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David Attenborough:
In this series,

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we have explored

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the earth's frozen frontiers.

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We have celebrated
the astonishing variety

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of animals
that are found there...

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And revealed

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the extraordinary ways

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by which they manage to survive.

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At a time when our icecaps
are melting

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faster than ever before...

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We will meet

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the scientists and people
who are dedicating their lives

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to protecting
our frozen planet...

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And striving
to turn things around

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while there is still time
to do so.

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It won't be easy,
but it's doable.

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It's crucial that we try
to understand

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what the impact will be,

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not just for the wildlife
and the people that live there,

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but for you and for me.

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We start our journey
in the high arctic,

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and the vast frozen expanse
of Greenland.

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This huge island is blanketed
by the largest store of ice

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in the northern hemisphere.

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But now it's shrinking.

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Professor alun Hubbard
is a glaciologist

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and he's spent over 30 years

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studying the movement of ice
along Greenland's coastline.

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Alun: It is quite a beast
of a glacier.

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It's just growling constantly.

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Thundenng". In the background.

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Ooh. There we go -
bit of activity.

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Alun: Calving icebergs
is a natural process,

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but what we've seen
in the last 20 years is

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there's been much more melt,

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and much more ice calving off,

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producing huge icebergs...

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So it's quite
an intimidating place

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to be hanging out.

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David: One thing in particular

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has caused this increase
in melting and calving.

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We put this weather station
here in 2010.

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And the hottest temperature
was...

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Two days ago...

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At 22.37 degrees centigrade.

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That is very, very hot
for Greenland.

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David: As the ice falls
into the ocean,

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it raises sea levels globally.

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These are now rising

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by an average
of four millimetres a year.

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A quarter of that comes
from the Greenland ice sheet,

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and scientists fear that this
figure could increase rapidly.

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To investigate, alun has
travelled 70 miles inland

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to the top of the ice sheet,

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where the glaciers start
their lives as compacted snow

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more than a mile thick.

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Here, the effects
of a warming climate

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are only too clear.

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Alun: There are thousands

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of these beautiful
azure-blue lakes

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littered across the surface
of the ice sheet.

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David: The surface has always
melted in the summer,

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but not on this scale...

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And alun wants to know

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what effect the increase
in meltwater

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is having on the ice sheet
as a whole.

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Alun: The sheer quantity
of water...

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Shifting through
this system is crazy!

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David: Powerful torrents of
meltwater are boring shafts -

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known as moulins -
into the ice sheet.

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Alun: This is nuts.

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This is a moulin
actively being formed,

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a moulin in Genesis.

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As we speak,
that water is finding

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the path of least resistance,

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sculpting this shaft
that's going deep into the ice.

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And here it is,

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just toppling
over a waterfall edge

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and dropping into the ice sheet.

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David: But where is
all this meltwater is going?

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And what impact is it having

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on the structure
of the ice sheet?

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To find out,

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alun decides to climb
inside a dried-up moulin.

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Alun: I think I must be
15, 20 metres down here,

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but I'm going to go down
a bit further.

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It's a very narrow shaft here.

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David: It's always been assumed
that the meltwater

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drains straight down and out
of the bottom of the ice sheet,

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but what alun discovers
is very different.

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I can hear

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a big amount of water
moving in this system,

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and the water's starting
to spread sideways, laterally,

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so the drainage system
is obviously complex.

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It's interlinked.

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David: These observations
suggest that the meltwater

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is branching out
in every direction,

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causing this once-rigid
structure to destabilise.

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Whoa.

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It's a bit rotten.

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Everything's rotting here.

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David: The implications
of this are frightening.

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Alun believes that as
the ice sheet begins to thaw,

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it's sliding towards the ocean
at a much faster rate.

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And he's now confirmed that
using time-lapse photography.

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Alun: The ice at the front
can be moving

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in excess of 20 metres a day,
which is fast.

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That is a huge quantity of ice
straight into the ocean.

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David: Some of Greenland's
glaciers are moving

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three times faster today
than they were 30 years ago.

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Alun: As the climate's warming,

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the rate at which
this ice sheet flows

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is absolutely critical.

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80 whereas, at the moment,

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we're thinking
this thing is going to take

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thousands of years to melt
and disintegrate,

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if it does move faster
and accelerate,

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it means centuries.

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That is a really contentious
and very important question -

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because this ice sheet
has enough water in it

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to raise global sea level
by over seven metres,

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and that's a total disaster
for humanity.

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David: Calculations predict

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that nearly half a billion
people

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living in coastal communities
around the world

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will be displaced by flooding
by the end of the century.

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But if the Greenland ice sheet

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slips into the ocean
more rapidly,

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this could all happen
far sooner.

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Greenland isn't the only large
body of ice in the arctic.

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In winter,
the ocean here freezes over,

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creating a cover of ice

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larger than
the entire United States.

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This sea ice has always
got smaller in summer,

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but today it's rapidly
disappearing.

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Hotter temperatures are melting
it at an unprecedented rate...

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With worrying consequences

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for the wildlife
that depends on it.

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For harp seals, the sea ice
is an excellent place

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for giving birth
out of the water.

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It provides the defenceless
newborn pups

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with a safe space
for their first six weeks,

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until they're big enough
to swim proficiently.

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But with the sea ice

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disappearing
increasingly fast...

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Will they be able to adapt?

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Radio: Coastguard 432.

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Coastguard radio.
Coastguard 432. Check out.

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David: In Canada's
Gulf of Saint Lawrence,

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a group of seal biologists
are trying to find out.

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It's a pretty dangerous,
pretty inhospitable place,

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but it's the perfect
environment for these seals

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to spend the first few weeks
of their lives.

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There's a group just down here
to the right now.

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David: But the fragile sea ice
is a challenging place

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in which to work.

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Here... let's go
a little further out.

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David: To support a two-tonne
helicopter, the ice must be

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at least 30 centimetres thick,

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and the only way to find out
if that's so is with a drill.

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It's just not safe here.

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There's a couple
just down here below us now.

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We've got a pretty
short window here.

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David: The team are trying
to discover

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where the seals go
when they become independent.

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So, this is
a juvenile harp seal.

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This is exactly what we've been
out on the ice trying to find.

