Jupiter. Various volcanoes might erupt often, spewing out vast amounts of lava of various colors to constantly resurface the inner moon. So each time that details of the inner moon were visible the surface patterns would be at least slightly different.
The problem with this is that the clouds and weather patterns on the gas giant planet would be visible all the time and would also change, thus possibly distracting the natives of the habitable moon from the show on the inner moon.
Possibly the moon in your story could suffer from tidal heating and constant resurfacing if it orbited a habitable planet in the right way. It would probably have to have an eccentric orbit which made it get noticeably farther and closer to the planet at various points in its orbit, and thus the patterns on its surface would only be visible when the moon was closer to the planet (and only in the parts of the moon that were lit by their star).
Possibly someone here can calculate if it is possible for a habitable planet to have a presumably recently captured moon with enough tidal heating to be constantly resurfacing itself.
$endgroup$
add a comment |
$begingroup$
Possibly there could be intelligence of some sort on the moon and their activities can make a big visual change in the appearance of large sections of the moon during short periods.
Possibly they are artists trying out various "paint" patterns to see which make the moon look best.
Perhaps they move countless millions of large vehicles of various colors around on the moon, arranging them in various patterns as part of some sort of "dance".
Maybe they are trying to send a message to the natives of the planet and thus making an ever changing series of patterns on the moon.
A century or so ago an astronomer believed that some tiny changes of color he observed on the moon were the results of vast hordes of insects moving around.
So possibly on your moon thick areas of vegetation spring up, changing the color of vast regions, and then vast wandering hordes of insects travel toward them, changing the face of the moon as they move. When the insects arrive at the forest or meadow or swamp their color mingles with the color of the plants and changes the color of the region as seen from the planet.
So the insects eat all the vegetation in the region, changing its color, and leave their wastes (containing many seeds) behind to fertilize the soil. The insects move on, searching for another area of vegetation, and the area is now a different color, barren of vegetation until the seeds sprout and start to grow. Eventually the plants become thick enough to change the color of the region back to vegetation colored, then the region retains that color until the same or a different horde of insects arrives to eat the vegetation.
Of course it seem rather doubtful that a planet small enough to be habitable would have a moon large enough to be habitable for at least some types of life. That would make them seem a lot more like a double planet than like a planet and its moon.
Of course the intelligent beings on the moon don't have to be living beings; they could be machines.
Or the two worlds could both be habitable planets orbiting their star if their orbits are a lot closer to each other than any planetary orbits in our solar system, so that when the planets pass closest to each other the natives of one can see surface features on the other. There is actually a known solar system where planets in the habitable zone of their star do sometimes orbit close enough for someone on one of them to see surface features on the other - TRAPPIST-1.
The distance between the orbits of TRAPPIST-1b and TRAPPIST-1c is only 1.6 times the distance between the Earth and the Moon. The planets should appear prominently in each other's skies, in some cases appearing several times larger than the Moon appears from Earth.[41] A year on the closest planet passes in only 1.5 Earth days, while the seventh planet's year passes in only 18.8 days.[38][34]
https://en.wikipedia.org/wiki/TRAPPIST-11
Or maybe the "planet" and "moon" are actually both moons that orbit a gas giant planet.
Your "planet" could actually be a giant, Earth sized habitable moon, and the "moon" would orbit closer to the gas giant. Sometimes your "planet" and the inner moon would be almost on opposite sides of the gas giant and the inner moon wouldn't look big enough for details to be visible. But at intervals, probably every few days, the inner moon would pass close to the outer habitable moon and the natives of the habitable moon could see details of the surface of the inner moon and note the changes (and only in the parts of the moon that were lit by their star) .
If the inner moon orbits close enough to the gas giant the tidal heating should make the inner moon hyper volcanic like Io, the innermost Galilean moon of Jupiter. Various volcanoes might erupt often, spewing out vast amounts of lava of various colors to constantly resurface the inner moon. So each time that details of the inner moon were visible the surface patterns would be at least slightly different.
The problem with this is that the clouds and weather patterns on the gas giant planet would be visible all the time and would also change, thus possibly distracting the natives of the habitable moon from the show on the inner moon.
