Waves, Signals, and Cosmic Aromas: A Q&A Journey Through Space
In this intriguing Q&A episode of Space Nuts, hosts Andrew Dunkley and Professor Jonti Horner tackle a variety of cosmic queries from listeners. Join them as they explore the fascinating world of radio telescopes and how they produce images from radio waves, delve into the complexities of gravitational waves, and ponder the sounds and smells of space.
Key topics include:
- How photographic images are generated from radio telescopes, despite only receiving radio waves, and the fundamental principles behind this technology.
- A deep dive into gravitational waves, their impact on space, and how LIGO detects these minute disturbances in the fabric of spacetime.
- An imaginative discussion on what sounds might exist in space and the potential smells one could encounter beyond Earth’s atmosphere, including the curious idea of cosmic fragrances.
Join Andrew and Jonty as they demystify these concepts, providing clarity and insights into the wonders of astronomy and space science.
00:00 - Space Nuts aims to answer questions from the audience about astronomy and space science
01:37 - Were the pyramids built by aliens or were they built by humans
04:26 - How is a photographic image produced from a radio telescope and not an optical telescope
12:36 - Dean: I often hear about gravity waves and I have a hard time visualising
20:15 - Andrew Dunkley: I think ideas become easier to explain over time
22:45 - Our next question comes from David from Port Washington, New York
30:37 - Several volcanoes have blown up since we've been to them
32:08 - The metropolitan area of Auckland contains 53 volcanoes
35:02 - If you could take a big inhale, what would space smell like
36:22 - If you would like to send us some questions, please do through our website
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts-astronomy-insights-cosmic-discoveries--2631155/support.
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Andrew Dunkley: Hello again. Thanks for joining us on a Q and
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A edition of Space Nuts, where we talk
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astronomy and space science and we
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endeavour to answer, uh, questions from
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our audience. We've got a few good questions
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today, unlike all the bad ones we had
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previously. Uh, we're going to talk about
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radio telescope imagery. What does that
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mean? How does it work? I don't understand.
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And that's just me. Um, we also
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are going to be talking gravity waves. Now,
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I'm not sure if it's gravity or
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gravitational. They are different things. Uh,
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and also, uh, sounds and smells in space.
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What would they be like if you could stick
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your schnoz beyond our atmosphere? We'll talk
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about all of that on this edition of space
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nuts.
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Generic: 15 seconds. Guidance is internal.
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10, 9. Uh, ignition
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sequence start.
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Jonti Horner: Space nuts.
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Generic: 5, 4, 3, 2, 1. 2, 3,
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4, 5, 4, 3, 2', 1.
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Jonti Horner: Space nuts.
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Generic: Astronauts report it feels good.
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Andrew Dunkley: He's back again. He is Professor Jonty
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Horner, professor of Astrophysics at the
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University of Southern Queensland. Hi, Jonty.
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Jonti Horner: Good afternoon. How are you going? I am well.
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Andrew Dunkley: Good to see you again.
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Jonti Horner: It's good to be back. I think I'm going to be
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doing a lot of. I'm not sure, but today I
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think we've got questions that are a little
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out of my area of expertise. Um, I'd always
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like to flag up at the start when things are
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less my field because we don't all know
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everything. And it's good to, rather than
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pretend, good to be open about what I do and
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don't know.
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Andrew Dunkley: Fair enough.
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Andrew Dunkley: But, uh, we'll do our very best. I
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got the easy part. I just get to ask the
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questions.
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Let's, uh, get straight to our first one.
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And this one, uh, asks how is
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a photographic image produced from a radio
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telescope when all they are receiving is
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radio waves and not an optical image through
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a telescope lens? Uh, that's, uh,
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from Thomas in Canberra. He's thrown in a
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supplementary Monty Python, Monty Python
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style question. Were the pyramids built
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by aliens? Does that sound
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fair enough?
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Andrew Dunkley: Uh,
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Andrew Dunkley: horrible, dad joke.
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Andrew Dunkley: Horrible.
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Jonti Horner: But if you want to keep your
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Andrew Dunkley: razor sharp, I did see an article only
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a few days ago about, uh, a new theory into
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the building of the pyramids. But we went to
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Egypt a few years ago and they are, uh, quite
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adamant that, um, not only were they built
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by humans, they were built by
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what you would call contractors. They were
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not slaves. The people that built the
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pyramids, according to the locals, were
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actually employed.
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Jonti Horner: Yeah, lots of discussion of that. My partner
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Ness, is an avid history buff and
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also Likes to watch a bit of TV when she's
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trying to relax, to go to sleep. So I'm m
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constantly seeing archaeological
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documentaries and things like that. And she
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loves the Egyptians. So I've seen lots and
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lots of documentaries talking about this. And
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it turns out, if what I've seen in these
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shows can be believed, that it was actually
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fairly prestigious and fairly good working
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conditions to be one of the contractors
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working on the pyramids kind of building
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that. So.
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Andrew Dunkley: Yeah, I heard that too. Yes, exactly.
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Jonti Horner: Crack the big whips and all the rest of it.
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Andrew Dunkley: But yeah, yeah, no, it's fascinating
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history. Wouldn't you love a time machine
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just to go back and go, ah, uh, look.
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Andrew Dunkley: Yeah,
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Andrew Dunkley: now that we're seeing it, it looks easy.
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Jonti Horner: Uh, absolutely. I mean, I probably end up
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being really kind of busman's holiday though,
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with the time machine and going back to
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different astronomical events and think like,
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trying figure out if Caesar's Comet was
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actually real, you know, and, you know,
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trying to see if there were multiple sun
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grazing comets visible with the naked eye in
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daylight in I think it was 363 A.D. so
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I'd probably end up picking myself an
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astronomical holiday tour, um,
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not getting distracted by all the kind of
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human history stuff.
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Andrew Dunkley: Yeah, fair enough. I mean, you go nuts
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thinking about things to go back and see.
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Absolutely.
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Jonti Horner: Or going forward. I've said a few times that
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given the predictions we talked about last
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year, that Comet Duchesso, Comic
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Linkenberg, will return in the year 2097.
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That could well be the best comet of this
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century. I'd quite like to see it, but
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unless I am fortunate enough to reach 119
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years old, I think it unlikely. So,
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you know, time machine would be welcome.
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Andrew Dunkley: Yeah, it would. I'm working on it.
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Uh, so let's go to the first part of the
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question. Uh, how is a photographic image
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produced from a radio telescope when
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all they receive is radio waves and not an
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optical image through a telescope lens? Yeah,
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I've got to admit, this one confuses me a
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bit.
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Jonti Horner: We could say the same for infrared. We could
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say the same for gamma rays or X rays or for
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optical photographs. Right. So all of those
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different forms of radiation I just mentioned
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are different, uh, parts of the
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electromagnetic spectrum. So they're
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fundamentally the same thing but with
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different wavelengths in just the same way
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that red light and blue light are
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electromagnetic waves, but blue has a shorter
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wavelength and red has a longer wavelength.
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And um, I've got an astro photo behind me of
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the Helix Nebula. If I had a camera that was
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more sensitive to infrared, I would have
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picked out some slightly different features
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there because there is radiation coming in of
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different wavelengths. The way it
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works with a radio telescope or the way that
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it works with an M infrared detector or
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whatever is, you've got a detector
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that can detect radiation of that
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wavelength. Um, with an optical photo,
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you have a DSLR camera or a CCD camera that
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is sensitive to optical light and
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you get photons hitting the detector and
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creating electrons that are countered in the
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same way. For a radio telescope, you have a
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detector that is sensitive to radio waves
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and when photons of the right energy hit the
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detector, they create electrons and they get
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countered. So what happens is you've got your
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radio telescope that can look at a patch of
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sky with some level of
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resolution and some telescopes have
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better resolution and some have blurrier
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vision linked to the size of the telescope.
