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Speaker 1: Welcome to Thrilling Threads, the show where we pull on

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the most fascinating and sometimes terrifying threads of global knowledge

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and unpack them for you.

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Speaker 2: Today, we are staring down a timeline that feels frankly,

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less like a century long climate projection and more like

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an uncomfortably specific deadline.

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Speaker 1: Yeah, it really does. We're talking about the year twenty

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fifty exactly, and our source material for this deep dive

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focuses on a pretty unnerving premise. Why are so many

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of the world's largest, most vital coastal cities facing this

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existential crisis right now?

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Speaker 3: And why twenty fifty? Why that specific date.

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Speaker 1: Right We often think about the thread as something external,

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you know, rising oceans, melting ice caps, way off in

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the distance. But the surreal reality for people in Maggie

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these areas today is just so much more immediate. You

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wake up, it's a beautiful clear day, no hurricane, no storm,

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and the streets are flooded.

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Speaker 3: Yeah.

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Speaker 1: Our sources put as so simply. They say the ocean

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is just pushing its way inland.

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Speaker 2: That phrase, I think it just captures the shift perfectly

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for Deck. Yes, the warning was always about this gradual

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universal sea level rise, something.

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Speaker 1: That would happen everywhere.

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Speaker 2: Slowly exactly, but now the projections for several major cities

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are incredibly localized and specific. The messages if nothing changes,

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these places fail by twenty fifty.

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Speaker 1: So our mission today is really to unpack that, to

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get into the complex physics that the sources reveal. We

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have to distinguish between that big global factor, the sea

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level rise, and the localized land collapse the subsidence, which is,

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and this is the key part, often entirely human made.

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Speaker 3: That's the core of it.

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Speaker 2: The story isn't just that the water is rising, it's

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that the ground at the same time is falling, and

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in some cases it's falling much much faster.

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Speaker 1: We're basically looking for those surprising insights that explain why

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a city built on say, soft river delta mud like

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New Orleans face is a totally different but just as

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urgent threat as a financial hub sitting on porous sponge

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like rock like Miami.

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Speaker 2: Or a massive city that literally and I mean literally

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durraining itself dry like Jakarta. These local conditions, as you said,

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they're the true accelerators of the crisis.

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Speaker 1: And this isn't just abstract environmental news. I mean, this

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is essential knowledge because we're talking about the foundations of

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global infrastructure.

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Speaker 2: Massive population centers, trillions of dollars in economic activity all

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over the next twenty five years. We're analyzing why some

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of the world's biggest cities are already below sea level

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today and.

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Speaker 1: What happens when the land sinks faster than the sea rises.

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Understanding that dual dynamic, that's the key to the twenty

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fifty line.

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Speaker 2: Okay, So to start, we have to establish the primary

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factor that is catastrophically amplifying the global sea level threat

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for dozens.

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Speaker 1: Of major cities, especially in Asia right.

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Speaker 2: Especially across Asia. The thing is, for many of them,

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it is not the rising ocean that is their biggest

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enemy right now.

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Speaker 1: It's the ground itself.

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Speaker 2: It's the rapid, anthropogenic, so human caused collapse of the

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ground beneath them. In several documented cases, the sources make

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it crystal clear. The land is sinking faster than the

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ocean is rising.

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Speaker 1: That's a true dual calamity. The sea is coming up

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and the city is simultaneously pulling itself down. And nothing

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illustrates this better than Jakarta, the capital of Indonesia. When

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I read the figures on Jakarta, I mean I was

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genuinely shocked by how immediate the problem is. It's not

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a projection, No, this is measured data. It's showing the

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ground in some neighborhoods is dropping by more than ten

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inches per year annually, annually. I mean, can you just

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picture that a foot of land, a foot of concrete

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just sinking every single year. It's almost unbelievable rate of

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land loss.

