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This white wilderness, this emptiness is the North Pole. I'm
standing in the middle of a frozen ocean. Beneath my feet
and for over 500 miles in every direction there are several
meters of ice. But something significant is likely to happen
here at the North Pole soon. Chances are that sometime
within the next few decades, perhaps even as soon as 2020,
there will be open water here for the first time in human recorded history.
The Arctic and Antarctic are changing. Enormous masses
of ice that have been frozen for thousands of years are
breaking apart and melting away.
Ice scientists are going to extremes to find out exactly
what's going on. For them, these are exciting times. But the
transformation that's being seen here will be felt far beyond the polar wilderness.
In this program, I'll be trying to understand what these
changes mean not just to the wildlife and people that live
around the poles, but to the whole planet.
I'm starting my journey in the Arctic, the far north of our planet.
It's still very cold outside by most people's standards, but
the Arctic has been warming fast, twice as fast as the rest
of our planet. My first mission is to find out what effect
that's having on the animals, although first we have to find
them. It's April in Svalbard. We're a thousand miles north
the Arctic Circle in search of the region's top predator.
We need to travel away from the land and out over the frozen sea.
Over there.
I'm with a Norwegian team which is giving the
polar bears of Svalbard their yearly health check.
She's under us now. Come round for a clean shot.
The team works together to give an anesthetic injection from
a dart gun without hurting the bear. It takes tremendous
skill.
Nobody likes to see a magnificent animal like a polar bear
lolling about unconscious on the ice, but it's only by
darting them in this way and keeping check on them year
after year that we can be sure that we know what is
happening to them and the population of polar bears as a
whole. Over the last 30 years, many teams have been seeing
the condition of their local bears deteriorate,
although not every bear is suffering.
How much? 96 here. And 102 here. 197. Is that good? It's not
too bad. It's a bit above our reach, so she's a bear in a
good condition for Svalbard to be. The trouble is that if
this was underweight, she would be in trouble, not only from
our own point of view, but from the point of view of
our cubs, because an underweight female gives birth to
underweight cubs and underweight cubs have a great
problem of surviving their difficult first year in these
circumstances. It can be minus 40 degrees centigrade when
polar bear cubs emerge at the start of the Arctic spring
from their dens where they were born.
This mother hasn't eaten for half a year. She and her cubs
need to fatten up fast over the next few months and their
chances of survival depend on what's happening beneath their feet.
These polar bears aren't walking on land. They're
roaming across the frozen surface of the sea.
And the bear's food lives under the ice.
Ring seals are hunted by polar bears. In fact, in some
parts polar bears eat almost nothing else, so it's fairly
understandable that this little mother ring seal is
looking at me now. She should be a little apprehensive.
That pup of hers is only about three or four days old and
the pup won't be able to swim for another two or three days.
Seals have good reason to be nervous around their holes.
They need the holes to breathe when the sea is frozen, but
this makes them easy to find.
Polar bears can sniff out seal holes even if they're covered in snow.
Spring is the best hunting season.
This mother's found a food store under the snow that was
probably made by an Arctic fox. It's a time of plenty now,
but the bear family need to make the best of it
because the good times are about to come to an end.
As the weather warms, the ice beneath the bear's feet starts
to break up and then melt. And as the ice dwindles, so do
the bear's chances of a successful hunt.
Most of the ice is lost over the shallow
coastal waters where most of the seals live.
It's now summer and these bears have a choice. Take their
chances on the shrinking ice floes or make for the safety of
the land.
It's a case of sink or swim.
Bears have always gone hungry in the summer, but the length
of time when there's enough ice for them to go hunting is
getting shorter and shorter across much of the Arctic.
This is hitting cubs particularly hard because they can't
survive for as long without feeding as their mother. Cubs
that were born underweight are at the greatest risk.
