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It's a tornado! | 0:00:02 | 0:00:03 | |
Look at that! | 0:00:04 | 0:00:06 | |
Our planet is home to some spectacular natural wonders. | 0:00:11 | 0:00:15 | |
THUNDERCLAP | 0:00:17 | 0:00:19 | |
Yet exactly how and why they form is still a mystery. | 0:00:19 | 0:00:25 | |
But now, new camera technologies are revealing | 0:00:27 | 0:00:31 | |
their inner workings in stunning detail. | 0:00:31 | 0:00:34 | |
My name is Dr Helen Czerski | 0:00:38 | 0:00:41 | |
and I'll be looking at how these extraordinary images | 0:00:41 | 0:00:44 | |
are transforming our understanding of the natural world. | 0:00:44 | 0:00:49 | |
In this programme, | 0:00:53 | 0:00:54 | |
we reveal the latest scientific insights into icebergs. | 0:00:54 | 0:00:59 | |
Ever since one sank the Titanic, | 0:01:03 | 0:01:05 | |
icebergs have been seen as a menace, a hazard on the polar seas. | 0:01:05 | 0:01:09 | |
But each iceberg is also a beautiful ice sculpture, | 0:01:09 | 0:01:13 | |
with a fascinating history and future all of its own. | 0:01:13 | 0:01:17 | |
Now, side scanning sonar is unveiling | 0:01:20 | 0:01:22 | |
what happens at the edge of glaciers, where icebergs are born. | 0:01:22 | 0:01:26 | |
Satellite images are showing that icebergs create hot spots | 0:01:28 | 0:01:32 | |
for life in the polar seas. | 0:01:32 | 0:01:34 | |
And eyewitness pictures are giving us | 0:01:35 | 0:01:38 | |
a unique glimpse of how icebergs transform over time. | 0:01:38 | 0:01:42 | |
And all these new findings also give us vital clues | 0:01:45 | 0:01:49 | |
about our changing planet. | 0:01:49 | 0:01:51 | |
-Wow! -Oh! | 0:02:17 | 0:02:19 | |
I'm in Greenland to witness one of nature's most violent | 0:02:19 | 0:02:23 | |
and dramatic events - the birth of an iceberg. | 0:02:23 | 0:02:27 | |
Just phenomenal. | 0:02:28 | 0:02:30 | |
Catching on camera 500 million tons of ice | 0:02:30 | 0:02:33 | |
breaking away into the sea, it's an awe-inspiring sight. | 0:02:33 | 0:02:38 | |
Oh, oh! | 0:02:47 | 0:02:49 | |
There's a wave of kind of fractures going along the top end of it, | 0:02:49 | 0:02:53 | |
so all the stuff that WAS the cliff is now just crumbling. | 0:02:53 | 0:02:57 | |
And that's the first time the water in that | 0:03:00 | 0:03:02 | |
has seen the light of day for thousands of years. | 0:03:02 | 0:03:05 | |
In recent years, the number of icebergs | 0:03:08 | 0:03:10 | |
calving from the world's glaciers has been increasing steadily. | 0:03:10 | 0:03:14 | |
Which is why it's never been more important | 0:03:17 | 0:03:20 | |
for scientists to study the birth and life cycle of an iceberg. | 0:03:20 | 0:03:24 | |
Research has shown that 95% of all icebergs in the northern hemisphere | 0:03:33 | 0:03:38 | |
come from one place - Greenland. | 0:03:38 | 0:03:40 | |
It's an island covered by a giant ice sheet, up to 3km thick. | 0:03:46 | 0:03:51 | |
Greenland's many glaciers transport these vast masses of ice | 0:03:59 | 0:04:03 | |
towards the sea, where they pump out 20,000 icebergs every year. | 0:04:03 | 0:04:09 | |
Icebergs aren't just broken chunks of sea ice. | 0:04:10 | 0:04:13 | |
They begin their life in a glacier | 0:04:13 | 0:04:16 | |
and are made from frozen fresh water. | 0:04:16 | 0:04:18 | |
But Greenland's glaciers are dwarfed | 0:04:22 | 0:04:24 | |
by those on the other side of our planet. | 0:04:24 | 0:04:27 | |
