Browse content similar to The Vanishing Antarctica. Check below for episodes and series from the same categories and more!
Line | From | To | |
---|---|---|---|
between 18-60. Now it is time for Our World. British scientists are | :00:34. | :00:36. | |
in ing dramatic and potentially dangerous changes to | :00:36. | :00:39. | |
the west Antarctic ice shelf. There is a strange and mysterious place | :00:39. | :00:43. | |
at the edge of our planet which most of us will never see. 1.5 | :00:43. | :00:47. | |
times the size of the United States, it holds just ice. Now one of | :00:47. | :00:50. | |
Antarctica's greatest glaciers has begun to race into the ocean, | :00:50. | :00:53. | |
putting more ice into the sea than any other in the world. Nobody | :00:53. | :00:57. | |
knows what the consequences for the world's oceans will be. Just one | :00:57. | :01:07. | |
:01:07. | :01:43. | ||
thing is certain: If you want It is brass monkeys out there! You | :01:43. | :01:47. | |
would think that after six trips to this icy continent, I would be used | :01:47. | :01:50. | |
to the cold but it is impossible to grow complacent about any aspect of | :01:50. | :01:54. | |
Antarctica. For 20 years, I have been reporting on how it has | :01:54. | :01:57. | |
changed. The seas around the Antarctic Peninsula have changed | :01:57. | :02:00. | |
almost beyond recognition, and climate change is also having a | :02:00. | :02:07. | |
dramatic effect. I am talking to scientists both here and in the UK | :02:07. | :02:17. | |
:02:17. | :02:27. | ||
about something they are reporting as a major global concern: The | :02:27. | :02:30. | |
oddly named Pine Island Glacier is one of the world's largest rivers | :02:30. | :02:34. | |
of ice and it has almost doubled its speed in the last 30 years. Its | :02:34. | :02:37. | |
behaviour has left scientists confused and concerned. The ice | :02:37. | :02:40. | |
here is melting faster than just about anyone thought possible. We | :02:40. | :02:50. | |
:02:50. | :02:54. | ||
have front-row seats here. The story begins here on the Antarctic | :02:54. | :03:04. | |
:03:04. | :03:05. | ||
Peninsula. Until the 1800s, Antarctica was nothing more than a | :03:05. | :03:09. | |
myth and even when we discovered it was real, it retained a mythic | :03:09. | :03:14. | |
status. We thought of it as the last great wilderness, untouched, | :03:14. | :03:24. | |
:03:24. | :03:37. | ||
unchanging. We were wrong. This man is an aero-geophysicist. In 1997 he | :03:38. | :03:47. | |
:03:48. | :03:49. | ||
was working on a vast expanse of floating ice called the Larsen B. | :03:49. | :03:52. | |
Each ice shelf has its own character but this one has rifts | :03:52. | :03:56. | |
and it is likely it could go. years ago, we were sitting in a | :03:56. | :04:00. | |
small boat off the Antarctic Peninsula when you said this could | :04:00. | :04:07. | |
be the next glacier to go. How did you know? In hindsight I should | :04:07. | :04:15. | |
have been more forthright. There were three of us on the plane and | :04:15. | :04:19. | |
we could see the enormous rifts and the way it was open. After the | :04:19. | :04:22. | |
flight we were chatting. We all felt melancholy because we knew it | :04:22. | :04:29. | |
was going to go at some point. could see its number was up. Hugh | :04:29. | :04:39. | |
:04:39. | :04:43. | ||
was right. So that is the place where the glacier should begin but | :04:43. | :04:47. | |
instead it is full of water and Larsen B is gone. It is an | :04:47. | :04:51. | |
extraordinary sight. In 2002, it was plain to see in the satellite | :04:51. | :05:01. | |
:05:01. | :05:06. | ||
images. In March, there was heavy cloud and when it cleared the | :05:06. | :05:09. | |
glacier had vanished. It had become tiny shards which would eventually | :05:10. | :05:15. | |
float out to sea. Scientists stared at their computer monitors in | :05:15. | :05:22. | |
astonishment. We knew that other ice shelves had disintegrated as | :05:22. | :05:26. | |
well but in a piecemeal fashion. Pieces would fall off and then more | :05:26. | :05:29. | |
bits but this one was very different. The whole ice shelf | :05:29. | :05:39. | |
:05:39. | :06:01. | ||