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Hey, little guy.

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They're absolutely beautiful.

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We'll be putting
a satellite transmitter

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on the top
of this animal's head,

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so that every time the animal
comes to the surface,

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we can get a location estimate
for where he is at sea.

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It won't harm them in any way,
and, in return,

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the amount of information
we get from them is invaluable.

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It'll be really interesting
to see where these animals go

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as the ice starts to break up
over the coming months.

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David: The results
from the study so far

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do not look encouraging.

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Despite migrating
huge distances,

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when the time comes
to have pups of their own,

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harp seals almost always
return to the area

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where they themselves were born.

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But as the sea ice shrinks,

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so does its suitability
as a nursery.

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The problem really comes
about if the only ice available

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in the traditional areas
is very thin.

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They'll still use that ice
and then you get

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an increased mortality.

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David: In short,
the pups risk drowning

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if the ice isn't thick enough.

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And the bigger question is,

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will the ice continue
to exist at all?

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In my lifetime, we've lost
about two-thirds

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of the summer sea ice
in the arctic.

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And it's likely that
in the next 30 years

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we're going to end up with an
ice-free arctic in the summer.

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I think one of the issues
with climate change

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is that it's really difficult
to see.

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But in the case of harp seals,
it's really quite simple.

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If we lose the sea ice
in the arctic,

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we lose the harp seals.

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For harp seals, their future,
it has to be said,

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appears uncertain.

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But what about the most famous
face of climate change -

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the polar bear?

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Can this keenly intelligent
animal

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adapt to
a rapidly changing world?

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As the summer sea ice
melts away,

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many polar bears are forced
to head for dry land.

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Some swim up to 400 miles
to get there.

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This is wrangel,

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a remote island
in arctic Russia.

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David: Without the sea ice, the
hungry bears cannot hunt seals

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and feed on
their calorie-rich flesh,

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but find other sources of food,
including human food supplies.

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Each summer, gennadiy
is joined by polar bear expert

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dr Eric regehr.

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- We need to cross that Ridge.
- Ok.

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David: Eric wants to find out

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just how many bears
are ending up here.

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Eric: In 20 years of studying
polar bears,

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I've never been anywhere
like wrangel island.

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The density of bears is unlike
anything I've ever seen before.

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This past two years,
we've seen about 500 bears.

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My sense is that's just a
fraction of how many are here.

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David: But with so many hungry
animals in one place...

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Is there enough food
to go round?

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Gennadiy, if you can keep
an eye out for us, please,

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like up on the hill

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or just wherever you've got
a good view.

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All right, thank you.

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This is a hair trap.

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So, bears like anything
that smells strong,

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and so this has a little bit
of spoiled cheese,

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milk and fish in it.

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The goal here is to get
a polar bear to come in

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and put its hand or its head
inside this box,

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and when that happens,

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these little wire brushes will
pull out a few pieces of hair

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that we can use
for scientific analysis.

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You can learn a lot
about polar bears

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just from a piece of their hair.

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We can figure out
which individual it is,

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or you can get information
on what they're eating.

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There we go - hair collected.

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David: Eric's molecular studies
of the polar bear's hair

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show that the bears on wrangel

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appear to be finding
enough food.

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But with more and more bears
coming here,

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will there still be enough food
to go round?

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One of the main things
we expect to happen

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with sea ice loss
is changes in the movements

254
00:20:40,320 --> 00:20:42,960
and the distribution
of polar bears, so polar bears

255
00:20:43,080 --> 00:20:45,120
are going to appear in places
they never were before

256
00:20:45,160 --> 00:20:47,441
and they're going to disappear
from places that they were.

257
00:20:54,480 --> 00:20:57,720
David: Some coastal towns
in Siberia

258
00:20:57,840 --> 00:21:01,320
have been overrun
with up to 50 bears at a time.

259
00:21:08,400 --> 00:21:11,360
They are desperate
to eat whatever they can.

260
00:21:13,360 --> 00:21:16,880
And in the city of norilsk,

261
00:21:17,000 --> 00:21:18,600
one female was found

262
00:21:18,720 --> 00:21:21,680
an incredible 250 miles away
from the coast.

263
00:21:27,480 --> 00:21:32,080
Lost and starving,
she was eventually rescued.

264
00:21:34,280 --> 00:21:37,200
But many are not so lucky.

265
00:21:40,200 --> 00:21:42,600
They are intelligent animals,
but there's simply

266
00:21:42,720 --> 00:21:45,360
no food on land
that can compare to the seals

267
00:21:45,480 --> 00:21:47,760
that the bears eat
on the sea ice.

268
00:22:01,800 --> 00:22:06,720
A future without polar bears
would be very sad,

269
00:22:06,840 --> 00:22:10,400
but the sea ice is not just
essential for animals.

270
00:22:11,640 --> 00:22:14,400
It's a lifeline for many
of the four million people

271
00:22:14,520 --> 00:22:17,440
who call the arctic their home.

272
00:22:35,880 --> 00:22:39,320
David: Aleqatsiaq peary
lives in qaanaaq

273
00:22:39,440 --> 00:22:40,920
on Greenland's west coast,

274
00:22:41,040 --> 00:22:44,360
the most northerly inuit town
in the world.

275
00:22:48,000 --> 00:22:52,640
For centuries, life here
has depended on the sea ice.

276
00:23:13,720 --> 00:23:15,160
Not only are dog sleds

277
00:23:15,280 --> 00:23:17,720
a way to reach
neighbouring communities,

278
00:23:17,840 --> 00:23:20,360
which can be over
100 miles away,

279
00:23:20,480 --> 00:23:23,920
but, in a land where
no crops can grow,

280
00:23:24,040 --> 00:23:28,000
travelling over the sea ice
is a vital route to food,

281
00:23:28,120 --> 00:23:29,760
fur and livelihood.

282
00:24:05,560 --> 00:24:08,200
But the dwindling of the sea
ice is making this way of life

283
00:24:08,320 --> 00:24:13,040
not only difficult,
but increasingly dangerous.

284
00:25:03,240 --> 00:25:06,120
Today, they must turn back.

