Original subtitles

♪ ♪

NARRATOR: What happens when a frozen world locked away for millennia

starts to thaw?

In 2014, a helicopter crew flying over Siberia

discovers something mysterious:

a crater more than 80 feet wide

and deeper than a 15-story building.

Sinkholes are nothing new,

but this is no ordinary sinkhole.

SUSAN NATALI: The ground has exploded.

There's no way... This is not real.

NARRATOR: More Siberian craters have since been discovered.

There's even evidence they may be appearing in Alaska.

TAYLOR SULLIVAN: The lake bottom went from being

flat, flat, flat, and then it just dropped out.

NARRATOR: And they show no sign of stopping.

Now, scientists from around the globe race to understand

a hidden world:

permafrost, a layer of frozen earth

spanning a quarter of the Northern Hemisphere's land mass.

This ancient freezer is beginning to thaw,

revealing its deepest secrets...

Pretty exciting, this is a mammoth bone right here.

NARRATOR: releasing over half a billion tons of carbon every year...

JANELLE SHARP: It was just insane, like, the water

is boiling around you.

NARRATOR: and threatening local communities.

LARS NELSON: Houses need to be torn down.

We're in the middle of a housing crisis.

♪ ♪

NARRATOR: Are the craters warning shots for our climate future?

KATEY WALTER ANTHONY: That is not included in climate models.

That's a scary wildcard in the climate change story.

NARRATOR: What new dangers lurk beneath

this vast frozen landscape?

And could they warm our planet even further?

"Arctic Sinkholes."

Right now, on "NOVA."

♪ ♪

(wildlife chirping, chittering)

NARRATOR: The Yamal peninsula, Siberia.

47,000 square miles of freezing tundra.

♪ ♪

Located in Northern Russia,

the Yamal lies well above the Arctic Circle.

It's home to around 10,000 Indigenous Nenet people,

most living as nomadic reindeer herders.

♪ ♪

In their language, Yamal means "end of the land."

It's now beginning to look like it.

♪ ♪

Giant craters were spotted in the North of Russia.

They popped up out of nowhere in the Yamal peninsula.

NATALI: When I first heard about the crater, I didn't believe it.

I actually thought it was a made-up story.

♪ ♪

MARINA LEIBMAN: Believe me, I remember this date,

and I will remember it forever,

because it was absolutely exciting,

something I have never seen before.

NARRATOR: The mysterious crater is 150 feet deep.

Filled up with rainwater,

its volume is greater than ten Olympic swimming pools.

The striking images go viral worldwide

because no one can answer, what caused it?

♪ ♪

Vasily Bogoyavlensky is an expert

on the geology of the Yamal.

With other scientists, he choppers out to the scene.

♪ ♪

BOGOYAVLENSKY: When we just came to this crater, of course,

we didn't know for sure what was there.

We never saw something like that, never.

♪ ♪

NARRATOR: This isn't the first massive pit to open up.

(people crying out)

♪ ♪

Across the world, gaping sinkholes

have appeared due to water

or erosion weakening the ground beneath,

swallowing cars whole

and wreaking havoc in towns and cities.

But while the Yamal crater looks at first

like an ordinary sinkhole,

there's something unusual visible around the edges.

(Bogoyavlensky speaking Russian)

♪ ♪

NARRATOR: Most sinkholes have a rim that is flat, not raised.

And while sinkholes collapse inwards,

the team discovers debris spread far outside the crater.

Pieces of rocks and ice are flying,

sometimes in quite long distance,

from 200 meters to 500 meters.

And in one case, it was distance to 900 meters.

NARRATOR: Debris like this

can be thrown out by the impact of an asteroid.

But there are no other signs of a massive object

striking Earth.

For the scientists, that leaves only one

reasonable explanation.

A gigantic natural explosion.

NATALI: I don't know if there are many

Earth system processes that have never occurred...

I mean, in my lifetime,

or at least to scientific understanding...

that have never occurred and that we're starting to see

as a new process.

NARRATOR: So what could have provided the power for such a massive blast?

There is no sign of lava or volcanic rock,

so this clearly isn't a volcano.

But exploring inside the crater,

sampling the air and water at the bottom,

the scientists do discover an intriguing clue:

unusually high levels of a single gas, methane.

♪ ♪

Used for cooking and heating,

methane is a flammable gas made from carbon and hydrogen.

(exploding)

When combined with air, it ignites easily.

