Will We Ever Find Alien Civilizations?
Will We Ever Find Alien Civilizations?
Introduction
Does intelligent life exist elsewhere in the universe? The question has captivated us for centuries, but despite decades of searching it remains frustratingly unanswered. Every so often a curious signal appears â fossilized structures in a meteorite, say, or an unusual gas in an exoplanetâs atmosphere â and for a moment it seems possible that we are not alone before the excitement gives way to a more mundane explanation.
So what would it actually take to find life in the cosmos â and how would we know when we saw it?
David Kipping, an astronomer at Columbia University, has spent his career finding better ways to answer these questions. His approach is statistical: rather than chasing individual detections, he develops mathematical frameworks for reasoning about where habitable worlds are likely to exist and how confidently we can interpret the signals they produce. In this episode of The Joy of Why, Kipping joins co-host Janna Levin to discuss efforts to frame one of humanityâs oldest existential questions as a tractable scientific problem, why biosignatures have proved so difficult to interpret, and why he believes exomoons may be an overlooked place to search for life.
Listen on Apple Podcasts, Spotify, TuneIn or your favorite podcasting app, or you can stream it from Quanta.
Transcript
[Music plays]
JANNA LEVIN: Iâm Janna Levin.
STEVE STROGATZ: And Iâm Steve Strogatz.
LEVIN: And this is The Joy of Why.
STROGATZ: A podcast from Quanta Magazine where we discuss some of the biggest unanswered questions in math and science today.
LEVIN: So Steve, I really have a good topic today.
STROGATZ: Hmmm.
LEVIN: Itâs aliens. First of all, have you ever seen a flying saucer? Letâs just have it out, Steve.
STROGATZ: Okay, this is where I have to admit, no. But I would like to talk to you about aliens.
LEVIN: Okay, thatâs really good because this is serious. I think scientists take very seriously the idea that thereâs life out there. Have you ever pondered the question, are we alone?
STROGATZ: A little bit. Years and years ago, I read a book by Francis Crick, you know, better known for his work on structure of DNA. But Crick wrote a book called Life Itself, and he was interested in the idea that life on this planet might have been seeded by a process that people were calling directed panspermia, that maybe life had been sent here.
LEVIN: Yeah.
STROGATZ: But the thing that really sticks with me from Crickâs book was a point that he made, which is about whatâs the probability of life starting on a given planet. And he said, âWe really donât know.â
LEVIN: Mmm-hmmm.
STROGATZ: Like, we just really donât know. And if the number is sufficiently small, like astronomically improbable, it could be that weâre the only life in the universe. Thatâs not impossible. You know, you always hear people say, âOh, thereâs so many stars and so many galaxies,â that people just assume thatâs a big number, so of course there must be life everywhere. But in my heart, I really donât know. There might be none or there might be a lot. I donât know.
LEVIN: Yeah. Well, I think thatâs exactly the question, that this isnât just a matter of belief, right? Itâs not, I believe in aliens or I donât. And itâs also no longer beyond quantifiability. We actually have concrete questions we can ask, parameters we can estimate, satellites that search for planets that give us data and intel. And this is kind of a modern and more sophisticated version of something called the Drake equation.
So I spoke to someone who studies deeply the mathematical underpinnings of making these kinds of assessments, and that is David Kipping, who is a colleague of mine. David is an astronomer at Columbia University, where he studies exoplanets and exomoons, and heâs really focused on developing new statistical methods in particular to detect potentially habitable worlds, which I think is a very intriguing way to get ultimately to the question that I think haunts him, which is, are we alone?
So, hereâs David Kipping.
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LEVIN: Welcome to The Joy of Why, David. So great to have you here.
DAVID KIPPING: Itâs a pleasure to finally be on. Yeah, itâs great to be here.
LEVIN: I know. Itâs so great. Usually weâre in the same building at Columbia, but not today.
KIPPING: Yeah, or a bar having a cocktail or something.
LEVIN: Right. We should do this there, thatâs for sure. I have to say, for a Columbia astronomy lab, you have one of the best names around. So you call your lab the Cool Worlds Lab. Can you help people understand the origin of this name?
KIPPING: Right, so when I was applying for faculty jobs way back, I was doing that usual thing of trying to come up with a good name, and my PhD advisor, GĂĄspĂĄr Bakos, he said, âWhatever you do, donât call the lab âKipping Lab.â Donât call it after yourself. Donât be that guy.â
And, there was a group in San Diego called the Cool Stars Group, and thereâs a big conference called Cool Stars. So Cool Stars, obviously, focusing on these M dwarf stars, these low-mass stars, which itâs really easy to detect planets around them. Thereâs a lot of interest astrobiologically around these sorts of stars. So there was a huge amount of interest about those, and I thought, âHey, by extension, itâs the cooler worlds that we also care about.â Itâs not the hot Jupiters so much, at least not for me. Itâs not the hot Neptunes. Itâs the planets that are further out in the temperate zone where life is possible, where moons can be possible, not because of the thermal temperature, but almost the dynamical temperature has cooled down. So everything just gets more interesting when youâre far away from the star. So that was the story behind the name.
LEVIN: Yeah, thatâs interesting. Youâre already raising scientific questions because people are hearing terms like, certain dwarf stars, but also Jupiters and Neptunes. So this idea that planets are replicated, the ones that we see in our solar system, here we are with our eight planets, and then we see similar kinds of planets around other stellar systems. Is that a surprise?
KIPPING: If you go back 20, 30 years ago, before I was in the field, I think people didnât know. There was an expectation. [Carl] Sagan was the eternal optimist, and he wrote about this a lot, and he really did expect, and many others expected there to be lots of planets out there.
But you can make an anthropic argument that itâs perfectly consistent that the solar system could be the only place that has planets, and it would be perfectly natural that we would happen to be born in the one place where there are planets, âcause of course, we couldnât be born anywhere else. So you could make that argument, but I think it would be surprising, a little bit intuitively, and indeed, once we started finding planets, it reinforced that view.