285
00:25:27,760 --> 00:25:31,000
For qaanaaq's 650 residents,

286
00:25:31,120 --> 00:25:36,600
the loss of sea ice is the loss
of an entire way of life,

287
00:25:36,720 --> 00:25:40,040
and it is creating
an uncertain future.

288
00:26:11,440 --> 00:26:13,800
And there's a reason

289
00:26:13,920 --> 00:26:15,880
for this accelerating
rate of change.

290
00:26:19,680 --> 00:26:22,280
In the last 30 years,

291
00:26:22,400 --> 00:26:25,880
over 14 trillion tonnes of ice

292
00:26:26,000 --> 00:26:28,280
have been lost from the arctic,

293
00:26:28,400 --> 00:26:30,560
creating a vicious cycle

294
00:26:30,680 --> 00:26:33,240
of ever-increasing temperatures.

295
00:26:35,360 --> 00:26:36,480
Normally,

296
00:26:36,600 --> 00:26:40,400
large areas of snow and ice
would act as a mirror,

297
00:26:40,520 --> 00:26:46,760
reflecting up to 85% of
the sun's rays back into space.

298
00:26:46,880 --> 00:26:49,240
But as the ice melts,

299
00:26:49,360 --> 00:26:52,640
the great white mirror
is being replaced

300
00:26:52,760 --> 00:26:55,200
by the darkness
of the ice-free ocean.

301
00:26:58,560 --> 00:27:01,240
The dark ocean absorbs
the sun's rays,

302
00:27:01,360 --> 00:27:04,480
so causing even more ice
to melt,

303
00:27:04,600 --> 00:27:09,520
creating a feedback loop that
contributes to further warming.

304
00:27:12,880 --> 00:27:14,360
Because of this,

305
00:27:14,480 --> 00:27:18,040
the arctic is now warming
more than twice as fast

306
00:27:18,160 --> 00:27:20,360
as the earth as a whole.

307
00:27:24,080 --> 00:27:26,840
That has far-reaching
consequences,

308
00:27:26,960 --> 00:27:29,080
not just for the arctic ocean,

309
00:27:29,200 --> 00:27:33,120
but for the vast frozen lands
that surround it -

310
00:27:33,240 --> 00:27:35,120
the tundra.

311
00:27:39,600 --> 00:27:42,440
In summer, the open tundra
provides refuge

312
00:27:42,560 --> 00:27:45,080
for great concentrations
of life.

313
00:27:54,960 --> 00:27:57,680
But today,
its thick surface soil

314
00:27:57,800 --> 00:28:00,560
that has been deeply frozen
for thousands of years

315
00:28:00,680 --> 00:28:02,080
is thawing...

316
00:28:03,800 --> 00:28:07,360
And the pooling water is
creating millions of new lakes.

317
00:28:13,200 --> 00:28:14,840
Katy: Here in Alaska,

318
00:28:14,960 --> 00:28:19,080
we've seen a 40% increase in
the lake area since the '80s.

319
00:28:21,360 --> 00:28:23,800
David: Professor
Katy Walter Anthony

320
00:28:23,920 --> 00:28:26,880
has worked across Alaska
and Siberia

321
00:28:27,000 --> 00:28:28,720
studying their lakes.

322
00:28:28,840 --> 00:28:32,640
She is interested not so much
in the lakes themselves

323
00:28:32,760 --> 00:28:36,120
but in what is seeping out
of them.

324
00:28:36,240 --> 00:28:39,360
We are seeing a bright spot
in the satellite image

325
00:28:39,480 --> 00:28:42,000
that we suspect is gas bubbling.

326
00:28:45,640 --> 00:28:48,640
To identify the gas
in these bubbles,

327
00:28:48,760 --> 00:28:50,960
Katy must collect some of it.

328
00:28:53,160 --> 00:28:57,400
I'm surrounded by tiny bubbles
that are rising.

329
00:28:58,920 --> 00:29:01,520
Methane appears
to be the dominant gas.

330
00:29:04,400 --> 00:29:07,240
David: Methane is produced
by the decaying remains

331
00:29:07,360 --> 00:29:09,040
of prehistoric plants
and animals.

332
00:29:10,320 --> 00:29:13,480
As the frozen soil beneath
the lake starts to thaw,

333
00:29:13,600 --> 00:29:17,920
it releases stores
of this potent greenhouse gas,

334
00:29:18,040 --> 00:29:22,160
which is up to 30 times more
effective than carbon dioxide

335
00:29:22,280 --> 00:29:25,040
when it comes to trapping heat
in the atmosphere

336
00:29:25,160 --> 00:29:27,800
and accelerating global warming.

337
00:29:29,440 --> 00:29:32,640
Katy: 45 parts per million
are these tiny bubbles.

338
00:29:32,760 --> 00:29:34,320
It's rising higher and higher.

339
00:29:34,440 --> 00:29:36,760
Now it's going above 70.

340
00:29:38,680 --> 00:29:41,120
This is a huge amount
of methane.

341
00:29:41,240 --> 00:29:43,560
It could be a mega seep.

342
00:29:47,560 --> 00:29:50,080
Katy: We are discovering
more and more

343
00:29:50,200 --> 00:29:51,960
of these methane mega seeps,
so streaming out

344
00:29:52,080 --> 00:29:53,640
and entering into
the atmosphere.

345
00:30:00,480 --> 00:30:03,840
David: Methane can be seen
escaping from lakes...

346
00:30:07,960 --> 00:30:10,600
But it also rises from the land

347
00:30:10,720 --> 00:30:13,400
wherever the frozen soil,
known as the permafrost,

348
00:30:13,520 --> 00:30:15,960
begins to thaw.

349
00:30:22,680 --> 00:30:26,560
And the arctic tundra is thawing

350
00:30:26,680 --> 00:30:28,400
and collapsing

351
00:30:28,520 --> 00:30:31,440
at an unprecedented rate.

352
00:30:33,480 --> 00:30:36,400
Katy: It's concerning
because permafrost,

353
00:30:36,520 --> 00:30:40,480
or frozen ground,
occupies about a quarter

354
00:30:40,600 --> 00:30:43,600
of the northern hemisphere
land surface.

355
00:30:45,280 --> 00:30:48,040
As permafrost thaws,
if even a small fraction

356
00:30:48,160 --> 00:30:50,720
of that trapped methane
escapes”.