♪ ♪

BOGOYAVLENSKY: So this is huge bomb.

Methane bomb.

NARRATOR: But before scientists can determine

where the methane came from...

...more giant craters are discovered.

Investigating, scientists find new evidence of methane.

Since 2014, at least eight confirmed craters

have been found on or close to the Yamal.

But the growing number of craters

isn't the scientists' only concern.

They notice a climate connection.

(birds twittering)

2014, when the first crater appears,

followed one of the hottest years on record in Russia.

And all the craters are discovered during a period

of uncharacteristically warm weather in Siberia.

Since the late 19th century, the average global temperature

has risen around two degrees Fahrenheit.

But the Arctic is warming faster.

It's currently heating up around twice as fast

as the rest of the planet.

♪ ♪

The scientists begin to ask:

could the explosive craters be connected to climate change?

If so, what might they be telling us

about Earth's climate future?

♪ ♪

While scientists on the Yamal study the crater,

elsewhere in the Arctic, another team is about to discover

new pieces of the puzzle.

This time, in Alaska.

♪ ♪

Kotzebue, near Alaska's northwest coast.

In 2017, a local pilot reports a lake that's behaving oddly.

Now, a team of scientists

that had been investigating returns to the site

to continue its work.

PHIL HANKE: So we just left Kotzebue,

and then we crossed the Kotzebue Sound,

and into the mouth of the Noatak,

which was this, like, beautiful, sweeping landscape.

SHARP: Look, there's the lake right there!

Man, that's exciting!

♪ ♪

NARRATOR: Far from the nearest town lies Esieh Lake.

Field technician Phil Hanke proceeds cautiously,

hoping to avoid surprises.

Hey, bear!

SHARP: Hey, bear!

HANKE: Hey, bear!

Bear scat.

Well, there's, uh,

definitely bears around here,

so we're going to have to take that into account

when setting up camp.

♪ ♪

NARRATOR: Esieh Lake is located on the lands of

the Indigenous Inupiat people.

The state is home to over 13,000 Inupiaq people,

whose traditional lands stretch across Northern Alaska.

One of the scientists on the team has special ties

to this community.

My name is Janelle Sharp, my Inupiaq name is Anausuk.

My mom is originally from Kotzebue.

My family is from this region.

And so this project is really

special to me, because it's kind of, like,

me coming back to my roots.

♪ ♪

NARRATOR: In 2017, Sharp and other scientists

asked the local community to help them identify

unusual features in the wilderness.

A pilot named Eric Sieh told them that while flying over

the area, he'd spotted something unusual.

♪ ♪

SHARP: If you fly low enough, even from the air,

you can see the bubbling.

♪ ♪

HANKE: It's just mysterious.

It looks like a Jacuzzi.

And so you, you get up to it, and you can hear this...

(imitates bubbling)

Like, the water is boiling around you.

(water bubbling loudly)

♪ ♪

NARRATOR: On their first visit, the team wanted to investigate,

what's causing the bubbles?

SHARP: We took gas samples,

and then those were sent to the lab for analysis,

and they found that it is a super-high amount of methane.

NARRATOR: Methane leaks, known as seeps,

have been found elsewhere in the Arctic.

But they're usually much smaller.

The team's measurements reveal that Esieh Lake is belching out

over ten tons of methane every day.

SULLIVAN: This is the highest flux

methane seep that humans have discovered in the Arctic.

The amount of methane you see is staggering.

♪ ♪

NARRATOR: From the shore, it's difficult to see

where the methane is coming from.

So the team decides to get closer to the source.

SULLIVAN: Hypothermia is obviously the main danger.

Second is me getting air.

I'm very curious about what's down there.

♪ ♪

NARRATOR: Sullivan finds that the lake is shallow... just a few feet deep.

But then, he follows the lake floor

towards the source of the bubbles.

SULLIVAN: I was kicking really hard

to stay down along the bottom,

and I was moving my hands along it.

And it went from this mushy lake bottom

that was flat, flat, flat,

and then it just dropped out.

♪ ♪

SULLIVAN: That gets deep so quickly.

HANKE: Yeah. It's like you're on the bottom,

you're on the bottom, bottom's gone.

NARRATOR: Sullivan finds the methane bubbles are streaming up

from the hole in the lake floor.

SULLIVAN: The bubbling,

it, it sounded like seeping gas,

as if it was even from a propane tank.