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Speaker 2: It is an astronomical rate. And the mechanism behind it

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is maybe the most sobering part of this whole story, because,

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like we said, it's completely self inflicted, a side.

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Speaker 1: Effect of failed infrastructure.

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Speaker 2: Exactly. You have to understand a little bit about aquafer mechanics.

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So Jakarta sits on this massive, deep basin of soft alluvial.

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Speaker 3: Soil basically river sediment, river sediment.

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Speaker 2: Yeah, and underneath that soil are these vast aquifers, underground

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reservoirs of water trapped in the rock and sediment.

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Speaker 1: So the water is essentially holding up the ground above it.

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It's like a structural support.

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Speaker 3: It's the structural support.

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Speaker 2: But for decades, because of this massive population boom and

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a public water system that was unreliable, too expensive, or

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just didn't exist in large parts.

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Speaker 3: Of the city.

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Speaker 1: People had to find their own water.

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Speaker 2: They did, residents and businesses, they drilled their own private wells,

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millions of them, and they pulled that water out from

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those deep aquifers. And when you pull the water out,

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the pressure that held the grains of sediment apart just

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dissipates the weight of the city, all the buildings and

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the concrete. It presses down, compacting and crushing those soft

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clay layers.

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Speaker 1: It's like squeezing the water out of a massive sponge.

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That's the perfect analogy it is. And that compaction process,

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over decades, repeated millions of times, resulted in the land

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literally lapsing into the void.

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Speaker 2: And that explains the ten inches per year. It is

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a geological time bomb that was triggered by a failure

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of public works.

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Speaker 1: And the consequence is just staggering. I mean, the sources

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point out that forty percent of Jakarta is already below

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sea level. Right They've built and rebuilt flood walls taller, stronger,

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but the ground underneath the wall just keeps dropping. The

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ocean just finds a way.

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Speaker 2: In you can see this grim history laid out in

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the data. The two thousand and seven flooding.

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Speaker 1: Four hundred thousand people displaced.

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Speaker 2: Then in twenty thirteen, floodwaters reached the presidential palace.

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Speaker 3: I mean, that's not some coastal district. That's a national

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security issue.

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Speaker 1: And then dozens killed in one of the worst floods

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in twenty twenty. I mean, it seems fair to say

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the government's failure to provide reliable pipe water is what

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accelerated this to the point of no return.

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Speaker 2: I think the sources absolutely support that conclusion. It's a

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tragedy rooted in a socioeconomic problem that turned into a

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geological crisis, and.

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Speaker 1: That crisis ultimately led to what is I mean, it's

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arguably the most dramatic urban response to this kind of

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threat in modern history.

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Speaker 3: It really is.

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Speaker 2: The Indonesian government publicly acknowledged that parts of the city

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will become permanently uninhabitable.

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Speaker 1: They just admitted defeat.

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Speaker 2: They did, and that's why they announced the plan to

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move the national capital entirely. They're relocating the heart of

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the nation to a brand new city called New Santara

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on the island of Borneo.

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Speaker 1: Just think about that for a second. That is an

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unprecedented admission of vulnerability, a government choosing to spend what

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potentially thirty five billion dollars a massive sum, to physically

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move the seat of power the historical cultural political center

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of the country, rather than fight a battle they know

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they cannot win. By twenty fifty. That just sets the

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stage for every other city we're going to talk about.

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Speaker 3: It really does.

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Speaker 2: So let's connect that case to others where the soft

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soil plays a role, but maybe the dynamics are a

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bit different.

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Speaker 3: Let's look at Bangkok and Shanghai, Okay.

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Speaker 1: So Bangkok it has a similar profile to Jakarta, at

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least in the early stages, though maybe not quite as extreme.

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It also sits on incredibly soft clay soil sometimes called

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marine clay, and it's sinking for that same combination of reasons.

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Historic groundwater extraction, though that is regulated now.

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Speaker 2: And the sheer weight of its buildings, the non stop construction.