357
00:30:52,200 --> 00:30:55,040
It will accelerate
climate warming...

358
00:30:56,560 --> 00:30:58,600
And you cannot reverse it.

359
00:31:04,560 --> 00:31:07,000
David: It's clear
that in the arctic,

360
00:31:07,120 --> 00:31:09,760
changes to permafrost
on the land

361
00:31:09,880 --> 00:31:12,440
and floating ice on the sea

362
00:31:12,560 --> 00:31:14,760
will have
far-reaching consequences

363
00:31:14,880 --> 00:31:17,960
to the planet as a whole.

364
00:31:19,600 --> 00:31:22,400
And there is nowhere better
to see the extent

365
00:31:22,520 --> 00:31:24,200
of these global changes...

366
00:31:26,480 --> 00:31:28,080
Than from space.

367
00:31:30,960 --> 00:31:33,360
Woman: All of my life,
I've thought about

368
00:31:33,480 --> 00:31:34,920
how this would feel -

369
00:31:35,040 --> 00:31:39,240
to gaze back on the planet
with my own eyes.

370
00:31:39,360 --> 00:31:42,240
David:
NASA scientist Jessica meir

371
00:31:42,360 --> 00:31:44,880
has spent six months in orbit.

372
00:31:45,000 --> 00:31:48,000
Jessica: From the space
station, you have the planet

373
00:31:48,120 --> 00:31:50,080
spinning beneath you,

374
00:31:50,200 --> 00:31:54,520
and you're passing over it
at 17, 500mph.

375
00:31:54,640 --> 00:31:59,120
And we are going around the
entire planet every 90 minutes.

376
00:31:59,240 --> 00:32:03,400
So you can begin to see
larger-scale phenomenon

377
00:32:03,520 --> 00:32:07,360
in ways that you just can't
experience on the ground.

378
00:32:07,480 --> 00:32:12,760
And we can see the change
in these systems over time.

379
00:32:12,880 --> 00:32:15,080
We cannot deny
that we are having

380
00:32:15,200 --> 00:32:17,640
an incredible effect
on the fate of our planet,

381
00:32:17,760 --> 00:32:22,480
and the effect that we have
as humans on our planet.

382
00:32:22,600 --> 00:32:27,280
Right there, actually, I'm
looking down at several fires.

383
00:32:27,400 --> 00:32:30,800
I'm not sure where those are.

384
00:32:30,920 --> 00:32:33,440
Let's take a quick peek.

385
00:32:37,040 --> 00:32:39,000
So, right now
we're flying over Europe

386
00:32:39,120 --> 00:32:42,120
and I can see some fires
over in that direction.

387
00:32:43,680 --> 00:32:45,160
And that is, of course,

388
00:32:45,280 --> 00:32:48,560
something that we have to
contend more and more with,

389
00:32:48,680 --> 00:32:50,840
as our climate changes.

390
00:32:53,120 --> 00:32:54,880
David: As the arctic warms,

391
00:32:55,000 --> 00:32:57,720
wildfires are not only
getting more intense,

392
00:32:57,840 --> 00:32:59,000
but they're breaking out

393
00:32:59,120 --> 00:33:01,480
in parts of
the northern hemisphere

394
00:33:01,600 --> 00:33:03,680
where they have never
occurred before.

395
00:33:16,240 --> 00:33:19,480
Some scientists believe
that unusually warm air

396
00:33:19,600 --> 00:33:21,040
rising in the arctic

397
00:33:21,160 --> 00:33:24,160
is disturbing
high-altitude wind currents,

398
00:33:24,280 --> 00:33:25,920
like the polar jet stream.

399
00:33:27,760 --> 00:33:29,240
Once disturbed,

400
00:33:29,360 --> 00:33:32,320
the jet stream produces
hotter and drier conditions

401
00:33:32,440 --> 00:33:34,080
much further south.

402
00:33:37,240 --> 00:33:41,080
All of these factors
that contribute to wildfires -

403
00:33:41,200 --> 00:33:43,240
the temperature,
the soil moisture,

404
00:33:43,360 --> 00:33:46,080
the presence of trees
and shrubs and other fuel -

405
00:33:46,200 --> 00:33:49,760
have either strong
direct or indirect ties

406
00:33:49,880 --> 00:33:51,520
to climate change.

407
00:33:53,240 --> 00:33:54,840
David: A warming arctic

408
00:33:54,960 --> 00:33:58,320
may not only be responsible for
the outbreak of wildfires...

409
00:34:02,640 --> 00:34:05,600
But it may also be leading
to extreme weather conditions

410
00:34:05,720 --> 00:34:08,640
across the whole of
the northern hemisphere.

411
00:34:12,280 --> 00:34:14,680
I've always cared so much
about the environment

412
00:34:14,800 --> 00:34:17,680
and known that we all need to
do our part in protecting it,

413
00:34:17,800 --> 00:34:21,800
but after seeing this view
with my own eyes,

414
00:34:21,920 --> 00:34:25,240
after seeing all of those
ecosystems from up here,

415
00:34:25,360 --> 00:34:27,720
it really makes it resonate
even more loudly.

416
00:34:37,600 --> 00:34:39,400
David: Outside the arctic,

417
00:34:39,520 --> 00:34:42,440
there's another frozen realm

418
00:34:42,560 --> 00:34:45,600
that stretches across
the world's continents -

419
00:34:45,720 --> 00:34:47,800
our high mountains...

420
00:35:04,480 --> 00:35:07,840
Home to an extraordinary
array of species.

421
00:35:31,960 --> 00:35:34,480
But here, too,
there's a problem.

422
00:35:40,440 --> 00:35:44,040
Across the world, mountain
glaciers which have existed

423
00:35:44,160 --> 00:35:46,320
for tens of thousands of years

424
00:35:46,440 --> 00:35:49,040
are shrinking and vanishing.

425
00:35:59,480 --> 00:36:00,960
By the end of this century,

426
00:36:01,080 --> 00:36:04,480
some ranges may have no ice
remaining at all,

427
00:36:04,600 --> 00:36:09,320
and this will affect not just
animals, but people too.