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Typically, the bigger a telescope is, the
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better its resolution will be. For optical
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telescopes, the atmosphere puts a cap on
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that. Uh, unless you can do things to filter
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it out at about 1 arc second, very
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roughly, the turbulence of the
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atmosphere is a bit of a pain. But in theory,
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if you could take the atmosphere away, you
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would be able to see smaller things on the
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sky with a 10 metre diameter telescope than a
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1 metre telescope in the optical. And there's
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a mathematical relation for this that we
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teach our students at undergrad level. The
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resolution of the telescope, so what the
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smallest thing it can see is, if you ignore
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the atmosphere, if you look purely on the
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physics of it, is related to
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the diameter of the telescope. A bigger
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telescope will see a smaller resolution, but
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it's also related to the wavelength. So if
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you've got two telescopes of identical size
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and one's looking at optical and one's
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looking at radio waves, the radio waves are
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much longer wavelength, so the resolution of
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that telescope will be much lower.
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So radio telescopes of the same size as an
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optical telescope will get a blurrier image,
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but we can build radio telescopes much
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bigger. So there's swings and
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roundabouts there. But effectively what
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happens is you've got your image
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of the sky, the telescope looking at a patch
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of sky, and you've got a detector that
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counts the amount of radio waves
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impacting upon it in the form of photons
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impacting upon it. And that gives you a
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measure of how bright that bit of sky is.
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Now, if you've got multiple pixels, you can
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see different bits of that, uh, image
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in the same way as with a normal camera. One
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way. I think that this used to be done back
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in the very early days of radio or Ah, with
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very simple radio telescopes was all you're
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doing is you're counting the amount of radio
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waves hitting your detector. So you've got
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one pixel for your entire field of view and
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then you move your field around to make an
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image. So this part of the sky is this
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bright, the one next to it is this bright and
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so on, and you raster around to build up an
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image, you move around. Nowadays I
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think that you can get multiple pixels per
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field of view. In fact, you can get many.
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That's why we can get these beautiful high
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resolution images. And, uh, it's effectively
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working, albeit at different wavelengths, in
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the same kind of general science way as an
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optical detector. In that you've got a grid
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of pixels. Each pixel is sensitive
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to light falling upon that pixel and that
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pixel is seeing a certain bit of the sky. So
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you get a measure of how bright one bit of
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the sky is, how bright the next one is, how
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bright the next one is. That then gives you
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bright and faint. So you can then make a
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monochrome image where you plot
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those brightnesses as colours, from black
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being no light to white being some light and,
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um, really bright white being the
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brightest. Right. So you can build up an
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image where each pixel is a different
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brightness. Suddenly you've got a picture.
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Andrew Dunkley: Yeah.
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Jonti Horner: What you can do then is if you're sensitive
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to different wavelengths, you can
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combine those monochromatic images to make a
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colour image just the same way as I did with
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the one behind me. So the picture I've got on
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my screen, and this is useless to those of
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you listening, but anybody live in the
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studio, I've got a picture behind me of the
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Helix Nebula, which I took with my telescope
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here. And it's a beautiful kind of true
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colour image with a little bit of hydrogen
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alpha added for those listening in. But what
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I've done here is taken images that were
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black and white, that were taken through
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filters of blue, green and
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red and combine them to make a colour image.
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So you can do that to make false colour
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images in infrared or radio, uh,
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or whatever. Sometimes what you're seeing
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is effectively a monochromatic image, but
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instead of black and white, they've used
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black and yellow to make it look nice and
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colourful. But that's effectively what's
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going on. Now, I'm not a radio astronomer.
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There's subtleties and differences in the
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technology you need to observe at, ah,
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different wavelengths compared to optical.
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And I know that's equally true of the very
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high energy stuff like gamma rays and X rays
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that need clever little Bits of technology.
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Technology to be done. But fundamentally what
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you're doing to get an image is you're
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measuring the brightness of the sky in a
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given position at the wavelength you're
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interested in and ascribing that a colour.
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And then you're building a grid of those to
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make a picture which shows you the brighter
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areas and the fainter areas. And that's
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pretty much the same no matter what you're
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looking at. It's the same technique. It's
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just using different technology because
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you're looking at different energy levels,
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different wavelengths,
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Andrew Dunkley: which is how they got the, uh,
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image of Sagittarius A and
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m. Was it M37?
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Jonti Horner: Was it the one at the middle of M81?
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Andrew Dunkley: I think M81, yeah.
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Jonti Horner: So that's the, um, big global Black hole
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telescope. I can't remember the exact name of
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it, that took advantage of the
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long wavelength because you can do very
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clever things if you can work out
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where in a particular way of your
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detectors picking things up. So you can have
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distributed detectors that are part of the
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same telescope. Now, it's really hard to
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do this with optical. So, uh, people are
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playing with interferometry and things like
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that, uh, optical wavelengths. But for
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radio waves, it's possible for you to use
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detectors scattered all around the world to
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mimic having a detector that is a radio
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telescope that is the size of the Earth.
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Andrew Dunkley: Yeah.
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Jonti Horner: Um, and that then overcomes the problem that
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the wavelengths are longer by having a
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detector that is much, much bigger to get the
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kind of resolution that you get with an
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optical telescope or even better. And it's
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using that that they were able to get these
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beautiful resolved radio images of these
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black holes. They overcame the tyranny of
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resolution being, you know,
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limited by wavelength by making a really,
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really, really big telescope, effectively.
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Andrew Dunkley: M. Yeah, it worked really well. And so those
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images are a fair representation of what
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with the naked eye, from a distance.
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Jonti Horner: I suppose if you could see radio waves.
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Andrew Dunkley: Yeah, if you could, yes.
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Jonti Horner: Things will look different at, ah, different
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wavelengths. And you see that if you do play
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with astrophotography and you look through
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different filters, it is quite striking how
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different the same object will look in
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different colours when you're just looking in
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monochrome. And that's fundamentally how we
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do a lot of the science, how we work out what
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things are made of.
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Andrew Dunkley: Yeah, thank you, Thomas, Great question.
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Lovely to hear from you. Um, notwithstanding
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the Monty Python joke,
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Generic: Roger
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Jonti Horner: in your lives right here. Also space nuts.
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Andrew Dunkley: Our, uh, next question comes from
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Dean. Uh, he's not far from
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you Hi
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Andrew Dunkley: Fred Watson and Andrew, this is Dean in
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Redcliffe in Queensland. I often hear about
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gravity waves and I get a mental picture of a
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compression wave with dispersed particles in
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space getting closer together, then further
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apart as the wave passes. But I have a
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harder time visualising what happens as the
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wave passes through a solid body such as the
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Earth, where it can be detected by the LIGO
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interferometer. I think
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that it is space that is expanding and
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contracting rather than matter. But I'm not
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sure LIGO detects the
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gravity wave because the length of the four
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kilometre tunnel changes slightly.
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What's happening at a quantum scale
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as there is space within an atom, does the
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size of the atoms change or is it just the
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space between the atoms? I know
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that the effect at quantum scale would be
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minute. It's interesting to think about where
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the limit of space stretching might be. I
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suspect that I'm missing something with my
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understanding of this. I hope you can make
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some sense of it. Thanks for the podcast.