literally disintegrated. A complete shock? Yes, it was not expected. | :06:01. | :06:04. | |
soon as the weather permitted, scientists returned to the | :06:04. | :06:08. | |
peninsula to try to work out why it had collapsed. It did not take them | :06:08. | :06:11. | |
long. This is a meteorologist who tracks climate on the peninsula. | :06:11. | :06:14. | |
She is watching as the climate behaves in an extraordinary way. | :06:14. | :06:24. | |
:06:24. | :06:30. | ||
Can you give me an overview of what has happened to temperatures? | :06:30. | :06:33. | |
Antarctic Peninsula is one of the fastest warming places on the | :06:33. | :06:36. | |
planet. Temperatures have risen by three degrees in 50 years, which is | :06:36. | :06:39. | |
about ten times the global average. Scientists concluded that warming | :06:39. | :06:42. | |
air was responsible for the glacier's demise. Climate change | :06:42. | :06:47. | |
had claimed its first high-profile Antarctic victim. After the | :06:47. | :06:57. | |
:06:57. | :07:08. | ||
collapse of Larsen B, the focus was on the ice and who works on it. A | :07:08. | :07:14. | |
world-leading glaciologist remembers the time very well. | :07:14. | :07:18. | |
the biggest thing we have seen for many decades - an ice shelf that we | :07:18. | :07:21. | |
thought was permanent suddenly collapsing in a short period. It | :07:21. | :07:31. | |
was enormously important. This is the main research station of the | :07:31. | :07:40. | |
British Antarctic Survey. Scientists and support staff stay | :07:40. | :07:46. | |
here for stretches of up to 18 months at a time. One of their aims | :07:46. | :07:56. | |
:07:56. | :07:59. | ||
is to track every move that the ice makes. Some people take a little | :07:59. | :08:02. | |
persuading, like this climate change scientist. I studied | :08:02. | :08:05. | |
oceanography and wanted to work in the tropics, somewhere warm. | :08:05. | :08:15. | |
:08:15. | :08:15. | ||
Somewhere along the line I was diverted to the polar region. It is | :08:15. | :08:24. | |
incredible! This is something many people can only dream about. A | :08:24. | :08:30. | |
glacier is always on the move. Glaciers are always moving towards | :08:30. | :08:39. | |
the sea. You can really see that in this fissure which has opened up. | :08:39. | :08:46. | |
You can walk around and see that it is moving. Why are the icicles at | :08:46. | :08:56. | |
:08:56. | :08:57. | ||
right angles here? The larger ones have formed over many years. They | :08:57. | :09:02. | |
are dripping down vertically but the ice itself is moving. When it | :09:02. | :09:06. | |
is quiet, you can hear cracks and creaks and groans. That is another | :09:06. | :09:16. | |
indication that it is moving and really quite fast. Movement is one | :09:16. | :09:20. | |
of the basic principles of ice. As snow falls across the continent, it | :09:20. | :09:30. | |
:09:30. | :09:35. | ||
is slowly compressed into giant frozen rivers. Gravity and fresh | :09:35. | :09:38. | |
snowfall force these glaciers to float towards the sea. There they | :09:38. | :09:41. | |
edge out in vast floating platforms called ice shelves. Their tips | :09:41. | :09:51. | |
:09:51. | :10:01. | ||
break into icebergs and float away to sea. Until the collapse of | :10:01. | :10:06. | |
Larsen B, scientists had thought that this happened very slowly. | :10:06. | :10:10. | |
They had a theory that an ice shelf was like a cork in a bottle, | :10:10. | :10:13. | |
holding back a glacier. If you take away the cork, the glacier just | :10:13. | :10:23. | |
:10:23. | :10:39. | ||
hotly-contested but then the Larsen B broke away and melted. Now we | :10:39. | :10:43. | |
know that the ice shelf restrains the glacier behind it. If you take | :10:43. | :10:53. | |
:10:53. | :10:59. | ||
away the ice shelf, the glacier will speed up. It was like pulling | :10:59. | :11:06. | |
a cork from a bottle. The ice shelf has stabilised the glaciers. When | :11:06. | :11:10. | |
it was gone, the glaciers sped up. They are still retreating at this | :11:10. | :11:20. | |
:11:20. | :11:23. | ||
moment. An ice shelf floats and has no effect on sea levels, unlike the | :11:23. | :11:33. | |
:11:33. | :11:37. | ||
