Latest / Talking Science / The Ice Ages — When the World Froze Over
Transcript
- 0:00Imagine you could step into a time machine and
- 0:02travel back exactly 20 ,000 years. Which, you
- 0:05know, in geological time is basically nothing.
- 0:08Right. It's just a fraction of a blink. I mean,
- 0:10modern humans are already walking the Earth.
- 0:12We're painting those incredible scenes in caves.
- 0:15We have music, complex tools. But the world itself.
- 0:19It would look entirely alien to us today. Exactly.
- 0:22Because, well, you look up, and sitting directly
- 0:25over what is now Canada and the northern U .S.
- 0:28is just this solid, towering sheet of ice. Yeah,
- 0:32and we weren't just talking about a bad winter
- 0:33frost here. No, we're talking about an ice sheet
- 0:35up to three kilometers thick. Just three kilometers
- 0:39of crushing weight. And it wasn't just North
- 0:42America either. Right. Northern Europe was buried
- 0:45too. Yeah. If you tried to stand where London
- 0:46or Berlin are today, you'd be trapped under thousands
- 0:49of feet of permanent blue ice. And, you know,
- 0:51to build ice sheets that massive, all that water
- 0:53had to come from somewhere. It came directly
- 0:55from the oceans. Right. It evaporated, fell as
- 0:58snow, and just never melted. Exactly. So because
- 1:01so much of the Earth's water was literally locked
- 1:04up on land, global sea levels were drastically
- 1:07different. They were roughly 120 meters lower
- 1:11than today. Which means the maps we rely on just
- 1:14completely wouldn't apply. I mean, you could
- 1:17have walked on dry land all the way from Asia
- 1:19to America across the Beringland Bridge. You
- 1:21could stroll from the Australian mainland right
- 1:23over to Tasmania without getting your feet wet.
- 1:25It's wild. And this was the absolute peak of
- 1:28the last frozen era. So the mission. of our deep
- 1:31dive today is to explore this reality, because
- 1:34this frozen world didn't just happen once in
- 1:37some freak accident. No, it's happened over and
- 1:39over again on this strikingly regular beat. Yeah,
- 1:41so today we're going to unpack the astronomical
- 1:43clockwork that controls that rhythm. And this
- 1:46journey is just so essential. I mean, what's
- 1:48at stake here is far more than just trivia about
- 1:50woolly mammoths. Oh, for sure. Understanding
- 1:52this deep past is basically the ultimate key
- 1:54to understanding the climate machinery of our
- 1:56present. It shows us how the entire planetary
- 1:59system operates when you start, you know, aggressively
- 2:02pushing its buttons. Okay, but before we get
- 2:05into how a planet freezes, we need to clear up
- 2:08a massive popular misconception. Oh, definitely.
- 2:10The terminology trips everyone up. Yeah, because
- 2:13when I hear Ice Age, my brain instantly... Goes
- 2:17to the movie version. I picture the whole globe
- 2:19covered in frost, eternal blizzards, just a total
- 2:23deep freeze. Right. But scientifically speaking,
- 2:26that pop culture image is actually entirely misleading.
- 2:29OK, let's unpack this. What is the actual definition
- 2:32then? So using the strict scientific definition,
- 2:34an ice age is simply any period in Earth's history
- 2:37where there is permanent ice at the poles. That's
- 2:39it. Wait. Permanent ice at the poles. But Greenland
- 2:44has a permanent ice sheet. and antarctica is
- 2:46totally covered in ice yeah are you telling me
- 2:48that scientifically i'm sitting in an ice age
- 2:50right now you are firmly inside an ice age right
- 2:52now we have been for a couple of million years
- 2:54actually that is wow that completely flips the
- 2:56whole cultural narrative on its head it really
- 2:59does what you're picturing with the mammoths
- 3:01and the three kilometer thick ice burying new
- 3:03york is more precisely called a glacial period
- 3:06okay a glacial period right it's a specific intensely
- 3:11cold phase that happens within a larger ice age.
