Feb. 3, 2025
Cosmic Questions, Solar Mysteries & Lunar Dreams: #492 - The Great Space Q&A
Space Nuts Episode 492: Tidal Locking, Solar Mysteries, and Moon Travel
Join Andrew Dunkley and Professor Jonti Horner in this engaging Q&A edition of Space Nuts, where they tackle a variety of cosmic questions from our curious listeners. From the...
Space Nuts Episode 492: Tidal Locking, Solar Mysteries, and Moon Travel
Join Andrew Dunkley and Professor Jonti Horner in this engaging Q&A edition of Space Nuts, where they tackle a variety of cosmic questions from our curious listeners. From the complexities of tidal locking in celestial systems to the intriguing heat discrepancies in the Sun's layers, and even how to get to the Moon, this episode is filled with fascinating insights that will deepen your understanding of the universe.
Episode Highlights:
- Tidal Locking Explained: Jake from Tennessee asks about the possibility of tidal locking between stars and their orbiting planets. Jonti dives into the mechanics of tidal interactions, using examples from our own solar system, including the Earth-Moon relationship and Pluto's moons.
- Solar Mysteries: Clint from Georgia raises a thought-provoking question about the Sun's corona, which is millions of degrees hotter than its surface. Andrew and Jonti explore the latest theories on how gravitational interactions and magnetic fields could contribute to this phenomenon.
- How to Get to the Moon: Emily from Melbourne wants to know how humans travel to the Moon. Jonti breaks down the journey, explaining the rocket science behind space travel, the challenges of exiting Earth's atmosphere, and the exciting prospects of future lunar missions.
- Listener Engagement: Andrew and Jonti encourage listeners to submit their own questions, highlighting the importance of curiosity in the scientific community.
For more Space Nuts, including our continually updating newsfeed and to listen to all our episodes, visit our website. Follow us on social media at SpaceNutsPod on Facebook, X, YouTube Music Music, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favorite platform.
If you'd like to help support Space Nuts and join our growing family of insiders for commercial-free episodes and more, visit spacenutspodcast.com/about
Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.
00:00 - Introduction to the episode and topics
02:15 - Discussion on tidal locking and celestial mechanics
10:30 - Insights into the Sun's corona and heat discrepancies
18:00 - How to travel to the Moon explained
26:45 - Listener Ash engagement and questions
30:00 - Closing thoughts and future episodes
✍️ Episode References
NASA's Lunar Missions
https://www.nasa.gov/
Tidal Locking
https://en.wikipedia.org/wiki/Tidal_locking
Solar Corona Studies
https://www.nasa.gov/solar-system/
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts--2631155/support.
Join Andrew Dunkley and Professor Jonti Horner in this engaging Q&A edition of Space Nuts, where they tackle a variety of cosmic questions from our curious listeners. From the complexities of tidal locking in celestial systems to the intriguing heat discrepancies in the Sun's layers, and even how to get to the Moon, this episode is filled with fascinating insights that will deepen your understanding of the universe.
Episode Highlights:
- Tidal Locking Explained: Jake from Tennessee asks about the possibility of tidal locking between stars and their orbiting planets. Jonti dives into the mechanics of tidal interactions, using examples from our own solar system, including the Earth-Moon relationship and Pluto's moons.
- Solar Mysteries: Clint from Georgia raises a thought-provoking question about the Sun's corona, which is millions of degrees hotter than its surface. Andrew and Jonti explore the latest theories on how gravitational interactions and magnetic fields could contribute to this phenomenon.
- How to Get to the Moon: Emily from Melbourne wants to know how humans travel to the Moon. Jonti breaks down the journey, explaining the rocket science behind space travel, the challenges of exiting Earth's atmosphere, and the exciting prospects of future lunar missions.
- Listener Engagement: Andrew and Jonti encourage listeners to submit their own questions, highlighting the importance of curiosity in the scientific community.
For more Space Nuts, including our continually updating newsfeed and to listen to all our episodes, visit our website. Follow us on social media at SpaceNutsPod on Facebook, X, YouTube Music Music, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favorite platform.