This mother and her cubs may well not get another chance at
hunting, but they do have a meal until the sea freezes again
in winter. There's not much to eat on land and the fact is
that the longer the cubs have to wait until the ice returns,
the more likely they are to die.
Longer summers with no ice are probably the main
reason why many polar bear populations are dropping.
To help monitor bears into the future, this female is
being fitted with a radio collar to track her movements.
It's an extraordinary sensation to be so close to such a
powerful animal with luck carrying that collar. She will
have more years to go yet and be telling us a great deal
about herself and the rest of the race of polar bears as
they face this very uncertain future.
The future of the ice cover on the sea isn't just an issue
for the animals. It's a big concern for the people who live
in the Arctic and travel across the ice every day.
David Ikakwalu is an Inuit from the village of Clyde River in the Canadian Far North.
There are very few roads up here so David and his community
like most Inuit people have always traveled across the
frozen sea.
Dog sleds are the safest way to get around because the
dogs feel thin ice underfoot and won't lead travelers into
trouble.
Old timers like David know the ice as we know the streets in our local neighborhood.
Every spring cracks have always formed in the same places
at the same time. It's going to be big very soon after two
weeks maybe. We'll be more open. But now cracks are
appearing where they never did before so David and his
friend Laimiki have taken on a new job. They are using
special GPS units to record the position of new cracks or
weak ice.
These findings will be used by locals for their own safety
but they're also being studied by ice scientists who want to
predict how the ice will change in years to come.
The Inuit are keen to know what the future holds too because
they've seen with their own eyes the changes that the
scientists have seen from space. This satellite photo from
1980 shows the Arctic Ocean at the end of the summer when
ice cover is at its minimum. Since then there's been a 30%
drop in the area covered by ice. But these images can't tell
us about changes to the most important factor, the thickness of the ice.
Measuring thickness across the whole ocean was beyond
scientists for many years until help came from an unexpected
source.
The Arctic Ocean is of huge military importance as it's
the shortest route between North America and Russia.
Since the late 1950s, British, US and Russian
submarines have been patrolling the Arctic Ocean.
But as well as looking out for enemy activity, they've
also been measuring the thickness of the ice, critical when
looking for a place to surface.
When scientists got permission to look at the submarine
crew's records, they discovered that the ice has been
thinning fast. In fact, it's nearly halved in thickness since 1980.
Across most of the Arctic Ocean there are now just a couple of meters of ice.
It's so thin that it could melt away almost entirely in the
summertime and that includes the ice at the North Pole. If
current trends continue then there will be an open ocean
here by summer's end sometime within the next few decades.
So the days of the Arctic Ocean being covered by a
continuous sheet of ice seem to be past. Whether or not
that's a good or bad thing, of course, depends on your point of view.
Nobody has had a better view of the changes to the Arctic
Ocean than the people of Barrow, the most northerly town in
Alaska. The people here have always survived by hunting on
the frozen sea and they celebrate this at a festival every
year. The blanket toss was once the best way to spot distant
animals to hunt, as lifelong resident Lewis Brower explains.
When we throw ourselves up into the blanket, you know, you
get that much more of an awe of seeing further and further
out. So sometimes you'll jump 15, 20 feet in the air and
hopefully you're being caught right back into the blanket.
But the old way of life is under threat. When Lewis was
young the sea stayed frozen to the horizon until July and
some ice remained offshore all summer. But now it's breaking
up in June and melting away completely for two or three
months. I used to go out on the ice all the time this time
of the year but we can't do that anymore because there's no
more no more ice. Lewis can also see that the loss of sea
ice is affecting the animals he hunts for a living. Since
2007 something very strange has been happening
on the stretch of coastline close to Barrow.
Mother walruses, confused by the lack of ice, are crowding
onto the land with their pups. This very tight crowding
isn't normal and it's caused many youngsters to be crushed to death.
Many Arctic animals are threatened by the changing
conditions and that's also bad news for the traditional
hunters. But the ice loss could be good news for some people.