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Andrew Dunkley: Thank you, Dean. And uh, yeah,
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I think he's actually referring to
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gravitational waves because that's what LIGO
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searches for. But um, yeah, I've made that
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same mistake in the past where I call them
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gravity waves. Um, but
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gravity waves, wave is a different thing.
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They exist too, I think.
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Jonti Horner: Um, yes and no. So what's strange here is
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that I think you hear different terminology
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in different disciplines. So I think a lot of
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astronomers I've heard use the term gravity
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waves and gravitational waves almost
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interchangeably because that's what they're
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thinking about. But it's a really good
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example of how language is contextual
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in that the words you use, you use meaning
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one thing but another person may hear them
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and hear something entirely different because
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that same word can mean a different thing to
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someone else. So one other place I've heard
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the term gravity wave is actually in
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atmospheres and um, to do with fluid
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movement. And so you see
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things like um, I think lens clouds, delta
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cumulus lenticularis and um, wave
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clouds are associated with something that
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atmospheric scientists describe as gravity
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waves, which are things that happen when
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you've got the interface between two fluids
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and you've got steady airflow over things.
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And if you actually do a quick Google, I just
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fired this up and found the Wikipedia page
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for gravity wave. There are some absolutely
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beautiful images of
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wind driven gravity waves in the Timor Sea.
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You've got some beautiful wave clouds over
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the us, Little bits of maths. But this ties
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into, I think, something I used to see when I
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was doing weather recordings as a teenager in
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Yorkshire at school, because of the shape of
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the Pennines and the kind of airflow we got,
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we got lens clouds relatively frequently. And
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I think they are linked to the phenomenon
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that atmospheric scientists would often
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describe as gravity waves. For clarity,
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then, I think we should call what we're
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talking about here gravitational waves. And
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I think that's probably more accurate.
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And I think possibly astronomers slipping
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into calling gravitational waves gravity
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waves could be the cause of confusion to
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people who are thinking about weather.
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Gravitational waves, Dean was
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right. Are, uh, perturbations in the
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structure of space rather than
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matter itself shifting. This
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makes my head hurt. I should stress that I'm
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very much not an expert here and I know I say
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that very, very often, but I'm. You know,
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it's important to note that I'm not speaking
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from a position of great authority here,
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but what you're getting are, uh, a
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phenomenon that was first predicted in the
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late 1800s and early 1900s. Apparently the
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predictions predated Einstein, but he kind of
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formalised it through general relativity
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in the form of extreme, extreme
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events causing perturbations to space time
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that ripple outwards at the speed of light,
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causing, effectively, waves in
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the spacetime continuum, effectively
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in space itself, in the same thing that is
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stretching with the expansion of the
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universe. Those waves,
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as they pass through, are almost
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imperceptible. They don't really interact
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much with anything. But because
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they perturb, um, space, they can have a
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measurable effect in that they can change the
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distance between two points as the wave
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passes through. Now, there's some little
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animations trying to illustrate how waves
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would look, um, on the Wikipedia
439
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article about gravitational waves that are
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not really helping me because they're looking
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at what would happen if you had a circle of
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points and a wave pass through. And there's
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two ways it can wibble and it can go like a
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cross, or it can go like a square, like a
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plus sign. Sorry, that doesn't particularly
446
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help me visualise it. But what's happening,
447
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to the best of my understanding, is that
448
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you have this tiny little
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shift in space as the wave passes through,
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which means that ligo, which has
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these two arms at right angle to each other
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that are like four kilometres long, has light
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bouncing along these two arms. And when
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the length of one of those arms, um, shifts
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very slightly, the light will change from
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being constructively to destructively
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interfering with each other. So a very small,
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very, very small shift in distance
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means that the light, when it goes along and
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bounces back, will have travelled a slightly
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different distance and Then when you
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recombine it with the light that goes down
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the other arm, there'll be a little bit more
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in phase, out of phase. So you'll see the
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intensity of the result changing.
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Andrew Dunkley: Gotcha.
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Jonti Horner: What's astonishing about this is the
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figure that um, one of these gravitational
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waves that they detect is changing the
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length of one of those four kilometre arms
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by a thousandth of the width of a proton
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of a subatomic particle.
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Andrew Dunkley: That is a quantum level.
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Jonti Horner: Yeah, it's utterly quantum level. It's
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astonishing. The analogy that's been
476
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published about that, to put it into scale,
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is if you think about the distance between
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the sun and Proxima Centauri, it's like
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changing that distance by the width of a
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human hair. It's
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utterly mind boggling that we can detect
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this. It's an astonishing achievement. Now,
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my understanding is limited
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and, you know, really want to stress that
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what would happen as I understand it though
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is that it isn't just a distance between the
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subatomic particles that are changing, but
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they themselves will change. We would change
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as that wave goes through us because space
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itself would change, would fly us, but we
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wouldn't notice it. You know, that kind of
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change is tiny compared to us. But my
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understanding, Dean, is very
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much that, uh, the particles would change and
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the distance between them would change and
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everything will be slightly compressed and
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slightly relaxed. But I stand to be
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corrected in that. Yeah,
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it's very difficult to visualise and
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challenging to understand.
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Andrew Dunkley: Yeah. Um, so the wave moves through space,
502
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it affects space, but the space doesn't
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actually move with the wave. It's just like a
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wave in the ocean. It doesn't like the wave.
505
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Isn't the water moving?
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Jonti Horner: The water still moves up and down kind of
507
00:19:55.040 --> 00:19:56.920
thing. I think the water actually goes in a
508
00:19:56.920 --> 00:19:58.700
certain way circle, doesn't it, in a wave? So
509
00:19:58.700 --> 00:20:00.460
its average position is the same, but it
510
00:20:00.460 --> 00:20:02.540
rolls back and forth and the energy is
511
00:20:02.540 --> 00:20:03.540
propagated through.
512
00:20:03.860 --> 00:20:05.700
Andrew Dunkley: Correct. That's the way I understand
513
00:20:06.660 --> 00:20:09.500
it seems logical that waves in space would be
514
00:20:09.500 --> 00:20:12.500
the same. Um, completely
515
00:20:12.500 --> 00:20:14.340
different setup, but same effect
516
00:20:15.140 --> 00:20:15.820
essentially.
517
00:20:15.820 --> 00:20:17.620
I imagine what I think will be
518
00:20:17.620 --> 00:20:19.020
Jonti Horner: interesting, and I mean this is going
519
00:20:19.020 --> 00:20:21.140
slightly off topic into philosophy, is
520
00:20:22.250 --> 00:20:24.300
uh, how these ideas will become easier to
521
00:20:24.300 --> 00:20:27.180
explain over time. So I think when
522
00:20:27.420 --> 00:20:30.220
I was at uni, people were teaching special
523
00:20:30.220 --> 00:20:32.500
and general relativity and quantum mechanics
524
00:20:32.500 --> 00:20:35.340
as m modern physics as being quite
525
00:20:35.340 --> 00:20:38.300
new. And the students were understanding them
526
00:20:38.300 --> 00:20:40.660
a bit more easily than the people who taught
527
00:20:40.660 --> 00:20:42.060
them understood them when they were students,
528
00:20:42.780 --> 00:20:45.580
because we were about 80 years
529
00:20:45.740 --> 00:20:48.100
on from these discoveries. So the people who
530
00:20:48.100 --> 00:20:50.860
were teaching us had been taught by people
531
00:20:50.860 --> 00:20:52.780
where these discoveries had been made during
532
00:20:52.780 --> 00:20:54.820
their lifetimes, potentially. Given that
533
00:20:54.820 --> 00:20:56.700
you're often taught by the old academics.