90% of the world's freshwater ice can be found here, in Antarctica. | 0:04:27 | 0:04:33 | |
And the glaciers here are where the very biggest icebergs are born. | 0:04:35 | 0:04:39 | |
The largest ice stream in the Western Antarctic | 0:04:42 | 0:04:45 | |
is Pine Island Glacier. | 0:04:45 | 0:04:46 | |
In 2011, NASA scientists noticed a strange feature | 0:04:48 | 0:04:52 | |
across the top of it and here it is. | 0:04:52 | 0:04:54 | |
There's a dark line running all the way through the ice. | 0:04:54 | 0:04:57 | |
And when they went to have a look in a research plane, | 0:04:57 | 0:05:00 | |
they flew across the feature, | 0:05:00 | 0:05:02 | |
taking a photograph every two seconds, | 0:05:02 | 0:05:04 | |
and they stitched together this stunning video. | 0:05:04 | 0:05:07 | |
And you can see that that dark line is actually an ice canyon. | 0:05:07 | 0:05:11 | |
It's 50 metres deep, 70 metres across, | 0:05:11 | 0:05:15 | |
and it zigzags across the ice for 30km. | 0:05:15 | 0:05:19 | |
Scientists knew that such a wide crack wouldn't be able | 0:05:21 | 0:05:24 | |
to hold the ice sheet together for very long | 0:05:24 | 0:05:27 | |
and in 2013, 720 square kilometres of ice broke off... | 0:05:27 | 0:05:33 | |
..creating a gigantic iceberg. | 0:05:35 | 0:05:37 | |
You can see it really clearly here on this satellite sequence. | 0:05:40 | 0:05:43 | |
As time goes on into 2014, | 0:05:43 | 0:05:46 | |
it breaks away and the entire iceberg drifts out into the sea. | 0:05:46 | 0:05:51 | |
It's about 500 metres thick, at this point, | 0:05:51 | 0:05:54 | |
about 30km long and 18km wide. | 0:05:54 | 0:05:57 | |
It's gigantic and it became known as iceberg B31. | 0:05:57 | 0:06:01 | |
Three years on, B31 is still floating in the Southern Ocean, | 0:06:07 | 0:06:11 | |
around Antarctica. | 0:06:11 | 0:06:12 | |
And scientists are monitoring it every step of the way. | 0:06:16 | 0:06:20 | |
They're concerned it could travel as far as the South Atlantic, | 0:06:24 | 0:06:28 | |
posing a threat to shipping lanes. | 0:06:28 | 0:06:30 | |
Like any iceberg, | 0:06:33 | 0:06:34 | |
what you see above the water is only a fraction of what lurks beneath. | 0:06:34 | 0:06:38 | |
One of the reasons that icebergs are so dangerous | 0:06:41 | 0:06:44 | |
is that most of an iceberg is actually below the waterline. | 0:06:44 | 0:06:47 | |
You can see, if I put a big cube of ice into the water, | 0:06:47 | 0:06:51 | |
most of it sits below. | 0:06:51 | 0:06:54 | |
You can see that there's only this tiny bit here, the top 10%, | 0:06:55 | 0:06:59 | |
which is above the waterline. Everything else is down below. | 0:06:59 | 0:07:03 | |
And the reason for this | 0:07:03 | 0:07:04 | |
is all to do with the molecular structure of ice. | 0:07:04 | 0:07:07 | |
The secret lies at the heart of an ice crystal. | 0:07:11 | 0:07:14 | |
It's the way the ice crystal forms which is the key | 0:07:15 | 0:07:18 | |
to why it floats the way it does. | 0:07:18 | 0:07:20 | |
Water molecules are held together by loose bonds | 0:07:26 | 0:07:29 | |
which are constantly breaking and reattaching. | 0:07:29 | 0:07:32 | |
When the temperature drops to zero, these bonds begin to hold, | 0:07:33 | 0:07:37 | |
creating a hexagonal lattice. | 0:07:37 | 0:07:39 | |
In the lattice, the bonds hold the molecules further apart. | 0:07:43 | 0:07:46 | |
It's this opening out that makes ice less dense than liquid water. | 0:07:48 | 0:07:52 | |