Possibly the moon in your story could suffer from tidal heating and constant resurfacing if it orbited a habitable planet in the right way. It would probably have to have an eccentric orbit which made it get noticeably farther and closer to the planet at various points in its orbit, and thus the patterns on its surface would only be visible when the moon was closer to the planet (and only in the parts of the moon that were lit by their star).
Possibly someone here can calculate if it is possible for a habitable planet to have a presumably recently captured moon with enough tidal heating to be constantly resurfacing itself.
$endgroup$
add a comment |
$begingroup$
Possibly there could be intelligence of some sort on the moon and their activities can make a big visual change in the appearance of large sections of the moon during short periods.
Possibly they are artists trying out various "paint" patterns to see which make the moon look best.
Perhaps they move countless millions of large vehicles of various colors around on the moon, arranging them in various patterns as part of some sort of "dance".
Maybe they are trying to send a message to the natives of the planet and thus making an ever changing series of patterns on the moon.
A century or so ago an astronomer believed that some tiny changes of color he observed on the moon were the results of vast hordes of insects moving around.
So possibly on your moon thick areas of vegetation spring up, changing the color of vast regions, and then vast wandering hordes of insects travel toward them, changing the face of the moon as they move. When the insects arrive at the forest or meadow or swamp their color mingles with the color of the plants and changes the color of the region as seen from the planet.
So the insects eat all the vegetation in the region, changing its color, and leave their wastes (containing many seeds) behind to fertilize the soil. The insects move on, searching for another area of vegetation, and the area is now a different color, barren of vegetation until the seeds sprout and start to grow. Eventually the plants become thick enough to change the color of the region back to vegetation colored, then the region retains that color until the same or a different horde of insects arrives to eat the vegetation.
Of course it seem rather doubtful that a planet small enough to be habitable would have a moon large enough to be habitable for at least some types of life. That would make them seem a lot more like a double planet than like a planet and its moon.
Of course the intelligent beings on the moon don't have to be living beings; they could be machines.
Or the two worlds could both be habitable planets orbiting their star if their orbits are a lot closer to each other than any planetary orbits in our solar system, so that when the planets pass closest to each other the natives of one can see surface features on the other. There is actually a known solar system where planets in the habitable zone of their star do sometimes orbit close enough for someone on one of them to see surface features on the other - TRAPPIST-1.
The distance between the orbits of TRAPPIST-1b and TRAPPIST-1c is only 1.6 times the distance between the Earth and the Moon. The planets should appear prominently in each other's skies, in some cases appearing several times larger than the Moon appears from Earth.[41] A year on the closest planet passes in only 1.5 Earth days, while the seventh planet's year passes in only 18.8 days.[38][34]
https://en.wikipedia.org/wiki/TRAPPIST-11
Or maybe the "planet" and "moon" are actually both moons that orbit a gas giant planet.
Your "planet" could actually be a giant, Earth sized habitable moon, and the "moon" would orbit closer to the gas giant. Sometimes your "planet" and the inner moon would be almost on opposite sides of the gas giant and the inner moon wouldn't look big enough for details to be visible. But at intervals, probably every few days, the inner moon would pass close to the outer habitable moon and the natives of the habitable moon could see details of the surface of the inner moon and note the changes (and only in the parts of the moon that were lit by their star) .
If the inner moon orbits close enough to the gas giant the tidal heating should make the inner moon hyper volcanic like Io, the innermost Galilean moon of Jupiter. Various volcanoes might erupt often, spewing out vast amounts of lava of various colors to constantly resurface the inner moon. So each time that details of the inner moon were visible the surface patterns would be at least slightly different.
The problem with this is that the clouds and weather patterns on the gas giant planet would be visible all the time and would also change, thus possibly distracting the natives of the habitable moon from the show on the inner moon.
Possibly the moon in your story could suffer from tidal heating and constant resurfacing if it orbited a habitable planet in the right way. It would probably have to have an eccentric orbit which made it get noticeably farther and closer to the planet at various points in its orbit, and thus the patterns on its surface would only be visible when the moon was closer to the planet (and only in the parts of the moon that were lit by their star).