534
00:20:57.810 --> 00:21:00.210
And initially the understanding of quantum
535
00:21:00.210 --> 00:21:02.970
mechanics and relativity was way
536
00:21:02.970 --> 00:21:05.970
postdoc. And then PhD students learned it
537
00:21:05.970 --> 00:21:07.890
and then uni students learned it. And now I
538
00:21:07.890 --> 00:21:09.970
believe it's taught at high school. So as
539
00:21:09.970 --> 00:21:12.850
time goes on and people can
540
00:21:12.850 --> 00:21:14.920
explain things to the next generation, our,
541
00:21:14.920 --> 00:21:16.970
uh, kind of societal understanding of these
542
00:21:16.970 --> 00:21:19.250
concepts gets better and they get accepted.
543
00:21:19.810 --> 00:21:21.890
And you suddenly get to the point where
544
00:21:22.210 --> 00:21:23.970
primary school kids are talking about special
545
00:21:23.970 --> 00:21:25.370
relativity. I mean, they're probably not
546
00:21:25.370 --> 00:21:27.330
talking about it in the mathematical terms,
547
00:21:27.730 --> 00:21:29.790
but some of the concep are now really
548
00:21:29.790 --> 00:21:32.110
embedded in culture. And I think part of the
549
00:21:32.110 --> 00:21:35.070
problem I have with gravitational
550
00:21:35.070 --> 00:21:37.710
waves is that whilst they had been
551
00:21:37.710 --> 00:21:39.830
predicted in a kind of niche way so long ago,
552
00:21:39.830 --> 00:21:42.750
the first observations were so recent that
553
00:21:42.750 --> 00:21:44.630
I wasn't taught about gravitational waves at
554
00:21:44.630 --> 00:21:47.350
uni. They weren't part of our courses. It's
555
00:21:47.350 --> 00:21:50.350
still really cutting edge new concepts.
556
00:21:51.150 --> 00:21:53.990
And so my understanding, therefore
557
00:21:53.990 --> 00:21:56.720
my explanation, it's woolly because I've
558
00:21:56.720 --> 00:21:59.320
never had it explained by someone who has had
559
00:21:59.320 --> 00:22:01.360
it explained by someone who's had it
560
00:22:01.360 --> 00:22:03.160
explained by someone. We've not had that
561
00:22:03.160 --> 00:22:05.600
buildup of conceptual
562
00:22:05.600 --> 00:22:08.160
description, I guess, to really embed this.
563
00:22:08.160 --> 00:22:10.000
And I find it really hard to get my head
564
00:22:10.000 --> 00:22:13.000
around the first observed gravitational wave,
565
00:22:13.000 --> 00:22:15.600
I think was 2015. This is a
566
00:22:15.600 --> 00:22:18.160
decade old. So it's probably like someone
567
00:22:18.160 --> 00:22:20.880
calling into the podcast in 1925
568
00:22:20.880 --> 00:22:22.750
asking me to explain general relativity.
569
00:22:24.260 --> 00:22:27.030
Andrew Dunkley: Yes. Yeah, that's a good analogy. Um,
570
00:22:27.220 --> 00:22:29.500
Dean, thanks for the question. Hope we, we
571
00:22:29.500 --> 00:22:30.940
covered all those little gaps you were
572
00:22:30.940 --> 00:22:33.100
talking about. Boom, boom. Uh, this is Space
573
00:22:33.100 --> 00:22:35.980
Nuts with Andrew Dunkley and Professor Johnty
574
00:22:35.980 --> 00:22:37.700
Horner. A, uh, Q A edition.
575
00:22:39.780 --> 00:22:41.780
Generic: I think we need to do a little more all
576
00:22:41.780 --> 00:22:42.740
weather testing.
577
00:22:43.380 --> 00:22:45.140
Andrew Dunkley: Amen, Space Nuts.
578
00:22:45.460 --> 00:22:48.020
Our next question comes
579
00:22:48.260 --> 00:22:49.810
from David.
580
00:22:49.810 --> 00:22:52.690
Andrew Dunkley: This is David from Port Washington, New York.
581
00:22:53.410 --> 00:22:55.170
And I was thinking back to when I was a
582
00:22:55.170 --> 00:22:57.970
teenager and I heard the recording of
583
00:22:57.970 --> 00:23:00.770
the resonant frequency of the universe and I
584
00:23:00.770 --> 00:23:02.810
thought it was very cool. I'm wondering if
585
00:23:02.810 --> 00:23:05.810
there was some kind of medium that sound
586
00:23:05.810 --> 00:23:08.430
could pass through in space, like, uh,
587
00:23:08.690 --> 00:23:11.250
water, uh, or even air.
588
00:23:11.570 --> 00:23:14.250
What would I be hearing? Uh, and would it be
589
00:23:14.250 --> 00:23:17.240
beautiful or would it be terrifying? What are
590
00:23:17.240 --> 00:23:19.640
the different resonant frequencies going on
591
00:23:19.640 --> 00:23:20.840
and big explosions?
592
00:23:21.640 --> 00:23:21.650
Generic: Really?
593
00:23:21.650 --> 00:23:22.920
Andrew Dunkley: Um, interested to know.
594
00:23:23.480 --> 00:23:23.550
Generic: Bonus.
595
00:23:23.550 --> 00:23:25.720
Andrew Dunkley: Um, question. If I could breathe in space,
596
00:23:25.800 --> 00:23:27.760
what would it smell like? But I'm more
597
00:23:27.760 --> 00:23:30.200
interested to know about the sounds. Okay,
598
00:23:30.200 --> 00:23:30.920
thanks guys.
599
00:23:31.720 --> 00:23:34.080
Andrew Dunkley: Thank you. David. I love this question. It's
600
00:23:34.080 --> 00:23:36.110
a little bit different. We haven't had uh,
601
00:23:36.200 --> 00:23:38.280
one like that for a while. Although I do
602
00:23:38.280 --> 00:23:41.080
recall we did talk about
603
00:23:41.160 --> 00:23:43.920
some time back about, um, I
604
00:23:43.920 --> 00:23:46.560
can't remember exactly what the object was,
605
00:23:46.560 --> 00:23:48.380
but they were talking about what it would
606
00:23:48.380 --> 00:23:50.500
smell like if you could smell it. And
607
00:23:50.950 --> 00:23:53.900
um, you know, and that was fascinating
608
00:23:53.900 --> 00:23:55.740
in itself. But don't ask me to remember what
609
00:23:55.740 --> 00:23:58.260
it was. I think it was rotten eggs.
610
00:23:58.260 --> 00:23:58.700
Andrew Dunkley: It is.