But I think whatâs really took us aback is just the diversity of worlds. I mean, we really expected the solar system to be a template of what other systems would look like, and itâs not, Janna. It looks radically different from place to place, and that has really blown our minds.
LEVIN: So, when Carl Sagan was working, it wasnât clear that there were other planetary systems. That is quite amazing. When you started entering the field, it was already accepted that there were tons of exoplanets and the search for life was a real scientific pursuit. Would that be fair to say?
KIPPING: Yeah, I mean, so I was doing my PhD up to 2011. Kepler launched, 2009. This was a mission that NASA launched which really transformed our understanding of planetary systems because it discovered not only thousands of them â we went from dozens to thousands in the space of a couple of years â but it also probed down to really small worlds.
So before we were only really sensitive to largely Jupiter mass, Jupiter-size planets, and Kepler pushed us all the way down to Neptunes, super Earths and even some planets comparable to the size of the Earth. So that blew us away. But at the same time, I was thinking, âHey, if we are able to detect Earth-sized planets, why couldnât the universe be a little bit more creative and start making Earth-sized moons around Jupiter-sized planets?â And that was, yeah, really where I got into this idea of looking for moons.
LEVIN: So why is it important that it be Earth-sized? Whatâs wrong with 40% the size of the Earth for a moon?
KIPPING: Nothingâs wrong with that. Itâs still fascinating. Itâs still wonderful. It might be a challenge for life.
When you make a worldânot necessarily just a planet or a moonâbut just a world smaller and smaller, obviously, its surface gravity decreases, its escape velocity decreases, and thus itâs easier for gas, for an atmosphere to leak off through whatâs called Jeans escape or even hydrodynamic escape if thereâs ultraviolet radiation smashing into the top of the atmosphere.
So those processes erode away atmospheres, and we think thatâs why Mars doesnât really have a thick atmosphere. The atmosphere of Mars is 0.6%, I think, the density of Earthâs atmosphere, yet itâs further away from the sun, so it should be easier in a thermal sense for it to hold onto an atmosphere. But of course, itâs only 10% the mass of the Earth, so that explains it.
We think that it probably did have a thick atmosphere in the past because we see all this evidence for liquid water. We see these, riverbeds and river deltas and valleys that have been carved out by water. So it somehow lost it because it essentially wasnât massive enough.
So therefore, that could be a problem. If you wanna have a habitable moon, you probably want it to be larger than that of Mars. Otherwise, you might be restricted to things which are beneath the surface. And of course, there is interest in that with Europa, Enceladus, of subsurface life.
But if something like, like we have, doing agriculture and a civilization, that might be difficult to have if youâre too small.
LEVIN: There seem to be a lot of things that went into the reason that the Earth, if itâs not the only planet in our system that evolved life ever, itâs the only one that radiated plentifully as we see now. And the factors, as youâve already mentioned, this kind of temperate zone, the existence of oceans, and things like plate tectonicsâthat really surprised meâand maybe even the spin axis of the Earth, which could have been from an early collision. So how much do all of these factors participate in the ability for life to take hold and really radiate?
KIPPING: Truthfully, we donât know. We can speculate about each of these factors, and thereâs reasonable speculation about all of those. Plate tectonics, we think thatâs probably necessary for a carbon cycle, and we think a carbon cycle is probably essential for having enough carbon left over for life to thrive and to keep going on the surface. Otherwise, you could just deplete it over time.
And then, you know, youâve got other factors like the axial tilt, and again, people argue about that. You could think that an axial tilt is essential because if you had the North Pole pointed right at the sun for three months of the year or something, that would seem bad news for life. But on the other hand, we have extremophiles who seem very robust and can thrive in all sorts of environments. So maybe life would be fine without that?
But maybe itâs us really that weâre talking about. You know, itâs agriculture. Itâs a Neolithic revolution. Can you really do farming and have civilizations if your climate is wildly swinging? Like in Game of Thrones, you have these insane winters, right?
LEVIN: Winter is coming, yes.
KIPPING: The winter is coming. Itâd be like that kind of situation where you get these very deep winters and very extreme summers, and maybe that might be difficult to imagine a civilization thriving. Itâs difficult to know exactly where these boundaries are.
But there may be a lot of other parallel tracks to the way life arrived here. Maybe on Titan. Titanâs a very alien moon. It has methane and ethane lakes. Very, very different thing from the Earth. But perhaps there is life thereâsome form that we canât really even imagine thriving on the Earth.
LEVIN: Yeah. It sort of seems an insane trend to fall into given that we keep getting deposed from being special. And when we think about the kinds of organisms that exist here on Earth, the variety is tremendous.
Yeah, so youâve made the transition from just life, which could have been bacterial, to technologically sophisticated life, which sometimes is called intelligent life, but then that has all kinds of philosophical pit holes.
And so youâve just given this really interesting set of examples which are technological, space-faring civilizations that are trying to harness the energy and the resources, not only around them, but maybe of the entire galaxy, right? And that historically had a sort of origin in the Drake equation, which might have fallen out of favor, but really structured the conversation for a long time. Can you tell us a little bit about the 1960s astronomer Frank Drake and what he was after in terms of trying to write an equation to predict the probability of the emergence of so-called intelligent life?
KIPPING: My understanding of this story, obviously, itâs way before my time, this is back in the â60s, was that Frank Drake had organized a meeting to talk about searching for alien signals, radio communications. I think probably inspired by the paper by Morrison and Cocconi, the famous Nature paper which really triggered this thinking about looking for alien transmissions.
And so he had a little conference, and I believe there was only like seven or eight people at this conference, and it included evolutionary biologists, it included astronomers. Carl Sagan was in attendance at this meeting famously. They called themselves the Order of the OctopusâI do know that. But I think âcause there was an octopus expert there, and they were inspired to name themselves the Order of the Octopus after he gave a great talk about octopuses. It would have been a fascinating meeting to have been historically tracked.