But only just. | 0:07:53 | 0:07:55 | |
The density of the water in this tank | 0:07:59 | 0:08:01 | |
is about 1,000 kilograms per cubic metre. | 0:08:01 | 0:08:04 | |
But the density of the ice is less, | 0:08:04 | 0:08:06 | |
it's only about 920 kilograms per cubic metre. | 0:08:06 | 0:08:09 | |
And that's because when the ice froze, it expanded, | 0:08:09 | 0:08:13 | |
so the ice takes up more space. | 0:08:13 | 0:08:15 | |
If this ice cube was to melt completely, | 0:08:15 | 0:08:18 | |
it would only take up exactly the volume of water | 0:08:18 | 0:08:21 | |
that is below the waterline. | 0:08:21 | 0:08:23 | |
And so, all that bit above, that's how much the ice has expanded by. | 0:08:23 | 0:08:27 | |
But it's the 90% of an iceberg below the ocean surface | 0:08:29 | 0:08:32 | |
that worries mariners most. | 0:08:32 | 0:08:34 | |
Since the sinking of the Titanic in 1912, | 0:08:37 | 0:08:41 | |
icebergs have been a major concern for shipping. | 0:08:41 | 0:08:43 | |
-RECORDED FOOTAGE: -'Drifting down from the north, | 0:08:45 | 0:08:47 | |
'after breaking away from a glacier, | 0:08:47 | 0:08:48 | |
'the icebergs making their way towards the shipping lanes, | 0:08:48 | 0:08:51 | |
'become a grave danger to navigation.' | 0:08:51 | 0:08:53 | |
The Titanic collided with an iceberg in Iceberg Alley... | 0:08:54 | 0:08:58 | |
..a now notorious stretch of the North Atlantic, | 0:09:00 | 0:09:03 | |
that sees a high number of icebergs. | 0:09:03 | 0:09:05 | |
'There seems to be plenty of ice about. | 0:09:07 | 0:09:09 | |
'Maybe that's had an effect on our weather over here. | 0:09:09 | 0:09:11 | |
'It felt like it anyway.' | 0:09:11 | 0:09:12 | |
To ensure safe passage through the area, | 0:09:14 | 0:09:17 | |
the International Ice Patrol was set up. | 0:09:17 | 0:09:19 | |
It's purpose? To track icebergs and warn ships. | 0:09:22 | 0:09:26 | |
'Never mind how she got there. She WAS there. | 0:09:26 | 0:09:29 | |
'Something had to be done right away. | 0:09:29 | 0:09:32 | |
In its early years, the Ice Patrol didn't just track icebergs... | 0:09:32 | 0:09:36 | |
EXPLOSION | 0:09:36 | 0:09:39 | |
..they tried to destroy them. | 0:09:39 | 0:09:41 | |
EXPLOSIONS | 0:09:41 | 0:09:43 | |
But the experiments proved unsuccessful | 0:09:44 | 0:09:47 | |
and the Ice Patrol eventually abandoned the project. | 0:09:47 | 0:09:50 | |
Today, the Ice Patrol still monitors the North Atlantic | 0:09:57 | 0:10:00 | |
and warns mariners of dangerous icebergs. | 0:10:00 | 0:10:03 | |
Icebergs may be a threat for some | 0:10:11 | 0:10:14 | |
but, for others, they're veritable treasure troves. | 0:10:14 | 0:10:18 | |
In fact, rather than being inert lumps of ice... | 0:10:18 | 0:10:22 | |
..new research shows that icebergs can transform the oceans. | 0:10:23 | 0:10:27 | |
Jemma Wadham collects samples from the bottom of glaciers | 0:10:35 | 0:10:38 | |
just before they turn into icebergs | 0:10:38 | 0:10:40 | |
and brings them back to this low-temperature facility | 0:10:40 | 0:10:44 | |
here, at the University of Bristol. | 0:10:44 | 0:10:46 | |
So, what we've got here is a large chunk of ice | 0:10:49 | 0:10:52 | |
that we've chain sawed out from the bottom of an ice sheet. | 0:10:52 | 0:10:55 | |
And you can see, very clearly, | 0:10:55 | 0:10:56 | |
there's a very thick band of sediment through the middle | 0:10:56 | 0:11:00 | |
and that sediment will then eventually end up in icebergs | 0:11:00 | 0:11:03 | |