611
00:23:58.700 --> 00:24:00.660
Jonti Horner: I think that's a concept that's often used a
612
00:24:00.660 --> 00:24:01.900
bit like we talked about in the Last
613
00:24:01.900 --> 00:24:04.500
Questions episode about the raining diamonds
614
00:24:04.500 --> 00:24:06.820
and raining, um, precious gems,
615
00:24:07.620 --> 00:24:10.540
where people try to give you a
616
00:24:10.540 --> 00:24:12.460
hook that fits in with your day to day lived
617
00:24:12.460 --> 00:24:14.260
experience to help you visualise something
618
00:24:14.260 --> 00:24:16.260
more clearly. And the
619
00:24:16.900 --> 00:24:19.500
recording of the resonant frequency of the
620
00:24:19.500 --> 00:24:22.230
univers. It's another one of those. I think
621
00:24:22.230 --> 00:24:23.710
what we're talking about there is the
622
00:24:23.710 --> 00:24:25.510
microwave background, cosmic microwave
623
00:24:25.510 --> 00:24:28.430
background, which is this very low
624
00:24:28.430 --> 00:24:31.310
frequency now radio detection, um,
625
00:24:31.670 --> 00:24:34.670
equivalent to a black body at about 2.7
626
00:24:34.670 --> 00:24:37.350
Kelvin. That is a leftover hiss from
627
00:24:37.990 --> 00:24:40.790
the Big Bang, which, when Big bang happened
628
00:24:40.790 --> 00:24:43.150
about 300,000 years later, the universe went
629
00:24:43.150 --> 00:24:45.070
from being opaque to transparent. And all the
630
00:24:45.070 --> 00:24:47.150
radiation from the heat of the universe at
631
00:24:47.150 --> 00:24:49.990
that time went out into space. Universes
632
00:24:49.990 --> 00:24:52.530
got bigger, everything's got redshifted. So
633
00:24:52.530 --> 00:24:54.410
the peak of that spectrum now looks like a
634
00:24:54.410 --> 00:24:56.760
source. That was 2.7 Kelvin. And,
635
00:24:56.760 --> 00:24:59.250
um, that microwave
636
00:24:59.250 --> 00:25:01.610
background is the source of a lot of the
637
00:25:01.610 --> 00:25:03.730
static that you used to get if you tune your
638
00:25:03.730 --> 00:25:05.970
radio between stations or if you had an old
639
00:25:05.970 --> 00:25:07.850
TV where you had to tune in on the dial or
640
00:25:07.850 --> 00:25:09.930
move the antenna around and you just got the
641
00:25:09.930 --> 00:25:12.090
noise on the screen. A significant component
642
00:25:12.090 --> 00:25:14.450
of that was a macro background. And people
643
00:25:14.450 --> 00:25:17.210
have often tried to convert that into
644
00:25:17.210 --> 00:25:20.010
a sound to give people a kind of
645
00:25:20.010 --> 00:25:21.970
emotional connection, a way of visualising
646
00:25:21.970 --> 00:25:24.930
this. Um, although that's
647
00:25:24.930 --> 00:25:27.690
turning radio waves into a sound. Well, I
648
00:25:27.690 --> 00:25:29.930
guess we do that all the time with FM and AM
649
00:25:29.930 --> 00:25:31.050
broadcast, right?
650
00:25:31.290 --> 00:25:31.690
Andrew Dunkley: Yep.
651
00:25:31.690 --> 00:25:34.290
Jonti Horner: So, uh, it kind of makes sense to people in
652
00:25:34.290 --> 00:25:36.890
terms of what the universe would sound like.
653
00:25:36.890 --> 00:25:39.730
If there was a medium in space to transmit
654
00:25:39.730 --> 00:25:42.130
the sound, it would actually depend to some
655
00:25:42.130 --> 00:25:44.170
degree of the density of that medium as well.
656
00:25:44.170 --> 00:25:46.730
So the frequency that a given sound
657
00:25:46.890 --> 00:25:49.660
will sound like changes with
658
00:25:49.900 --> 00:25:52.660
atmospheric pressure. And I've seen examples
659
00:25:52.660 --> 00:25:54.860
of this where people have put an alarm bell,
660
00:25:55.500 --> 00:25:57.980
kind of alarm clock type, ringy bell noise
661
00:25:58.380 --> 00:26:01.300
in a big bell jar and evacuated the air
662
00:26:01.300 --> 00:26:02.700
from it. And as the air pressure got lower
663
00:26:02.700 --> 00:26:04.260
and lower, I think the pitch got higher and
664
00:26:04.260 --> 00:26:07.180
higher until the sound disappeared. So you've
665
00:26:07.180 --> 00:26:09.340
got a lot of different factors that would
666
00:26:09.340 --> 00:26:12.300
come into this to do with the composition
667
00:26:12.300 --> 00:26:14.500
of the medium, the density of the medium and
668
00:26:14.500 --> 00:26:17.250
stuff like that. But let's imagine just for a
669
00:26:17.250 --> 00:26:18.650
minute, because I think this is more of a
670
00:26:18.650 --> 00:26:21.090
science fiction question than a science fact
671
00:26:21.090 --> 00:26:22.970
one in a way. And I do love it as a question
672
00:26:22.970 --> 00:26:25.450
like that. If you were floating around in the
673
00:26:25.450 --> 00:26:27.610
solar system and you were uh, beyond the
674
00:26:27.610 --> 00:26:30.050
Earth's atmosphere, what would be the main
675
00:26:30.130 --> 00:26:32.450
source of noise that you'd experience?
676
00:26:33.010 --> 00:26:35.010
To me, I would actually guess the solar wind.
677
00:26:35.330 --> 00:26:37.330
Cause you have this flow of particles coming
678
00:26:37.330 --> 00:26:39.490
past you at a speed measured in hundreds of
679
00:26:39.490 --> 00:26:42.010
kilometres a second, 100, 200, 300 kilometres
680
00:26:42.010 --> 00:26:44.890
a second. So to me, I guess the main sound
681
00:26:44.890 --> 00:26:46.890
you would hear if you were beyond the Earth's
682
00:26:46.890 --> 00:26:49.170
atmosphere and there was enough medium for
683
00:26:49.170 --> 00:26:51.290
you to listen to, would actually be the sound
684
00:26:51.290 --> 00:26:53.290
of the wind blowing, but a really intense
685
00:26:53.850 --> 00:26:56.810
gale blowing. There have been
686
00:26:56.810 --> 00:26:59.210
discussions about what you'd hear on Mars.
687
00:26:59.210 --> 00:27:01.370
Now of course, on Mars the atmospheric
688
00:27:01.370 --> 00:27:03.410
pressure is much, much lower than even at the
689
00:27:03.410 --> 00:27:06.330
altitude of Everest. So that frequency
690
00:27:06.330 --> 00:27:08.210
shifting phenomenon would come in. So
691
00:27:08.210 --> 00:27:10.090
something that you'd hear as an ice deep bass
692
00:27:10.090 --> 00:27:12.570
note on Earth, I believe, would be a higher
693
00:27:12.570 --> 00:27:14.730
pitch on Mars quite markedly.
694
00:27:14.970 --> 00:27:15.370
Andrew Dunkley: Yeah.
695
00:27:15.370 --> 00:27:18.350
Jonti Horner: Darren Squeaky Y if you're listening
696
00:27:18.350 --> 00:27:20.310
to this podcast on Mars, please wear
697
00:27:20.310 --> 00:27:22.390
headphones. Otherwise I'll sound even more
698
00:27:22.390 --> 00:27:25.300
stupid than normal, I guess. Um,
699
00:27:25.910 --> 00:27:28.670
I would imagine that in terms
700
00:27:28.670 --> 00:27:30.510
of the concept of whether it would be
701
00:27:30.510 --> 00:27:33.030
beautiful or scary, I suspect it'd be like
702
00:27:33.030 --> 00:27:35.190
white noise with a lot of different
703
00:27:35.350 --> 00:27:38.350
components coming in. If you could visualise
704
00:27:38.350 --> 00:27:39.830
different astronomical phenomena
705
00:27:39.830 --> 00:27:42.550
contributing, a lot of them are time varying,
706
00:27:42.550 --> 00:27:45.120
a lot of them are bright flashes or
707
00:27:45.120 --> 00:27:47.200
whatever. So you'll probably have an
708
00:27:47.200 --> 00:27:49.800
underlying bass noise of whatever
709
00:27:49.880 --> 00:27:52.320
with lots of other things impinging on it.