Possibly someone here can calculate if it is possible for a habitable planet to have a presumably recently captured moon with enough tidal heating to be constantly resurfacing itself.
$endgroup$
Possibly there could be intelligence of some sort on the moon and their activities can make a big visual change in the appearance of large sections of the moon during short periods.
Possibly they are artists trying out various "paint" patterns to see which make the moon look best.
Perhaps they move countless millions of large vehicles of various colors around on the moon, arranging them in various patterns as part of some sort of "dance".
Maybe they are trying to send a message to the natives of the planet and thus making an ever changing series of patterns on the moon.
A century or so ago an astronomer believed that some tiny changes of color he observed on the moon were the results of vast hordes of insects moving around.
So possibly on your moon thick areas of vegetation spring up, changing the color of vast regions, and then vast wandering hordes of insects travel toward them, changing the face of the moon as they move. When the insects arrive at the forest or meadow or swamp their color mingles with the color of the plants and changes the color of the region as seen from the planet.
So the insects eat all the vegetation in the region, changing its color, and leave their wastes (containing many seeds) behind to fertilize the soil. The insects move on, searching for another area of vegetation, and the area is now a different color, barren of vegetation until the seeds sprout and start to grow. Eventually the plants become thick enough to change the color of the region back to vegetation colored, then the region retains that color until the same or a different horde of insects arrives to eat the vegetation.
Of course it seem rather doubtful that a planet small enough to be habitable would have a moon large enough to be habitable for at least some types of life. That would make them seem a lot more like a double planet than like a planet and its moon.
Of course the intelligent beings on the moon don't have to be living beings; they could be machines.
Or the two worlds could both be habitable planets orbiting their star if their orbits are a lot closer to each other than any planetary orbits in our solar system, so that when the planets pass closest to each other the natives of one can see surface features on the other. There is actually a known solar system where planets in the habitable zone of their star do sometimes orbit close enough for someone on one of them to see surface features on the other - TRAPPIST-1.
The distance between the orbits of TRAPPIST-1b and TRAPPIST-1c is only 1.6 times the distance between the Earth and the Moon. The planets should appear prominently in each other's skies, in some cases appearing several times larger than the Moon appears from Earth.[41] A year on the closest planet passes in only 1.5 Earth days, while the seventh planet's year passes in only 18.8 days.[38][34]
https://en.wikipedia.org/wiki/TRAPPIST-11
Or maybe the "planet" and "moon" are actually both moons that orbit a gas giant planet.
Your "planet" could actually be a giant, Earth sized habitable moon, and the "moon" would orbit closer to the gas giant. Sometimes your "planet" and the inner moon would be almost on opposite sides of the gas giant and the inner moon wouldn't look big enough for details to be visible. But at intervals, probably every few days, the inner moon would pass close to the outer habitable moon and the natives of the habitable moon could see details of the surface of the inner moon and note the changes (and only in the parts of the moon that were lit by their star) .
If the inner moon orbits close enough to the gas giant the tidal heating should make the inner moon hyper volcanic like Io, the innermost Galilean moon of Jupiter. Various volcanoes might erupt often, spewing out vast amounts of lava of various colors to constantly resurface the inner moon. So each time that details of the inner moon were visible the surface patterns would be at least slightly different.
The problem with this is that the clouds and weather patterns on the gas giant planet would be visible all the time and would also change, thus possibly distracting the natives of the habitable moon from the show on the inner moon.
Possibly the moon in your story could suffer from tidal heating and constant resurfacing if it orbited a habitable planet in the right way. It would probably have to have an eccentric orbit which made it get noticeably farther and closer to the planet at various points in its orbit, and thus the patterns on its surface would only be visible when the moon was closer to the planet (and only in the parts of the moon that were lit by their star).
Possibly someone here can calculate if it is possible for a habitable planet to have a presumably recently captured moon with enough tidal heating to be constantly resurfacing itself.
answered 8 hours ago
M. A. GoldingM. A. Golding
8,021425
8,021425
add a comment |
add a comment |
$begingroup$
An alien race has covered the planet, or whatever percentage you see fit with a giant TV screen.