There are trillions of dollars worth of oil and gas under
the Arctic Ocean but the only way to get to them until now
has been by building expensive artificial islands like this.
But if the sea ice goes it will be much easier to drill for
the huge riches below so the countries that surround
the Arctic are scrambling to stake their claims.
This daring attempt by the Russians to claim the disputed
seabed at the North Pole in 2007 caused fury among the
competing countries and it's unlikely to be the last such dispute.
The Arctic has never been so important and not just because of its resources.
The Northwest Passage, a legendary sea route around the
north of Canada and Alaska, cleared of ice in the summer of
2007 for the first time since records began. This promises a
much faster and cheaper shipping route between the Atlantic
and Pacific Oceans.
And some wildlife could benefit from an ice-free Arctic too.
Bowhead whales are one of just a few whales that can live
year-round in the Arctic because they have no dorsal fin.
This means they can come up for air in small spaces and
travel easily under the ice. Their unique body shape used to
mean that the Arctic whales have the seas to themselves for
most of the year but now some cousins from down south are
moving in.
Killer whales are now a much more common sight in the
Arctic. Their tall fins make it difficult for them to travel
under ice but the longer summers mean they can travel much
farther north and make the most of the rich Arctic seas.
For animals and people, it will be those who
can adapt who will thrive in a changing Arctic.
But the loss of sea ice isn't just an issue for the Arctic
because the state of the ice affects the climate of the
whole planet.
Because it's white, the ice reflects up to 90% of the sun's
energy. This is called the albedo effect and it's why we
often see heat haze in the Arctic even when the air feels cold.
The frozen Arctic Ocean acts as a huge reflector bouncing
back the sun's heat into space. Throughout history that has
helped to cool the planet but when the ice melts it's a different story.
Because sea water is dark it absorbs most of the sun's
heat. In the Arctic this can trigger a chain reaction as the
warming water melts more ice exposing more water to the sun's heat.
This cycle of warming as huge areas start to absorb rather
than reflect heat is the main reason why the Arctic, a
region the size of North America, is warming
twice as fast as the rest of the Earth.
So melting sea ice is a big issue but there's another kind
of ice that could have an even more dramatic impact on our
world. The Arctic is a place where the Arctic is the most
important in the world. The ice that is found on land.
This is freshwater ice formed from thousands of years of accumulated snowfall.
This is the front of the glacier, quite a small one believe
it or not. Glaciers are like rivers of frozen freshwater
flowing across the surface of the land. This one like most
polar glaciers is flowing down from a vast inland ice sheet
and it's what happens to those ice sheets that could
radically alter the face of the planet. The Greenland ice
sheet is by far the largest in the Arctic. It's two miles
thick in places and six times the size of the United
Kingdom.
Every summer some of the surface of the ice sheet melts
forming sapphire blue lakes of meltwater. More and more of
these lakes have been forming as Greenland has warmed over
the last 20 years. This lake has grown over several weeks
and now it's overflowing carving a deep channel through the ice.
A network of channels crisscrosses the ice
sheet but many of them come to an abrupt end.
Huge holes like this can open up quite suddenly, draining the meltwater away.
Alan Hubbard is a glaciologist studying the enormous power
of these waterfalls which are known as moolands. We've got
this amazing mooland going on here today. The water is
overflowing from the lake which is beginning to drain. Tons
of water cascading down this pipe that is effectively
plummeting to the depths of the ice sheet through over a
kilometer of vertical ice.
Alan is here to study where the meltwater goes and what
effect it has on the remaining ice. To do that he needs to
find a mooland that has recently run dry.
Just a week ago there was a three mile long 10 meter deep
lake here. The weight of all that water cracked the ice
beneath and the lake drained in just a few hours with incredible force.
A thousand ton ice boulders were tossed about like dice.
Alan's team have found the hole down which the lake
disappeared and they want to have a closer look. It's not a
job for anyone with a fear of heights.