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Speaker 1: Exactly Unlike Jakarta, Bangkok did try to implement pretty stringent

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groundwater regulations and they have slowed the rate of subsidence

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a lot.

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Speaker 2: Which is a success story in its own way.

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Speaker 1: It is, but the pressure is still immense because the

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city's growth just continues, and the construction deep foundations, basement parking,

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all of that adds this colossal weight to that yielding soil, and.

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Speaker 2: The city is just so exposed geographically incredibly.

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Speaker 1: The sources note that parts of the city are already

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less than three feet above sea level. This is not

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a city that needs a hurricane to cause a catastrophic problem.

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Speaker 3: No, it's just a high tide.

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Speaker 1: Just a slightly higher than average high tide, especially during

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monsoon season. The stark warning is that by twenty fifty,

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tidal flooding is going to become routine, even without major storms.

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That makes huge parts of the city just well unusable

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for days at a time.

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Speaker 2: I'm thinking about the catastrophic floods back in twenty eleven

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that shut down global supply chains. That was driven by rainfall,

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but it exposed that fundamental vulnerability it did so.

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Speaker 3: When we contrast this.

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Speaker 2: With Shanghai, we see a city that, because of really

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intense and early regulation starting decades ago, has managed to

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slow its subsidence dramatically from.

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Speaker 1: Fee per decade to millimeters per year.

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Speaker 2: Which shows what's possible with that kind of centralized action.

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But Shanghai's sheer scale magnifies any remaining vulnerability. It's sitting

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on soft sediment near the Yangsee River delta, with.

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Speaker 1: Over twenty five million people.

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Speaker 2: Twenty five million people and just colossal infrastructure right there

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on the coast.

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Speaker 1: So for Shanghai, the threat isn't so much constant sinking anymore.

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It's more about threat amplification during extreme weather like typhoons exactly.

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Speaker 2: The storm surges from typhoons are already severe and getting

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more intense. When you combine that with even a small

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increase in overall water levels, the consequences are disproportionately enormous.

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Speaker 1: The city has invested heavily in defenses though, yeah, massive

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coastal dykes floodgates they have.

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Speaker 2: But the sources caution that the soft foundation, combined with

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that sheer mass of humanity and steel, all sitting right

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on the coast facing the Pacific, it means the safety

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margin is continuously shrinking.

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Speaker 1: So, even with the regulations, that underlying soil of vulnerability

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means that when a big typhoon hits, the city is

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just much more susceptible to catastrophic damage than a city

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built on say, bedrock.

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Speaker 2: The battle is constant, even if they've won that first

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big fight against subsidence.

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Speaker 1: That transition brings us directly to our next big point.

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We need to shift the discussion to cities where geography

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doesn't just make defenses difficult, it dictates the terms. It

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renders standard flood defenses like a simple sea wall, almost useless.

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Speaker 2: And this is where we have to talk about Miami.

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Speaker 1: Miami its threat profile is completely different from Jakarta's.

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Speaker 2: Completely Jakarta is sinking because it's draining its water table.

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Miami is in trouble because it sits on something called

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Kars topography, specifically porous limestone.

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Speaker 1: Okay, let's really unpack that, because this is where the

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physics gets so interesting. Kar's topography means the bedrock is

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basically riddled with holes and cracks, right like.

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Speaker 2: A sponge exactly, The limestone bedrock acts less like a

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solid foundation and more like a colossal, rigid sponge or

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Swiss cheese. Most coastal cities fight the ocean with a

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vertical barrier, a concrete.

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Speaker 1: Wall to keep the water out.

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Speaker 2: To keep the water out, Miami can't rely on that

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because the ocean water moves through the ground itself. Beneath

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the wall around the wall via that porous limestone. It's

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a hydraulic connection that a wall simply cannot break.