which melt into the ocean. | 0:11:03 | 0:11:05 | |
The sediment is the really interesting bit. | 0:11:05 | 0:11:08 | |
Jemma wants to know which elements are present in the sediment layer. | 0:11:11 | 0:11:15 | |
To analyse it, she first needs to prepare the sample. | 0:11:17 | 0:11:20 | |
When she gets the results, they reveal something extraordinary. | 0:11:24 | 0:11:28 | |
We can see, here, a really nice well-defined bump. | 0:11:32 | 0:11:36 | |
And that bump indicates the presence of iron in our ice samples, | 0:11:36 | 0:11:40 | |
which is really quite astonishing | 0:11:40 | 0:11:41 | |
because you might look at an iceberg sometimes | 0:11:41 | 0:11:43 | |
and think, "There's nothing in it", | 0:11:43 | 0:11:45 | |
but, actually, there's quite a lot of iron. | 0:11:45 | 0:11:47 | |
Iron is a key nutrient for life in the oceans. | 0:11:51 | 0:11:55 | |
But it can't be used by marine life in all of its forms. | 0:11:57 | 0:12:01 | |
The cool thing about icebergs is because they freeze this sediment | 0:12:03 | 0:12:06 | |
into their underbellies, that freezing process preserves the iron. | 0:12:06 | 0:12:11 | |
And as the icebergs move out into the ocean, they melt | 0:12:12 | 0:12:15 | |
and, as they do, that sediment drops out of the iceberg into the ocean | 0:12:15 | 0:12:20 | |
and releases that really nice, tasty iron. | 0:12:20 | 0:12:23 | |
Jemma's research shows that ice can preserve the iron | 0:12:25 | 0:12:28 | |
for thousands of years. | 0:12:28 | 0:12:30 | |
And when an iceberg melts, | 0:12:31 | 0:12:33 | |
it releases the iron into the surrounding oceans. | 0:12:33 | 0:12:36 | |
There, it's used by phytoplankton - tiny floating plants. | 0:12:43 | 0:12:48 | |
Each phytoplankton is scarcely bigger than a speck of dust. | 0:12:49 | 0:12:53 | |
But, ultimately, they feed almost all the life in the sea... | 0:12:55 | 0:13:00 | |
..from tiny fish to the giants of the ocean. | 0:13:01 | 0:13:05 | |
This is a picture created by scientists | 0:13:13 | 0:13:15 | |
at the University of Sheffield. | 0:13:15 | 0:13:18 | |
It's based on satellite images of the ocean around Antarctica | 0:13:18 | 0:13:22 | |
before and after several giant icebergs have passed by. | 0:13:22 | 0:13:26 | |
So, in the wake of this iceberg, | 0:13:27 | 0:13:29 | |
you can see this yellow colour and this red colour, | 0:13:29 | 0:13:32 | |
just is a band in the wake of the iceberg and the surface ocean, | 0:13:32 | 0:13:36 | |
and what that is is satellites, seeing from space, | 0:13:36 | 0:13:40 | |
chlorophyll concentrations in the surface ocean. | 0:13:40 | 0:13:43 | |
Now, chlorophyll is a pigment required for photosynthesis. | 0:13:43 | 0:13:46 | |
The more chlorophyll, the more productive the phytoplankton are | 0:13:46 | 0:13:50 | |
in the surface ocean, so we've got a really nice high productivity band | 0:13:50 | 0:13:53 | |
of phytoplankton here, in the wake of the iceberg. | 0:13:53 | 0:13:57 | |
And it's really fascinating | 0:13:57 | 0:13:59 | |
that they can see the product of the ocean from space. | 0:13:59 | 0:14:02 | |
The oceans flourish in the wake of melting icebergs. | 0:14:04 | 0:14:07 | |
But on their journey through the seas, | 0:14:21 | 0:14:24 | |
icebergs don't simply melt. | 0:14:24 | 0:14:26 | |
They're also battered by collisions with other bergs | 0:14:28 | 0:14:32 | |
and eroded by waves. | 0:14:32 | 0:14:34 | |
And so, over time, | 0:14:36 | 0:14:38 | |