As you can see it's dry up here but if you listen you can
hear the thunder of there's a lot of water entering it at
some depth. Alan wants to place a sensor deep into the
mooland to discover how much water is flowing through the
ice.
As they drop they travel back in time. 30 meters down and
they reach ice formed from snow that fell 10,000 years ago
in the last ice age.
When this lake drained and the plug got pulled and the whole
lot flushed down through here this ice sheet it rose by a
meter as that water accessed the bed and force jacked up the
ice sheet. So we know that the water and this whole plumbing
cavity system down here we know that shoots straight through
the ice and actually hits the bed of the ice sheet. We've
hit the water, can see the water now. Great, nice work.
This daring experiment is measuring how the water flowing
under the ice sheet affects the speed with which the
glaciers flow from it down to the sea. The theory is that
the water is acting as a lubricant so the more water there
is the faster the glacier flows. To the naked eye, glaciers
don't appear to move at all, but move they do. These unique
time lapse images were captured over the last four years.
Through long observations we now know that Greenland's ice
is flowing down to the sea twice as quickly as it was 20
years ago. The speed of the glaciers affects our sea levels
because when they reach the water they break apart into
icebergs. Occasionally a real mega-burg is born.
This is the store glacier in May 2010.
This is the store glacier in May 2010. This is the
store glacier
in May 2010. 75 million tons of ice that have been
sitting on land for thousands of years has broken away.
Events like this have become increasingly common
as Greenland's glaciers flow faster into the sea.
Every single one of these icebergs raises the sea level a
small amount. Scientists monitoring the ice sheet predict
that Greenland might add as much as a half meter to world
sea levels by the end of the century, enough to swamp many
of the world's low-lying islands.
99% of the Arctic's freshwater ice is in Greenland. It's a
staggeringly big ice sheet but it's just a drop in the ocean
compared to that at the southern end of our planet.
In Antarctica there is 10 times more ice, by
far the largest concentration of ice on Earth.
Our exploration of the Antarctic only began a little over a hundred years ago.
The study of ice retreat here was unwittingly begun on
an expedition led by the great early explorer Ernest
Shackleton.
In 1916, after their expedition boat was crushed and sunk by
ice, Shackleton and two companions set off to summon help in
a tiny boat.
They sailed over 800 miles across the Southern Ocean to
the island of South Georgia on the edge of the Antarctic.
Near starving and dressed in rags, the three men walked
across the ice sheet at the center of the island, knowing
there was a wailing base on the opposite coast where they could summon help.
This team of Royal Marines is retracing the steps of that
journey in tribute to Shackleton and his men. But for all
their efforts, they can't exactly copy the
Great Walk because the ice is not as it was.
A number of South Georgia's glaciers were photographed by
Shackleton's cameraman. Frozen planets saw a dramatic change
when they returned 94 years later.
Most of South Georgia's glaciers have shrunk since
Shackleton's time, and most of that has happened since I
first went to the Antarctic 30 years ago. I've been to South
Georgia several times and seen how greatly the glaciers
there have changed.
This photograph of a glacier reaching right down to the sea
was taken just six years before I first visited in 1981. Now
that glacier has retreated by 400 meters away from the beach.
Temperatures in South Georgia have risen sharply, but the
southern hemisphere's most dramatic warming has happened a
little further south. In recent years, stronger winds
blowing over the southern ocean have brought warmer air to
the 800-mile-long finger of land that forms the
northern extremity of the Antarctic continent.
Here on the Antarctic Peninsula, the changing wind patterns
have driven temperatures up by nearly 3 degrees Centigrade
over the last 50 years, 10 times the average rate of the rest of the planet.
The rapid warming is having a big effect on the bird life.
The daily penguin is the most southerly nesting of all
penguins. And like the polar bear up in the north, their
lives are dependent on the sea ice. A daly spent their whole
lives near ice. These birds have spent the winter feeding at
the ice edge, but now it's spring and they've
started a long trek over the frozen sea towards land.