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Speaker 1: And I find that mechanism so insidious because it just

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bypasses all our traditional defenses. It's the exact reason for

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that phenomenon they call sunny day flooding. You can build

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the tallest sea wall you can imagine, but on a

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high tide, the ocean level is higher than the city's

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drainage level, so the water doesn't wait for a storm.

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Speaker 2: It just pushes up up through the storm drains, through

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cracks in the sidewalks, right through the foundations of low

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lying buildings. The city floods on a clear day. It's

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geology literally vetoing human engineering.

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Speaker 1: There must be a constant maintenance nightmare too.

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Speaker 2: It is because the water pushing up isn't just fresh water,

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it's saltwater. So you get chronic saltwater intrusion, which contaminates.

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Speaker 1: The fresh groundwater that people rely on.

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Speaker 2: And it rapidly corrodes the subterranean infrastructure, pipes, electrical conduits,

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road foundations.

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Speaker 3: It eats them away from the inside out.

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Speaker 1: And the data just confirms this is getting worse NOAA

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data shows sea levels in South Florida have risen over

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eight inches since nineteen fifty, and that's accelerating. Projections are

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for another ten to seventeen inches by twenty fifty.

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Speaker 2: And you might hear that and think, seventeen inches and

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twenty five years, we.

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Speaker 1: Can manage that, but not in Miami.

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Speaker 2: Not in Miami's geological context, those seventeen inches are catastrophic.

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The sources note that even a a few inches makes

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neighborhoods unlivable.

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Speaker 1: Why just because it increases the frequency that's sunny day

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flooding exponentially.

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Speaker 2: It shifts the high tide mark just enough to make

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what used to be a rare nuisance a chronic, regular

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intrusion that never fully drains away.

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Speaker 1: So by twenty fifty, we're looking at large parts of

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Miami Beach other low lying areas just experiencing chronic flooding,

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not from storms, but from the daily tides.

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Speaker 2: They're deploying massive pumps, they're raising roads, but those pumps

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are fighting a rising water table that is constantly connected

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to the ocean beneath the bedrock. It's a relentless structural challenge.

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Speaker 1: It really is the difference between trying to keep water

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out of a sealed barrel and trying to keep it

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out of a basket made of stone.

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Speaker 3: A perfect way to put it. So.

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Speaker 2: If Miami is fighting porous rock, let's look at New Orleans,

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which is fighting an equally difficult but geologically different battle

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against soft delta sediment.

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Speaker 1: New Orleans is the definition of a survival machine. It's

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famous for its whole ecosystem of levees, pumps, flood walls.

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Without them, much of the city would immediately.

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Speaker 2: Flood because it sits almost entirely below sea level.

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Speaker 1: Right It's built on delta sediment silt, sand clay deposited

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by the Mississippi River over millennia, and that sediment naturally

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compacts over time. The land is inherently designed to sink.

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Speaker 2: But here's the double edged sword of human intervention. The

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Mississippi River used to flood regularly, and when it did,

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it would deposit fresh sediment across the delta.

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Speaker 1: It was rebuilding the land.

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Speaker 2: It was a dynamic, sustainable cycle. The river built the land,

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and the land would slowly sink and the river would

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build it up again.

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Speaker 1: And for decades we've stopped that from happening.

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Speaker 3: Precisely.

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Speaker 2: Decades of intensive river control, These massive levees built to

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prevent flooding and promote shipping, have prevented that fresh sediment

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from reaching the delta. The ground continues to compact, but

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nothing is there to rebuild it.

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Speaker 1: The land is being starved.

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Speaker 3: It's being starved.

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Speaker 2: It's a compound failure of geology and our own infrastructure choices.

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Speaker 1: So if the river is supposed to rebuild the delta,

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why don't we just dredge the sediment that builds up

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further north and I don't know, pipe it back down

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into the wetlands. That seems like a logical engineering fix.

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Speaker 2: And that's a critical question. Engineers have been working on

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that for decades. They are attempting that through these massive,

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multi billion dollar sediment diversion projects.

