Ice Station Antarctica: Part One

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:00:10. > :00:18.This is Antarctica, the last great wilderness.

:00:19. > :00:24.It's the coldest, windiest, driest and most isolated place

:00:25. > :00:29.on Earth, and it's home to the British Antarctic Survey's

:00:30. > :00:36.Here, cutting-edge science is making vital discoveries

:00:37. > :00:41.about how our lives are vulnerable to the sun's activities

:00:42. > :00:47.and threatened by man-made climate change.

:00:48. > :00:52.It's 27th of January, 2016, and we're at 75 degrees south.

:00:53. > :00:55.For the last couple of weeks, we've been on this ship behind me,

:00:56. > :01:01.the RRS Ernest Shackleton, crossing the Southern Ocean.

:01:02. > :01:04.We're making this journey to resupply the research station,

:01:05. > :01:11.but this is also something of a rescue mission.

:01:12. > :01:15.Although it appears to be on solid ground, Halley actually sits

:01:16. > :01:20.on a constantly-moving and cracking ice shelf - an ice shelf that's

:01:21. > :01:25.developed a chasm that threatens to cast the station adrift

:01:26. > :01:28.on a massive iceberg - and our cargo is part of the effort

:01:29. > :01:39.I'm Peter Gibbs, and my job is working for the Met Office

:01:40. > :01:42.as a BBC weatherman, but back in my younger days I worked

:01:43. > :01:45.as a meteorologist in Antarctica for over two years, and I never,

:01:46. > :01:51.ever thought I'd get the opportunity to return.

:01:52. > :01:54.'This is my journey to investigate the threat to Halley's

:01:55. > :01:56.future...' OK, Hilmar, here we go, then.

:01:57. > :02:01.It's going over the edge that's the worst bit.

:02:02. > :02:03.'..and science at the end of the world.'

:02:04. > :02:24.My journey starts at the southern tip of Africa.

:02:25. > :02:31.Here, the Royal Research Ship Ernest Shackleton is waiting for me.

:02:32. > :02:34.As I go below to find my cabin and stow my bags...

:02:35. > :02:46.We're heading out of Cape Town harbour -

:02:47. > :02:51.you can probably see Table Mountain in the background behind me -

:02:52. > :02:55.on our way to the frozen continent of Antarctica.

:02:56. > :02:58.Now, we're expecting it to take about two weeks.

:02:59. > :03:02.We'll be going at ten to 12 knots, so at just

:03:03. > :03:07.We're also heading through some of the roughest seas in the world,

:03:08. > :03:10.so I'm a little bit nervous about that, but really,

:03:11. > :03:47.really excited to be heading for Antarctica.

:03:48. > :03:49.The Ernest Shackleton has been making this long journey

:03:50. > :03:51.across the Southern Ocean to resupply Halley since 1999,

:03:52. > :03:53.but British scientific research goes back much further and has

:03:54. > :03:57.The modern-day British Antarctic Survey actually has its roots

:03:58. > :04:00.in a secret wartime mission from World War II, which was based

:04:01. > :04:01.up here on the peninsula at Port Lockroy

:04:02. > :04:05.The idea of the operation was to protect the waters around

:04:06. > :04:07.Antarctica, particularly towards the Drake Passage

:04:08. > :04:23.towards South America, from Nazi submarines.

:04:24. > :04:25.After the war, territorial claims led to 12 nations signing

:04:26. > :04:27.the Antarctic Treaty, and this untouched landscape

:04:28. > :04:29.became a home purely for scientific exploration.

:04:30. > :04:31.For the British Antarctic Survey, this meant a research station

:04:32. > :04:38.And that's our destination - Halley Research Station.

:04:39. > :04:43.Even the buildings I lived in have long since drifted off,

:04:44. > :04:49.We've still got a long way to go - the best part of a week.

:04:50. > :05:07.In fact, we are not even on the edge of this map yet.

:05:08. > :05:13.Various incarnations of the Halley Research Station have

:05:14. > :05:15.endured some of the most hostile conditions found

:05:16. > :05:26.Temperatures drop to over minus 50 Celsius, winds can reach almost

:05:27. > :05:36.150km an hour, reducing visibility to just a few metres...