428
00:36:15,320 --> 00:36:17,840
Hamish: Ice loss
from the mountain glaciers

429
00:36:17,960 --> 00:36:21,080
from the great ranges
of the world

430
00:36:21,200 --> 00:36:24,800
have a huge consequence
for the populations downstream,

431
00:36:24,920 --> 00:36:28,200
and that consequence
is their water supply.

432
00:36:31,440 --> 00:36:33,760
Davi d:
Glaciers in the himalayas

433
00:36:33,880 --> 00:36:37,680
are the source of ten
of the largest rivers in Asia,

434
00:36:37,800 --> 00:36:40,680
which together provide
reliable fresh water

435
00:36:40,800 --> 00:36:43,800
for around a billion people
downstream.

436
00:36:45,320 --> 00:36:47,240
If the glaciers disappear,

437
00:36:47,360 --> 00:36:50,520
so too will the water
they supply.

438
00:36:53,120 --> 00:36:55,800
Hamish: We know that
these glaciers are losing

439
00:36:55,920 --> 00:36:58,560
about half a metre of ice
a year.

440
00:36:58,680 --> 00:37:01,560
What we don't know
is how much ice is left.

441
00:37:03,120 --> 00:37:06,080
So if we know how many metres
of ice are left,

442
00:37:06,200 --> 00:37:07,960
we can work out
how long they'll last,

443
00:37:08,080 --> 00:37:12,080
how long this water supply
will keep going.

444
00:37:13,080 --> 00:37:17,600
David: Dr Hamish pritchard
is part of a team of scientists

445
00:37:17,720 --> 00:37:19,640
who have devised
a new instrument

446
00:37:19,760 --> 00:37:22,760
to measure one of the largest
himalayan glaciers.

447
00:37:24,240 --> 00:37:27,680
What we're putting together
here is a long frame structure,

448
00:37:27,800 --> 00:37:31,400
and it's designed to hang
underneath a helicopter.

449
00:37:31,520 --> 00:37:34,080
We're going to put a radar
on it,

450
00:37:34,200 --> 00:37:37,200
and the radar will send out
the radio waves

451
00:37:37,320 --> 00:37:38,960
and then they'll bounce back

452
00:37:39,080 --> 00:37:40,920
off the bottom of the glacier

453
00:37:41,040 --> 00:37:43,880
and we'll be able to measure
how thick the ice is.

454
00:37:45,160 --> 00:37:47,680
David: Once his team know
how thick the ice is,

455
00:37:47,800 --> 00:37:51,080
they can start to work out
how long it will last.

456
00:37:54,120 --> 00:37:56,240
Yeah, it's a nervous moment.
We're just waiting

457
00:37:56,360 --> 00:37:58,040
for it to get lifted up
for the first time.

458
00:37:58,160 --> 00:38:00,600
We're hoping it's going to be
nice, steady, stable,

459
00:38:00,720 --> 00:38:02,200
a nice easy liftoff.

460
00:38:02,320 --> 00:38:04,120
But we're about to find out.

461
00:38:10,400 --> 00:38:12,040
Radio: Line is clear.

462
00:38:19,280 --> 00:38:20,960
Line is lifting.

463
00:38:33,560 --> 00:38:36,760
Hi, it's Hamish here.
How is it flying?

464
00:38:36,880 --> 00:38:38,936
Radio: Yeah, when the wind
picks up, it's a little...

465
00:38:38,960 --> 00:38:42,200
A little more squirrel/y,
but no problems otherwise.

466
00:38:42,320 --> 00:38:44,920
Yeah, you might want to gain
a little bit of height there.

467
00:38:45,040 --> 00:38:46,200
Yeah, no problem.

468
00:38:48,800 --> 00:38:51,360
Yeah, we'll fly out
and then head towards Everest.

469
00:39:02,840 --> 00:39:05,200
David: After hours of scanning,

470
00:39:05,320 --> 00:39:07,520
the projection
for this particular glacier

471
00:39:07,640 --> 00:39:09,240
is finally revealed.

472
00:39:13,440 --> 00:39:14,960
Yep, that's pretty nice
and clear.

473
00:39:15,080 --> 00:39:17,000
I can see exactly how thick
that ice is.

474
00:39:17,120 --> 00:39:18,680
That's about 150 metres.

475
00:39:21,920 --> 00:39:24,920
So, at the current rate
of melting,

476
00:39:25,040 --> 00:39:28,120
this section would last maybe
200 to 300 years.

477
00:39:28,240 --> 00:39:31,080
But we know that
the melt rates are increasing.

478
00:39:34,480 --> 00:39:36,840
And this is one of
the biggest glaciers,

479
00:39:36,960 --> 00:39:38,816
so there are many, many
glaciers which are much smaller

480
00:39:38,840 --> 00:39:40,480
than this, much thinner ice...

481
00:39:41,600 --> 00:39:42,840
And they're going to be

482
00:39:42,960 --> 00:39:45,520
disappearing much, much earlier
than that.

483
00:39:49,680 --> 00:39:53,160
David: Water is already scarce
in parts of Asia

484
00:39:53,280 --> 00:39:56,760
and as glacial water supplies
dry up,

485
00:39:56,880 --> 00:39:59,560
there will be even less
to go round.

486
00:40:02,880 --> 00:40:05,760
Hamish: So what happens
if these glaciers disappear...

487
00:40:07,800 --> 00:40:10,320
Is that in dry summers
the rivers dry up...

488
00:40:12,760 --> 00:40:14,840
Tensions rise...

489
00:40:14,960 --> 00:40:16,680
Especially between nations

490
00:40:16,800 --> 00:40:18,560
that share water
across borders...

491
00:40:22,480 --> 00:40:25,360
So one of the big risks
of losing this ice

492
00:40:25,480 --> 00:40:28,160
is that it raises
the risk of conflict.

493
00:40:30,840 --> 00:40:33,240
And that's
a frightening prospect.

494
00:40:34,960 --> 00:40:36,480
I have a one-year—old son.

495
00:40:36,600 --> 00:40:39,720
Children born at the same time
as him will see this happen.

496
00:40:44,560 --> 00:40:48,120
We need to act now to turn
those trajectories round.

497
00:40:56,840 --> 00:41:00,080
There's no doubt that
large tracts

498
00:41:00,200 --> 00:41:04,480
of our frozen wilderness are
undergoing dramatic changes.