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Speaker 1: But the scale is the issue.

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Speaker 2: The scale is immense. The amount of sediment needed to

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restore thousands of square miles of disappearing wetlands and counteract

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the sinking is just enormous. Plus diverting it requires making

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deliberate cuts in the levee system, which carries its own risks.

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It's not a quick fix.

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Speaker 1: And we all remember what happened when those defenses failed

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during Hurricane Katrina in two thousand and five that was catastrophic.

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Speaker 2: Eighty percent of the city flooded. Since then, billions have

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been spent on upgrades, creating one of the most sophisticated

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defense systems in the world.

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Speaker 1: But the challenges just keep stacking up.

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Speaker 3: They do.

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Speaker 2: On top of the compaction, sea levels in the Gulf

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of Mexico are rising faster than the global average, and critically,

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those coastal wetlands, the natural storm buffers, they're disappearing at

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an alarming.

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Speaker 1: Rate, which exposes the city even more it does.

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Speaker 2: The projection for twenty fifty is sobering. Without constant upgrades,

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which require continuous funding and political will, parts of New

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Orleans will face chronic flooding even without major hurricanes. The

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city survival is entirely dependent on technology remaining operational two

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hundred and four seven.

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Speaker 1: It's a heroic but just exhausting race against geology, the sea,

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and your own budget.

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Speaker 3: It really is.

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Speaker 1: It's one thing to see these newer cities built on

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soft clay struggle with modern growth. It's another thing, entirely

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to see ancient cities. Metropolis is built to last for millennia,

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now succumbing to this rapid modern environmental change.

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Speaker 2: Yeah, we're talking about places where adaptation has worked for

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a thousand years, but that historical limit has been reached.

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Speaker 1: Yeah, and Venice is the quintessential, just heartbreaking example of that.

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Speaker 3: Absolutely.

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Speaker 2: It was founded over a thousand years ago on a

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shallow lagoon, famously built on millions of wooden piles driven

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into the sediment, and for most of its history it

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survived through remarkable ingenuity and adaptation to the rhythm.

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Speaker 3: Of the tides.

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Speaker 1: But that rhythm, that timeline, it has accelerated past the

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point of sustainability. The city floods during these high tide events,

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called aqua alta. Historically, these were rare, spectacular occurrences.

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Speaker 2: Part of the city's unique character. The sources remind us

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that the massive nineteen sixty six flood was considered a

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once in a century thing. Now similar floods happen multiple

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times in a decade. The character of the city is

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changing from one of romance to one of chronic crisis.

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Speaker 1: That twenty nineteen event was particularly devastating. Water levels reached

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nearly six feet above normal, flooding over eighty percent of

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the city. Saint Mark's Square historic buildings.

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Speaker 2: We saw permanent damage to centuries old structures, widespread electrical failures.

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Speaker 3: The very fabric of the city was at risk.

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Speaker 1: So the city responded with this massive, multi billion dollar project,

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the may Dell Flood Barrier System.

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Speaker 2: It's an incredible feat of engineering designed to physically block

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the lagoon with these massive submerged gates that rise during

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high tides.

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Speaker 1: But it's not a permanent solution, is.

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Speaker 2: It No, because it only addresses the external rising sea,

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not the internal sinking land. Venice has its own subsidence issues,

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and the most system has limits. You can't just use

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it every day.

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Speaker 1: Why not? If it works, why can't they just keep

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it closed?

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Speaker 2: That's the critical compromise. If you seal the lagoon too often,

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you stop the natural tidal fleshing that's essential for cleaning

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the water for the ecosystem. The lagoon becomes stagnant.

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Speaker 4: An ecological choke hold, a different kind of disaster, And

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the models show that by twenty fifty, sea level rise

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combined with subsidence will mean they'd have to operate the

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MOST systems so frequently that the cost, economic and ecological

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become unsustainable.