But during that meeting, Frank Drake apparently wrote down the Drake equation for the first time, and the purpose of it was really to organize the meeting. And so it was a way of just like breaking out the problem into these bite-sized pieces. You know, how often does life start? How often does intelligence get going? How often do they communicate? Wasnât really intended, in my interpretation, to be a calculator, and I think thatâs where itâs been abused and why it has been sullied, over the years, because there have been numerous papers where astronomers have just plugged in numbers for the frequency of intelligence. And I mean, how does anyone know these numbers? Itâs all just guesswork.
LEVIN: Now, you have tried to, in technical papers, reframe the Drake equation in a way where youâve considered birth and death of civilizations, and again, returning to this possibility that we shouldnât overestimate. We should entertain the possibility that we are alone in the universe. Can you tell us about this approach and why you think it was worth pursuing, even after everything you just said?
KIPPING: Yeah, I prefer the birth-death formalism. It wasnât just me thatâs proposed this. A few of those people have converged on this idea as well. But the attraction of it is that you get rid of a lot of these terms which seem really arbitrary.
For instance, we talked about these different qualities, like the axis of the Earth has to be tilted within a certain range or something. Thatâs not actually in the Drake equation, but you could imagine someone adding in more and more parameters like that. The fraction of civilizations that choose to communicate via radio. Well, what about if they choose to communicate via something else? Its utility is questionable, I think.
And so for me, I was just interested in, you know, all models are wrong, but some models are useful. Make the model as simple as you can get away with. And the simplest model you can possibly imagine is that there is some rate at which these entities, civilizations, intelligence, whatever you wanna call them, emerge, and thereâs some rate at which they die.
And thatâs useful to think about that way because then you would expect there to be an equilibrium over a certain amount of time after some settling time. And so you can actually do that kind of calculation of what would be the settling time for given rates? And I think you can make a fairly convincing argument that given the age of the universe and the age of the galaxy right now, you would expect to be in the equilibrium state at this point.
And so thatâs interesting, I think for just dialing it back to the simplest bare bones you can. But it still leaves you ultimately with this question. And so what we argued in this paper, is that the actual number of extant present-day civilizations out there ends up being dominated by purely the ratio of the birth and the death rate. Thatâs it. So itâs actually just one number, the birth to death ratio. Thatâs all that matters.
LEVIN: It has an outsized influence on the result of the equation.
KIPPING: Itâs the only thing that matters for the population. Itâs exclusively down to that ratio.
In statistics, we often want priors, right? To predict a distribution, you have to have some distribution that you assume for the birth to death ratio. And so we argued that the most agnostic and least informative prior if you plug it in, it ends up giving you a very bifurcated distribution. So you end up with there either being a very crowded universe or a very lonely universe. Itâs very difficult to get it intermediate.
And I think this intuitively makes sense. There was a physiologist John Haldane about a century ago who pointed this out. He said, âWell, imagine you approached a bench and there was beakers of water, and the beakers of water are almost the same.â They have more or less the same temperature, the same salinity, but there might be slight differences between them. And then you have some random chemical, letâs call it chemical X, and youâre gonna pour it into these 20, 30 beakers, letâs say. And his challenge to the listener was this: What fraction of the time would you expect this random chemical X to dissolve amongst these beakers?
And he reasoned that you should expect either it to be almost 100% or 100%, or almost 0% or 0%. But itâd be very weird if half of the time this chemical dissolved in the water and half of the time it didnât, given the water is more or less the same water. Itâs more or less the same stuff each time.
And so by the same extension, thereâs all these Earth-like planets out there. You would expect that once the rules are in place, if life is the way it goes, then life will just pop up everywhere. Or itâs incredibly unlikely to get to life, and therefore we would necessarily live in one of those rare places.
So we kind of argued this bifurcation that you would end up with either a crowded universe or a lonely universe. And then we more provocatively said that we think the crowded universe is, certainly for technology, incompatible with observations. It is a very quiet cosmos out there.
LEVIN: The famous question Fermi asked many years ago in the wake of the UFO craze and the Roswell incident and all of these sightings of flying saucers. He said, âWhere is everybody?â It did raise a question. And in this statistical distribution that youâre suggesting, wouldnât we already know if it was crowded?
KIPPING: I think we would. I mean, so our claim is that if youâre an optimist for SETIâ
LEVIN: Search for extraterrestrial intelligence. Just for the rare person who doesnât know SETI.
KIPPING: Correct. Yes. So conventional SETI is listening for radio waves, right? Theyâve surveyed now millions of starsâwhich is still only a tiny fraction of the galaxy, but millions of stars. Theyâve done it for seven decadesânot continuously, but on and off. So lots of gaps, Iâll grant you, but thereâs been a lot of SETI work.
And certainly the universe is not screaming. It is not full. It is not saturated with radio transmitters. We are absolutely confident that is not the case. So in this framework where you would expect to have either crowded or empty, it more or less rules that out ab initio. Itâs done. You canât possibly have that.
So therefore, in our thinking, a SETI optimist has to live in this valley where itâs not zero, but itâs not 100%. And they are hoping that basically 10 more years of SETI will push us just over the edge from 55% coverage to, you know, thereâll just be enough that youâll get over. And we just argue thatâs statistically very unlikely that youâd live on that knife edge where weâre just behind the curve.
So I donât want to say donât do SETI, âcause itâs always a surprise, especially if weâre gonna in different ways rather than radio SETI, looking for laser signals, thinking about other means of communication, even neutrino beams, gravitational waves. But I think looking for simple life is a complete unknown. Like in that dichotomy of crowded or empty, it could be full. Like Mars could have life beneath its surface, Europa, Enceladus. We have no constraint on that. Itâs just that for whatever reason, it doesnât ever get to radio transmitters all over the place.