♪ ♪

HANKE: How'd it go?

SULLIVAN: Still going down! SHARP: Wow.

(breathing heavily)

NARRATOR: With the lake bottom too dark to see,

the team deploys a sonar scan.

Most of this bed is around three feet deep.

But beneath the streams of bubbles,

the ground abruptly falls away,

at its deepest reaching 50 feet.

Why does a lake floor

otherwise flat and shallow contain such a massive hole?

(rotor blades whirring)

On the Yamal, scientists believe a methane leak

blew out a huge crater.

Esieh Lake is another sign within the Arctic

that beneath the surface, methane is stirring.

So could more craters...

And more methane... Be on the way?

♪ ♪

As well as methane, there's one more clue that links

Esieh Lake and the Yamal craters.

(birds twittering)

Both are located on the same type of frozen terrain:

permafrost.

♪ ♪

Most permafrost is found in the land masses

of high northern latitudes,

including Russia, Canada, and most of Alaska,

Covering an area almost as large as the U.S. and Canada combined.

Permafrost can stretch almost a mile beneath Earth's surface.

It's defined as any ground whose temperature remains at

or below 32 degrees Fahrenheit

for two or more consecutive years.

But it can remain frozen for millennia.

♪ ♪

Recently, rising Arctic temperatures have meant that

in some regions, the permafrost has started to thaw.

(birds twittering)

Just how fast

and the danger this may pose to our climate

is revealed 450 miles from Esieh Lake.

Near the town of Fox, in Interior Alaska,

something strange is happening in the woods.

(birds twittering, branches rustling)

♪ ♪

TOM DOUGLAS: This is what people refer to

as this drunken forest.

You can see a bunch of these have kind of started to go.

They're just having a hard time getting enough rooting in

to grow straight.

NARRATOR: This forest sits on top of permafrost.

Scientist Tom Douglas has been tracking some

surprising changes taking place

as the permafrost starts to thaw.

DOUGLAS: I mean, look at those huge birch trees.

They're literally just

riding down those slopes as it's all degrading.

♪ ♪

I mean, this goes a good 20 or so meters below us.

This is a giant hole.

You can hear water in there. (water rushing)

This whole landscape is just very slowly

sliding downhill with gravity.

♪ ♪

This is a very dramatic

and very rapid change in the landscape here

that, again, we're seeing in a matter of years.

Not decades, not 20 years, not by 2100.

Since 2018.

It's pretty dramatic.

♪ ♪

NARRATOR: This rapid thaw is also affecting human settlements.

Like Utqiagvik, the most northern city

in the United States.

♪ ♪

This entire community sits on top of the Alaskan permafrost.

Locals call it "the top of the world."

♪ ♪

GORDON BROWER: If you point that way,

that's Greenland over there.

Canada is over here.

And that way is, guess what.

(laughing): Russia.

NARRATOR: Gordon Brower

is a Native Alaskan Inupiaq whaling captain.

His people have lived in this region for thousands of years.

BROWER: Communities like these, they're special.

A lot of the cultures in the world

are assimilated, and we're assimilated here,

but we brought our culture and our ways

to the future with us.

And you can come here and still see the same celebration

that took place 10,000 years ago.

♪ ♪

NARRATOR: For five decades, Brower has been hunting in these waters,

part of an ancient Inupiaq tradition of living off the land

and the sea.

We don't have Walmart or we don't have McDonald's up here.

We have other small restaurants

and other things to do like that.

But the majority of food resources

are still hunted today: seals, whales, belugas,

ducks, geese,

caribou, wolves...

All of those are still traded and used.

NARRATOR: With little fresh food available

in winter, generations of Native Alaskans have depended on

cellars carved out of the permafrost.

BROWER: Well, we're in an ice cellar.

My folks used this ice cellar for years and years.

This is where I put a whale

and store it in trust for the community.

NARRATOR: But thawing permafrost means this natural deep freeze

isn't as cold as it used to be.

As Brower discovered.

BROWER: I had checked on the meat and told my brothers,

you know, "We got to pull that meat out.

It's draining, and we don't want that."

I've resorted to pulling a whole whale out of there

and putting it into walk-in freezers.

♪ ♪

NARRATOR: Thawing ice cellars aren't the only threat rising temperatures

pose to this community.

Recently, sea ice that used to protect the shore

from storms has begun to melt.