They're heading for areas of exposed rock where they gather
to breed in colonies that can be over 100,000 strong.
But it seems that a daly's don't find the conditions on the
peninsula to their liking anymore. 17 years ago, when I was
last in the Antarctic, there were large colonies of a daly
penguins all along the Antarctic Peninsula. Now, warming
temperatures have meant less sea ice and a daly penguin numbers are in decline.
Many colonies have been empty and fast.
It may be that penguins are starving or it may be that
they're heading south to colder climes where there's still
plenty of ice on the sea.
But as in the Arctic, while ice-loving animals are feeling
the heat, animals that like it a bit more cosy are moving
in.
The bright orange beaks of gentoo penguins are a much more
common sight on the peninsula these days. I always used to
know them as residents of the slightly warmer islands
north of the Antarctic, but they've moved south in numbers.
They're thought to be 10 times more gentoos
on the peninsula now than just 30 years ago.
The peninsula has warmed a great deal, but the same is not true further south.
The Antarctic continent is smothered by the world's greatest
ice sheet, one and a half times the size of Australia and up
to three miles thick.
A staggering 75% of the Earth's fresh water is locked up in this ice.
Global sea levels would rise by some 60 metres if all this was to melt.
But what chance is there of that happening here
in the coldest, most hostile place on Earth?
The ice beneath me up here on top of the ice cap is so thick
that I am short of breath simply because of the altitude.
This is midsummer and the average temperature is some 20
degrees below freezing. I can tell you it feels much lower
than that. And even the worst predictions don't suggest that
the air is going to warm enough to melt the ice. But now
scientists are asking a different question. Could the speed
at which the Antarctic ice flows off the land be increased
by a warmer ocean? Where the ice sheet meets the sea,
scientists are going to extreme lengths to find out.
Andy Smith works for the British Antarctic Survey. What we
have here is a one kilogram of pentelite explosive. We're
going to use this to generate a shockwave and record
the echoes that come back from underneath the ice.
Andy is particularly interested in mapping the underside of
the ice around the coast. Because here it isn't resting on
land, it's floating on seawater. So if sea temperatures
rise just a little, it can be melted from below.
Around the coast of Antarctica, the glaciers have flowed out
across the sea to form immense masses of floating freshwater
ice called ice shelves.
These freeze to the land around them, sticking fast and
acting like bath plugs, holding back the flow of the
glaciers into the sea.
On the Antarctic peninsula, a one degree sea temperature
rise has helped to break apart seven major ice shelves in
the last 30 years. This is the Larson B ice shelf, three
times the size of Greater London breaking apart in 2002.
Afterwards, the glaciers it had been holding
back started flowing up to six times faster.
In 2008, a much larger ice shelf at the southern end of the
peninsula started to break up. It's an enormous event that's
never been filmed before.
Andy Smith is flying down the peninsula to study this
phenomenon firsthand. We're flying to a place called Wilkins
Ice Shelf. It's an ice shelf that over the last couple
of years has showed a very sudden and dramatic breakup.
The Wilkins Ice Shelf is a two hour long flight south from
his research base. But Andy can start to see the evidence of
ice shelf breakup a long way before he gets there. As we're
heading further south, we can see more and more icebergs in
the ocean. And most of the big ones will be ones
that have broken off the ice shelves in this area.
Once we cross the mountains, we should be able to see
Wilkins Ice Shelf. And then it's not far then to the ice
front here where it's collapsing.
As Andy's team reaches their destination, the scale of
what's been happening sooner Here, for thousands of years,
an area the size of Yorkshire has been covered by a sheet of ice 200 metres thick.
But now, over half of that has broken apart.