- 3:15It's when those polar ice sheets aggressively
- 3:18advance and crush the continents. OK, so if the
- 3:22freezing mammoth heavy part is a glacial period,
- 3:25what do we call the phase we're in today? Because
- 3:27I definitely don't see any glaciers advancing
- 3:29down my street. We are in what climatologists
- 3:32call an interglacial period. Basically, these
- 3:35are the relatively brief, warmer gaps between
- 3:38the deep freezes. The ice retreats, sea levels
- 3:40rise. Exactly. The planet gets a bit of a breather.
- 3:43And our current interglacial gap began about
- 3:4511 ,500 years ago. That timeline is genuinely
- 3:48staggering to think about. It really puts things
- 3:51in perspective. It does, because all of human
- 3:53civilization, I mean, the invention of agriculture,
- 3:55the first cities in Mesopotamia writing, the
- 3:57Roman Empire, smartphones, all of it fits entirely
- 4:00inside this one brief, mild interglacial window.
- 4:03It just highlights how delicate our global civilization
- 4:06really is. For millions of years, the Earth has
- 4:08been trapped in this rhythm. Cycling back and
- 4:11forth. Right. Brutal glacial phases lasting tens
- 4:15of thousands of years. And then these very brief
- 4:18warm gaps. We just happen to build our entire
- 4:21society during one of the warm gaps. Which introduces
- 4:23a massive mystery, honestly. If human history
- 4:27is just a warm gap in a deep freeze. What actually
- 4:30flips the switch? That is the million dollar
- 4:33question. I mean, we're talking about moving
- 4:35oceans of water onto land and freezing them.
- 4:38What kind of force can reliably turn an ice age
- 4:41on and off? Well, the answer comes from the sky.
- 4:44And the guy who first figured this out was a
- 4:46Serbian mathematician named Milutin Milankovic.
- 4:49Okay. His story is pretty incredible. During
- 4:51the First World War, he was actually interned
- 4:53as a prisoner of war. Wow, really? Yeah. And
- 4:56while he was a prisoner and for years afterward,
- 4:59he just dedicated himself to calculating the
- 5:01Earth's orbital variations by hand with paper
- 5:04and a pencil. Hold on. You're telling me a mathematician
- 5:07sitting in a World War I internment camp was
- 5:09doing hand calculations to figure out the climate
- 5:12from hundreds of thousands of years ago. That's
- 5:14exactly what he did. How could he possibly know?
- 5:17what the Earth's orbit was doing before human
- 5:19beings even existed. Well, celestial mechanics
- 5:22are incredibly predictable if you know the physics.
- 5:24His core insight was that the Earth's journey
- 5:27around the sun isn't a static, unchanging loop.
- 5:31Right. It's not a perfect track. Exactly. It
- 5:33gets tugged on. Massive planets like Jupiter
- 5:35and Saturn exert their own gravity on the Earth.
- 5:38So over tens of thousands of years, that gravity
- 5:41slowly warps our orbit. And as our orbit changes,
- 5:45it slightly shifts. exactly how and where sunlight
- 5:48hits the planet. Yes, and he broke this... shifting
- 5:51down into three distinct orbital cycles. Let's
- 5:54walk through them because this is really the
- 5:55clockwork of the ice ages. Yeah. Cycle number
- 5:57one is the shape of Earth's orbit, right? Correct.
- 6:01It is in a perfect circle. Over about 100 ,000
- 6:03years, the gravity of those other planets slowly
- 6:06stretches our orbit out. So it becomes slightly
- 6:09more elliptical, like a stretched oval. Right.
- 6:11And then it slowly relaxes back into a more circular
- 6:13shape. That's the first cycle. Got it. And the
- 6:15second cycle is the tilt of the Earth's axis.
- 6:18Yeah. The Earth isn't perfectly straight. up
- 6:20and down. It's tilted, which is why we have seasons.
- 6:23But that tilt isn't permanently fixed. It changes
- 6:27over time. It does. Over roughly 41 ,000 years,
- 6:31the Earth slowly nods back and forth, changing
- 6:35its tilt from about 22 degrees to 24 .5 degrees.
- 6:39So a steeper tilt would just mean more extreme
- 6:41seasons, right? Exactly. The summer hemisphere
- 6:43points more directly at the sun, and the winter
- 6:46points further away. Okay, and the third cycle
- 6:48is the rubble. Yes, the wobble. If you've ever
- 6:51watched a toy top spinning, you know it doesn't
- 6:54stay perfectly upright. As it spins, the top
- 6:56of the axis slowly wobbles around in a circle.