BROWER: Storm surge is pretty dramatic.

And it's going to

wreak havoc on your coastline here.

And the thing about is, when it's reaching the edge,

a lot of the banks are permafrost-rich,

and it undercuts them.

NARRATOR: Exposed by the storms,

permafrost is thawing and crumbling away.

Now communities like Utqiagvik

are trying to protect their homes.

BROWER: These are all

our local efforts to stop the storm surge.

This is our way of trying to save the town.

NARRATOR: With a retreating coastline

and warming ice cellars,

local communities are hit twice by thawing permafrost.

But the big thaw is an Arctic-wide problem.

NATALI: Through the next decades and century,

we expect anywhere, across the Arctic,

between 30% and 70% of near-surface permafrost

will be lost.

That range partly has to do with just some uncertainty

in the science, but largely has to do with

how much warming will happen in the future.

NARRATOR: Arctic communities are facing the immediate effects now.

But scientists are concerned this loss has implications

for the entire planet.

So why is permafrost thaw so dangerous?

And what is the link to methane?

(birds twittering)

Back near Fox in Interior Alaska,

Tom Douglas is about to do something only possible

in a few places on Earth...

Walk deep down into the permafrost itself.

The Fox permafrost tunnel reveals there's more

to permafrost than frozen earth.

DOUGLAS: That's a horn.

That's from the longhorn steppe bison.

And they are extinct now,

but back 18,000 to 40,000 years ago,

you know, there were steppe bison here.

Pretty exciting,

this is a mammoth bone right here.

You can just see kind of the

piece of it sticking out right there.

It's pretty big.

NARRATOR: The tunnel reveals that permafrost contains

vast quantities of organic matter.

DOUGLAS: So these are,

these are sedges, kind of like grass.

And you can see that they, they're green.

They still have their chlorophyll in 'em.

They're also upside down.

This block fell into a water feature that then froze,

probably 20,000 or so years ago.

♪ ♪

NARRATOR: This ancient organic matter,

like all life on our planet, contains carbon.

(birds twittering)

And is part of a vital Earth system called

the carbon cycle.

♪ ♪

As they grow, plants absorb carbon dioxide.

When they die, they, or the animals that have eaten them,

decompose,

releasing some of this carbon back into the atmosphere.

But in the freezing Arctic,

decomposition happens slowly.

So over millennia,

a huge amount of organic matter became permafrost

before it could decompose,

its carbon frozen in time.

DOUGLAS: In the late '90s into the 2000s,

people start to look at the stocks of carbon in permafrost.

And it's, it's a lot, it's about 1,400 billion metric tons.

It's almost twice as much carbon

as is currently in Earth's atmosphere.

When we walked in, we noted that smell, right?

You're smelling ancient bacteria and carbon being oxidized.

It's almost like a, well, I've heard anything from, like,

a French cheese, to barnyard,

but it's kind of that organic, almost a late fall,

wet leaf kind of organic smell.

You are smelling permafrost carbon being oxidized.

And so the big question

is, that carbon that we smell, that's all over

this tunnel walls,

what's its ultimate fate?

And there's a lot of people working on that.

NARRATOR: In other words, how much of this carbon

will end up in the atmosphere?

And most importantly, how fast?

♪ ♪

Falmouth, Massachusetts.

3,000 miles from the ice tunnel.

Arctic ecologist Susan Natali investigates

samples of permafrost

to find out what happens when it thaws.

NATALI: So these are permafrost cores that were collected

from different locations across Alaska.

Some of these are really dark, like particularly this one.

And that dark color

means that that has a lot of carbon in it.

♪ ♪

NARRATOR: As permafrost warms, its carbon thaws.

And the carbon cycle starts up once again.

So that carbon then is available for microbes to break down.

And they use it for energy and they decompose it.

And in that process, they're releasing

carbon dioxide or methane.

♪ ♪

NARRATOR: Carbon dioxide and methane are both greenhouse gases.

As Earth's surface absorbs energy from the sun,

it radiates some of it back out as heat.

In the atmosphere, greenhouse gases absorb this heat,

radiating part of its energy back at Earth

and heating up our planet.

NATALI: Greenhouse gases are a concern because they trap heat.

They're helpful to us because

they, they make this habitable planet,

but because there's too much in the atmosphere,

they're now making this an unhabitable planet,

or less habitable planet.