710
00:27:52.320 --> 00:27:54.760
But it's really hard to say because we're
711
00:27:54.760 --> 00:27:56.370
trying to imagine a reality that is so, ah,
712
00:27:56.400 --> 00:27:59.040
different to our own. So I'm trying to find a
713
00:27:59.040 --> 00:28:01.000
way to contextualise that, I guess.
714
00:28:01.630 --> 00:28:04.280
Um, so it'd probably be a lot more like a
715
00:28:04.280 --> 00:28:07.160
white noise machine than something clear and
716
00:28:07.240 --> 00:28:09.640
beautiful. Possibly a white noise machine on
717
00:28:09.640 --> 00:28:10.330
a very windy day.
718
00:28:11.200 --> 00:28:13.870
Andrew Dunkley: Yeah. Sounds, um, in space, um,
719
00:28:16.000 --> 00:28:18.840
it's a difficult thing to try and get your
720
00:28:18.840 --> 00:28:21.800
head around because sound needs something to
721
00:28:21.800 --> 00:28:24.440
move through and space doesn't offer a lot of
722
00:28:24.440 --> 00:28:24.720
that.
723
00:28:25.360 --> 00:28:28.240
Jonti Horner: Absolutely. And I mean to maybe give you a
724
00:28:28.240 --> 00:28:29.640
different illustration of that. If you think
725
00:28:29.640 --> 00:28:31.160
about how sounds change when you go
726
00:28:31.160 --> 00:28:33.840
underwater, how different the world
727
00:28:33.840 --> 00:28:35.640
seems if you're snorkelling or you're doing a
728
00:28:35.640 --> 00:28:36.220
scuba Dive.
729
00:28:36.690 --> 00:28:36.930
Andrew Dunkley: Yeah.
730
00:28:36.930 --> 00:28:39.170
Jonti Horner: How all the sounds are so different to you.
731
00:28:39.650 --> 00:28:42.410
Andrew Dunkley: Yeah. I'll give you an example of sound
732
00:28:42.410 --> 00:28:45.370
and witnessing its movement. Uh, and this is
733
00:28:45.370 --> 00:28:48.090
not something I'd recommend, but, uh, we were
734
00:28:48.090 --> 00:28:50.770
standing on the rim of a volcano some years
735
00:28:50.770 --> 00:28:53.490
ago, and it was active and it was going
736
00:28:54.450 --> 00:28:56.690
in our faces. Actually, we had to leave
737
00:28:56.690 --> 00:28:59.480
because it was getting in our faces. Um,
738
00:28:59.650 --> 00:29:02.450
but watching the process of the eruption,
739
00:29:02.450 --> 00:29:04.730
you see it, it before
740
00:29:05.690 --> 00:29:08.410
you hear it, but you feel it
741
00:29:09.610 --> 00:29:12.010
also before you hear it, but not until after
742
00:29:12.010 --> 00:29:12.650
you see it.
743
00:29:12.650 --> 00:29:13.130
Andrew Dunkley: Yeah.
744
00:29:13.770 --> 00:29:16.130
Andrew Dunkley: So, uh, you see the explosion, you feel the
745
00:29:16.130 --> 00:29:19.050
rumble, and then you hear it, and
746
00:29:19.050 --> 00:29:22.050
then the shockwave hits you. Yeah, it's
747
00:29:22.050 --> 00:29:24.410
a really weird combination. And look, you're
748
00:29:24.410 --> 00:29:26.970
talking about a matter of
749
00:29:27.530 --> 00:29:29.650
all of this happening over in the course of
750
00:29:29.650 --> 00:29:31.210
about a second or a second, a half,
751
00:29:32.570 --> 00:29:35.430
depending on distance. But you see it, you
752
00:29:35.430 --> 00:29:37.510
feel it, you hear it,
753
00:29:38.230 --> 00:29:40.070
you feel it in the ground, and then you feel
754
00:29:40.070 --> 00:29:40.790
the shockwave.
755
00:29:40.790 --> 00:29:41.350
Andrew Dunkley: Yeah.
756
00:29:41.830 --> 00:29:44.310
Jonti Horner: And I mean, that fits in with how
757
00:29:45.110 --> 00:29:47.070
sound travels at different speeds. So what
758
00:29:47.070 --> 00:29:49.950
you feel under your feet is effectively waves
759
00:29:49.950 --> 00:29:52.910
that you'd probably hear as sound. But going
760
00:29:52.910 --> 00:29:54.630
through a solid medium, they travel faster.
761
00:29:54.870 --> 00:29:55.310
Andrew Dunkley: Exactly.
762
00:29:55.310 --> 00:29:57.110
Jonti Horner: Shockwaves are quicker. And I mean, that
763
00:29:57.190 --> 00:29:59.750
links in part to, uh, how we know so much
764
00:29:59.750 --> 00:30:01.190
about the interior of the Earth. Because
765
00:30:01.430 --> 00:30:04.110
shock waves from earthquakes travel at
766
00:30:04.110 --> 00:30:06.110
different speeds through different media. And
767
00:30:06.110 --> 00:30:08.210
you've got T waves and S waves
768
00:30:08.450 --> 00:30:10.210
propagating around the Earth. Ah, some going
769
00:30:10.210 --> 00:30:11.850
through the Earth's, uh, interior, being
770
00:30:11.850 --> 00:30:13.810
picked up at seismographs around the world
771
00:30:14.370 --> 00:30:16.570
that very clever people can use to reverse
772
00:30:16.570 --> 00:30:18.210
engineer what the interior structure of the
773
00:30:18.210 --> 00:30:21.010
Earth's like by those differences in speed.
774
00:30:22.610 --> 00:30:25.090
Andrew Dunkley: Yeah, it was a strange experience.
775
00:30:25.250 --> 00:30:27.890
And that was the last thing I expected to
776
00:30:27.890 --> 00:30:30.530
witness. I was a bit more concerned about
777
00:30:30.610 --> 00:30:32.770
what was falling out of the sky at the time.
778
00:30:33.170 --> 00:30:35.770
I'll tell you, though, um, I took a great
779
00:30:35.770 --> 00:30:37.370
photo as we were walking off.
780
00:30:37.690 --> 00:30:39.570
Uh, when you're in tour groups, there's
781
00:30:39.570 --> 00:30:41.970
always a straggler. So we're all halfway off
782
00:30:41.970 --> 00:30:44.250
the mountain, but someone decided to stay
783
00:30:44.250 --> 00:30:47.210
behind. And that's when the biggest bang of
784
00:30:47.210 --> 00:30:50.210
the day happened. And it flung lava bombs up
785
00:30:50.210 --> 00:30:52.570
in the sky the size of soccer balls.
786
00:30:53.210 --> 00:30:55.930
And I had already put my camera in my
787
00:30:55.930 --> 00:30:57.850
pocket. I, uh, turned it off. I had enough
788
00:30:57.850 --> 00:31:00.250
time to pull the camera out, turn it on
789
00:31:01.010 --> 00:31:03.370
focus, and take a photo of this woman staring
790
00:31:03.370 --> 00:31:05.010
up at lava bombs coming down.