LEVIN: So whatâs also interesting is the sort of mathematical techniques that you use to explore these problems theoretically. Itâs not simply evaluate this parameter, plug it into the equation. Youâre actually thinking more about this in a statistical approach that allows you, in some sense, to transcend some of the details precisely because you can make assessments. Itâs sort of fine-tuning, right? Itâs either crowded or rare.
So in a way, you seem to be saying that just statistically using that kind of analysis, technology might be rare, but life could still be plentifulâjust simpler life.
KIPPING: I mean the idea of SETI pessimism, you might call it, of being down on the odds of this. This actually goes all the way back to Sagan, who was an optimist, but he got into a big debate with Frank Tipler in the 1980s because Tipler pointed out that imagine we have self-replicating probes, right? A machine that can make another version of itself, duplicate itself. Now then, in the 1960s, John Von Neumann, who first imagined that, that seemed kind of fantastical. He was looking at trends in technology and doing a big extrapolation.
But I think today it seems quite prescient. It seems possible. There was a recent study that estimated a machine now could reproduce 70% of its mass. So weâre 70% of the way there to a self-replicating probe. Itâs not that hard to imagine someone launching one of these things.
And in some extreme versions of this, you could imagine it just propagating across the galaxyâ1% the speed of light is plentyâand you could convert the entire galaxy into computer substrate, which the galaxy just becomes a giant data center in space for AI training or something. It does feel very prescient right now, and that clearly has not happened. The galaxy hasnât been converted into a giant computer substrate because otherwise we wouldnât be here.
So Tipler argued that this is the strongest constraint that we have. This requires that less than one in a hundred billion stars ever produces self-replicating probes that just do their own thing. Now, however contrived you think that might be, one in a hundred billion is a really small odds for, like, just someone somewhere has to do it once.
And so Sagan didnât like that because Sagan was an optimist, and so he was pushing back saying, you know, thereâs all these reasons, like the probe might have finite range. It might be like thereâs a zoo hypothesis. Aliens is watching us. Itâs like the Star Trek Prime Directive a little bit.
But, all of those have been studied really in-depth. We could talk about any of them, but theyâve all been thrown aside, largely. And I think the original claim by Tipler that this is really difficult to reconcile with our very existence, that self-replicating machine has never done this. The universe has not woken up. Matter has not transformed into intelligent substrate at this point. Apart from like our brains maybe. And so that, that is kind of a profound constraint on what happens in the universe.
LEVIN: Yeah. Okay, so I have to, at this juncture, ask you to address the issue of the UFO files. People are very caught up in this. What do you say when people are arguing, âWell, how do you explain three dots on the horizon from the Apollo mission?â Or, âHow do you explain these grainy photos these expert pilots are seeing in their equipment?â Whatâs the response you have to that?
KIPPING: Well, obviously, thereâs a lot we canât explain. You just have to be candid about that. I mean, thereâs plenty of observations that James Webb has taken that we canât explain. We donât fully understand why galaxies are so fully formed in the early universe as they are, and why there are quasars in the early universe. I mean, thereâs always stuff we donât understand.
LEVIN: Itâs aliens, David.
KIPPING: Yeah. And thatâs actually exactly the point that worries me, Janna. That the aliens is like the Band-Aid explanation. Itâs God. Itâs just saying God did it. Aliens did it. Because itâs too flexible as a hypothesis. It can explain anything you want. Why did your alarm clock not go off this morning? Aliens did it, and so that worries me a bit as a hypothesis, just from the point of like the Popperian standards of how we even talk about falsifiability in science. So the fact we donât have an explanation is not evidence for aliens. Thatâs just the first thing we should discount.
And then the idea of more specific evidence for UFOs, itâs mostly actually personal testimony. But the actual videos weâve seenânot very convincing. So you know, thereâs these three videos the Pentagon released. Thereâs no range information on any of that. So itâs very difficult to know whether youâre looking at something like right in front of you in the foreground or far away. And the pilot said, âOh, no, I had a good idea of where it was. I knew where it was.â But itâs not reproducible and of course, science is all about reproducibility. If you canât reproduce it we just donât know what to do with that.
So I think, in a nutshell, my big issue with the UFO claims has been that we canât even ingest it into science. If Iâm going to ingest any scientific claim, I need to know two numbers: the false positive rate of that experiment and its true positive rate. And Iâve proven this in a Bayesian paper, thereâs no way to interpret an experiment if you donât know those two numbers. Because if your false positive rate is 99% and someone says, âI saw a UFO,â itâs almost certainly a false positive. You have to know these numbers in order to make sense of it. Thereâs no way to even ingest these claims into science as they currently stand.
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STROGATZ: Oh, thatâs a very interesting take, the statistical argument from Bayesian thinking that we canât even assess these claims properly.
LEVIN: Thatâs very much his expertise. Heâs really brought to the fore these kinds of ways of thinking that have allowed him really to make progress instead of saying, âHey, does this specific one planet right here have life?â Right. Itâs easier to talk about the collective, and what trends we might expect and to deduce from there.
STROGATZ: Yeah, I was very interestedâI would say captivatedâbecause we are hearing so much these days from what seem like credible, maybe not quite credible? I guess what Iâm thinking is the people that were military, you know, that donât seem like theyâre prone to exaggeration.
LEVIN: Mmm-hmm.
STROGATZ: That saw something they canât explain.
LEVIN: Oh yeah.
STROGATZ: And I thought the humility of Davidâs reaction, that thereâs so much that we canât explain. Why would we leap to the alien idea? Why donât we just say thereâs a lot of things we canât explain and just live with that?
LEVIN: Yeah, I absolutely agree with you. I donât feel that we should be disparaging people who are coming forward and reporting sightings. We should absolutely be collecting all kinds of data and information on observations citizens and experts are making of unidentified aerial phenomena. Thatâs respectable, admirable. But the leaping to âthis is aliensâ is problematic.