♪ ♪

NARRATOR: It's estimated that in the mid-18th century,

there were over 2,000 gigatons of naturally occurring

carbon-based greenhouse gases in the atmosphere.

With industrialization,

human-made greenhouse gas emissions

began to add to this amount.

By 2019, it's estimated the total had risen

to over 3,000 gigatons.

Over the last century and a half,

Earth's average temperature increased around

two degrees Fahrenheit.

♪ ♪

Scientists agree human emissions caused this warming.

But recently, they've become concerned

greenhouse gases being released by permafrost

might be driving temperatures higher, too.

As the name suggests,

permafrost is permanently frozen ground.

So we thought,

"Okay, this carbon is

very stable, so nothing is going to happen."

But as permafrost starts to thaw,

this carbon becomes vulnerable.

NARRATOR: Since the mid-'70s,

carbon dioxide emissions

from the North Alaskan wilderness

have spiked by more than 70%.

But while we know a lot about carbon dioxide,

the impact of another greenhouse gas

coming out of the permafrost is less widely known...

the very one escaping from the Yamal and Esieh Lake,

methane.

Methane is really important,

because it's much more potent

in terms of its ability to trap heat.

So it's about 30 times more powerful than carbon dioxide.

♪ ♪

NARRATOR: Luckily, while carbon dioxide

lasts centuries or longer in our atmosphere,

methane only lasts around 12 years.

But as a far more potent greenhouse gas,

any large-scale increases in methane emissions

have climate scientists seriously concerned.

♪ ♪

For now, more than half of methane emissions

come from human sources like fossil fuels and agriculture,

sources well understood by climate experts.

But scientists are increasingly worried

about methane emissions from permafrost.

So far, they don't know

how much methane the permafrost is releasing.

And that's a big problem.

In order to control our temperature,

we have a certain amount of carbon

that humans can release... That's our carbon budget.

NARRATOR: In 2015,

the international Paris Agreement

set a target for limiting global warming.

Its goal was to keep the temperature rise

to well below two, preferably to 1.5 degrees Celsius.

To stand a good chance

of remaining below the 1.5-degree mark,

one estimate states that humans could release a maximum of

around 460 gigatons more carbon dioxide.

But recent climate calculations are based on computer models

with incomplete information.

LEE: Unfortunately,

a lot of these Earth system models

that contribute to such goals

do not take into account CO2 and methane emissions

from permafrost.

NARRATOR: The most recent carbon budgets

have started to include permafrost carbon.

But some scientists believe they still underestimate

the amount of carbon the warming Arctic will release,

making temperature goals harder to meet

and putting more pressure on societies

to dramatically cut their emissions to compensate.

NATALI: So we think we have

a certain amount of greenhouse gases

that humans can release,

but our target is wrong right now,

because we're not accounting for

potential permafrost emissions

of methane and carbon dioxide.

NARRATOR: Understanding the dynamics of thawing permafrost

is now critical to predicting our climate future.

So how much methane is permafrost emitting each year?

And is this annual amount going to increase?

(dogs yapping)

HANKE: Good dogs!

Straight ahead, on by, on by, on by.

NARRATOR: Fairbanks, Interior Alaska.

Ecologist Katey Walter Anthony

is heading out onto the frozen terrain.

HANKE: Haw! Haw!

Come on, Biggy, come on.

(dogs whining)

NARRATOR: Walter Anthony was

among the first to study Esieh Lake.

She's found concerning evidence

it's not the only lake in the permafrost region

that's releasing methane.

♪ ♪

WALTER ANTHONY: So when you spear the spot,

if I hear gas coming out,

I'm going to try to ignite it.

And if there's fire, we both need to get out of the way.

Okay.

Ready? Yep.

Whoa... (flames roaring)

That got me.

Oh, shoot.

Am I on fire?

No... I was wondering.

(both chuckle)

What's smoking?

(laughing) You okay?

(laughing): Yeah, I'm fine. (laughing)

That was a good one. That was a good one.

All right.

NARRATOR: The methane comes from

organic matter in permafrost thawing and decomposing

at the bottom of the lake,

then rising in methane bubbles to the surface.

Across the Arctic, permafrost thaw

is generating vast numbers of new lakes.

As the soil warms,

ice beneath the surface melts,

causing the ground to slump and fill with water.

And once a lake is formed, you can't stop it,

because that water has heat,

and it causes the ground to thaw so fast.

NARRATOR: The lakes then start releasing methane.