:05:37. > :05:50...and, for over three months every winter, the sun never rises.

:05:51. > :06:01.Antarctica is also about as remote a place as you can find on Earth...

:06:02. > :06:04...but it's this remoteness that allows experiments to be performed

:06:05. > :06:32.at Halley that simply can't be done anywhere else.

:06:33. > :06:36.through the Southern Ocean to get to Halley is a challenge.

:06:37. > :06:39.Well, we finally hit the edge of the Weddell Sea pack ice

:06:40. > :06:44.There was an almighty bang as we struck the first floe,

:06:45. > :06:47.The sound when you're actually inside the ship is just remarkable.

:06:48. > :06:50.It's almost like you're inside a war zone, and this

:06:51. > :06:59.I'll tell you what, it's still a bit nerve-racking until you

:07:00. > :07:07.As we crunch through the ice, the captain offers me

:07:08. > :07:10.the chance of a lifetime - something I'd secretly been hoping

:07:11. > :07:16.to do - drive his 1,800-tonne ship.

:07:17. > :07:18.Are you sure about this, John?

:07:19. > :07:25.At the moment we've got 83% pitch, which is basically your power,

:07:26. > :07:28.which is giving us about ten knots, but it will build up,

:07:29. > :07:33.cos we're in a patch of open water here.

:07:34. > :07:35.So, just be careful what you hit at that

:07:36. > :07:41.It's a strange sort of feeling of power and terror, actually.

:07:42. > :07:48.nice new ice coming up, here, and just aim for the crack

:07:49. > :07:58.That's incredible - the speed that crack's actually formed,

:07:59. > :08:01.There's a good covering of snow on most of these

:08:02. > :08:08.It's probably the best part of a metre thick, with

:08:09. > :08:13.It's certainly slowed us down a bit. Yes.

:08:14. > :08:16.And are we OK to hit this bit of ice coming up?

:08:17. > :08:19.You might want to just drop your pitch...

:08:20. > :08:32.Drop your power a bit there.

:08:33. > :08:34.My piloting skills have the local penguins fleeing

:08:35. > :08:36.in terror but I'm not stopping for anything.

:08:37. > :08:38.I have to say, this is fantastic fun.

:08:39. > :08:40.I can see why you keep coming back down here, John.

:08:41. > :08:44.We spend our whole careers at sea, trying to avoid

:08:45. > :08:52...and this is our one chance to hit everything in sight.

:08:53. > :09:05.is an unforgettable experience, like exploring another

:09:06. > :09:11.universe in a spaceship, but we're still a world away

:09:12. > :09:19.Even through the Halley Research Station appears

:09:20. > :09:23.to be built on solid ground, it isn't.

:09:24. > :09:30.Its home is the Brunt Ice Shelf - a seemingly endless frozen sea -

:09:31. > :09:45.and, for the research station, this is a problem.

:09:46. > :09:47.The ice shelves that surround Antarctica are glaciers

:09:48. > :09:52.that have flowed down from the continent's landmass.

:09:53. > :09:55.Hundreds of metres thick, they crack as they spread like a stiff honey

:09:56. > :10:15.So, ice shelves grow with time, as more and more ice is being added,

:10:16. > :10:18.and typically they then lose mass through an event that they call

:10:19. > :10:21.calving, which is basically the breaking off of a chunk

:10:22. > :10:24.of the ice shelf, which breaks away and then floats

:10:25. > :10:29.This is a natural process, which you always expect.

:10:30. > :10:35.It happens with other ice shelves as well and certainly will happen

:10:36. > :10:40.On Brunt Ice Shelf, we have a particular

:10:41. > :10:42.situation right now, which is that there's

:10:43. > :10:49.It was formed at least 30 years ago, but recently it has

:10:50. > :10:55.Now, if this crack were to continue to grow at the same rate as it has

:10:56. > :10:59.over the last few years, in the same direction,

:11:00. > :11:01.then eventually it will cut across the whole ice shelf.