STROGATZ: I wanted to ask you some things about that because it seems like itâs right in your wheelhouse. I mean, it is so problematic given what we know about cosmic distances. And given our understanding of the speed limit of the universe set by the speed of light.
LEVIN: Yeah.
STROGATZ: I mean, I was just looking up the numbers to remind myself this morning. Just within our galaxy, the types of numbers we would be talking about. Like, if we imagine that an alien came by spaceship from a planet around some star in our galaxy, that would be on the order of tens of thousands of light years. Even if they were going at the speed of light. We didnât even have civilization ten thousand years ago.
LEVIN: Yeah. Weâre talking to Davidâs point. Either there have to be a huge number of civilizations for that to be viable that we overlap and communicate. Huge number, because youâre traveling, letâs say, 100,000 light-years to cross the galaxy at the speed of light, right? To get all the way across the galaxy.
So yes, thereâs a lot of planets and star systems and moons within that range, but we havenât had civilizations for hundreds of thousands of years. Weâve had civilization, as you said, really just for a few thousand, and weâve only had technology for a couple hundred years, right? A couple hundred years, and itâs unclear that our technology is sustainable, that weâll be able to keep having electricity and energy for everybody on this planet sustainably. So we might only have had a few hundred years of technology total, and that might be it.
So youâre talking about trying to overlap across these incredibly vast spatial distances in this incredibly long timescales in a bleep, right? An absolute bleep. And then it becomes, well, if we do overlap, then probably there are a whole huge ton of civilizations âcause then theyâre in our backyard, and they came really close, and then by coincidence, they overlapped with us in time. And if we donât, well, you know, that kind of seems like, yeah, maybe thatâs just the odds.
STROGATZ: Can I just ask one thing thatâs silly? I mean, âcause thereâs always this question of is there biological evidence? Like, do we have the dead alien from the crash?
LEVIN: Right.
STROGATZ: And then theyâre⌠Itâs so perplexing that these civilizations would be good enough to travel at close to the speed of light, or they develop wormhole technology, but they canât land safely in Kansas.
LEVIN: Exactly. Or, where they canât keep hiding from us very successfully? Well, canât get enough of aliens. I think weâve locked that down.
STROGATZ: Good. Well, I wanna listen to more.
LEVIN: After the break, weâre gonna zoom out to exomoonsâand that refers to moons outside of our solar system. So weâre going to discuss what exomoons mean for the search for life in our universe.
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Welcome back to The Joy of Why. Weâve been speaking with Columbia University astronomer David Kipping about the probability of life in our universe.
So youâve used this sort of deep statistical thinking not just to analyze theoretical concepts like the Drake equation, but really importantly, to actually search for places where life might emerge, and we already mentioned it lightly, but the idea that moons are a really interesting place to consider.
From our own experience in our system moons are plentiful. There are hundreds of moons in our solar system, which is really kind of amazing. What advantage are the exomoons offering you over an exoplanet in the search for life?
KIPPING: Yeah, Iâll give you my sort of four boilerplate reasons why I always say we should look for moons. One is that, of course, as you alluded, they could be habitable themselves. Two is that they could influence the habitability of the planet they orbit. So you might have an Earth-sized planet, and I think an obvious question is, well, does it have a moon-like moon around it as well? Because that seems like it had a big influence on our history. We probably want to know that. So youâve got those two kind of habitability aspects.
Then thereâs just the pure, like, uniqueness question. Maybe come back down to that more kind of mechanistic astrophysicist view. Just how did we get here? Whatâs our origin story? Is the Moon like a one-off fluke that just very rarely happens, or is that an inevitable part of terrestrial planet formation, that you end up with these large, almost quasi-binary objects? Thereâs lots of strange moons, and itâs like Triton goes around backwards around its parent planet. Youâve got Uranus tilted over with its moon system. So thereâs lots of curiosities in the solar system that from a singular example, itâs difficult to know, like, really how does this story play out in other environments. So I think just uniqueness is another reason.
And the fourth one is kind of subtle, and thatâs thinking about next generation missions. I mentioned we wanna build a successor to James Webb one day, probably called at the moment the Habitable Worlds Observatory, HWO. But it will hopefully one day take a photo of another Earth. Itâll be a single pixel. Itâll be a single blob of light. Theyâre like the pale blue dot. And from that pale blue dot, weâll split the light up into a rainbow, essentially like the prism, like Newton did, and weâll look for those atmospheric biosignatures that weâre so interested in. And moons here can really screw us over.
If anyoneâs ever seen that famous pale blue dot image that I think it was Voyager 1 took, as it looked back at, sort when it was like the orbit of Neptune. It turned around, it looked back and took a picture of the Earth. Itâs this beautiful image if youâve never seen it before. And in that image, itâs not a pale blue dot, even though Sagan described it as a pale blue dot. Itâs a pale blue-gray dot because the Moonâs in there. The Moonâs right, itâs photobombing right along, right? You canât distinguish it. You canât separate it. Theyâre just one smudge of light.
So when HWO takes these images, itâs gonna be in the same situation. Itâs seeing what it thinks is a planet, but itâs really a planet plus however many moons it has. And when we look at moons like Titan. Titan has a methane atmosphere, methane lakes. Itâs full of interesting hydrocarbons. You could easily, if you didnât know that was a separate moon, get confused.
You could imagine having an ocean world, a terrestrial ocean world, where the water undergoes photolysis, and that means that the H2O splits into hydrogen and oxygen. So youâve got an oxygen-rich planet. No life involved, just oxygen from UV radiation. Thatâs it. And then youâve got Titan mixed in there, which has methane.
So now, from the astronomerâs perspective, everything looks beautiful. Youâve got methane, youâve got ozone, youâve got oxygen. Youâd be like, âWeâre done. Thatâs life.â But itâs a confounder. Itâs just something we hadnât thought of. So thatâs why I think moons are really important. I donât know how we could even look for life with HWO unless we resolve the moon problem.