Maybe they double as solar panels somehow.
Now they can literally change any part of the visible surface at whim.
Just wait till they spam you with moon sized commericials... muhhahahahaha!
$endgroup$
add a comment |
$begingroup$
An alien race has covered the planet, or whatever percentage you see fit with a giant TV screen.
Maybe they double as solar panels somehow.
Now they can literally change any part of the visible surface at whim.
Just wait till they spam you with moon sized commericials... muhhahahahaha!
$endgroup$
add a comment |
$begingroup$
An alien race has covered the planet, or whatever percentage you see fit with a giant TV screen.
Maybe they double as solar panels somehow.
Now they can literally change any part of the visible surface at whim.
Just wait till they spam you with moon sized commericials... muhhahahahaha!
$endgroup$
An alien race has covered the planet, or whatever percentage you see fit with a giant TV screen.
Maybe they double as solar panels somehow.
Now they can literally change any part of the visible surface at whim.
Just wait till they spam you with moon sized commericials... muhhahahahaha!
answered 8 hours ago
cybernardcybernard
2,03836
2,03836
add a comment |
add a comment |
$begingroup$
Long ago an intelligent species found this moon and made plans to inhabit it. They created a network of tunnels all across the planet just below its surface. They planted the seeds of life and prepared to begin settling, but for some reason, they never did. So the moon was left, carved tunnels beneath its surface with the beginnings of life sprouting.
Fast forward a few thousand years to today, and the moon is buzzing with life--but that life all lives underground. A specific creature, the Mitter, has thrived on the underground flora and fauna. They are a fast moving species that is nomadic by nature, constantly moving to different places in different patterns every day.
However, when they move, they let off an abundance of benign chemicals that rise to the surface. These chemicals glow when in contact with the outside air--glowing a slightly different hue for each Mitter. With the abundance of the creatures and their unusual travel patterns, the planet appears to glow in ever changing shades and hues. Perhaps the Mitters' chemicals glow different colors depending on the time of season so the moon will go through phases of colors throughout the year?
$endgroup$
add a comment |
$begingroup$
Long ago an intelligent species found this moon and made plans to inhabit it. They created a network of tunnels all across the planet just below its surface. They planted the seeds of life and prepared to begin settling, but for some reason, they never did. So the moon was left, carved tunnels beneath its surface with the beginnings of life sprouting.
Fast forward a few thousand years to today, and the moon is buzzing with life--but that life all lives underground. A specific creature, the Mitter, has thrived on the underground flora and fauna. They are a fast moving species that is nomadic by nature, constantly moving to different places in different patterns every day.
However, when they move, they let off an abundance of benign chemicals that rise to the surface. These chemicals glow when in contact with the outside air--glowing a slightly different hue for each Mitter. With the abundance of the creatures and their unusual travel patterns, the planet appears to glow in ever changing shades and hues. Perhaps the Mitters' chemicals glow different colors depending on the time of season so the moon will go through phases of colors throughout the year?
$endgroup$
add a comment |
$begingroup$
Long ago an intelligent species found this moon and made plans to inhabit it. They created a network of tunnels all across the planet just below its surface. They planted the seeds of life and prepared to begin settling, but for some reason, they never did. So the moon was left, carved tunnels beneath its surface with the beginnings of life sprouting.
Fast forward a few thousand years to today, and the moon is buzzing with life--but that life all lives underground. A specific creature, the Mitter, has thrived on the underground flora and fauna. They are a fast moving species that is nomadic by nature, constantly moving to different places in different patterns every day.
However, when they move, they let off an abundance of benign chemicals that rise to the surface. These chemicals glow when in contact with the outside air--glowing a slightly different hue for each Mitter. With the abundance of the creatures and their unusual travel patterns, the planet appears to glow in ever changing shades and hues. Perhaps the Mitters' chemicals glow different colors depending on the time of season so the moon will go through phases of colors throughout the year?