WALTER ANTHONY: As the methane escapes,

it causes more permafrost to thaw,

and more methane to be generated,

which is more warming, and you get what's called

a positive feedback cycle.

NARRATOR: Positive feedback cycles

from permafrost regions

are another scenario not sufficiently accounted for

in current climate models.

LEE: As permafrost thaws,

greenhouse gases like CO2 and methane

will be released back to the atmosphere much faster.

Warming is causing more warming.

NARRATOR: Due to positive feedback, permafrost emissions

could increase the rate of warming,

compounding the need for humans to reduce their emissions

if climate targets are to be met.

But permafrost carbon isn't the only potential driver

of a positive feedback cycle.

Permafrost is actually not the largest carbon reserve

on Earth.

There's much larger carbon reserve

in Earth's crust as fossil carbon.

But we often don't talk about this carbon.

This is because this carbon is considered very stable.

NARRATOR: But some scientists

now wonder if this mega source of carbon

is as stable as they thought.

Disturbing evidence

comes from the bubbles in Esieh Lake.

Methane released by thawing permafrost

has a particular chemical fingerprint.

When the scientists at Esieh Lake

studied the methane in the bubbles,

they discovered it originated deeper inside Earth.

Much deeper.

♪ ♪

Miles beneath the permafrost, deep in Earth's crust,

lie huge fossil methane reservoirs.

While methane from permafrost

comes from organic matter thousands of years old,

fossil methane comes from organisms

that decomposed millions of years ago.

But if it's miles beneath the surface,

how is this methane getting through Earth's crust?

And why here?

Above ground,

the landscape itself gives scientists a clue.

SULLIVAN: Looking up at the peaks around here,

and studying the local geology,

we know that this is

a highly fractured and faulted region.

NARRATOR: As of 2021, Alaska is the most

seismically active state in the U.S.

In the territory close to Esieh Lake,

scientists have discovered a network

of geological fault lines.

Although not on a tectonic plate boundary,

movements of Earth's crust have caused it to crack here.

The closest fault line discovered so far

is fewer than five miles from the lake.

Fault lines make cracks in Earth's crust

through which fossil methane can rise to the surface.

Though it hasn't been confirmed,

the scientists suspect a fault line lies near,

or directly beneath, Esieh Lake.

But if so, there's a mystery.

Seismic evidence from the area suggests

Esieh Lake sits above 500 feet of still-frozen permafrost.

This should form a rock-solid frozen barrier

trapping the fossil methane inside Earth.

So how are these deep stocks of greenhouse gas

breaking through to the surface?

So far, the team's sonar scan

has revealed a 50-foot hole in the lake floor.

But what if they could look deeper,

into the permafrost itself?

Geophysicist Nick Hasson

joins the team, with technology used

by the military.

75 just after the shrub.

HASSON: I'm essentially scanning the permafrost

using a geophysical method called Very Low Frequency.

NARRATOR: Very Low Frequency, or VLF,

measures a special kind of electromagnetic wave

as it moves through Earth.

These waves are sent out globally by the Navy

to communicate with submarines.

But as those waves pass through the Earth below,

Hasson's equipment can pick them up.

By measuring the speed the wave travels,

Hasson can tell whether the ground deep beneath him

is frozen or not.

When it moves through the ground,

if there's permafrost or ice,

these waves are coming up against

a lot of resistance.

But if there's no permafrost or ice,

it quickly moves through.

NARRATOR: If they're strong enough,

the electromagnetic VLF waves

should enable Hasson to see whatever lies beneath the lake.

And so we can scan the Earth similar to how a doctor

scans you with a MRI.

NARRATOR: Esieh Lake is the biggest

on-land methane seep yet found in the Arctic,

but no one has used VLF to look beneath it.

Until now.

HASSON: Wow.

Fantastic signals.

Yeah, so I'm starting to notice a change.

Well, we're over the largest seep,

and there's some sort of large anomaly

happening right here where I'm located.

And the VLF is picking it up.

It's very exciting.

The signals are just outstanding.

♪ ♪

NARRATOR: Back at camp,

Hasson takes the first ever high-resolution glimpse

beneath Esieh Lake.

This slice through 500 feet of ground below the lake

reveals an anomaly.

So the dark blue is the permafrost region.

So anything that's light blue to red is thawed.

And so this shouldn't be here.

There should be permafrost covering this entire area.