If you'd like to help support Space Nuts and join our growing family of insiders for commercial-free episodes and more, visit spacenutspodcast.com/about
Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.
00:00 - Introduction to the episode and topics
02:15 - Discussion on tidal locking and celestial mechanics
10:30 - Insights into the Sun's corona and heat discrepancies
18:00 - How to travel to the Moon explained
26:45 - Listener Ash engagement and questions
30:00 - Closing thoughts and future episodes
✍️ Episode References
NASA's Lunar Missions
https://www.nasa.gov/
Tidal Locking
https://en.wikipedia.org/wiki/Tidal_locking
Solar Corona Studies
https://www.nasa.gov/solar-system/
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts--2631155/support.
WEBVTT
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By there, Andrew Dunkley here and you're listening to Space
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Nuts Q and a edition. Glad to have your company
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once again. On this episode we will be answering an
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array of questions on very different topics. Jake is asking
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us about tidle Locke. That's not something to hold back
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the water in the Thames River, No, something completely different.
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Clint wants to talk about the heat of the sun. Emily,
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Sandy's daughter in Melbourne, wants to get to the moon
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and we're going to tell her how. And Fenton has
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asked a vast array of questions which could probably fill
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an episode on their own about the radiation of Jupiter.
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That's all coming up on this edition.
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Of Space Nuts Channel ten nine ignition Space Nuts or
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three two one spaces and I reported Neil's good and.
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Joining me once again is not Professor Fred Watson because
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he is overseas looking at the sky up in the
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Northern Hemisphere. But with us is Professor John D. Horner,
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Professor of astrophysics at the University of Southern Queensland. Johnty, Hello, Hey,
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how are you going? I am well, we're working on
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getting you your own intro, but we're in a time
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of year where all the radio stations in Australia want
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new jingles, and our studio producer who does all that
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work is flat out at the moment, so we've been
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put on the back burner, I think. But you can
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understand why all the radio stations want to ramp up
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how they sound so that they can get new audience.
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I worked in radio for forty years. I'm pretty sure
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changing the jingle doesn't actually do much, but just my
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observation in forty you'll look at it just in time
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for Fred to get buck. Yes, yes, I think that's
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exactly what I was about to say.
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Stole my joke.
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Never mind, But what we'll do right now is look
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at some audience questions. I love this particular episode every
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week because it's the audience's chance to get involved. And
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we've got a few audio questions coming up. But our
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first one comes from Jake, who actually sent this question
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via Facebook Messenger, which we don't often catch because we
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don't monitor it as much as we as we probably should.
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But we just haven't got the person power. But I
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just happen to be sort of on my iPad the
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other day and went, oh, hang on a minute, there's
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a little one there. Greetings from Tennessee, USA, Tennessee, home
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of the Titans.
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I know that.
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Several two body systems are in various stages of tidal locking.
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I was wondering if for star or planet with several
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orbiting bodies can even become tidally locked with a particular one.
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For example, can the Sun become tidally locked to one
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of our planets? Likewise, can Jupiter become tidally locked to
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one of its moons? I assume that if such tidal
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lock can occur, the larger body becomes locked with its
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most gravitationally attractive orbiting body. But if that's the case,
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how are the other orbiting bodies affected? Love the show
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And that was a question from Jake Tyler. I've got
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a feeling that he's going to some of the things
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he said in the question are the reality.
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Yes, So there's a lot of complete sit to this.
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It's a really really good question. Now we're familiar with
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tidal locking. Anytime we look up at the annoying source
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of light pollution in our scar that is the moon,
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you know, keeps one face pointed towards us all the time,
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with a little bit of rock and roll because it's
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been nudged by everything else. It's not on a perfectly
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circular orbit, but it essentially keeps the nest out of
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the moon festus towards the far side, festers away. It rotates.