- 6:59The Earth does the exact same thing. It takes
- 7:01about 23 ,000 years to complete one full wobble.
- 7:05And what this wobble does is change which season
- 7:07we're experiencing when the Earth is at its closest
- 7:10point to the Sun in that slightly oval orbit.
- 7:12Right. And when you put all three of these together,
- 7:15you have to remember one crucial fact. None of
- 7:17these changes actually alter the total amount
- 7:19of solar energy hitting the Earth. Wait, really?
- 7:21The total amount stays the same? Pretty much,
- 7:23yeah. The sun isn't getting hotter. We aren't
- 7:25moving drastically closer to it overall. What
- 7:28changes is purely the distribution. Okay. It
- 7:31alters the timing and the specific latitude of
- 7:34where that sunlight lands. So to visualize this,
- 7:38I'm picturing these three cycles. the shape,
- 7:41the tilt, the wobble, as three different metronomes
- 7:44sitting on a desk. That's a great way to look
- 7:46at it. Right. So one metronome is ticking every
- 7:48100 ,000 years, one every 41 ,000, and the third
- 7:51every 23 ,000. Totally out of sync most of the
- 7:54time. Exactly. They're a chaotic mess. But eventually,
- 7:57if you wait long enough, there comes a specific
- 7:59moment where all three metronomes finally click
- 8:02on the exact same beat. And that alignment is
- 8:05exactly what Milankovitch was looking for. He
- 8:07calculated when those celestial metronomes align
- 8:10to create one very specific condition. Which
- 8:13is? Exceptionally cool summers in the Northern
- 8:15Hemisphere. Okay, wait. That feels entirely backwards.
- 8:18Yeah. If I want to build a giant glacier that
- 8:20buries Canada, my brain instantly thinks I need
- 8:23the most brutal, freezing, apocalyptic winters
- 8:26possible. Right. It's totally counterintuitive.
- 8:29Yeah. So why is a cool summer the trigger for
- 8:32an ice age? It's all about geography. To understand
- 8:35it, just look at a globe. The vast majority of
- 8:37the landmass where an ice sheet can actually
- 8:39grow is mostly in the northern hemisphere. Right.
- 8:42You've got Canada, Siberia, northern Europe.
- 8:45Exactly. Antarctica is massive, sure, but it's
- 8:48isolated at the bottom of the world, surrounded
- 8:50by ocean. To change the global climate, you need
- 8:53ice spreading across northern continents. Okay.
- 8:56We have the real estate in the north. But that
- 8:59still doesn't explain why the freezing winters
- 9:01don't matter as much. Think about the winters
- 9:03in northern Canada right now. It is already dangerously
- 9:07cold. It's more than cold enough to snow. That's
- 9:09true. Making the winter even colder -like, dropping
- 9:13it from minus 30 to minus 40, doesn't fundamentally
- 9:15change anything. The snow is already guaranteed.
- 9:19So the critical vulnerability for a glacier isn't
- 9:21the winter at all. Nope. It's the summer. Oh.
- 9:23The snow has to survive July. Precisely. If the
- 9:27summer is just a little bit too cool to melt
- 9:29away all of the previous winter's snowfall, a
- 9:32layer of snow survives into the autumn. And then
- 9:35the next winter arrives and just dumps a fresh
- 9:37layer on top of it. Exactly. The pile never resets
- 9:41to zero. Year after year, it accumulates. And
- 9:44the sheer weight of those layers compacts the
- 9:47bottom into dense, solid ice. So warm summers
- 9:50mean the slate gets wiped clean every year. But
- 9:53cool summers mean the snow compounds into an
- 9:56ice age. Yes. And Milankovitch predicted that
- 9:59whenever his three metronomes aligned to deprive
- 10:02the north of summer heat, the ice would build
- 10:04up. It's an incredibly elegant mathematical theory.
- 10:07It really is. I mean, it's just math on a piece
- 10:10of paper, right? He's doing this a century ago.