791
00:31:06.210 --> 00:31:09.050
It's a great photo. Um, and then it was,
792
00:31:09.050 --> 00:31:11.970
uh, only a few weeks after I got home that my
793
00:31:11.970 --> 00:31:14.610
friend, uh, sent me a video that he'd Taken
794
00:31:15.170 --> 00:31:17.650
of one of those, uh, little eruptions and
795
00:31:18.210 --> 00:31:20.610
I didn't see it, but there was a lava bomb
796
00:31:20.610 --> 00:31:23.570
landed 20 metres in front of me. I never even
797
00:31:23.570 --> 00:31:26.570
saw it. And, yeah, that kind
798
00:31:26.570 --> 00:31:27.990
of freaked me out after the fact.
799
00:31:29.580 --> 00:31:32.460
Yeah, like I said, not something I recommend,
800
00:31:32.460 --> 00:31:35.100
but, boy, what an adrenaline jolt.
801
00:31:36.060 --> 00:31:38.740
Yeah, but there's a few
802
00:31:38.740 --> 00:31:40.940
volcanoes we've visited over the years and,
803
00:31:41.240 --> 00:31:43.340
um, they've all blown up since we've been to
804
00:31:43.340 --> 00:31:45.700
them. So the one at Vanuatu stopped air
805
00:31:45.700 --> 00:31:48.700
traffic. Uh, we were at Matt Etna,
806
00:31:49.140 --> 00:31:50.980
uh, a couple of years ago. Well, look what
807
00:31:50.980 --> 00:31:53.520
it's doing at the moment. Kilauea. It's gone
808
00:31:53.670 --> 00:31:55.670
off, like, several times since we were there.
809
00:31:55.990 --> 00:31:58.190
In fact, the observation deck in the
810
00:31:58.190 --> 00:32:00.790
caldera, uh, where we
811
00:32:01.190 --> 00:32:03.590
looked at Kilauea, was
812
00:32:03.590 --> 00:32:06.430
obliterated about a month after we were
813
00:32:06.430 --> 00:32:06.710
there.
814
00:32:08.230 --> 00:32:10.510
Jonti Horner: So when are you taking a holiday to Naples or
815
00:32:10.510 --> 00:32:11.590
to Yelliston?
816
00:32:11.830 --> 00:32:14.230
Andrew Dunkley: Well, actually, we've been to Naples, so,
817
00:32:14.710 --> 00:32:17.530
um, it wasn't, um,
818
00:32:17.530 --> 00:32:19.950
Vesuvius, though, that went off when we were
819
00:32:19.950 --> 00:32:21.710
there. It was, um, Stromboli.
820
00:32:21.710 --> 00:32:23.710
Jonti Horner: Yeah, well, they're quite worried about Campo
821
00:32:23.710 --> 00:32:26.050
Fiegri, I think it's called, which is Big
822
00:32:26.210 --> 00:32:29.210
Field under Naples. That, yes, will
823
00:32:29.210 --> 00:32:30.610
be a disaster when it goes.
824
00:32:31.010 --> 00:32:33.770
Andrew Dunkley: Well, like, if you go out
825
00:32:33.770 --> 00:32:36.370
into the. Into the bay and, and
826
00:32:36.530 --> 00:32:39.370
do a bit of, um, skin diving down to the. To
827
00:32:39.370 --> 00:32:41.689
the bottom, there's all this gas coming up
828
00:32:41.689 --> 00:32:42.770
through the sand, like.
829
00:32:43.170 --> 00:32:45.730
Jonti Horner: And I keep seeing reports of the amount of
830
00:32:45.730 --> 00:32:47.290
swelling of the lava dome and things like
831
00:32:47.290 --> 00:32:49.130
this. I mean, yeah, I personally would not
832
00:32:49.130 --> 00:32:51.570
feel all that comfortable living in that area
833
00:32:51.570 --> 00:32:52.660
or even necessarily visiting,
834
00:32:55.130 --> 00:32:57.370
but hopefully, you know, it will not be a
835
00:32:57.370 --> 00:32:59.810
problem within our lifetimes and the science
836
00:32:59.810 --> 00:33:01.570
will continue to improve to the level that
837
00:33:01.570 --> 00:33:03.170
they get enough warning to get everybody out
838
00:33:03.170 --> 00:33:03.930
when it goes.
839
00:33:04.330 --> 00:33:06.650
Andrew Dunkley: Yeah, that's the problem, isn't it? Uh, and
840
00:33:06.650 --> 00:33:09.610
even in, uh, New Zealand they've got, um, the
841
00:33:10.010 --> 00:33:12.690
dormant, uh, volcano in the
842
00:33:12.690 --> 00:33:15.050
harbour at Auckland. And
843
00:33:16.170 --> 00:33:18.730
I was talking to a journalist friend of mine
844
00:33:18.810 --> 00:33:21.370
who lived in New Zealand, uh, some years ago
845
00:33:21.370 --> 00:33:23.530
when I worked for the abc, and he was saying,
846
00:33:23.850 --> 00:33:26.390
look, it is a worry there too, if this thing
847
00:33:26.390 --> 00:33:28.750
ever wakes up. There are only two roads out
848
00:33:28.750 --> 00:33:31.270
of Wellington, uh, out of Auckland,
849
00:33:31.990 --> 00:33:34.350
and you've got a million people there or
850
00:33:34.350 --> 00:33:37.150
something. And how are they going to get
851
00:33:37.150 --> 00:33:37.430
out?
852
00:33:37.430 --> 00:33:39.310
Jonti Horner: It was actually fascinating. I was in New
853
00:33:39.310 --> 00:33:41.030
Zealand a couple of times earlier in the year
854
00:33:41.190 --> 00:33:43.430
and went through Auckland and spotted all
855
00:33:43.430 --> 00:33:44.710
these little humps and thought, that's
856
00:33:44.710 --> 00:33:46.710
interesting. Looked into it. I just pulled up
857
00:33:46.710 --> 00:33:49.710
the information here. The metropolitan area
858
00:33:49.710 --> 00:33:51.960
of Auckland contains 53
859
00:33:51.960 --> 00:33:54.680
volcanoes because it's a little volcanic
860
00:33:54.680 --> 00:33:56.920
field of these small little
861
00:33:57.320 --> 00:33:59.640
maas and tuff rings and all this stuff.
862
00:34:01.160 --> 00:34:03.520
Um, none of them are thought to have erupted
863
00:34:03.520 --> 00:34:05.800
more than once, except for one of them called
864
00:34:06.040 --> 00:34:09.040
Orangitoto. But it is
865
00:34:09.040 --> 00:34:10.960
an active volcanic area. Apparently the first
866
00:34:10.960 --> 00:34:13.920
vent in that area erupted 193,000
867
00:34:13.920 --> 00:34:15.760
years ago. And the most recent one was about
868
00:34:15.760 --> 00:34:16.730
600 years ago.
869
00:34:16.879 --> 00:34:17.119
Generic: Go.
870
00:34:17.359 --> 00:34:17.839
Andrew Dunkley: Yeah.
871
00:34:18.000 --> 00:34:19.599
Jonti Horner: Um, and that's from the one in the water,
872
00:34:20.460 --> 00:34:23.399
um, just east of the city. But,
873
00:34:23.399 --> 00:34:25.439
yeah, must be a fascinating place to live.
874
00:34:25.999 --> 00:34:28.879
But that plus the earthquakes,
875
00:34:29.039 --> 00:34:31.919
plus the psalms that get there. It's
876
00:34:31.919 --> 00:34:33.959
good to live in interesting times. But that
877
00:34:33.959 --> 00:34:35.359
might be a little bit too full on.
878
00:34:35.759 --> 00:34:38.239
Andrew Dunkley: Yeah. Well, we visited Christchurch,
879
00:34:38.310 --> 00:34:41.159
uh, coming up on four
880
00:34:41.159 --> 00:34:43.959
years ago now, and, uh, it had had that
881
00:34:43.959 --> 00:34:46.230
massive earthquake, that tragic earthquake.