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One something SUTs this and exactly the same time it
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takes to go around the Earth, essentially, so it's turning
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as it goes. The Earth is slowing down in its
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rotation as the Moon is getting nudged away. There's this
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tidal interaction between them that I always visualize essentially as
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being the result of the tidal bulges. The Moon res
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is on the Earth, so we get high tid and
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a low tide every day, and I view those a
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bit like break blocks on a wheel. They're kind of
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applying friction to the Earth because the Earth is turning
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under them once every twenty four hours or so, but
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those tidal bulges are doing one lap every twenty seven
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twenty eight days because they are tied to the location
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of the Moon and the Sun. So those bulges are
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drugged along by the friction of the Earth. They're pulled
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slightly away from that line between the Moon and the Sun,
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which means that they are then pulling a little bit
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on the Moon and causing the Moon to speed up,
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which means it moves away. They've got this transfer of
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energy and momentum between the rotation of the Earth and
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the orbit of the Moon, so the Earth's spin is
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slowing down and the Moon is moving further away. Now,
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in theory, if we could carry on full long enough,
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that would eventually slow the Earth rotation down such that
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it matched the orbital period of the Moon. There is
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some debate though, a that will not happen quick enough
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for it to happen within the age of the Solar
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System that's left. But there's also some debate as to
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whether that would happen before the Moon gets far enough
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away to escape the Earth gravity. So in the case
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of the Earth Moon system, it's not going to happen,
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but it illustrates that it could so move out further
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out of the Solar System to Pluto, the dwarf planet.
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And we talked about Pluto a couple of weeks ago
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having this big companion called Charon. Yeah, Pluto actually though
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has about five minutes. It's got Charen, which is huge,
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and then it's got four little ones in Kerberos, knicks, sticks,
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and hydra I think they're called, and then smaller ones
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further out. Now Pluto and Caron are tidly locked. Karen
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spins once in the time it takes to all bit
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the center of mass between Pluto and Karen once, so
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it always keeps the same side facing towards Pluto in
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just the same way that the Moon does going around
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the Earth. But Pluto has also tidally locked with Charon,
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so Pluto keeps the same face pointing towards Karen all
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the time. So that's a prime example of the kind
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of system Jake was asking about a case where the
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biggest body has locked to the second biggest body and
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they're both locked together, and there are other things in
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the system. When it comes to plantary systems, and when
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it comes to the more generality of it, it gets
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a bit more complicated. So there's a few things going on.
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It's not necessarily the most massive body going around a
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star that would be the one that it tidally locked up,
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because the distance is important as well, and tidal forces
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fall off incredibly rapidly as a function of distance, much
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more quickly than the asquad fall off of the gravitational attraction.
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I think it's either an arcugorn ark to the power
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for setup, which means that the closer you get to
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the star, the much more strongly you tidally interact. Now
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we see this with exo planets. We can see the
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exo planets that are very close to their stars are
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tidally locked. The ones that are further away are probably not.
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But we also see it in the form of tidal
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circularization of orbits. So you get a planet that is
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flung onto an elongated orbit where the closest point to
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the star is very near the star because of the
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degree to which tidal forces vary as a function of distance.
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That means a star will interact much more strongly with
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the planet in a tidal sense when it's near the
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closest approach, and when it's far away. That means that
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you will get a you'll get an attempt to tidally
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lock the planet, so the planet's rotation will be getting
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meedged into a rotation period that matches the overal period.
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But at the same time you get this dissipation of
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energy that tries to make the orbit more circular, and
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that dissipation of energy is happening at the perry apse
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of the orbit, the point of the orbit where it's
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closest to the star. The result of this is that
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that all bit gets more and more circular by bringing
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the appo apps the furthest point from the star closer
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to the star. So it ends up being circularized at
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that closest approach distance, and that happens more quickly than
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the tidal locking process. And that's the result of the
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fact that the tidal forces fall off much more strongly
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as a function of distance. We haven't yet found any
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stars that we think are definitely tidally locked to their planet.
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Now.