- 10:11A guy with a pencil claims he knows the global
- 10:14temperature from 200 ,000 years ago. The scientific
- 10:17community definitely didn't just take his word
- 10:18for it. Right. I mean, we needed physical proof,
- 10:21but... Time machines don't exist. How did anyone
- 10:25actually verify this? Well, it took arguably
- 10:28the greatest piece of scientific detective work
- 10:30of the 20th century. We needed a physical record
- 10:33of the Earth's atmosphere and we found it hiding.
- 10:37In the ice itself. Wait, you mean we just went
- 10:39out and dug up ancient ice? We drilled for it,
- 10:41yeah. In places like deep Antarctica and Greenland,
- 10:44it has been snowing for hundreds of thousands
- 10:47of years and it never melts. It just packs down.
- 10:50Right. So scientists go into these freezing landscapes
- 10:53and drill hollow tubes deep into the ice sheet.
- 10:56When they pull it up, they extract this long
- 10:58cylinder called an ice core. Because the layers
- 11:01build up year after year. Pulling up an ice core
- 11:04is literally pulling up a physical column of
- 11:06frozen time. Exactly. It's like tree rings. The
- 11:09deeper you drill, the older the ice. Okay, but
- 11:11a block of ice is just frozen water. Yeah. How
- 11:14does frozen water act as a thermometer for 100
- 11:16,000 years ago? This is where the chemistry comes
- 11:19in. Water is made of oxygen and hydrogen. But
- 11:22not all oxygen atoms are identical. Oh, like
- 11:24isotopes? Yes. Most oxygen is a lighter version,
- 11:28but a small percentage is slightly heavier. So
- 11:30you have heavy water and light water. Precisely.
- 11:33And think about evaporation. It takes heat from
- 11:36the sun to evaporate water out of the ocean so
- 11:38it can eventually fall as snow. Okay, I felt.
- 11:41Because those heavier molecules weigh more, it
- 11:43takes slightly more heat energy to lift them
- 11:45out of the ocean. Ah, I see where this is going.
- 11:48If the global climate is really cold, There isn't
- 11:51enough heat energy to evaporate the heavy water
- 11:53molecules. They just get left behind in the ocean.
- 11:56You nailed it. The mechanism is foolproof. Scientists
- 11:59melt a slice of ancient ice, measure the ratio
- 12:02of heavy to light water, and if there's very
- 12:05little heavy water, it proves that specific year
- 12:07was intensely cold. That is just brilliant. But
- 12:11there is something else trapped in that ice,
- 12:12isn't there? Yes, there is. Because as the snow
- 12:15gets crushed into solid ice, it traps air. Right.
- 12:18Microscopic bubbles of air get completely sealed
- 12:20in the ice. And those bubbles aren't a guess
- 12:22or a proxy. They are direct, pristine, physical
- 12:25samples of the Earth's atmosphere from the exact
- 12:28moment that snow fell. They're like tiny, frozen
- 12:31time capsules of ancient breath. That's a beautiful
- 12:33way to put it. We extract the air from those
- 12:36bubbles and measure precisely how much carbon
- 12:39dioxide was in the atmosphere 800 ,000 years
- 12:42ago. So we extract the ice cores, measure the
- 12:44temperature using the heavy water, and measure
- 12:47the CO2 using the bubbles. We build this massive
- 12:49timeline. And when we lay... that physical record
- 12:53over Milankovitch's hand -drawn predictions.
- 12:56It matches flawlessly. Wow. The physical evidence
- 12:59proved that the ice sheets advanced and retreated
- 13:02in exact rhythmic time with the orbital wobbles
- 13:05he calculated. That is an incredible triumph.
- 13:07But, you know, digging into this reveals a glaring
- 13:09logical problem. Optic energy problem. Yeah.
- 13:12We established that the three metronomes don't
- 13:14change the total amount of sunlight. They just
- 13:16shift it around slightly. It's just a tiny celestial
- 13:18nudge. Right. And a tiny nudge in summer sunlight
- 13:21simply... cannot possess enough raw energy to
- 13:24bury a continent under three kilometers of solid
- 13:26ice. The math doesn't add up. And physics completely
- 13:30agrees with you. The orbital cycles alone are
- 13:33profoundly weak. They might drop the temperature
- 13:35by a fraction of a degree. So how does a fraction
- 13:38of a degree cause an ice age? They require a
- 13:41mechanism to amplify that tiny nudge into a planetary
- 13:45catastrophe. They require climate feedbacks.