:11:02. > :11:07.We know there was a huge calving event between 1915 and 1956,

:11:08. > :11:13.when the coastline of the ice shelf dramatically changed,

:11:14. > :11:16.and now the ice shelf has almost extended to its 1915 profile,

:11:17. > :11:22.so another major calving event is due.

:11:23. > :11:26.If that happens, then the research station itself will be cast adrift

:11:27. > :11:44.into the Southern Ocean on a huge tabular iceberg.

:11:45. > :11:52.That glistening white line in the distance are the icy ramparts

:11:53. > :11:56.of the Caird Coast - the continent of Antarctica.

:11:57. > :11:58.A coast first spotted and named by Shackleton

:11:59. > :12:00.just over 100 years ago, before he got trapped in the ice

:12:01. > :12:07.just further down the coast here, and first spotted by me 36 years ago

:12:08. > :12:13.There's a bit of that young man certainly coming back as I stand

:12:14. > :12:31.My first sight of the ice shelf brings back a flood of memories.

:12:32. > :12:34.It's a bleak, beautiful place - an alien world, right

:12:35. > :12:49.And it's a treacherous landscape - at any moment, at the water's edge,

:12:50. > :13:10.'But we have a job to do, delivering supplies

:13:11. > :13:12.'for the research station.' And, with no docks, like everything else

:13:13. > :13:14.in Antarctica, you make what you need yourself.

:13:15. > :13:17.So, Captain Harper creates a berth by running the ship

:13:18. > :13:24.If the shelf doesn't collapse, so the theory goes,

:13:25. > :13:27.Violent southern ocean storms could drive the Shackleton

:13:28. > :13:30.off the ice shelf, so, as the weather closes in,

:13:31. > :13:34.the rest of our day is spent securing the ship.

:13:35. > :13:38.This means all hands, including me, go to work digging four massive

:13:39. > :14:15.The 30km snowcat ride across the blindingly white ice

:14:16. > :14:22.shelf seems endless but, after two weeks at sea

:14:23. > :14:29.waiting for this moment, I'm not disappointed.

:14:30. > :14:35.I mean, I've seen pictures, but when you see it for real it's

:14:36. > :14:38.I mean, it's like something out of The Martian or

:14:39. > :14:59.Built in 2012, the Halley Research Station consists of 'eight huge

:15:00. > :15:00.to maintain life in a hostile environment.

:15:01. > :15:04.to take you through from one end, right through to the other.

:15:05. > :15:13.So, we're starting in the quiet room, which doubles up as a library,

:15:14. > :15:15.and we move out of there into the first part

:15:16. > :15:18.Now, we're into a sort of admin area.

:15:19. > :15:21.We've got the communications room on the left.

:15:22. > :15:26.We've got the equipment here, on the right, in case of fire,

:15:27. > :15:30.and a board up here where you have to tag in and tag out -

:15:31. > :15:32.safety, a very big concern here at the moment.

:15:33. > :15:36.Now, we're moving through into the main dining

:15:37. > :15:42.So, this is the real, sort of, hub of the station far

:15:43. > :15:48.Oh, and along the wall on this corridor that

:15:49. > :15:50.we're just coming past, all the pictures of past winterers,

:15:51. > :15:59.starting from 1956, right through to the present day.

:16:00. > :16:03.And, of course, there's me and the rest of the guys in 1981,

:16:04. > :16:06.and you'll notice, back then, no women.

:16:07. > :16:14.Now, you'll start to hear a bit of a hum.

:16:15. > :16:19.We're going outside, through these heavy,

:16:20. > :16:36.And now we're on into the main science area,

:16:37. > :16:45.and now we're going to go up the stairs to the best view

:16:46. > :16:48.in Halley, which is the Met Office observation deck, where you get

:16:49. > :17:12.a panoramic view of the Brunt Ice Shelf.

:17:13. > :17:15.But, today, the very existence of this unique research

:17:16. > :17:18.A huge crack across the Brunt Ice Shelf is expanding,

:17:19. > :17:20.and it may cause the research station to float off

:17:21. > :17:26.For glaciologist Hilmar Gudmundsson, it's like watching geology in fast

:17:27. > :17:33.forward, so this faultline is constantly monitored,

:17:34. > :17:39.and there really is only one way to get a closer look.