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Speaker 1: So even with the barriers frequent flooding becomes unavoidable.

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Speaker 2: It does, and the chilling implication here is that parts

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of Venice might still exist, but they'll function more like

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aquarium than a city. They might have to permanently seal

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off entire sections. It's a tragedy where the act of

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preserving its past threatens its future as a living city.

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Speaker 1: From the Adriatic to the Mediterranean, we find another historical

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city facing a crisis that's less about sinking and more

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about literal erosion. You can see happening today Alexandria.

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Speaker 2: Egypt, founded over twenty three hundred years ago by Alexander

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the Great, a crucial center for ancient empires. Today it's

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one of the most threatened coastal cities in the entire

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Middle East.

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Speaker 1: A metropolis of over five million people.

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Speaker 2: And the crisis isn't about projections a generation away. It's

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happening right now. Satellite data shows parts of the coastline

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are eroding rapidly, and the Nile Delta itself is sinking

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for reasons similar to New Orleans. The Aswan High Dam

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traps the silt up river.

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Speaker 1: So we're seeing tangible immediate impacts. Widespread salt water intrusion,

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damaging roads and buildings.

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Speaker 2: Right, and the sources mentioned specific tanable losses. Recent storms

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causing damage that wouldn't have happened decades ago, Collapsed cemeteries,

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beaches that have just vanished. You can literally watch history

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being washed into the sea.

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Speaker 1: The Egyptian government has responded with concrete barriers, but that

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can sometimes just push the problem down the coast accelerate

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erosion elsewhere.

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Speaker 2: Exactly, and as profound as that loss of heritage is,

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we have to pivot to the immense human cost when

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this environmental threat meets explosive population density, the population collision exactly,

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This creates the potential for displacement on a terrifying global scale.

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Speaker 1: Let's start with Manila in the Philippines. This city just

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perfectly encapsulates that collision. It's one of the world's most

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densely populated and flood prone.

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Speaker 2: Cities, and just like Jakarta, the real local crisis is

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the land disappearing from underneath the residence. It's a textbook

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example of subsidence combined with population pressure.

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Speaker 1: We see that groundwater extraction issue again, but just amplified

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by this sheer density. Land has lef towered by several

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feet over the past century.

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Speaker 2: Which means coastal flooding reaches much further inland. It amplifies

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the damage from every single typhoon, every heavy rain.

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Speaker 1: And what does that mean for daily life for the

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thirteen million people in Metro Manila. It's a grim picture.

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Residents using boats on what used to be roads.

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Speaker 2: Schools, closing businesses, shutting down infrastructure, constantly water logged. Their

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lives are functionally defined by the water level. It's not

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an emergency, it's just the baseline reality, and.

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Speaker 1: The twenty fifty projection is a true humanitarian nightmare. The

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models project that parts of Metro Manila will face permanent

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inundation during high tides.

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Speaker 2: Permanent, not just flooded, but permanently underwater during high tides.

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These areas will no longer be functional neighborhoods.

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Speaker 3: They'll be tidal flats.

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Speaker 1: Which raises a huge logistics question. If millions of residents

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are displaced, where do you move them in an already

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densely populated island nation.

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Speaker 2: That is the crucial question, and the answer is rarely

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clean or orderly. This same dynamic applies just as intensely,

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maybe more so, to Lagos Nigeria.

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Speaker 1: What are the fastest growing megacities in the world. Lagos

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is the ultimate collision point of rapid, unmanaged population growth

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and extreme environmental vulnerability.

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Speaker 2: Millions of people in Lagos live in extremely vulnerable, low

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lying coastal areas, massive and formal settlements.

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Speaker 1: And what's crucial here is the interaction between that development

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and the environmental degradation.