882
00:34:46.230 --> 00:34:49.190
And, uh, even then you could. That
883
00:34:49.190 --> 00:34:51.590
they hadn't come close to rebuilding.
884
00:34:52.230 --> 00:34:55.030
And they even have, um, a
885
00:34:55.030 --> 00:34:57.750
museum, Quake City, I think it's called In
886
00:34:58.070 --> 00:35:00.310
Christchurch, which I highly recommend. It's
887
00:35:00.470 --> 00:35:01.670
fascinating. Yeah.
888
00:35:02.270 --> 00:35:04.030
Uh, we got off the topic, uh, did we talk
889
00:35:04.030 --> 00:35:06.030
about smells in space? If you could take a
890
00:35:06.030 --> 00:35:08.950
big inhale, what would it be like?
891
00:35:08.950 --> 00:35:09.550
Andrew Dunkley: I'm not sure.
892
00:35:09.550 --> 00:35:11.350
Jonti Horner: I mean, this is one of those things that
893
00:35:11.350 --> 00:35:14.260
people use to give you a handle
894
00:35:14.420 --> 00:35:17.220
to get on. So when we discover interesting
895
00:35:17.220 --> 00:35:19.540
things in the atmosphere of different places,
896
00:35:20.820 --> 00:35:23.140
usually, um, the things that relate to
897
00:35:23.460 --> 00:35:25.500
gases that we'd have on Earth are used to
898
00:35:25.500 --> 00:35:27.300
say, oh, this place would smell of whatever.
899
00:35:27.700 --> 00:35:29.980
Most common of them is hydrogen sulphide,
900
00:35:29.980 --> 00:35:32.780
which is your rotten egg smell, which is why
901
00:35:32.780 --> 00:35:34.940
people talk so much about exoplanets that
902
00:35:34.940 --> 00:35:37.420
smell like rotten eggs. But I think there was
903
00:35:37.420 --> 00:35:40.060
one recently that wasn't there. Something
904
00:35:40.060 --> 00:35:41.660
saying it was a giant gas cloud that would
905
00:35:41.660 --> 00:35:44.310
have smelled or tasted of strawberries. Big
906
00:35:44.310 --> 00:35:47.030
Said found a long chain hydrocarbon that was
907
00:35:47.030 --> 00:35:49.750
part of the test sensation. That is a nice,
908
00:35:49.830 --> 00:35:52.510
nice strawberry. So I think most of space
909
00:35:52.510 --> 00:35:55.150
would not smell particularly pleasant, but
910
00:35:55.150 --> 00:35:57.470
you wouldn't smell very much. But there's
911
00:35:57.470 --> 00:35:58.990
dust and debris around. But there's also a
912
00:35:58.990 --> 00:36:00.910
lot of gases that you really wouldn't want to
913
00:36:00.910 --> 00:36:02.950
inhale. I mean, I'm thinking of hydrogen
914
00:36:02.950 --> 00:36:05.530
cyanide and things like this. So, uh,
915
00:36:05.550 --> 00:36:06.950
inhale at your own risk.
916
00:36:07.270 --> 00:36:09.350
Andrew Dunkley: Well, I think you'd only inhale once in space
917
00:36:09.350 --> 00:36:10.470
and that'd be the end of that.
918
00:36:10.470 --> 00:36:11.500
Jonti Horner: Oh, absolutely, absolutely.
919
00:36:11.660 --> 00:36:13.230
Generic: Probably. All right.
920
00:36:13.230 --> 00:36:14.900
Andrew Dunkley: Uh, David, thanks for that. Great question.
921
00:36:14.900 --> 00:36:16.860
That was a lot of fun to discuss and brought
922
00:36:16.860 --> 00:36:18.700
up a lot of things in my mind about some of
923
00:36:18.700 --> 00:36:21.340
the experiences with sounds and smells I've
924
00:36:21.340 --> 00:36:22.060
had in my life.
925
00:36:22.650 --> 00:36:24.820
Uh, and that brings us to the end of a Q and
926
00:36:24.820 --> 00:36:26.500
A edition. If you would like to send us some
927
00:36:26.500 --> 00:36:28.620
questions, please do through our website
928
00:36:28.620 --> 00:36:31.260
spacenutspodcast.com spacenuts
929
00:36:31.340 --> 00:36:33.740
IO or do a search for SpaceNuts
930
00:36:33.740 --> 00:36:36.220
podcast in your favourite search engine. If
931
00:36:36.220 --> 00:36:37.980
you just do a search for Space Nuts, it'll
932
00:36:37.980 --> 00:36:39.420
take you to that horrible movie.
933
00:36:40.970 --> 00:36:42.950
Um, well, it's probably not that horrible,
934
00:36:43.110 --> 00:36:45.390
but anyway, uh, that's how you do it. Just
935
00:36:45.390 --> 00:36:47.910
click on the AMA tab and send us text or
936
00:36:47.910 --> 00:36:49.630
audio questions. And don't forget to tell us
937
00:36:49.630 --> 00:36:51.350
who you are and where you're from. And have a
938
00:36:51.350 --> 00:36:52.630
look around on our website while you're
939
00:36:52.630 --> 00:36:54.750
there. Jonty, thanks very much. Good to see
940
00:36:54.750 --> 00:36:55.110
you again.
941
00:36:55.110 --> 00:36:56.590
Jonti Horner: That's absolute pleasure. It's good to catch
942
00:36:56.590 --> 00:36:58.510
up and, you know, I'll catch you again the
943
00:36:58.510 --> 00:36:59.910
next time Fred Watson's on a jolt.
944
00:36:59.910 --> 00:37:01.470
Andrew Dunkley: Yeah, I think you'll be back after this
945
00:37:01.470 --> 00:37:03.550
episode, but we'll, um, we'll keep you on
946
00:37:03.550 --> 00:37:05.990
standby, but we'll talk again down the track.
947
00:37:06.150 --> 00:37:06.710
Jonti Horner: Absolutely.
948
00:37:06.710 --> 00:37:09.350
Andrew Dunkley: Look forward to it, Professor Jonty Horner,
949
00:37:09.350 --> 00:37:10.910
professor of Astrophysics at the University
950
00:37:10.990 --> 00:37:12.910
of Southern Queensland. And thanks to Huw in
951
00:37:12.910 --> 00:37:15.070
the studio, uh, who did actually turn up
952
00:37:15.070 --> 00:37:16.590
today, but they wouldn't let him in because
953
00:37:16.590 --> 00:37:19.230
he smells. And from me, Andrew Dunkley.
954
00:37:19.230 --> 00:37:20.910
Thanks for your company. We'll see you on the
955
00:37:20.910 --> 00:37:23.150
next episode of Space Nuts. Bye. Bye.
956
00:37:24.350 --> 00:37:26.630
You've been listening to the Space Nuts
957
00:37:26.630 --> 00:37:29.590
Jonti Horner: podcast, available at
958
00:37:29.590 --> 00:37:31.630
Apple Podcasts, Spotify,
959
00:37:31.790 --> 00:37:34.480
iHeartRadio or your favourite podcast
960
00:37:34.480 --> 00:37:36.200
player. You can also stream on
961
00:37:36.200 --> 00:37:37.880
demand@bytes.com.
962
00:37:38.200 --> 00:37:40.280
Andrew Dunkley: this has been another quality podcast
963
00:37:40.280 --> 00:37:42.440
production from bytes.um com.
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