glaciers behind them. In just six months, the glaciers dropped in | :11:37. | :11:41. | |
height by as much as 1.5 times the size of these peaks. Remove an ice | :11:41. | :11:45. | |
shelf and the glaciers behind will race to the seas. Ice can be swift | :11:45. | :11:48. | |
and volatile. It made them afraid of what would happen if rising | :11:48. | :11:58. | |
temperatures spread. The Antarctic Peninsula is a vast formation of | :11:58. | :12:02. | |
ice but it is dwarfed by the West Antarctic ice sheet further south. | :12:02. | :12:06. | |
Here the air is not warming nearly as fast, so scientists thought the | :12:06. | :12:10. | |
ice shelves were safe at least until now. Then something happened | :12:10. | :12:20. | |
which made them change their mind. 800 miles from the nearest British | :12:20. | :12:23. | |
base, Pine Island glacier has been tracked by satellite since the | :12:23. | :12:32. | |
1990s and it is acting up. It is one of the largest ice streams on | :12:32. | :12:36. | |
the planet - a large river on ice that drains the West Antarctic ice | :12:36. | :12:43. | |
shelf. It is changing very quickly. It was melting more than 100 times | :12:43. | :12:53. | |
faster than they had expected. Scientists did not know why and had | :12:53. | :12:57. | |
to go there to find out. Less than one thousandth of 1% of the world's | :12:57. | :13:06. | |
population has ever been to Antarctica. Science here still | :13:06. | :13:15. | |
pushes the limits of polar exploration. To get to this ice | :13:15. | :13:18. | |
shelf from the nearest base, scientists had to cross 800 miles | :13:18. | :13:22. | |
of the most inhospitable terrain on earth. It is a place so remote that | :13:22. | :13:32. | |
:13:32. | :13:33. | ||
more people have landed on the moon. Conditions here are so tough that | :13:33. | :13:37. | |
only one scientist has walked on a forward floating edge of the | :13:37. | :13:40. | |
glacier. He was an American from NASA. The pilot was so nervous that | :13:40. | :13:50. | |
:13:50. | :13:53. | ||
No one except a special robot. In January 2009, scientists sent a | :13:53. | :13:56. | |
remote-controlled submarine into a place no man or machine had ever | :13:56. | :14:05. | |
been before. In icy waters of the ice sheet its job was to collect | :14:05. | :14:11. | |
data from below the glacier. Adrian Jenkins is the oceanographer who is | :14:11. | :14:20. | |
in charge. This is a model of the submarine. It is seven metres long | :14:20. | :14:27. | |
and a metre in diameter. This is sophisticated technology. It is | :14:27. | :14:31. | |
amazing. It gives us an unprecedented view on the world | :14:31. | :14:38. | |
underneath the ice shelves. Frozen sea ice normally covers the bay but | :14:38. | :14:41. | |
a lucky break in the weather meant Adrian and the ship got within | :14:41. | :14:50. | |
three miles of the ice shelf. wanted to get in and we would tents | :14:50. | :14:57. | |
knowing this was the big moment. -- were tense. We were the first | :14:57. | :15:05. | |
mission below the glacier and have no idea what would come back. | :15:05. | :15:09. | |
the teams saw the data they were astonished. They thought the ice on | :15:09. | :15:13. | |
the underside of the Pine Island glacier was an kits to a ridge but | :15:13. | :15:20. | |
the Autosub had made its way 30 kilometres inland. The glacier had | :15:20. | :15:24. | |
come unstuck and it was floating. It wasn't warming air that was | :15:24. | :15:27. | |
causing it to melt, it was warming seas. Not just lapping against the | :15:27. | :15:31. | |
ice but eating away at its underbelly. It changed the way we | :15:31. | :15:38. | |
think about the system. It was jaw- dropping. What the submarine | :15:38. | :15:41. | |
revealed was the latest piece of evidence suggesting the melting of | :15:41. | :15:45. | |
the Pine Island glacier and the West Antarctic ice sheet may be the | :15:45. | :15:55. | |
:15:55. | :15:56. | ||
largest source of global sea level rise the century. In 2007, | :15:56. | :15:58. | |
governments commissioned a report written by scientists which | :15:58. | :16:08. | |
:16:08. | :16:11. | ||
estimated future sea-level rises around the world. By 2100, these | :16:11. | :16:15. | |