LEVIN: So can you catch us up to date as to where we are in terms of actually observing, not just theorizing, but actually observing with the satellite missions exo-moons.
KIPPING: So this has been obviously a long quest in my entire career. During my PhD, I came up with one of the methods that we are using today to try and look for these moons, thinking about the dynamical perturbations that a moon would impart upon its parent planet gravitationally. And thatâs kind of how we look for planets. We often look for planets by detecting the gravitational influence it has on the star. So we kind of extended that to looking for these moons.
And I think what we know for sure is that Kepler, which as I said, was this transformative mission, had this sensitivity down to about Earth-sized stuff â moons, planets, whatever it. And it really didnât throw out many candidates. Thereâs just not a lot there. So out of the 4,000, 5,000 candidate exoplanets, we have just a couple of hints of moons in that entire database. So that already tells you Earth-sized moons are not that normal. Iâm not saying they never happen, but theyâre certainly not par for the course.
We did find a couple of interesting candidates that I hinted at there, but they both have been very surprising because theyâre so large. They are Neptune-sized or even mini Neptune-sized moons orbiting Jupiter-sized or super-Jupiter-mass planets. So nobody really expected that. I mean, reminds me a bit of hot Jupiters, some of the first exoplanets ever found. Theyâre Jupiter-like worlds but are about 10 times closer to their star than Mercury is around the sun.
LEVIN: Very close.
KIPPING: Yeah, scorching temperatures, thousands of degrees Celsius, on their day side. And so it was very surprising. Actually, a lot of people didnât believe them. They thought, how could you possibly get Jupiter there? Because we think we know how Jupiter formed. It formed from ices. It formed from essentially the same kind of cometary material that you find out in the distant solar system. So that stuff just wouldnât be stable close to a star. It would boil off, so you canât make Jupiter-like planets there.
But we now know theyâre definitely real because weâve just found like so many of them, and it still puzzles us how they got there. We still donât understand it.
And so we found these two large moons. 1625b-i And then thereâs also Kepler-1708b-i. So the b is the planet, the number plate is the star, and then the -i is the moon. Those are the only two weâve found. Other teams have seen hints in different observations as well. No one yet has like a crisp, clear slam dunk signal.
And I think thatâs what we really need. The fieldâs in desperate need of that kind of clear signal. Obviously, a big thing close to the star is the easiest signal you can possibly get. And I think a general story in astronomy is that often the first examples of things we discover are not typical. Theyâre often very unusual beasts, and the reason we find them first is âcause theyâre so loud. Theyâre disproportionate. Theyâre tail-end members of their population. Theyâre not representative. And so it wouldnât surprise me if these things turn out to be real, but theyâre still requiring follow-up to ultimately figure out what they are. But James Webb has been opening up a lot of doors for that.
LEVIN: So the Kepler sample youâre talking about is within few thousand light years. So our galaxyâs over 100,000 light years across. So this is still pretty much, as youâve said, weâre really only probing our region of the galaxy. How is James Webb Space Telescope changing some of this story?
KIPPING: Yeah, so James Webb is not really trying to discover new planets. Itâs certainly more than capable of doing so. Itâs just that the telescope time is so precious, a better use of its time is to do stuff like look for exomoons. Weâve done that experiment recently. Unfortunately, it came out flat. We looked at this beautiful Jupiter analog planet. Itâs really kind of had a similar orbit, a similar star to our own solar system, this Jupiter-sized planet on a nice long orbital period far from its star. We searched it for moons down to about the size of sort of Ganymede, so the largest moons of Jupiter, and we donât see them. So thatâs already, really interesting.
Another experiment weâve been doing is actually measuring the oblateness of exoplanets, which has never been done before. But you can actually tell whether the planet is a pure sphere, or slightly ellipsoidalâwhich of course planets really are. Theyâre oblate spheroids, because as they rotate, they bulge out at the sides. And so they get these kind of love handles, like the Earth has, you know, slightly wider equator than it does the North-South Pole.
And Saturnâs actually pretty extreme. Thatâs actually quite detectable with James Webb. So itâs such an impressive machine. Thereâs no need to use it to find planets, âcause it can really characterize the planets, and especially atmospheres.
LEVIN: Well, letâs talk about atmospheres. Weâve talked a little bit about technological signatures. We havenât talked that much about the biosignatures. Would that be a reason why astronomers are obsessed with atmospheres, âcause theyâre looking for biosignatures for the emergence of life?
KIPPING: I think we wanna get there. I think a lot of us are dubious James Webb is sensitive enough to detect biosignatures. If you take the Earth, and even if you put the Earth around a very favorable star, so a nearby star, and make it a small star, because the smaller the star is, an Earth-sized planet will block out more of its starlight. And so itâs easier for us then to actually measure these atmospheric signals.
And even in those very favorable conditions, the signal weâre looking for is that the planet effectively appears different sizes at different wavelengths of light, and the wavelengths of light corresponding to, say, ozone absorption, you see the planet puff up a little bit. And what thatâs telling us is that thereâs a molecule, ozone in that case, that really likes to absorb that wavelength of light and therefore make the planet appear a little bit larger. So we think thatâs how you would potentially detect ozone. Itâs just that the telescope isnât quite sensitive enough, unfortunately, to get most of those biosignatures.
We think of things like methane, ozone, phosphine, dimethyl sulfide has been proposed recently as well. There was a claim actually of dimethyl sulfide, maybe some your listeners might know in that using James Webb, but itâs really spectacular levels compared to what we have on the Earth, so a lot of people are skeptical itâs remotely possible that could be a biosignature.
Thereâs just way too much of it to make sense for certainly an Earth-like biosphere. But thereâs a lot of controversy with some of these detections, but I think most of my colleagues think that itâs just beyond the ability of James Webb to detect biosignatures, but thatâs fine.