- 13:49Feedbacks. We hear this term constantly in modern
- 13:51climate science. Basically, think of it like
- 13:53a microphone and a speaker. Okay. If you whisper
- 13:56into a microphone, the speaker amplifies it.
- 13:58If you put the mic too close, it catches its
- 14:00own amplified whisper, feeds it back in, and
- 14:02suddenly it escalates into a deafening screech.
- 14:05So how does the Earth create a feedback loop
- 14:07like that? The first major amplifier is reflectivity,
- 14:10which scientists call albedo. It's just a measure
- 14:14of how much sunlight a surface bounces back into
- 14:16space. Like wearing a black shirt versus a white
- 14:18shirt on a hot day. Exactly. Dark things like
- 14:21forests or the ocean have low albedo. They absorb
- 14:24heat. White things like snow and ice have high
- 14:27albedo. They act like a giant mirror. Okay, so
- 14:30the celestial metronomes line up, provide a tiny
- 14:33nudge of cooling. A little extra snow survives
- 14:36the summer in Canada. And because that new snow
- 14:38is bright white, it reflects the sun's energy
- 14:41back out into space. That patch of land... isn't
- 14:45absorbing heat anymore. Which makes the surrounding
- 14:47air slightly colder. Yes. Which means the next
- 14:50year, even more snow survives. The white patch
- 14:53grows larger. The mirror gets bigger. Wow. It
- 14:56reflects even more heat away, aggressively dropping
- 14:59the temperature, creating even more ice. The
- 15:02whisper turns into a screech. That is the albedo
- 15:05feedback. But there is a second, far more powerful
- 15:08feedback loop, and it involves the oceans. Okay,
- 15:11how does the ocean fit in? As the planet cools
- 15:13from the ice mirror, the oceans also start to
- 15:16chill. And here's a fundamental law of chemistry.
- 15:19Cold water can hold much more dissolved gas than
- 15:22warm water can. Oh, it's the same reason a warm
- 15:24soda goes flat immediately if you leave it in
- 15:26the sun. But a cold soda kept in the fridge stays
- 15:28fizzy. A perfect analogy. As the global oceans
- 15:31cool, they act like a massive sponge, aggressively
- 15:34pulling carbon dioxide out of the atmosphere
- 15:36and dissolving it into the cold water. But carbon
- 15:39dioxide is a greenhouse gas. It traps heat in
- 15:42the atmosphere. Right. So as the ocean absorbs
- 15:44the CO2 out of the air, the Earth's thermal blanket
- 15:48gets thinner. The atmosphere loses its ability
- 15:51to hold onto heat. The planet plunges into an
- 15:54even deeper freeze, making the ocean even colder,
- 15:56which lets it suck even more CO2 out of the sky.
- 15:59You've got it. So the Earth's orbit is just the
- 16:02person lightly tapping the first domino. But
- 16:05the reflective ice and the CO2 are the actual
- 16:08heavy machinery doing all the physical work of
- 16:11freezing the planet. Exactly. And the ice cores
- 16:13confirm this mechanism with terrifying clarity.
- 16:16Across 800 ,000 years, CO2 and global temperature
- 16:20move in absolute unbroken lockstep. Wow. When
- 16:24CO2 drops, the temperature plummets. When CO2
- 16:27rises, the temperature spikes. Okay, so if the
- 16:30sky controls this whole natural rhythm, it inevitably
- 16:33leads to a massive question about today. I know
- 16:36exactly where you're going with this. Because,
- 16:37I mean, a really common argument is, look, the
- 16:39climate has always changed naturally. You just
- 16:41explain how ice ages come and go based on orbits.
- 16:44So modern warming is just another natural swing,
- 16:46right? It is a totally understandable assumption,
- 16:48honestly, if you only look at half the picture.
- 16:50But when you examine the full ice core record,
- 16:52it completely demolishes that argument. It does.