$endgroup$
Long ago an intelligent species found this moon and made plans to inhabit it. They created a network of tunnels all across the planet just below its surface. They planted the seeds of life and prepared to begin settling, but for some reason, they never did. So the moon was left, carved tunnels beneath its surface with the beginnings of life sprouting.
Fast forward a few thousand years to today, and the moon is buzzing with life--but that life all lives underground. A specific creature, the Mitter, has thrived on the underground flora and fauna. They are a fast moving species that is nomadic by nature, constantly moving to different places in different patterns every day.
However, when they move, they let off an abundance of benign chemicals that rise to the surface. These chemicals glow when in contact with the outside air--glowing a slightly different hue for each Mitter. With the abundance of the creatures and their unusual travel patterns, the planet appears to glow in ever changing shades and hues. Perhaps the Mitters' chemicals glow different colors depending on the time of season so the moon will go through phases of colors throughout the year?
answered 6 hours ago
scohe001scohe001
8051517
8051517
add a comment |
add a comment |
$begingroup$
Oceans of nonlinear chemical oscillator compound!
Imagine that there`s an ocean on the moon that is filled to the brim with e.g. malonic acid and potassium bromate. That would yield literal chaotic color patterns floating both on its surface and all the way down to the seabed.
This is called the Belousov–Zhabotinsky reaction.
All weather changes, including the amount of sunlight absorbed, the surface waves, the underwater currents (well, technically it`s not water, but whatever), the winds, the evaporation, the volcanic activity — everything of the sort would add to the total randomness and uniqueness of the pattern.
Here`s a video of it oscillating in a Petri dish. And here`s another one.
$endgroup$
add a comment |
$begingroup$
Oceans of nonlinear chemical oscillator compound!
Imagine that there`s an ocean on the moon that is filled to the brim with e.g. malonic acid and potassium bromate. That would yield literal chaotic color patterns floating both on its surface and all the way down to the seabed.
This is called the Belousov–Zhabotinsky reaction.
All weather changes, including the amount of sunlight absorbed, the surface waves, the underwater currents (well, technically it`s not water, but whatever), the winds, the evaporation, the volcanic activity — everything of the sort would add to the total randomness and uniqueness of the pattern.
Here`s a video of it oscillating in a Petri dish. And here`s another one.
$endgroup$
add a comment |
$begingroup$
Oceans of nonlinear chemical oscillator compound!
Imagine that there`s an ocean on the moon that is filled to the brim with e.g. malonic acid and potassium bromate. That would yield literal chaotic color patterns floating both on its surface and all the way down to the seabed.
This is called the Belousov–Zhabotinsky reaction.
All weather changes, including the amount of sunlight absorbed, the surface waves, the underwater currents (well, technically it`s not water, but whatever), the winds, the evaporation, the volcanic activity — everything of the sort would add to the total randomness and uniqueness of the pattern.
Here`s a video of it oscillating in a Petri dish. And here`s another one.
$endgroup$
Oceans of nonlinear chemical oscillator compound!
Imagine that there`s an ocean on the moon that is filled to the brim with e.g. malonic acid and potassium bromate. That would yield literal chaotic color patterns floating both on its surface and all the way down to the seabed.
This is called the Belousov–Zhabotinsky reaction.
All weather changes, including the amount of sunlight absorbed, the surface waves, the underwater currents (well, technically it`s not water, but whatever), the winds, the evaporation, the volcanic activity — everything of the sort would add to the total randomness and uniqueness of the pattern.
Here`s a video of it oscillating in a Petri dish. And here`s another one.
edited 5 hours ago
answered 6 hours ago
hidefromkgbhidefromkgb
20316
20316
add a comment |
add a comment |
$begingroup$
Here are some ideas, for a moon with a solid face:
- It could have really active plate tectonics moving the surface features around, which (as I understand it) would also imply a strong magnetic field and lots of volcanic activity.
- It could be very large, and the orbit of your planet could be just near-enough to an asteroid belt that whenever the moon moves toward the outer side of the orbit, it pulls asteroids into itself, actively rearranging the craters on its face
- If your planet is large, its moon could have a ring small of meteors around it, regularly falling into the moon (with no atmosphere to destroy them) and those could also rearrange the craters.