icebergs can take on the most bizarre shapes and forms. | 0:14:38 | 0:14:42 | |
And as they do so, they weaken. | 0:14:44 | 0:14:47 | |
Just occasionally, | 0:14:54 | 0:14:56 | |
there's an iceberg that looks completely different. | 0:14:56 | 0:14:58 | |
This photo was taken by Alex Cornell on a trip to Antarctica in 2014. | 0:15:01 | 0:15:07 | |
What we see here is the iceberg's underside. | 0:15:07 | 0:15:11 | |
Through years of melting and eroding, | 0:15:13 | 0:15:15 | |
its centre of gravity has shifted | 0:15:15 | 0:15:18 | |
and it became so unstable that it rolled over. | 0:15:18 | 0:15:21 | |
This is a spectacular image of a blue iceberg | 0:15:21 | 0:15:25 | |
and its true colour. The ice really is this colour. | 0:15:25 | 0:15:28 | |
It's not often that you see this, | 0:15:28 | 0:15:30 | |
but what's happening is that light comes in from the atmosphere | 0:15:30 | 0:15:34 | |
and, as it travels through the ice, very gradually, | 0:15:34 | 0:15:37 | |
the red light and the green light get absorbed | 0:15:37 | 0:15:39 | |
and by the time the light finds its way back out, | 0:15:39 | 0:15:42 | |
the only colour left is blue. So, this is the true colour of ice. | 0:15:42 | 0:15:46 | |
But that leaves a question, because normally, | 0:15:46 | 0:15:49 | |
when we see icebergs, they look white like this one. | 0:15:49 | 0:15:52 | |
And the reason is all to with a very small structure of the ice. | 0:15:52 | 0:15:56 | |
So, if we look in, zoom in to a small piece of iceberg, | 0:15:56 | 0:16:00 | |
you can see it's full of bubbles here, | 0:16:00 | 0:16:02 | |
because, perhaps thousands of years ago, | 0:16:02 | 0:16:04 | |
layers and layers of snow fell on top of a glacier | 0:16:04 | 0:16:08 | |
until the ice and snow underneath was crushed together. | 0:16:08 | 0:16:11 | |
So, the ice formed a solid block | 0:16:11 | 0:16:13 | |
and the air was squeezed into separate little bubbles. | 0:16:13 | 0:16:16 | |
So, when light hits an iceberg, white light comes in, | 0:16:16 | 0:16:20 | |
it bounces off all these internal surfaces, all the bubbles, | 0:16:20 | 0:16:24 | |
and white light comes back out. | 0:16:24 | 0:16:26 | |
And that's why icebergs look white, | 0:16:26 | 0:16:27 | |
even though the true colour of ice is blue. | 0:16:27 | 0:16:30 | |
Deep in the ice, these air bubbles are gradually squeezed out, | 0:16:32 | 0:16:35 | |
which is why the flipped iceberg looks blue. | 0:16:35 | 0:16:39 | |
But as long as the bubbles are present, icebergs look white, | 0:16:42 | 0:16:46 | |
as do glaciers and ice sheets. | 0:16:46 | 0:16:49 | |
And because they're so bright, | 0:16:51 | 0:16:53 | |
anything that isn't white, really stands out. | 0:16:53 | 0:16:56 | |
That's how Peter Fretwell from the British Antarctic Survey | 0:17:04 | 0:17:07 | |
made a surprising discovery. | 0:17:07 | 0:17:09 | |
He was using satellite images to map the Antarctic coastline, | 0:17:12 | 0:17:15 | |
when he spotted something unusual. | 0:17:15 | 0:17:17 | |
We were mapping Antarctica and the coastline for our pilots, | 0:17:19 | 0:17:22 | |
who need specific information on their maps. | 0:17:22 | 0:17:24 | |
This is a satellite image of Antarctica | 0:17:24 | 0:17:29 | |
and we can see here the coastline, this is the sea. | 0:17:29 | 0:17:32 | |
In between the coastline and the sea, these white areas are sea ice. | 0:17:32 | 0:17:37 | |
And there are some strange brown stains on it | 0:17:37 | 0:17:40 | |