499
00:41:04,600 --> 00:41:09,880
But what about the largest body
of ice of all - Antarctica?

500
00:41:13,640 --> 00:41:16,440
We have already seen how,
even here,

501
00:41:16,560 --> 00:41:19,520
animals living
around the fringes

502
00:41:19,640 --> 00:41:22,680
are starting to be affected by
climate change -

503
00:41:22,800 --> 00:41:25,240
including chinstrap penguins.

504
00:41:34,600 --> 00:41:37,320
But for another penguin,
the adelie,

505
00:41:37,440 --> 00:41:40,240
the consequences
are even more extreme.

506
00:41:48,840 --> 00:41:53,760
Man: I arrived here
for the first time in 1974.

507
00:41:58,560 --> 00:42:03,640
This part of the world was
just incomprehensibly wild.

508
00:42:06,320 --> 00:42:08,840
It was filled with life.

509
00:42:12,600 --> 00:42:16,960
Antarctica absolutely
captured me.

510
00:42:22,240 --> 00:42:24,120
David: Professor bill Fraser

511
00:42:24,240 --> 00:42:27,400
has dedicated
his entire 45-year career

512
00:42:27,520 --> 00:42:29,920
to studying the adélie penguin.

513
00:42:32,400 --> 00:42:37,040
Bill: What really fascinated me
was the incredible hardiness

514
00:42:37,160 --> 00:42:39,040
of these penguins -

515
00:42:39,160 --> 00:42:42,800
feisty, determined,

516
00:42:42,920 --> 00:42:44,560
beautiful little animal.

517
00:42:51,080 --> 00:42:53,720
But this environment
is changing.

518
00:42:56,080 --> 00:42:58,800
In the last 45 years,

519
00:42:58,920 --> 00:43:01,960
the tremendous warming
that has occurred

520
00:43:02,080 --> 00:43:04,440
has had an incredible impact.

521
00:43:04,560 --> 00:43:07,480
The changes
have been very rapid,

522
00:43:07,600 --> 00:43:10,360
more rapid
than anyone anticipated.

523
00:43:19,360 --> 00:43:22,800
David: Bill has witnessed
first-hand how these changes

524
00:43:22,920 --> 00:43:26,320
have affected one of the
largest colonies of adelies

525
00:43:26,440 --> 00:43:29,240
on the western side
of the antarctic peninsula.

526
00:43:30,920 --> 00:43:37,240
Bill: Four decades ago, this
area contained 20,000 adults.

527
00:43:37,360 --> 00:43:38,760
Currently, we only have

528
00:43:38,880 --> 00:43:41,960
somewhere in the order
of 400 breeding pairs.

529
00:43:43,720 --> 00:43:45,440
One of the issues

530
00:43:45,560 --> 00:43:48,800
that adélies are clearly
experiencing right now

531
00:43:48,920 --> 00:43:50,880
is just the increase
in rainfall.

532
00:43:53,320 --> 00:43:58,560
Adélies are a creature
of the high antarctic.

533
00:43:58,680 --> 00:44:02,960
They evolved
in a dry, cold polar system.

534
00:44:03,080 --> 00:44:07,520
They simply cannot tolerate
being continuously wet.

535
00:44:12,560 --> 00:44:14,560
The chicks are soaking.

536
00:44:16,840 --> 00:44:19,880
The rain is penetrating
their down,

537
00:44:20,000 --> 00:44:24,440
breaking down their ability
to insulate themselves.

538
00:44:26,400 --> 00:44:28,440
That's why you see
they're shivering -

539
00:44:28,560 --> 00:44:31,000
because they're just trying
to maintain

540
00:44:31,120 --> 00:44:33,480
their body temperature,
and they can't.

541
00:44:35,760 --> 00:44:37,240
It's sad.

542
00:44:50,200 --> 00:44:53,160
This tiny chick at this point

543
00:44:53,280 --> 00:44:56,400
has zero chances of surviving.

544
00:44:58,520 --> 00:45:01,280
They can't even react
to the presence of a predator.

545
00:45:13,440 --> 00:45:15,280
We are standing,

546
00:45:15,400 --> 00:45:17,480
looking at climate change

547
00:45:17,600 --> 00:45:21,640
actually killing off
these adélie penguins

548
00:45:21,760 --> 00:45:23,480
one at a time.

549
00:45:42,840 --> 00:45:45,680
David: Before he leaves
Antarctica for the last time,

550
00:45:45,800 --> 00:45:50,400
bill is visiting an island that
was once an adélie paradise.

551
00:45:53,920 --> 00:45:57,000
When we used
to walk onto this island,

552
00:45:57,120 --> 00:46:00,320
you could immediately hear
the adélies.

553
00:46:01,480 --> 00:46:03,080
They were everywhere.

554
00:46:05,640 --> 00:46:09,400
In 1974, the populations here

555
00:46:09,520 --> 00:46:13,560
were somewhere in the order
of 1,000 breeding pairs.

556
00:46:13,680 --> 00:46:17,520
All that remains
are these little pebbles

557
00:46:17,640 --> 00:46:21,040
scattered throughout the area,

558
00:46:21,160 --> 00:46:24,040
stones that were used
in former nest sites.

559
00:46:25,720 --> 00:46:28,880
The pebbles are still visible,
they're very abundant,

560
00:46:29,000 --> 00:46:31,680
but, uh, the birds are gone.

561
00:46:34,600 --> 00:46:36,880
This is where we recorded

562
00:46:37,000 --> 00:46:41,120
the first island-wide
extinction of adélie penguins.

563
00:46:42,840 --> 00:46:49,440
And now the silence that exists
here is pretty overbearing.

564
00:46:51,640 --> 00:46:52,640
Hold it.

565
00:47:10,240 --> 00:47:12,040
There's no...

566
00:47:12,160 --> 00:47:14,840
There's no words that can...

567
00:47:14,960 --> 00:47:19,120
Really describe what
I'm feeling at the moment.

568
00:47:26,280 --> 00:47:28,480
Bill: We're working with
canaries in the coalmine.