$endgroup$
add a comment |
$begingroup$
Here are some ideas, for a moon with a solid face:
- It could have really active plate tectonics moving the surface features around, which (as I understand it) would also imply a strong magnetic field and lots of volcanic activity.
- It could be very large, and the orbit of your planet could be just near-enough to an asteroid belt that whenever the moon moves toward the outer side of the orbit, it pulls asteroids into itself, actively rearranging the craters on its face
- If your planet is large, its moon could have a ring small of meteors around it, regularly falling into the moon (with no atmosphere to destroy them) and those could also rearrange the craters.
$endgroup$
add a comment |
$begingroup$
Here are some ideas, for a moon with a solid face:
- It could have really active plate tectonics moving the surface features around, which (as I understand it) would also imply a strong magnetic field and lots of volcanic activity.
- It could be very large, and the orbit of your planet could be just near-enough to an asteroid belt that whenever the moon moves toward the outer side of the orbit, it pulls asteroids into itself, actively rearranging the craters on its face
- If your planet is large, its moon could have a ring small of meteors around it, regularly falling into the moon (with no atmosphere to destroy them) and those could also rearrange the craters.
$endgroup$
Here are some ideas, for a moon with a solid face:
- It could have really active plate tectonics moving the surface features around, which (as I understand it) would also imply a strong magnetic field and lots of volcanic activity.
- It could be very large, and the orbit of your planet could be just near-enough to an asteroid belt that whenever the moon moves toward the outer side of the orbit, it pulls asteroids into itself, actively rearranging the craters on its face
- If your planet is large, its moon could have a ring small of meteors around it, regularly falling into the moon (with no atmosphere to destroy them) and those could also rearrange the craters.
answered 5 hours ago
boxcartenantboxcartenant
2,012117
2,012117
add a comment |
add a comment |
$begingroup$
A watery body, such as Enceladus (maybe Ceres as long as it has an icy core), orbits as a moon. This moon could have a very eccentric orbit, causing tidal forced to act upon it, causing cryo-volcanism. these cryovolcanos can cover the surface with various chemicals and minerals (water, salty brine, methane, ethane, or other organics) in an ever changing pattern.
The cracking and shifting of the fragile surface would also aid in the changing surface patterns.
$endgroup$
add a comment |
$begingroup$
A watery body, such as Enceladus (maybe Ceres as long as it has an icy core), orbits as a moon. This moon could have a very eccentric orbit, causing tidal forced to act upon it, causing cryo-volcanism. these cryovolcanos can cover the surface with various chemicals and minerals (water, salty brine, methane, ethane, or other organics) in an ever changing pattern.
The cracking and shifting of the fragile surface would also aid in the changing surface patterns.
$endgroup$
add a comment |
$begingroup$
A watery body, such as Enceladus (maybe Ceres as long as it has an icy core), orbits as a moon. This moon could have a very eccentric orbit, causing tidal forced to act upon it, causing cryo-volcanism. these cryovolcanos can cover the surface with various chemicals and minerals (water, salty brine, methane, ethane, or other organics) in an ever changing pattern.
The cracking and shifting of the fragile surface would also aid in the changing surface patterns.
$endgroup$
A watery body, such as Enceladus (maybe Ceres as long as it has an icy core), orbits as a moon. This moon could have a very eccentric orbit, causing tidal forced to act upon it, causing cryo-volcanism. these cryovolcanos can cover the surface with various chemicals and minerals (water, salty brine, methane, ethane, or other organics) in an ever changing pattern.