and we weren't sure what these brown stains were. | 0:17:40 | 0:17:43 | |
The sea ice, which is frozen seawater, should be pristine. | 0:17:43 | 0:17:47 | |
It should be pure white. | 0:17:47 | 0:17:49 | |
When we zoomed in with the satellite imagery, | 0:17:49 | 0:17:52 | |
it started to resolve itself as to what these were. | 0:17:52 | 0:17:55 | |
We had brown areas and strange black areas as well there. | 0:17:55 | 0:18:00 | |
And I put two and two together | 0:18:00 | 0:18:02 | |
and realised that what we were looking here, with the satellites, | 0:18:02 | 0:18:05 | |
wasn't just brown stains on the ice. It was actually penguins. | 0:18:05 | 0:18:08 | |
The brown area is the guano, | 0:18:09 | 0:18:12 | |
the stain that they leave on the ice from their droppings and their poo | 0:18:12 | 0:18:17 | |
over the eight months or so that they inhabit this area. | 0:18:17 | 0:18:20 | |
Peter had discovered an emperor penguin colony from space. | 0:18:22 | 0:18:26 | |
At well over one metre, emperors are the tallest penguins on Earth. | 0:18:34 | 0:18:38 | |
They live in large colonies and thrive in freezing conditions. | 0:18:41 | 0:18:45 | |
And they breed in the middle of the harsh Antarctic winter, | 0:18:50 | 0:18:53 | |
using frozen seawater as their breeding platform. | 0:18:53 | 0:18:56 | |
But Peter's most recent satellite images show something unexpected. | 0:19:18 | 0:19:22 | |
We found this colony, one where the penguins weren't on the sea ice. | 0:19:24 | 0:19:28 | |
In this case, they were actually on an iceberg. | 0:19:28 | 0:19:31 | |
Here, we can see a satellite image with a number of icebergs | 0:19:31 | 0:19:34 | |
and one of them is almost totally covered | 0:19:34 | 0:19:37 | |
in brown stain, guano, the penguin poo. | 0:19:37 | 0:19:41 | |
It seems that there wasn't enough sea ice for the emperor penguins | 0:19:42 | 0:19:45 | |
at the beginning of their breeding season. | 0:19:45 | 0:19:48 | |
Early in the season here, the sea ice hasn't formed | 0:19:48 | 0:19:51 | |
when the emperors have turned up at their breeding location. | 0:19:51 | 0:19:54 | |
So, the emperors have been left with nowhere to go, | 0:19:54 | 0:19:56 | |
but in this case, they've moved up onto the iceberg | 0:19:56 | 0:19:59 | |
to give them somewhere to do their courtship | 0:19:59 | 0:20:02 | |
and their mating and their breeding. | 0:20:02 | 0:20:04 | |
Peter has since observed emperors on icebergs in other locations | 0:20:04 | 0:20:09 | |
and it's something that's likely to become even more common | 0:20:09 | 0:20:12 | |
as the climate changes. | 0:20:12 | 0:20:14 | |
We've lost huge amounts of sea ice in the Arctic | 0:20:14 | 0:20:17 | |
as the climate's warmed. | 0:20:17 | 0:20:18 | |
And all of the predictions and the models suggest | 0:20:18 | 0:20:21 | |
that Antarctica will go the same way | 0:20:21 | 0:20:22 | |
and that we could lose lots of sea ice in Antarctica, | 0:20:22 | 0:20:25 | |
which will be terrible for the emperor penguins. | 0:20:25 | 0:20:27 | |
But having this adaptation, to be able to move onto icebergs | 0:20:27 | 0:20:32 | |
or, in some cases, up onto the ice shelf, | 0:20:32 | 0:20:34 | |
will be critically important to be able to save | 0:20:34 | 0:20:37 | |
some of those emperor penguin colonies from extinction. | 0:20:37 | 0:20:40 | |
Climate change isn't just having an effect on sea ice. | 0:20:49 | 0:20:52 | |
