Name: 初のエクソムーンを発見したかもしれない!| サイショウニュース (We May Have Found the First Exomoon! | SciShow News)
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It's been more than 20 years since astronomers discovered the first planet

And today, there's a catalog of more than 3700 confirmed exoplanets,

along with thousands more unconfirmed candidates.

But now, we might have found the very first moon beyond our solar system,

Last week, Science Advances published the first quote-unquote

Neptune-sized exomoon 8,000 light-years away.

In 2017, data from the Kepler Space Telescope seemed to contain hints that an

The data revealed that a body the size of a gas

giant was orbiting a larger body called Kepler-1625b.

Now, two astronomers from Columbia University have used the even-stronger

Hubble Space Telescope to further explore the system.

And from what they saw, it looks like that exomoon signature

In the new study, the team used the transit method to study 1625b.

In other words, they analyzed the light coming from its star and how it dims

as the planet passes between the star and us.

The weird thing was, about 3.5 hours after the planet's transit ended, there was

That suggests the planet has a moon trailing it.

To the disappointment of space nerds everywhere (including us) the team

ran out of observation time before the potential moon had finished its own transit.

So they don't have a full set of data to analyze.

The good news is, there is a little more data

that supports the planet having a natural satellite:

The planet's transit started over an hour earlier than was predicted.

That could happen if it had a moon tugging on it

and changing the system's center of gravity.

So far, all this evidence suggests this moon, if it exists,

is comparable in mass and size to Neptune.

But since the planet is around the same size as Jupiter

and a few times more massive, it makes sense.

Then again, these properties aren't based on the strongest models,

It could be that our data is a bit off and that there isn't a moon at all.

Instead, there could be a second planet in the system that's responsible,

although there hasn't been any evidence of that so far.

It's also possible that 1625b could just have

Or it could be orbiting at such a distance or angle that it's not transiting every

time we look at it, which could be why our predictions were off this time.

Right now, the authors of this paper confess this first exomoon has to survive

years of scrutiny and follow-up before its existence can be confirmed.

But if it does end up being a moon beyond our solar system,

it will be a really important target to continue studying.

For example, since it's likely much, much larger than any moon in our system,

it opens the question of how planetary systems form and evolve.

And the moon's origins at the moment are a total mystery.

Like, was it captured, or did it form alongside its partner?

In other moon news, a study published online this week in Nature Geoscience

predicts a decent chunk of Jupiter's moon Europa

Officially, these blades are called penitentes.

They're formed when large chunks of frozen water heat up and sublimate,

turning directly from a solid into a gas.

On Earth, we see this happen in places like the top of the Andes Mountains.

But we've also seen evidence of these blades on Pluto.

For penitentes to form, the environment has to be super dry and cold,

the air has to be really still, and the sunlight has to hit the ice

at just the right angle and for long enough periods of time.

Then, the Sun's radiation causes heaps of water molecules to sublimate,

carving deep depressions into the surface and turning everything really spiky.

In other words, the penitentes don't grow up like stalagmites do

Eventually, penitentes smooth out or break apart,

either from geologic activity beneath the surface or space debris

But the amount of time that takes can vary.

To learn more about Europa, astronomers wanted to determine the likelihood,

It took into account things like how Europa is tilted toward the Sun,

its range of temperatures, and the reflectivity of its surface.

They also needed to estimate how often space debris would crash into

Europa's surface, which would smooth out its features.

According to their model, water could sublimate faster than erosion could

smooth things out at latitudes below 23° or so.

That means, for a large band around Europa's equator,

we'd likely see a healthy population of penitentes.

The team also calculated that, over 50 million years

which is the average age of Europa's surface

the blades could get up to 15 meters tall.

That's three times taller than what we usually see on Earth.

Of course, all their stats are averages, and don't take into account local

geologic features, or exactly how impurities in the ice will play a role.

Unfortunately, our technology near Europa doesn't have the proper resolution

to find photographic evidence of this spiky surface.

But there is both ground-based radar and thermal data

from the 1990s Galileo probe that suggests penitentes could be there.

Studies like this are cool, but they're about more than just uncovering giant ice

To scientists and engineers, this kind of information is really important

to know when planning a future lander mission to Europa.

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初のエクソムーンを発見したかもしれない!| サイショウニュース (We May Have Found the First Exomoon! | SciShow News)

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