seas were unlikely to rise by more than 59 centimetres, they said. But | :16:15. | :16:19. | |
they also admitted not enough was known to fully include the ice in | :16:19. | :16:22. | |
west Antarctica and I think what is happening now makes that report | :16:23. | :16:32. | |
:16:33. | :16:34. | ||
obsolete. David Vaughan here, I have been looking at the figures. | :16:34. | :16:41. | |
David will be a lead author of the next IPCC report. The predictions | :16:41. | :16:44. | |
are predictions of climate change are out of date when they are | :16:44. | :16:49. | |
published. We are working in the IPCC to begin the process of doing | :16:49. | :16:55. | |
that, complete and consolidated estimates. I will not prejudge the | :16:55. | :16:58. | |
outcome of that but everything we had seen coming out of the science | :16:58. | :17:02. | |
suggests Antarctic could contribute more than was known at the time of | :17:02. | :17:10. | |
the last report. The world's oceans could rise 30 centimetres. Great | :17:10. | :17:14. | |
coastal cities could be swamped by five metres of water if the West | :17:14. | :17:24. | |
:17:24. | :17:24. | ||
Antarctic ice sheet follows it. events we have seen in Pine Island | :17:24. | :17:30. | |
glacier make us more concerned than we were five or 10 years ago. More | :17:30. | :17:40. | |
:17:40. | :17:40. | ||
than a metre of sea-level rise is potentially with us by 2100. | :17:40. | :17:44. | |
Certainly by 2150. It seems increasingly likely the future of | :17:44. | :17:48. | |
these coastal cities will be shaped by a piece of ice at the end of the | :17:48. | :17:51. | |
Earth. It is a future scientists are struggling to bring into | :17:51. | :17:57. | |
clearer relief. Ed King is one of a handful of scientists who have made | :17:57. | :18:01. | |
it to the glacier itself. Accompanied only by an assistant | :18:01. | :18:09. | |
and a camera. We had all sorts of issues to do with getting cross | :18:09. | :18:12. | |
country into Pine Island glacier from another glacier we were | :18:12. | :18:20. | |
studying. It should have taken three days, it took us 11. The | :18:21. | :18:24. | |
weather clamped in on us, we sat in the tent seven days straight with | :18:24. | :18:34. | |
40-knot winds blowing past. Blizzard conditions. Things broke. | :18:34. | :18:37. | |
By the time we finally got to Pine Island glacier there was quite a | :18:38. | :18:44. | |
lot of fixing to do. Despite the extreme conditions, he has mapped | :18:44. | :18:51. | |
the glacier bed using radio waves. The image of the bed we have | :18:51. | :18:56. | |
created was eated was dar survey. It is the most detailed image of | :18:56. | :19:01. | |
this glacier ever created. And we can see straight away from that | :19:01. | :19:09. | |
there is melting going on down there. There is water being | :19:09. | :19:16. | |
produced and ice melting right under our feet at the moment. | :19:16. | :19:20. | |
pioneering results are his swansong. After 17 tough seasons on the ice | :19:20. | :19:28. | |
he has decided this is his final trip. It is an extraordinary place, | :19:28. | :19:38. | |
:19:38. | :19:45. | ||
it has been a privilege to be able to work here. Sometimes you can | :19:45. | :19:51. | |
recognise that the time has come for something to end. This is that | :19:51. | :20:01. | |
time. I bid farewell to the situation in the Antarctic. And it | :20:01. | :20:11. | |
:20:11. | :20:31. | ||
feels quite hard. For generations scientists have suffered out on the | :20:31. | :20:39. | |
ice, trying to unlock its secrets. Now, technology is lending a hand. | :20:39. | :20:43. | |
This is the wonderful world of aerogeophysics. Nothing can remain | :20:43. | :20:50. | |
hidden for long. We have four utility aircraft, they are work | :20:50. | :20:55. | |
horses for the survey. This is special in that it has been | :20:55. | :20:59. | |
equipped to do airport geophysics. There are cables down the wings to | :21:00. | :21:06. | |
the antenna. It is hoped by scanning Pine Island this play will | :21:06. | :21:11. | |
show what is happening deep inside the ice. -- plane. Where do you | :21:11. | :21:16. | |
take it? When we get the equipment installed and do a test flight and | :21:16. | :21:20. | |