The cracking and shifting of the fragile surface would also aid in the changing surface patterns.
edited 5 hours ago
answered 5 hours ago
sonvarsonvar
414
414
add a comment |
add a comment |
$begingroup$
Arctic sea ice is constantly changing, although not on a daily timescale:
https://thumbs.gfycat.com/BothDismalEmperorpenguin.webp
$endgroup$
add a comment |
$begingroup$
Arctic sea ice is constantly changing, although not on a daily timescale:
https://thumbs.gfycat.com/BothDismalEmperorpenguin.webp
$endgroup$
add a comment |
$begingroup$
Arctic sea ice is constantly changing, although not on a daily timescale:
https://thumbs.gfycat.com/BothDismalEmperorpenguin.webp
$endgroup$
Arctic sea ice is constantly changing, although not on a daily timescale:
https://thumbs.gfycat.com/BothDismalEmperorpenguin.webp
answered 3 hours ago
Keith McClaryKeith McClary
1492
1492
add a comment |
add a comment |
$begingroup$
Your planet is tidally locked and it's moon is made of something with a low melting point.
This means that it's eternal twilight on the narrow band of habitable terrain on your planet, and that the day is marked by the ascent of the moon, which, continually melted by the sun and frozen by the planet's shadow, changes each day.
$endgroup$
add a comment |
$begingroup$
Your planet is tidally locked and it's moon is made of something with a low melting point.
This means that it's eternal twilight on the narrow band of habitable terrain on your planet, and that the day is marked by the ascent of the moon, which, continually melted by the sun and frozen by the planet's shadow, changes each day.
$endgroup$
add a comment |
$begingroup$
Your planet is tidally locked and it's moon is made of something with a low melting point.
This means that it's eternal twilight on the narrow band of habitable terrain on your planet, and that the day is marked by the ascent of the moon, which, continually melted by the sun and frozen by the planet's shadow, changes each day.
$endgroup$
Your planet is tidally locked and it's moon is made of something with a low melting point.
This means that it's eternal twilight on the narrow band of habitable terrain on your planet, and that the day is marked by the ascent of the moon, which, continually melted by the sun and frozen by the planet's shadow, changes each day.
answered 3 hours ago
Iron GremlinIron Gremlin
6497
6497
add a comment |
add a comment |
$begingroup$
The surface of the moon is covered in an exotic lifeform with an exceedingly rapid lifecycle. Colonies of this lifeform grow to cover large portions of the lunar surface in as little as 12 hours, competing for space with surrounding colonies, before rapidly crashing as soil fertility is depleted. No sooner has one colony collapsed, than another has begun its growth on another part of the moon's surface.
$endgroup$
add a comment |
$begingroup$
The surface of the moon is covered in an exotic lifeform with an exceedingly rapid lifecycle. Colonies of this lifeform grow to cover large portions of the lunar surface in as little as 12 hours, competing for space with surrounding colonies, before rapidly crashing as soil fertility is depleted. No sooner has one colony collapsed, than another has begun its growth on another part of the moon's surface.
$endgroup$
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The surface of the moon is covered in an exotic lifeform with an exceedingly rapid lifecycle. Colonies of this lifeform grow to cover large portions of the lunar surface in as little as 12 hours, competing for space with surrounding colonies, before rapidly crashing as soil fertility is depleted. No sooner has one colony collapsed, than another has begun its growth on another part of the moon's surface.
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The surface of the moon is covered in an exotic lifeform with an exceedingly rapid lifecycle. Colonies of this lifeform grow to cover large portions of the lunar surface in as little as 12 hours, competing for space with surrounding colonies, before rapidly crashing as soil fertility is depleted. No sooner has one colony collapsed, than another has begun its growth on another part of the moon's surface.
answered 2 hours ago
Arkenstein XIIArkenstein XII
2,320425
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Related: Always a full Moon for the Emperor - Can this be achieved with solar panels and LEDs?
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– Alexander
7 hours ago
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It's Io! Of course, you'd be hard pressed to find a moon with a lot of geological activity without also having Io's conditions. (I.e. Orbiting a gas giant and surrounded by many other moons.) Maybe if the moon somehow formed very recently?
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– Lemma Prism
5 hours ago
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Clouds don't necessarily look the same from space as they do from the ground. If you look at images of Earth from space, the clouds look pretty other-worldly to me. Plus, if your moon has a different chemistry from the planet, the clouds will look very different anyway - think about the clouds on Venus, or any of the gas giants.
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– Nathaniel
44 mins ago