It's also affecting the world's glaciers | 0:20:55 | 0:20:57 | |
that are pumping out more icebergs than ever before. | 0:20:57 | 0:21:01 | |
To find out why this is happening, | 0:21:03 | 0:21:05 | |
we need to go dangerously close to the glacier front. | 0:21:05 | 0:21:08 | |
It's all in a day's work for Alun Hubbard | 0:21:11 | 0:21:14 | |
from Aberystwyth University. | 0:21:14 | 0:21:16 | |
Could you go up front and just tell me left or right, please? | 0:21:16 | 0:21:20 | |
On board the research yacht Gambo, | 0:21:23 | 0:21:25 | |
he's trying to map the front of Greenland's Store Glacier. | 0:21:25 | 0:21:29 | |
Alun uses a powerful tool - side scanning sonar. | 0:21:33 | 0:21:36 | |
It reveals the hidden part of a glacier that's under water. | 0:21:36 | 0:21:40 | |
That's the actual equipment | 0:21:41 | 0:21:43 | |
that sends out the sound wave, the acoustic wave, | 0:21:43 | 0:21:46 | |
which bounces off the glacier and we pick it up. | 0:21:46 | 0:21:49 | |
So, we, hopefully, will be able to scan | 0:21:49 | 0:21:51 | |
the whole face of the glacier and its toe. | 0:21:51 | 0:21:54 | |
To get a detailed picture, | 0:21:55 | 0:21:58 | |
Gambo needs to go right up to the ice front, | 0:21:58 | 0:22:00 | |
just where the icebergs calve. | 0:22:00 | 0:22:02 | |
-We are 150 metres now. I would like to keep 200 or 300. -Yeah, OK. | 0:22:05 | 0:22:10 | |
How are we for bergs there? | 0:22:11 | 0:22:14 | |
Have to go a bit starboard, I think. | 0:22:14 | 0:22:16 | |
It's the first attempt by any research team | 0:22:16 | 0:22:20 | |
to image the entire underwater ice front of a glacier as big as this. | 0:22:20 | 0:22:25 | |
But just then, the giant glacier reminds them of the risks. | 0:22:25 | 0:22:29 | |
CREW MEMBERS SHOUT | 0:22:33 | 0:22:36 | |
Back in the UK, Alun has had a chance | 0:23:06 | 0:23:09 | |
to analyse the sonar images from Store Glacier. | 0:23:09 | 0:23:12 | |
This is the result from the side scanning sonar. | 0:23:14 | 0:23:17 | |
We've got the seabed here and this is the glacier front here. | 0:23:17 | 0:23:22 | |
And it shows us that the glacier front is far from a plane | 0:23:22 | 0:23:25 | |
or flat block surface. And this is 5km, so it's a big place. | 0:23:25 | 0:23:30 | |
But what I love here is, all the way along here, | 0:23:30 | 0:23:34 | |
we're getting very obvious undercuts at the base, | 0:23:34 | 0:23:38 | |
where the ice is sitting on the sea floor. | 0:23:38 | 0:23:42 | |
To find out why the glacier front is so undercut, | 0:23:43 | 0:23:46 | |
Alun had to compare scans from several different days | 0:23:46 | 0:23:50 | |
and when he analysed the data, | 0:23:50 | 0:23:53 | |
he discovered that the glacier front is melting at an extraordinary rate. | 0:23:53 | 0:23:58 | |
Here we get submarine melt rates | 0:23:58 | 0:24:01 | |
in excess of four or five metres a day, | 0:24:01 | 0:24:05 | |
which is pretty phenomenal when you think about it. | 0:24:05 | 0:24:08 | |
So, that's actually four metres of ice flowing into that front | 0:24:10 | 0:24:15 | |
every day and it's just being taken away, melted away. | 0:24:15 | 0:24:19 | |
Where that is really focussing is at the base of the glacier | 0:24:19 | 0:24:24 | |
and that's what's leading to these big undercuts | 0:24:24 | 0:24:27 | |
that we're seeing in the front of the glaciers. | 0:24:27 | 0:24:30 | |
It's this submarine melting | 0:24:30 | 0:24:32 | |
that's causing the huge undercut at the bottom of Store Glacier. | 0:24:32 | 0:24:36 | |