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Part of this is down to the mass difference, so
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the small thing will tidally lock on much more quickly
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than it's bigger companion. That's what we're seeing with the
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Earth and the Moon. But it's not beyond the bounds
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of possibility. And there are suggestions that tidal interactions between
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really massive planets planets a lot bigger than Jupiter, and
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stars when the planets are really close in, can have
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a significant impact on the spin of those stars and
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also the energy dynamics of what's going on in their interiors.
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Not totally my area of expertise. I've got a flag that,
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but this is something that people have having to think
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about when they come to looking at ways of measuring
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the age of stars. Now there's a few ways you
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can do this. I've got colleagues at UNISQ who work
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on astero seismology. They're looking at how stars wobble and wibble,
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ringing like bells that have been struck, and you can
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look at the different frequencies at which they're wobbling and
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wibbling to learn a lot about their interior. And that
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kind of study can give you an estimate of the
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ages that's really quite accurate, but it's really resource intensive.
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You need to stare at a star for a long
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time doing a lot of observations. If you're trying to
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just get the age of stars in general. There's a
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technique called gyro chronology or gyro chronology, which is essentially
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measuring the rotation speed of the star and using that
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to get a first estimate of its age, which will
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have quite big uncertainties, but seems to do a reasonably
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good job. And the idea here is that when stars
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are bond, they're bond from material collapsing, in which spins
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faster and faster. So typically a newly born star will
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spin quite quickly every day or two, but over billions
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of years, all the masts losing through the stellar wind
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what kind of act as a break on the star's rotation,
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taking away that angular momentum, causing its spin to slow
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down over time. So if you know the degree to
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which stars slow down as a function of time, and
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you measure how quick a star's spinning, it gives you
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an estimate of its age. BECs an old star will
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spin slower than a young star, but if that star's
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got a really close in planet that's interfering with it tidally,
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that will impact that process. Yeah, so there's a lot
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of aspects to this. I appreciate I'm going a little
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bit off topic from Jake's question, but it shows you
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the complexity of it. And it's why it's such a
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good question because it's something that we don't know the
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final answer to. It's going to depend very much on
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each individual system. For the Earth and the Moon, we're
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probably never going to get fully tidally locked to the Moon,
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but we know that when the dinosaurs walk the Earth,
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the Earth was spinning quicker and we've had independent verification
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of that. Not only do we know that from the
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tidal motion of the Moon moving away, we can measure
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the speed of the Moon's moving away, but there are
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also measurements that have been made of fossil beds that
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show that there were about three hundred and eighty three
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hundred and ninety days a year back in the Cretaceous. Now,
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the soorbital period hasn't changed, as mentioned in the number
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of seconds. So how do you get more days in
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the year. You get more days in the year by
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making the days shorter. So that's the direct outcome of
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that tidal reaction between the Earth and the Moon. Pluto
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is a stage further along that's fully lopto. You've got
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an interesting case in our sol system of mercury, which
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is trapped in a three to two spin orbit resonance,
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so it's tidally locked, but it's not locked in one
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to one, and the only reason that works is that
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mercury is on an elongated orbit and is also not
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a perfectly spherical object. Gets quite complicated, yeah, but this
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gets odder the more you study it basically, and there's
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a lot of depth to it, so it makes it
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a fabulous question.
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He certainly is. Thank you, Jake. A question popped into
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my head while you were talking. You talk about the
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effect of the moon on Earth's oceans, the tides. Would
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it be to an too extreme a thought to suggest
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that the tides are actually just a slow motion tidal wave.
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You could possibly think of that way. I never have
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done before, but it's an interesting one because the phrase
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tidal wave in itself is quite misleading because they're not
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really waves in the same sense as the waves we
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see on the beach. So this is where when you
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see disaster movies and you get this enormous toll breaking wave,
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that's not really what a tidal waves like. A tidal
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wave is a huge body of water rising and falling.
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So it's more like the surface of the ocean getting
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higher or lower, and it's probably when it gets really
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close to the coast that that can break. So I
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know people who are into geophysics and ocean dynamics who
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get grumpy at disaster movies for getting tidle waves totally
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