But for some reason,

what you can see here is a thaw chimney

going from somewhere below 150 meters

to the surface,

where we see the rising bubbles.

And so this is really unique.

NARRATOR: So far, the scientists have only seen

50 feet beneath the lake.

Now, Hasson's VLF image lets them look ten times deeper.

Below the lake stretches a deep layer of permafrost.

But the scientists now know

this hasn't just thawed at the surface.

Instead, a chimney of material has thawed

right through the frozen permafrost:

a warmer, semi-permeable passageway

through which fossil methane rises to the surface.

So, thawing permafrost means not one,

but two sources of methane for our atmosphere.

As it warms,

permafrost releases its own methane gas.

And as thaw chimneys form within it,

they provide an escape route for fossil methane

that has been safely trapped for millions of years.

Scientists estimate there are around 1.3 trillion tons

of methane stored beneath the Arctic.

That's nearly 250 times as much methane

as there is in Earth's atmosphere today.

So is Esieh Lake's thaw chimney unique?

Or is fossil methane escaping elsewhere?

While the leak in Esieh Lake is unusually large,

smaller seeps of fossil methane

are being discovered across the Arctic.

In Alaska alone, over 70 sites have been found.

♪ ♪

There's no current sign the entire reserve

of fossil methane is moving toward the surface.

But the appearance of even small amounts

of this ancient greenhouse gas has some scientists concerned.

WALTER ANTHONY: If permafrost thawed,

then that's a scary wildcard in the climate change story,

because we think there's a huge amount

of methane and natural gas

trapped inside permafrost and under permafrost.

So if permafrost becomes like Swiss cheese,

with lots of holes in it,

then you can have chimneys where that gas is erupting out.

And that is not included in climate models.

♪ ♪

NARRATOR: If only a tiny fraction

of the fossil reservoirs were to reach the atmosphere,

it could intensify warming,

putting even more pressure on human emissions targets.

How fast that's going to happen

and just how much methane will come out, we don't know.

NARRATOR: Scientists don't currently understand

how fast such a cycle might occur,

or what it would look like.

But there's one place on Earth

that gives a chilling example

of how a human-made permafrost feedback cycle actually works.

Northeast Siberia is home to the Chersky Mountains.

In the 1960s, in a place called Batagaika,

a stretch of forest was cleared to make a road.

Stripped of its tree cover,

the permafrost was exposed to the warming sun.

As it thawed, the ground sank,

pulling down trees at its edge and exposing more permafrost:

a positive feedback cycle.

♪ ♪

Today, the strip of cleared forest

is a depression nearly 300 feet deep

and over half a mile wide.

And it's growing.

Scientists call it a megaslump.

LEIBMAN: Batagaika,

it is very big,

but this, the size is because of the initial human impact.

And this one is already more than one kilometer,

and growing every summer.

NARRATOR: Batagaika reveals how a small human impact

can start a devastating feedback cycle in permafrost.

(birds chirping)

Scientists are now trying to discover

what a feedback cycle

could mean for the entire permafrost region

and whether it could reach a point where it becomes

irreversible.

Such a phenomenon is called a tipping point.

SULLIVAN: A tipping point is

the proverbial straw that broke the camel's back.

You can get away with adding straw for so long,

and then you can't.

And the tipping point is the point of no return.

♪ ♪

NARRATOR: It's a controversial idea among climate scientists.

But the prospect of a tipping point

has been raised for a number of global climate systems,

including Arctic sea ice

and deforestation in the Amazon.

So far, there's no conclusive evidence

that a tipping point is near for permafrost.

However, some scientists believe aspects of the thaw

are now irreversible.

(ground squelching)

Vladimir Romanovsky has spent decades studying

the changing permafrost.

Near Utqiagvik in Northern Alaska,

he investigates

what happens as large wedges of ice in the ground

start to melt.

ROMANOVSKY: Before,

it was more or less flat area,

but then ice melts

and surface subsides.

NARRATOR: Romanovsky believes

lakes formed by melting permafrost ice

have passed a point of no return.

ROMANOVSKY: It took tens of thousands of years

to put this ice into the ground.

Now, it's, it's melting.

To put all this ice into the ground back,

you will need several tens of thousands of years.

So that's, for humans, definitely irreversible process.

It is tipping point.

NARRATOR: While melting ice forms lakes in the wilderness,

just a few miles away, it's causing very different problems

for the local community.