Probably a more basic question you might ask is, do Earth-like planets even have atmospheres to begin with? Or are they barren rocks? âCause the Moon doesnât have an atmosphere, Mars doesnât have much of an atmosphere, Mercury doesnât have an atmosphere.
And so thereâs a huge program right now with James Webb called the Cosmic Shoreline Program, which is to look at a group of planets which are Earth-sized in the habitable zones of their stars. And the question is whether the planets even have atmospheres, because M dwarfs are quite active. They throw out these huge coronal mass ejections, these stellar flares, and so there is a concern that maybe the atmospheres are gone. Maybe these planets canât even sustain an atmosphere.
James Webb can answer that question, so thatâs what this programâs doing. So it should be able to tell whether Earth-sized habitable zone planets have an atmosphere or not. And that would already be a massive breakthrough.
LEVIN: Amazing. So clearly, if they have atmospheres, the prospects for life goes up, loosely speaking, in that Drake equation kind of a way. Some of these biosignatures, though, are confounding. If you could find the atmospheres, and you were to look for some of these signatures, youâve mentioned certain elements that weâre looking for, certain molecules that weâre looking for in the atmospheres, because the presumption is that these are outgassings of metabolism presumably or something like that. But we donât even really know that, do we?
KIPPING: No, I mean, we just have one example, right? The confounders is a really big problem, and Iâve been thinking about that a lot. And what worries me a lot is that when you look at the history of biosignatures, just very broadly thereâs been so many spurious claims.
I mentioned very briefly the Allan Hills meteor, which was a rock on Mars 4 billion years ago that knocked off, it landed on the Earth, landed in Antarctica, I think in 1984 or something. And they collected it, they studied it, and they found these, like things which looked like little worms under the electron microscope.
And so that was essentially a biosignature. Itâs not a gas, but it is a biosignature. Itâs a signature of biology. And it turned out that even though it looked like life, other geochemists and scientists were able to show that you can make structures like that without biology involved whatsoever, just basically through water and high pressure water in particular. And so that really killed the momentum behind that claim.
Another example, if we go really far back, would be Martian canals. Seems silly now, but Percival Lowellâhe thought there was canals on Mars âcause he thought that was a biosignature. He saw these lines on Mars, and he thought, âI know what causes that. Itâs a canal system.â So often we are tripped by what we donât know. Itâs not Percival Lowellâs fault that he didnât know about those psychological biases âcause nobody had published on them yet.
And a very recent example was DMS, dimethyl sulfide. Dimethyl sulfide was claimed, as we mentioned earlier, in the, in an exoplanet atmosphere recently, K2-18b. Cambridge University did a huge press release talking about this being, you know, a historic moment in the search for life. But we now know that DMS is on comets in the solar system. Unless you think thereâs living creatures on all the comets, it seems difficult to believe that this is an unambiguous biosignature anymore. So just time after time after time, itâs like Groundhog Day, Janna. You just keep waking up, we hear these claims of life, and then we all know whatâs gonna happen. Happens every time. It just dissolves.
So Iâve been thinking about this really hard recently. And yeah, I do kind of make the case that I think the current approach weâre using just will never work, and we do need to really rethink how we do this.
LEVIN: And have you made progress in suggesting a way that we should do this differently?
KIPPING: Yeah. So my tentative suggestion is to do what I call A/B testing, which in YouTube landscape is something weâre very familiar with. Like, you have two thumbnails, and you challenge them against each other and see which one gets the most clicks. And so the way we do it here is youâd have two samples of planets, for example, and you have some reason to believe this is the condition for this experiment to work. You have reasons to believe that the occurrence rate of life is different. It canât be the same. If theyâre the same, this doesnât work. There has to be a difference in the life occurrence rate. But the confounder rateâhow often natural geochemistry or whatever it is producing ozone or whatever signature youâre looking forâthat has to be the same.
So the confounder rateâs the same between the two samples, but the life rate is different. And so really then youâre doing a differential measurement. Any difference you observe in biosignatures between those two populations, therefore, in a differential sense, has to be due to life.
It doesnât tell you how much life there is in an absolute sense. You still donât know, but you know that that excess must be driven by life. So that statistically is very clean. It resolves a lot of these problems and these unknowns. But you might reasonably question whether itâs even possible to set up such an experiment, and thatâs what Iâm thinking about now.
LEVIN: Amazing, so again youâre kind of returning to those statisticianâs roots, right? That the observations arenât going to be one moon with one obvious signal. Itâs more large samples, and large statistics.
KIPPING: Yeah, Iâm skeptical it would be a slam dunk in the same way maybe weâve had with other fields. To quote Donald Rumsfeld, itâs the âunknown unknownsâ that get you, right? And so thereâs so much we donât know about chemistry and geochemistry and other planetary environments that it feels like we are doomed to always be caught out by those things.
I think the only exception to this I can imagine is actually a really strong information-rich SETI signal. So if it was like a laser beam with a video transmission encoded within it, thereâs just no plausible natural confounder to that. You just canât imagine it. It just seems impossible.
But with biosignatures, those gases are very information weak. Really, all you measure is that gas is there and an abundance maybe, if youâre lucky. And thatâs about it. So itâs that informatics perspective, I think, that really endangers biosignatures. They just donât carry a lot of information to begin with.
LEVIN: So, how do you place yourself in the optimism-pessimism spectrum? Are you searching for life scientifically because you believe that this is a viable result within your scientific lifetime? Or are you more, âIâm interested in planets and moons from the aspect of astronomy, regardless of the discovery of life?â
KIPPING: Iâd say Iâm hoping and Iâm more interested in the idea of life. That is a great dichotomous split I think that you just gave there, and I think a lot of astronomers are driven by how does the universe work or are we alone? And those are like two very basic drivers to a lot of astrophysicists in different ways. I mean, Iâm interested in both, but Iâd say Iâm probably more driven by the latter.