569
00:47:30,280 --> 00:47:33,200
Adélie penguins are,
without a doubt,

570
00:47:33,320 --> 00:47:36,400
indicator species
that are telling us

571
00:47:36,520 --> 00:47:38,240
that the globe is changing,

572
00:47:38,360 --> 00:47:40,720
the globe is getting warmer.

573
00:47:40,840 --> 00:47:42,600
It's happening.

574
00:47:42,720 --> 00:47:44,920
And we need to do
something about it.

575
00:47:53,320 --> 00:47:56,240
David: The disappearance
of adélie penguins

576
00:47:56,360 --> 00:47:58,160
along the antarctic peninsula

577
00:47:58,280 --> 00:48:02,120
is just one example of how
record warming temperatures

578
00:48:02,240 --> 00:48:04,840
are affecting life here.

579
00:48:07,640 --> 00:48:10,160
But warming temperatures
are also affecting

580
00:48:10,280 --> 00:48:12,360
the very coastline itself...

581
00:48:13,680 --> 00:48:18,240
With serious implications
for global sea levels.

582
00:48:23,120 --> 00:48:25,720
Man: Across
the glaciological community,

583
00:48:25,840 --> 00:48:29,200
we've identified that sea-level
rise from Antarctica

584
00:48:29,320 --> 00:48:31,320
is the most pressing question

585
00:48:31,440 --> 00:48:33,520
for the next 50 to 100 years.

586
00:48:34,920 --> 00:48:37,840
And we as a collaborative group

587
00:48:37,960 --> 00:48:40,040
have come together
to try and understand it,

588
00:48:40,160 --> 00:48:41,440
and governments

589
00:48:41,560 --> 00:48:43,560
have come together
to try and understand it,

590
00:48:43,680 --> 00:48:46,480
because it's important.

591
00:48:47,960 --> 00:48:50,360
David: Professor
sridhar anandakrishnan

592
00:48:50,480 --> 00:48:52,320
has been working
in the polar regions

593
00:48:52,440 --> 00:48:54,800
for over three decades.

594
00:48:56,160 --> 00:48:59,000
He's part of a team
of scientists undertaking

595
00:48:59,120 --> 00:49:01,400
the largest antarctic expedition

596
00:49:01,520 --> 00:49:03,320
for more than 70 years.

597
00:49:05,720 --> 00:49:09,520
Their destination is a remote
part of western Antarctica

598
00:49:09,640 --> 00:49:12,240
called the thwaites ice shelf.

599
00:49:15,560 --> 00:49:19,160
Sridhar: Without getting out
on the ice, you can't measure

600
00:49:19,280 --> 00:49:21,200
things underneath the ice.

601
00:49:22,320 --> 00:49:23,480
Radio: And take-off.

602
00:49:25,400 --> 00:49:29,400
Sridhar: Those kinds of things
can't be done from space.

603
00:49:29,520 --> 00:49:31,480
They can't be done by drones

604
00:49:31,600 --> 00:49:33,080
or aircraft flying over it.

605
00:49:33,200 --> 00:49:37,120
You actually have to go and put
your instruments on the ice.

606
00:49:43,960 --> 00:49:46,800
David: The interior
of Antarctica is covered

607
00:49:46,920 --> 00:49:48,720
in a giant sheet of ice...

608
00:49:51,160 --> 00:49:52,880
Which for millennia

609
00:49:53,000 --> 00:49:56,080
has been slowly flowing
to the coast.

610
00:50:00,520 --> 00:50:03,120
But because it's so cold here,

611
00:50:03,240 --> 00:50:05,720
rather than calve into the sea,

612
00:50:05,840 --> 00:50:09,320
the ice continues
to flow out into the ocean,

613
00:50:09,440 --> 00:50:13,440
forming a floating platform
known as an ice shelf.

614
00:50:19,120 --> 00:50:24,240
As an ice shelf grows,
it begins to act as a dam,

615
00:50:24,360 --> 00:50:27,040
preventing more
of the ice sheet behind it

616
00:50:27,160 --> 00:50:28,960
from slipping into the sea.

617
00:50:30,800 --> 00:50:33,520
And the thwaites ice shelf

618
00:50:33,640 --> 00:50:35,760
holds back a body of ice

619
00:50:35,880 --> 00:50:37,880
the size of Florida.

620
00:50:40,240 --> 00:50:42,760
But scientists are concerned

621
00:50:42,880 --> 00:50:45,720
that the ice shelf itself
is now at risk of melting.

622
00:50:47,480 --> 00:50:50,680
We're going down
through 600 metres of ice.

623
00:50:50,800 --> 00:50:52,640
Once we drill the hole,

624
00:50:52,760 --> 00:50:55,920
I'm going to put
the explosive charge down.

625
00:50:59,200 --> 00:51:01,640
David: Small seismic surveys...

626
00:51:01,760 --> 00:51:03,480
Ok. Firing the hole.

627
00:51:05,400 --> 00:51:08,160
Help establish
exactly where to sink

628
00:51:08,280 --> 00:51:10,520
their robotic underwater probe,

629
00:51:10,640 --> 00:51:13,560
which the team hope
will record the temperature

630
00:51:13,680 --> 00:51:17,800
of the seawater directly
beneath the ice shelf.

631
00:51:17,920 --> 00:51:19,880
Ok, Andy, ready to descend.

632
00:51:20,000 --> 00:51:22,360
Radio:
Try to go a little slower.

633
00:51:23,960 --> 00:51:25,640
Coming up on 75 metres.

634
00:51:25,760 --> 00:51:27,200
75 metres now.

635
00:51:36,120 --> 00:51:37,720
425 metres.

636
00:51:40,000 --> 00:51:42,640
We've arrived
at the ice-ocean interface.

637
00:51:45,640 --> 00:51:49,240
David: Early results
are not encouraging.

638
00:51:49,360 --> 00:51:51,640
Have we noticed a huge change
in the temperature?

639
00:51:51,760 --> 00:51:55,320
Er, yeah. It is warm water.

640
00:51:55,440 --> 00:51:57,920
Can you see it melt?
Like, what is going on there?

641
00:52:01,160 --> 00:52:03,120
David:
Because of climate change,

642
00:52:03,240 --> 00:52:06,000
warmer seas
directly beneath the ice shelf

643
00:52:06,120 --> 00:52:08,120
are melting it from below...