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Speaker 2: We have to look at the unintended consequences. Land reclamation

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projects intended to create new, modern, safe areas for business,

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like the Eco Atlantic project, they've actually increased the city's

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risk by altering natural waterflow. When you fill in wetlands

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to build up, you disrupt the natural drainage and storm

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buffer systems for the adjacent areas.

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Speaker 1: So you solve one problem, but you create a new

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and profound one for the older existing.

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Speaker 2: Settlements, precisely a self inflicted risk multiplier, and the most

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vulnerable are those informal settlements built without protection or drainage.

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By twenty fifty, scientists project widespread coastal flooding that will

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displace millions. Lagos is growing at an incredible rate directly

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into the rising water.

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Speaker 1: We've painted a really sobering picture here sinking land, porous rock,

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geopolitical surrender, massive population threats we have. So now let's

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turn to the city that has fought this battle the

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longest and the hardest, the one that provides a benchmark

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for what's possible and crucially, what his limits are. We

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had to discuss Rotterdam.

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Speaker 2: Rotterdam is the ultimate technological fortress. The Netherlands very existence

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is a millennia long fight against the sea. They have

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the most advanced flood defense system in the world, the Delta.

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Speaker 1: Works, including the massive Maizelant Barrier, this huge gait that

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protects Rotterdam by swinging shut across the waterway.

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Speaker 2: This is a city sitting largely below sea level, protected

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by this colossal, multi layered system of barriers, dikes and

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immense pumping stations. Netherlands invests billions every single year just

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to maintain it.

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Speaker 1: They're defining what the peak of human intervention looks like.

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Speaker 2: And yet even here in the best defended place on Earth,

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the engineers themselves acknowledge there are limits. The sources show

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that as sea level rise projections get worse, the pressure

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on these defenses increases.

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Speaker 1: So systems like the Maslond Barrier, which were designed for

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occasional use during a severe storm, may need to operate constantly.

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Speaker 2: By mid century, that shift from occasional defense to constant

477
00:23:28,119 --> 00:23:31,160
life support just fundamentally changes the sustainability equation.

478
00:23:31,359 --> 00:23:33,400
Speaker 1: It becomes chronic maintenance, not preventative.

479
00:23:33,680 --> 00:23:37,359
Speaker 2: Think about the logistical and financial strain running billion dollar

480
00:23:37,440 --> 00:23:42,440
machinery non stop, plus closing a barrier constantly disrupts shipping,

481
00:23:42,640 --> 00:23:44,799
and Rotterdam is one of the busiest ports in Europe.

482
00:23:45,400 --> 00:23:48,440
The defense mechanisms start to undermine the very economy they

483
00:23:48,440 --> 00:23:49,359
were built to protect.

484
00:23:49,640 --> 00:23:52,680
Speaker 1: That's the paradox of Rotterdam. By twenty fifty, the city

485
00:23:52,759 --> 00:23:56,839
is expected to remain standing, but only through extreme, ongoing intervention.

486
00:23:57,400 --> 00:24:01,039
It shows what's physically possible when a wealthy commits vast

487
00:24:01,119 --> 00:24:02,359
resources to the problem.

488
00:24:02,400 --> 00:24:05,000
Speaker 2: But it also shows how fragile even the best defenses

489
00:24:05,039 --> 00:24:07,119
can be and at what cost. It gives us a

490
00:24:07,160 --> 00:24:09,920
price tag, a benchmark for what it takes to defeat

491
00:24:09,960 --> 00:24:11,720
this dual calamity.

492
00:24:11,240 --> 00:24:13,480
Speaker 1: And we have to apply that benchmark to the rest

493
00:24:13,480 --> 00:24:13,960
of the world.

494
00:24:14,039 --> 00:24:17,200
Speaker 2: So if we synthesize everything we've looked at, from Jakarta's

495
00:24:17,279 --> 00:24:21,599
drained aquifers to Miami's porous Rock to Venice's sinking foundations.

496
00:24:21,799 --> 00:24:23,079
Speaker 3: The central theme is clear.