Andy has been studying Antarctic ice for 25 years, but
even he is blown away by what he's seeing. That is pretty
awesome. That is remarkable. The edge of the ice shelf has
just kind of disintegrated. Some of the big pieces look like
they could be a mile or more in size. It's almost like a
sort of a slow motion explosion. It all pushes outwards very
quickly.
Every one of these huge icebergs will slowly drift out to sea.
To study how fast that happens, Andy needs to get closer
to the action. We're going to look around and see if we can
find a place where we can land. But if we can, we'll be able
to put on an instrument that will help us monitor the big
icebergs that are breaking off as the ice shelf breaks up.
Landing on an iceberg is another first for Andy's team.
This satellite transmitter will help to track
the continued breakup of this colossal ice shelf.
The remainder of the Wilkins looks set to break apart soon.
It's the latest ice shelf to disintegrate in a wave that's
been traveling southwards, playing a major role in the loss
of ice from the peninsula.
Next in line, and already weakening in place, is the first
ice shelf to disintegrate. The only places are the ice
shelves that hold back Antarctica's gigantic continental
ice sheet. And it would only take a small corner of this to
slide into the sea to have major global consequences.
We've only started to see changes in the Arctic and
Antarctic recently, so it's hard to predict exactly what
impact these changes will have. But we can see for ourselves
that these places are changing and on a scale that is hard
to ignore.
The poles, north and south, may seem very remote. But what
is happening here is likely to have a greater effect upon us
than any other aspect of global warming. If the Arctic sea
ice continues to disappear, it will drive up the planet's
temperature more quickly. And the melting ice sheets
could contribute to a sea level rise of a meter, enough to
threaten the homes of millions of people around the world's
coasts by the end of the century. We've seen that the
animals are already adapting to these changes. But can
we respond to what is happening now to the frozen planet?
The Ice The increasing unpredictability of the ice was a
big issue for the frozen planet team, who spent three years
working on top of it.
Whether on sea, land, lake or river, the state of
the ice was the first concern for most filming crews.
Unexpected breakups left many a cameraman in need of a swift
rescue. Sometimes help came by boat and sometimes by air.
The North Pole I had a chance to see the changing ice
conditions for myself when I visited the North Pole. I flew
with the team to a temporary camp that is set up every
year in the center of the frozen Arctic Ocean to support
expeditions to the pole.
The North Pole I had never visited the North Pole before, so
this was a great highlight for me. But it was hard going in
temperatures of minus 40, so as soon as filming finished, we
flew south. Little did we know that we had made it out just
in time. We got back from the pole camp last night and I've
just bumped into the Russian commander, who's just heard
from the camp. And the news is that a little crack, which
I'd seen in the ice between our tent and the airstrip, which
was no more than an inch or so wide, has overnight widened
to 20 meters. Temporary breakups caused by stormy weather
and strong winds have happened before, but they've been
getting more and more frequent over recent years as the ice
has got weaker.
It was only swift action by the staff that prevented
a lot of valuable equipment going in the drink.
The biggest concern was that the ice airstrip might break
apart, but luckily it held and everyone was able to evacuate
when the weather improved.
The frozen planet team's clearest demonstration of the power
and unpredictability of breaking ice came when they went to
film the melting of a frozen planet. Producer Mark Linfield
and researcher Matt Swarbrick have travelled to the far
north of Canada.
They've driven through the vast northwest territory on a
mission to film the moment when this frozen waterfall breaks
apart.
The breakup, when the frozen river above the waterfall
thaws and masses of water start to flow again, can be a
spectacular event. But predicting exactly when it's going to
break is the big challenge if Mark and Matt want to get the
best shots.
And they're not the only ones who want to know. When the
waterfall breaks, it can flood the town of Hay River just
downstream with millions of tons of water and ice. Mark is
taking advice from the scientist Faye Hicks, who has the job
of predicting when the ice will break. What happens is you
get ice jams form upstream and they start to dam up the
water and it builds and builds and builds and that can let
go and that's a much bigger wave of water than just the
normal flow. So it just depends upon how dramatically it
unfolds. Faye takes her research helicopter to monitor the
situation upstream of the waterfall.