However, am I an optimist or a pessimist? Iâd honestly try to be, itâs a little bit of a cop-out, but agnostic and forcefully agnostic because Iâm so terrified of experimenterâs bias. And weâve seen this so many times in history of scientists even claiming life, claiming this comet is an interstellar ship, claiming this little rock on Mars is a face, claiming this fossil from the Allan Hills meteorâBill Clinton stood on the White House lawn and talked about that as evidence for life on Mars, and now nobody believes it.
So many times weâve got caught up in that excitement of optimism, and I think the lesson for me has always been like just try and remain sober. Just try and look at it objectively and require those high standards of evidence that we apply in all other aspects of our science. It is not different when we look for life. So I try to remain objective, and I think honestly, it is perfectly consistent with everything we know about the universe that we are alone. Thereâs nothing we know about the universe that rules that out. It is within the realms of possibility.
LEVIN: Well, given that weâre alive and weâre here and we have the luxury of looking deep into the sky, what is it about this exploration that makes this the way you wanna spend this precious life that we have?
KIPPING: For me, itâs very much just curiosity-driven. Itâs just these are the things Iâve always wondered about life in the universe, what else might be out there. Iâve always dreamed of visiting other stars and seeing their planets. Itâs just that pure very simple curiosity-driven fascination with whatâs out there. And I think if you donât have that life can feel a bit empty, at least for me.
Like, I always get a little bit depressed when weâre asked sometimes as scientists to defend the technologies or industrial applications of searching the universe for gravitational waves or something. Sure, there is many side benefits, and we can list those off. But in a very pure sense, the reason for doing it is the same reason why we do poetry. Itâs the same reason why we do art. Itâs that, what is the point of being on this Earth if our sole interest is bread on the table, feeding myself, going to sleep, waking up the next day, going back to work, and thatâs your whole life? Itâs just this pure machine-like process.
Weâre more than that, I believe. And I think looking out and wondering about the universe, it enriches our soul, enriches our human nature. I would hate to live in a world where we didnât ask these questions. And I think itâs a real privilege, certainly, that Iâve had a career where Iâve been able to dwell on some of these questions and think about them so much.
LEVIN: Such a pleasure to talk to you and to share your stories and your insights and your ideas about the future of discovering whether or not weâre alone. This is really a delight. Thank you so much.
KIPPING: Itâs always a pleasure, Janna.
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STROGATZ: Well, I want to agree with that. I have often tried to make that argument myself about enriching our soul. But thereâs very natural reaction to have to that, which is we fundâor at least we used to fund scienceâbut we donât really fund poetry. You know, why should the taxpayer invest in science if itâs another form of poetry?
LEVIN: Yeah. And what do you think the answer to that question is?
STROGATZ: I think itâs much more than poetry. Itâs at least itâs very different from poetry. Itâs partly poetry. Itâs many things. I mean, itâs a really serious question, especially in the age of artificial intelligence, where so many of the things that weâre doing, we have to ask why are we doing them. I donât know. Yes, part of it is for soul enrichment, part of it is for helping future technology or helping, you know, new medicine or improve the quality of life of all of us. I want all of it. I donât know. What do you think?
LEVIN: Well, I would say, that it obviously really resonates with me what Davidâs saying, but for a reason that I think is also transformative for humanity. If you think about the shift with Copernicus from thinking weâre at the center of the universe to understanding and comprehending that we are not, that has untold implications, consequences, ramifications for the entire paradigm of civilization, and what weâre doing here and how we handle each other.
And so I think it can both be the dreaming blue skies approach and have implications for the future of humanity. I think Earthrise is a very good example of that. Looking back at the Earth as it rose over the moon in the Apollo missions initiated environmental movements. It really gave people a strong sense of connectivity on the Earth and kind of the limitations and evils of tribalism. So it changed culture, right? It changed civilization. So I think we can do both those things.
STROGATZ: Hmm, I like your answer a lot, that it gives, that this cosmic perspective as someone like Carl Sagan might have called it, maybe he even used that phrase, gives us a kind of humility and maybe makes us better people. You know, and if, as you say, like when weâre talking about alien civilizations, that our whole civilization is a blip in time, each of our individual lives is an even shorter blip in time, and why not be as good as we can be for that blip?
You know? I mean, this, here weâre getting into theology and ethics and all of that, but maybe science, which is often seen as somehow separate from all of that, is really a very good teacher about how to live ethically.
LEVIN: I think it is. Yes, And I think about how to cooperate internationally, how to transcend belief systems and trappings of nation and faith and, and to instead view ourselves as one species playing out on this one place. Together. Well, on that note, man, yeah, I, I need to go meditate.
STROGATZ: Okay. Ommm.
LEVIN: Yeah, exactly. I need some universal transcendence, yeah.
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STROGATZ: If youâre enjoying The Joy of Why and youâre not already subscribed, hit the subscribe or follow button wherever youâre listening. You can also leave a review for the show. It helps people find this podcast. Find articles, newsletters, videos and more at quantamagazine.org.
The Joy of Why is a podcast from Quanta Magazine, an editorially independent publication supported by the Simons Foundation. Funding decisions by the Simons Foundation have no influence on the selection of topics, guests, or other editorial decisions in this podcast or in Quanta Magazine.
The Joy of Why is produced by PRX Productions. The production team is Caitlin Faulds, Jade Abdul-Malik, Genevieve Sponsler, and Merritt Jacob. The executive producer of PRX Productions is Jocelyn Gonzales. Edwin Ochoa is our project manager.
From Quanta Magazine, Simon Frantz and Samir Patel provided editorial guidance with support from Samuel Velasco, Simone Barr, and Michael Kanyongolo. Samir Patel is Quantaâs editor-in-chief.
The episode art is by Chanelle Nibbelink and our logo is by Jaki King and Kristina Armitage. Special thanks to Garth Avery at the Cornell Broadcast Studio.
Iâm your host, Janna Levin. If you have any questions or comments, please email us at [email protected]. Thanks for listening!
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