We've come to realise that submarine melting | 0:24:36 | 0:24:39 | |
has a really important role to play, in terms of undercutting the glacier | 0:24:39 | 0:24:44 | |
and preconditions the glacier to fail in particular places. | 0:24:44 | 0:24:48 | |
The undercut makes the glacier above unstable, | 0:24:53 | 0:24:56 | |
which is why so many icebergs are calving off it. | 0:24:56 | 0:24:59 | |
And when the underside of an iceberg rises above the ocean's surface, | 0:25:00 | 0:25:04 | |
you can see evidence of submarine melting. | 0:25:04 | 0:25:07 | |
The grooves on this mega berg are caused by it. | 0:25:08 | 0:25:12 | |
The fresh melt water from the base of the iceberg | 0:25:14 | 0:25:16 | |
rushes to the surface because it's less dense than seawater. | 0:25:16 | 0:25:20 | |
And it brings with it the warmer ocean water from the seabed, | 0:25:22 | 0:25:26 | |
creating grooves in the ice as it rises up. | 0:25:26 | 0:25:29 | |
Since the year 2000, the sea temperatures around Greenland | 0:25:47 | 0:25:51 | |
have gone up by one degree, exacerbating submarine melting | 0:25:51 | 0:25:55 | |
and the effect it has on iceberg production. | 0:25:55 | 0:25:58 | |
But the melting doesn't just weaken the glacier. | 0:26:01 | 0:26:04 | |
It leads to an overall loss of ice from the ice sheet. | 0:26:04 | 0:26:07 | |
Climate change, without doubt, | 0:26:10 | 0:26:12 | |
is happening in Greenland and affecting Greenland. | 0:26:12 | 0:26:15 | |
The ice sheet used to be in balance with its climate | 0:26:15 | 0:26:17 | |
just two decades ago. | 0:26:17 | 0:26:19 | |
It's certainly not in balance with its climate at the moment. | 0:26:19 | 0:26:23 | |
The Greenland ice sheet is losing | 0:26:26 | 0:26:28 | |
around 300,000 million tons of ice per year | 0:26:28 | 0:26:33 | |
that's not being replaced by snowfall in the middle, | 0:26:33 | 0:26:37 | |
so it's losing that mass | 0:26:37 | 0:26:38 | |
and that's going into a global sea level rise | 0:26:38 | 0:26:41 | |
which is about a millimetre per year. | 0:26:41 | 0:26:43 | |
So, Greenland's the largest contributor | 0:26:43 | 0:26:45 | |
to global sea level rise - | 0:26:45 | 0:26:47 | |
much greater than all of Antarctica put together. | 0:26:47 | 0:26:50 | |
The Arctic and the Antarctic are covered in and shaped by ice. | 0:26:54 | 0:26:58 | |
We see ice as harsh and unyielding, | 0:26:58 | 0:27:01 | |
but these frozen places are particularly sensitive | 0:27:01 | 0:27:04 | |
to warming temperatures. | 0:27:04 | 0:27:06 | |
Although the polar regions are remote, | 0:27:06 | 0:27:08 | |
they're an important part of the Earth's system, | 0:27:08 | 0:27:10 | |
linked into all our lives, | 0:27:10 | 0:27:13 | |
so what happens at the poles affects all of us, no matter where we live. | 0:27:13 | 0:27:17 | |
In recent years, new camera technologies have allowed us | 0:27:30 | 0:27:34 | |
to get closer to icebergs than ever before. | 0:27:34 | 0:27:36 | |
We now have a much greater understanding | 0:27:43 | 0:27:45 | |
of the complex processes that lead to the birth of an iceberg... | 0:27:45 | 0:27:49 | |
..determine its life cycle... | 0:27:53 | 0:27:55 | |
..and how it can transform the surrounding polar seas. | 0:27:59 | 0:28:03 | |
And the study of icebergs is also giving us an important insight | 0:28:17 | 0:28:22 | |
into how climate change is affecting our planet. | 0:28:22 | 0:28:25 |