Just ten miles upriver, the ice is starting to break. The
locals are concerned because huge amounts of water can build
up if these ice chunks dam the river and that can lead
to devastating flooding in the town when the dams burst.
Using cameras and sonar to assess the state of the river,
Faye makes her best guess of when this breakup will hit the
waterfall just above the town. So now guys, I think we have
about 48 hours to go. Faye's prediction of the 24th of April
is exciting news for the team.
Upstream from here, it's already starting to melt and Faye
thinks that we may only have another one or two days before
this whole thing goes, which is almost impossible to imagine
looking at it now, but that's what she says. With the
breakup seemingly imminent, the team set up their cameras in anticipation.
Over the next 48 hours, the weather warms to well above
freezing, but there's no sign of the breakup. The team waits
and waits and waits. Mark is
concerned that the crew have to return home soon, so he
heads into town to get the advice of long-term resident Red
McBrien. We just have to live with it and take whatever base
of action we can. Red has had 50 years of witnessing the
power of the river. Well, we're hoping that she may break
up in two or three days even. Oh, no, no, no, no. That's too
soon. You think it'll be longer? Oh, no, no. Boys, you're
looking at seven or eight days before she breaks of any
significance. And if she breaks, she can jam and hold up.
She'd be down here probably around the fifth or sixth of
May. The townspeople are on tenterhooks, waiting for the big
day, but another week goes by before anything starts to happen.
Finally, it seems that things might be happening. We've just
heard some cracks from upstream, so if we're lucky, we might
get some action. Seven o'clock, which gives us two hours
light. If it happens at night, we're going to miss the whole
thing.
Sure enough, the town is put on red alert that the river
is about to break in the middle of the night. They've just
called a full evacuation of the island where we're staying.
If we don't move now, we're all going to be underwater and
possibly get trapped here for a few days. The team have to
move out and get up to the waterfall, hoping that it doesn't
break before it's light enough to film.
Luckily, the sun is up before the main event begins.
That is a serious amount of ice coming around the corner.
After weeks of waiting, sleeping giant of a river, we
thought nothing was going to happen, and suddenly, look at
this! This is what we're here for. Unbelievable! Absolutely
unbelievable! Holy ****! How are you? The team is used to
handling multiple cameras, but they don't usually have to
dodge. They can even dodge 10-ton ice flows at the same
time. You can see it racing over at an unbelievable speed.
The power, if you are here to feel this, it's the deep
rumbling sound of the river. I can feel it up to my feet.
The power, I just can't imagine. It has to crush a house in
no time. The team takes to the air to witness the
destruction that's unleashed. Huge ice blocks are pushed
downstream on the wave of water released by the breaking waterfall.
This could devastate the town.
But this year, the townspeople's luck is in. The town has escaped flooding.
Crucially, the ice blocks did not dam the river. It's
running free. And the date of the break-up? 6th of May.
Red's got it right again. I don't use any of these gauges
and mechanical assistance. I just go by what I see on the
river as I walk it down. And I say, I walk it down, I back
and forth every day on the river, to see what's happening,
and from that I gauge when it's going to hit here, and what
the situation's going to be like when it does get here. You
know, when it went this morning, I said to my students,
guess what the date is. Red told us it's the 6th of May. And
I'm not surprised because we've been here a couple times
and that's happened. Ten days, two weeks out, he just looks
around and goes, 5th of May. How does he know that? It's
incredible. It's because he just has lived on this river and
lived this break-up for 50 years. I see scientists on
improving the accuracy of their predictions all the time,
but in the meantime, the people of Hay River have a
remarkable guardian. Red, you were completely right this
year. Are you right every year? No, I missed
the odd one. Yes. In 1985, I missed it.
Music
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