In the roads outside Utqiagvik,

the effects of rising Arctic temperatures

are easy to see.

NELSON: Just from observation, growing up here,

coming out here since I was a kid,

the roads were a lot higher than they are now.

It is literally sinking.

His bumper might get wet.

NARRATOR: Native Alaskan Inupiaq Lars Nelson

is an infrastructure consultant.

He knows firsthand

what permafrost thaw is doing to his community.

NELSON: This road is for subsistence use;

we come out here and stage our hunts.

It's a big part of our history, and it's important that

we're able to access it in case of an emergency.

NARRATOR: And it's not just the roads that are sinking.

In downtown Utqiagvik,

Nelson meets Inupiaq Anthony Edwardsen.

These ones are subsiding, too.

Yeah.

NARRATOR: He's an expert on the Inupiaq community

with four decades' experience in the construction industry.

Yeah, look at... This one is really messed up.

Look at how it's just...

EDWARDSEN: That's where the houses are sinking.

NARRATOR: Local houses are built on wooden pilings.

If they were built on the ground,

the heat used to warm the homes

would thaw the permafrost below.

But now the permafrost is thawing by itself,

and the pilings are starting to sink.

EDWARDSEN: When the piling is a very small base,

it doesn't hold its structure.

The communities,

they need the house leveling,

move houses, houses need to be torn down.

We're in the middle of a housing crisis.

NARRATOR: Nelson believes

strategic building is the answer.

We're on to it right now,

and we're refining it right now.

We can build nice, good, healthy homes.

We just got to pay attention to our foundation,

pay attention to the tundra we're building on more closely.

Because it's such an awesome spot, you know?

It's the top of the world.

♪ ♪

NARRATOR: But as the permafrost continues to thaw,

others in Alaska are looking at more drastic solutions.

GRIFFIN HAGLE: So this is our portable, adjustable,

sled-base home.

It is on a giant steel sled,

as opposed to the pilings.

NARRATOR: C.E.O. of the regional housing authority Griffin Hagle

has a more radical plan for sinking homes.

HAGLE: What we would do if we needed to, to move this,

we would be hooking up our tow chains

to these two attachment points.

We've got one on this side

and one on that corner of the building over there.

Hook that up to a piece of heavy equipment, Caterpillar,

and then drop it off the pads

and basically tow it across the snow

in the wintertime.

♪ ♪

NARRATOR: As temperatures rise,

Hagle is searching for ways

to protect some of the most isolated communities

in the United States.

HAGLE: This is the largest

municipality in the world, I think, by land area.

We provide affordable housing

in eight villages across an area the size of Minnesota,

only without any roads.

NARRATOR: No Alaskan homes have been sledded away,

yet.

But Arctic warming has forced some towns to relocate.

And Hagle thinks houses will soon be on the move.

And there are several, you know, communities,

especially in rural Alaska, Native communities,

that are increasingly at risk of relocation

due to global warming.

And so this gives us an advantage

in having the option, the adaptability,

to move that, that structure if it becomes necessary.

Native people, the Indigenous communities

that have called this place home for thousands of years,

have come up with all sorts of innovations

to make life work here.

So we draw a lot of inspiration from that,

and we see that as kind of the continuation

of a long, long tradition of innovation.

♪ ♪

NARRATOR: As inhabitants across the Arctic

adapt to their changing world,

scientists strive to build a better picture

of our climate future.

The methane craters are just one sign of

a region undergoing unprecedented changes...

...placing communities with deep ties to this land

at risk.

BROWER: We've been whaling here

well over 4,000 years.

(birds cawing)

We've adapted time and time again.

Today, we might not be able to do it by ourselves.

NARRATOR: But the big thaw is not just a regional problem.

What's happening in the Arctic could really affect

everyone on Earth.

NARRATOR: Arctic greenhouse gases

will intensify future global warming.

How quickly is difficult to predict.

And positive feedback cycles

could accelerate beyond human control,

making our choices today even more urgent.

LEE: Because it's very difficult to take control

over the natural systems,

it's even more important for us to lower our emissions.

NATALI: These craters are

a really important and concerning indicator

that things are changing, and the Arctic is melting,

and the Arctic is thawing.

And the future of the Arctic

is a very different place than it was

several decades ago.

♪ ♪

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ANNOUNCER: Episodes of "NOVA" are available with Passport.

This program is also available on Amazon Prime Video.

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