644
00:52:10,320 --> 00:52:12,200
So it's no longer a question

645
00:52:12,320 --> 00:52:14,520
of if this giant dam
will disappear,

646
00:52:14,640 --> 00:52:16,360
but when.

647
00:52:18,720 --> 00:52:20,400
When the vast ice sheet
behind it

648
00:52:20,520 --> 00:52:22,520
spills into the ocean,

649
00:52:22,640 --> 00:52:25,600
it could have
catastrophic consequences

650
00:52:25,720 --> 00:52:29,280
for global sea levels
over the coming centuries.

651
00:52:33,440 --> 00:52:36,800
Sridhar: The amount of water
that Antarctica contains

652
00:52:36,920 --> 00:52:39,480
that could go into the ocean
is so huge.

653
00:52:42,880 --> 00:52:45,560
This is a global problem.

654
00:52:45,680 --> 00:52:48,680
The oceans are
all connected together,

655
00:52:48,800 --> 00:52:53,520
so as soon as a glacier
puts water into the ocean,

656
00:52:53,640 --> 00:52:55,520
it rises all over the world.

657
00:52:59,160 --> 00:53:01,520
Da vid: If sea levels rise
as predicted,

658
00:53:01,640 --> 00:53:03,640
by the year 2050,

659
00:53:03,760 --> 00:53:09,040
150 million people could be
displaced from coastal areas.

660
00:53:13,760 --> 00:53:15,280
And by 2070,

661
00:53:15,400 --> 00:53:20,560
cities, including Miami,
New York, Shanghai and Mumbai,

662
00:53:20,680 --> 00:53:24,520
will be at risk
of serious flooding.

663
00:53:27,760 --> 00:53:30,720
Sridhar: How much water
will Antarctica contribute

664
00:53:30,840 --> 00:53:32,520
to sea-level rise?

665
00:53:32,640 --> 00:53:34,560
The biggest wildcard
in all of that

666
00:53:34,680 --> 00:53:39,000
is how we as humans
affect climate.

667
00:54:03,840 --> 00:54:09,920
Recently, at cop26,
120 nations came together

668
00:54:10,040 --> 00:54:14,080
in an effort to limit
global warming to 1.5 degrees.

669
00:54:17,360 --> 00:54:19,440
While a 1.5-degree rise

670
00:54:19,560 --> 00:54:22,240
will still bring significant
changes with it,

671
00:54:22,360 --> 00:54:24,000
to stand any chance

672
00:54:24,120 --> 00:54:26,160
of saving what remains
of our frozen planet,

673
00:54:26,280 --> 00:54:27,720
and saving ourselves

674
00:54:27,840 --> 00:54:31,960
from the devastating
consequences of its loss,

675
00:54:32,080 --> 00:54:35,720
we must stick to this
commitment, and honour it,

676
00:54:35,840 --> 00:54:38,520
no matter how challenging
it might be.

677
00:54:39,760 --> 00:54:42,680
James: We know that
climate change is happening.

678
00:54:42,800 --> 00:54:46,360
We know that the main driver
of climate change

679
00:54:46,480 --> 00:54:49,400
is human activities,
it's human emissions.

680
00:54:50,800 --> 00:54:53,520
Jessica:
As a whole human species,

681
00:54:53,640 --> 00:54:55,576
we are not recognising
the impact that we're having

682
00:54:55,600 --> 00:54:57,560
and the fact that
we do need to do something.

683
00:54:58,840 --> 00:55:01,120
Alun: But the important thing
is that

684
00:55:01,240 --> 00:55:05,040
I believe all of these
processes are reversible.

685
00:55:06,280 --> 00:55:08,280
Jessica: If everybody
can make the effort

686
00:55:08,400 --> 00:55:09,560
of doing just one thing -

687
00:55:09,680 --> 00:55:11,840
reducing their carbon footprint.

688
00:55:11,960 --> 00:55:13,320
Alun: Consume less,

689
00:55:13,440 --> 00:55:15,680
think about what we need,
what we really want.

690
00:55:15,800 --> 00:55:19,640
Think more sensibly about
the journeys we take,

691
00:55:19,760 --> 00:55:23,160
about the food we eat,
how that's produced.

692
00:55:23,280 --> 00:55:25,880
Figure out a lifestyle
that is sustainable.

693
00:55:29,720 --> 00:55:31,800
Sridhar:
And we're right at the point

694
00:55:31,920 --> 00:55:37,600
where we can generate
all the power that we need

695
00:55:37,720 --> 00:55:43,240
from renewable sources,
like solar and wind.

696
00:55:44,480 --> 00:55:45,480
To do that,

697
00:55:45,600 --> 00:55:49,360
you need to really transform
society as a whole.

698
00:55:51,200 --> 00:55:53,520
James: We can speak
to our representatives to try

699
00:55:53,640 --> 00:55:55,120
and reconsider energy policies.

700
00:55:57,120 --> 00:55:59,720
If enough of us are educated

701
00:55:59,840 --> 00:56:04,320
about the effects of carbon
in the atmosphere,

702
00:56:04,440 --> 00:56:08,640
even the most poorly educated
politician will respond

703
00:56:08,760 --> 00:56:11,040
to what their citizenry wants.

704
00:56:12,800 --> 00:56:15,680
Hamish: The awareness
and the concern is greater now

705
00:56:15,800 --> 00:56:18,880
than it ever has been,
so that gives us some hope.

706
00:56:20,160 --> 00:56:24,040
It won't be easy,
but it's doable.

707
00:56:25,080 --> 00:56:27,040
Aleqatsiaq: If you can
do something about it,

708
00:56:27,160 --> 00:56:28,160
then do it...

709
00:56:30,040 --> 00:56:32,640
Instead of just
thinking about it.

710
00:56:32,760 --> 00:56:35,320
If you can do something
about it, then do it.

711
00:56:42,800 --> 00:56:44,560
David: We can do it.

712
00:56:45,680 --> 00:56:49,000
It's within our power to do it.

713
00:56:49,120 --> 00:56:51,760
We can do it.

714
00:56:53,120 --> 00:56:55,520
We must do it.

715
00:57:02,000 --> 00:57:05,840
Then there will be
a future for the planet.