- 16:55Completely. The history of the ice ages doesn't
- 16:58reassure us that modern warming is natural. It
- 17:01explicitly warns us that it isn't. Let's break
- 17:04down exactly why the ice cores destroy that argument,
- 17:07because this is crucial. Point number one has
- 17:09to be the sheer speed. Speed is the great biological
- 17:12filter. When we look at natural cycles driven
- 17:14by Milankovitch's clockwork, they are agonizingly
- 17:17slow. The transition from a deep freeze to a
- 17:20warm period takes roughly 10 ,000 years. Right,
- 17:23so a forest can't pack up and move. But over
- 17:2610 ,000 years, an ecosystem can slowly migrate
- 17:28further north. Animals have hundreds of generations
- 17:32to evolve and adapt. But the warming we are subjecting
- 17:35the planet to right now is happening over a century
- 17:37or two. We are taking a 10 ,000 year warming
- 17:40phase and compressing it into a single human
- 17:43lifetime. It's dizzyingly fast. By biological
- 17:46standards, it's violently destructive. Ecosystems
- 17:50just cannot migrate or evolve fast enough to
- 17:52keep up. Yeah. And point number two is the actual
- 17:55trend we're supposed to be on right now. Because
- 17:58if we check the three celestial metronomes today,
- 18:00the shape, tilt, and wobble, what are they telling
- 18:03the Earth to do? Well, if humans had never discovered
- 18:06fossil fuels, the natural orbital cycles are
- 18:09currently nudging us gently toward a cooling
- 18:11phase. Wait, we should be cooling right now.
- 18:14Yes. Over the next several thousand years, we
- 18:17should be sliding back toward the next deep freeze.
- 18:20The natural trajectory is cooling, but instead
- 18:23the planet is experiencing explosive warming.
- 18:27So we are literally swimming directly against
- 18:29the astronomical current. We are fighting the
- 18:31sky and we are winning. Which brings us to the
- 18:36third and most critical point, the control knob.
- 18:39The deep past proves beyond any doubt that carbon
- 18:42dioxide is the primary amplifier. It's the master
- 18:45control knob for the global thermostat. And right
- 18:48now, by burning fossil fuels, we've injected
- 18:50massive amounts of it back into the atmosphere.
- 18:52Exactly. The concentration of CO2 has shot higher
- 18:54and faster than anything seen in the entire 800
- 18:58,000 -year ice core record. So we took the microphone,
- 19:01hooked it up to the biggest amp we could find,
- 19:03and cranked the volume dial to 11. Pretty much.
- 19:06The deep past isn't a comforting reassurance
- 19:09that everything is fine. It is the ultimate warning
- 19:12label on the climate machine. It proves that
- 19:14CO2 dictates the temperature. And we're turning
- 19:17that knob harder and faster than nature ever
- 19:20did. Because the fundamental physics haven't
- 19:22changed. The greenhouse effect works exactly
- 19:25the same today as it did 200 ,000 years ago.
- 19:28The only variable that has changed is who is
- 19:31operating the machinery. That is wow. Here's
- 19:35where it gets really profound. The next time
- 19:37you look at a map of the world, I really want
- 19:39you to see the ghosts of the ice. Yeah, those
- 19:41invisible connections. Alright. When you notice
- 19:44that narrow stretch of water between Britain
- 19:46and France or the shallow sea between Alaska
- 19:48and Russia, remember that those maps are temporary.
- 19:52Human beings, people just like us, walked across
- 19:55those gaps on dry land. They live their lives
- 19:58on the edge of a world dictated by the slow ticking
- 20:01of a celestial clock. It's an incredible piece
- 20:04of planetary machinery. It is. And it leaves
- 20:06us with a profound, almost existential reality
- 20:09to mull over. I mean, every empire we've built,
- 20:13every technological leap only exists because
- 20:15the Earth's orbit happened to grant us this brief,
- 20:18fragile window of warmth. So what does it mean
- 20:21for the future of our species now that we have
- 20:23taken the climate control knob out of the hands
- 20:26of the cosmos and put it directly into our own?
- 20:29A heavy but totally essential question to leave
- 20:32lingering in the air. So take a look outside
- 20:34at this rare, beautiful, interglacial world we
- 20:36inherited, and just remember, the massive force
- 20:39is operating out of sight. Thanks for diving
- 20:41deep with us today, and we'll catch you on the
- 20:43next one.