497
00:24:23,240 --> 00:24:24,480
Speaker 1: The threat isn't uniform.

498
00:24:24,759 --> 00:24:27,519
Speaker 2: No, it is defined by a local factor, whether that's

499
00:24:27,559 --> 00:24:31,400
subsidence or geology that dramatically amplifies the global factor of

500
00:24:31,400 --> 00:24:34,119
sea level rise. We have to see twenty fifty not

501
00:24:34,240 --> 00:24:37,240
as a distant projection, but as a hard operational deadline

502
00:24:37,240 --> 00:24:38,799
for adaptation or relocation.

503
00:24:39,200 --> 00:24:42,880
Speaker 1: The timelines are collapsing. We've seen cities where land subsadan's

504
00:24:42,880 --> 00:24:45,799
forced the government to literally move its capital. We've seen

505
00:24:45,839 --> 00:24:50,559
others where survival requires billions in annual investment just to

506
00:24:50,599 --> 00:24:54,000
stay dry. The sheer scale of these interventions is what

507
00:24:54,200 --> 00:24:57,839
must stick with us. The cost is staggering.

508
00:24:57,400 --> 00:25:00,559
Speaker 2: And the Rotterdam case provides the ultimate be benchmark for

509
00:25:00,599 --> 00:25:05,960
survival extreme ongoing intervention. It shows what's possible, but with

510
00:25:06,000 --> 00:25:07,359
an astonishing.

511
00:25:06,799 --> 00:25:09,559
Speaker 1: Resource cost, which brings us to a really provocative thought.

512
00:25:09,880 --> 00:25:12,839
We've seen cities sinking under their own weight, others being

513
00:25:12,839 --> 00:25:15,759
eroded back into the sea. The question is last about

514
00:25:15,920 --> 00:25:18,319
if we can save every threat in city, and more

515
00:25:18,319 --> 00:25:21,680
about who gets that extreme ongoing intervention right.

516
00:25:21,839 --> 00:25:24,680
Speaker 2: Not every nation has the engineering budget of the Netherlands.

517
00:25:24,799 --> 00:25:27,599
Speaker 1: So if you had to globally allocate the billions required

518
00:25:27,599 --> 00:25:30,960
for these constant battles for survival. What measure do you

519
00:25:31,000 --> 00:25:32,440
think should be the deciding factor?

520
00:25:32,559 --> 00:25:36,319
Speaker 2: And that's the difficult choice facing policymakers. Do you prioritize

521
00:25:36,319 --> 00:25:38,680
cities based on the raw speed of the threat, the

522
00:25:38,720 --> 00:25:39,759
subsidence rate.

523
00:25:39,839 --> 00:25:42,640
Speaker 1: Or do you prioritize them based on the scale of

524
00:25:42,680 --> 00:25:46,119
the human impact, the population density, the number of people

525
00:25:46,119 --> 00:25:47,039
who will be displaced?

526
00:25:47,240 --> 00:25:51,119
Speaker 2: Or is it the historical or economic significance of the metropolis.

527
00:25:51,160 --> 00:25:54,119
Speaker 1: We've discussed cities where technology saves them and cities where

528
00:25:54,160 --> 00:25:57,559
the government accepted defeat. If you were in charge of

529
00:25:57,559 --> 00:26:03,400
allocating those billions, what measures sidence rate, population density, historical significance,

530
00:26:03,480 --> 00:26:06,319
or something else entirely do you think should be the

531
00:26:06,359 --> 00:26:09,640
deciding factor in which cities fight for survival by twenty.

532
00:26:09,480 --> 00:26:12,440
Speaker 2: Fifty A difficult question to ponder. Thank you for joining

533
00:26:12,480 --> 00:26:14,680
us on this vital and urgent exploration.

534
00:26:14,799 --> 00:26:16,720
Speaker 1: We'll catch you next time on thrilling Threads.