if all goes well, off we go to Ireland and the idea is to survey | :21:20. | :21:27. | |
the ice shelf, the plug holding back Pine Island. -- Pine Island. | :21:27. | :21:30. | |
Pine Island could answer the trillion dollar question about sea | :21:30. | :21:36. | |
levels rising coming from the West Antarctic ice sheet. You're excited. | :21:36. | :21:42. | |
Excited and worried. We want to a good job. It is a huge challenge. A | :21:42. | :21:45. | |
huge challenge we have everything right because it is a one-shot | :21:45. | :21:49. | |
chance. We have limited time and weather window and we must get it | :21:49. | :21:59. | |
:21:59. | :22:27. | ||
I have been have been e as a TV correspondent since the mid-1990s. | :22:27. | :22:30. | |
It is interesting to reflect that back then it was thought the sort | :22:30. | :22:34. | |
of changes we're seeing here would not happen until the time of my | :22:34. | :22:38. | |
grandchildren or long after that. And yet it is happening now and it | :22:38. | :22:40. | |
is happening much faster than thought possible. Scientists | :22:40. | :22:43. | |
working here say the rapid changes on the peninsular are being driven | :22:43. | :22:46. | |
by human activity. But they have not drawn any definite conclusions | :22:46. | :22:50. | |
about Pine Island for one simple reason. They just don't think they | :22:50. | :22:57. | |
have observed enough. Yet. We have seen dramatic changes but they are | :22:57. | :23:02. | |
for a short time period. They have only been monitoring what is going | :23:02. | :23:11. | |
on since the satellite era, the late 1970s. In terms of a time | :23:11. | :23:14. | |
period to understand the changes, 30 years is very difficult to get | :23:14. | :23:19. | |
any statistical significance. next step is to look at ice drilled | :23:19. | :23:24. | |
from deep down in the ice sheet to hope it will unlock the past. | :23:24. | :23:27. | |
cores are a fantastic resource because they show an archive of the | :23:27. | :23:37. | |
:23:37. | :23:37. | ||
climate. The most interesting one is past temperatures. Liz Thomas | :23:37. | :23:41. | |
has spent a season during ice cores at the edge of the West Antarctic. | :23:41. | :23:45. | |
What we are interested in finding out is how the climate of the West | :23:45. | :23:52. | |
Antarctica has been changing over the last 200 years. We are | :23:52. | :23:56. | |
interested in the causes of whatever is happening. Is this part | :23:56. | :24:02. | |
of a natural cycle? So, the climate has been changing many times over | :24:02. | :24:06. | |
the past million years, so it is this part of natural change or is | :24:06. | :24:09. | |
this something that is more recent effect like something like human | :24:10. | :24:17. | |
induced warming and change. Everyone I spoke to about Pine | :24:17. | :24:20. | |
Island says the same. At the moment they have more questions than | :24:20. | :24:25. | |
answers. But there is one thing about which they are all in | :24:25. | :24:32. | |
agreement. It is one of the biggest questions facing science. Science | :24:32. | :24:37. | |
and society as well. Because there is potential for the changes we see | :24:37. | :24:47. | |
:24:47. | :24:48. | ||
to affect all this. Regardless of the cause of the changes, it is | :24:48. | :24:51. | |
something, with regard to sea level rises, it will affect everyone. | :24:51. | :24:54. | |
does concern me. People have said to me, these things have happened | :24:54. | :24:59. | |
in the past, that is true and the sea level has been higher than at | :24:59. | :25:02. | |
the moment but back then the humans there were around were few and | :25:02. | :25:07. | |
minimal. But back then, the humans were few in number and were nomads. | :25:07. | :25:11. | |
They could move away from rising sea levels. Now we have 7 billion | :25:11. | :25:14. | |
people on the planet. That is a thought echoed by everyone who | :25:14. | :25:19. | |
works down here. It has made me think about things in a different | :25:19. | :25:25. | |
way. So, consider this. In a way it really doesn't matter whether you | :25:25. | :25:28. | |
think the changes in Antarctica are natural phenomena or global warming | :25:28. | :25:31. |