:17:40. > :17:42.The last time I abseiled was 35 years ago, so I'm a

:17:43. > :17:49.It's going over the edge that's the worst bit for me.

:17:50. > :17:54.It's quite a long way down, isn't it?

:17:55. > :17:57.I've been looking at this crack from satellite images, and now

:17:58. > :18:02.This is a feature which has been here for ages.

:18:03. > :18:08.When low cloud and snow reflect and diffuse the sunlight,

:18:09. > :18:11.the full extent of the chasm is difficult to see,

:18:12. > :18:23.but when the sun comes out, it's a different story.

:18:24. > :18:25.This is, as you can see, a fairly large crack.

:18:26. > :18:27.It's a chasm, that's what they call it.

:18:28. > :18:31.Yeah, chasm, chasm sounds about right from where I'm sitting.

:18:32. > :18:34.Across, I would say this is maybe 80...80m at least...

:18:35. > :18:39...and the whole thing is getting wider as we speak,

:18:40. > :18:44.Every day? Every day.

:18:45. > :18:48.15cm from this edge here to the other one over there,

:18:49. > :18:53.and it's been going like a clock ever since we started

:18:54. > :18:59.And, Hilmar, the bottom of the chasm, there,

:19:00. > :19:02.looks very different to the ice round about.

:19:03. > :19:05.It's much darker down in the bottom, there.

:19:06. > :19:11.Yeah, I suspect down there we're literally at sea level.

:19:12. > :19:15.It is the colour of the ocean which is causing this slight tint.

:19:16. > :19:19.Hilmar is keen to investigate whether we are actually at sea

:19:20. > :19:25.level, and that means going right to the very bottom of the chasm.

:19:26. > :19:32.It's a huge relief getting down, but we don't take off

:19:33. > :19:37.With the freezing Southern Ocean just beneath our feet,

:19:38. > :19:43.Matt, are you happy with us going down here?

:19:44. > :19:45.If you follow the trail we've made previously,

:19:46. > :19:54.OK. Are you OK?

:19:55. > :20:05.OK, I'll follow - maybe not quite as elegantly as you did.

:20:06. > :20:21.It really is? Oh.

:20:22. > :20:26.Yeah, yeah, I thought we had, maybe, one or two metres

:20:27. > :20:31.So we're on this huge, floating mass of ice,

:20:32. > :20:34.We've had a journey up from the coast of three

:20:35. > :20:41.We've come an hour and a half in from the base, across this

:20:42. > :20:45.featureless snow plain, to this massive, great chasm,

:20:46. > :20:49.and you get down to the bottom of it and you actually

:20:50. > :20:53.It feels like you're in the belly of the ice shelf,

:20:54. > :20:56.and it just brings it home how sort of precarious this whole

:20:57. > :20:59.I guess, because it's always breaking up, it's growing,

:21:00. > :21:04.it's widening by about 15cm a day, the sea ice formation just

:21:05. > :21:09.This rapid expansion of the chasm may prevent sea ice from forming,

:21:10. > :21:12.but it's not the width that's the threat to

:21:13. > :21:18.the Halley Research Station - it's the length.

:21:19. > :21:21.At the same time that this gets wider, it also gets longer

:21:22. > :21:31.So, if it kept on going at that rate, in that direction,

:21:32. > :21:35.eventually it's going to reach the sea at the other side of the ice

:21:36. > :21:37.shelf, and you've got a massive iceberg.

:21:38. > :21:40.And, of course, the problem here is, Halley, the station,

:21:41. > :21:41.is on that developing iceberg.

:21:42. > :21:57.As it lengthens, the greater the chance that the research station

:21:58. > :21:59.finds itself floating into the Southern Ocean.

:22:00. > :22:01.But there's another unusual feature in Halley's design,

:22:02. > :22:04.the first of its kind, which will help it survive.

:22:05. > :22:09.At the bottom of its hydraulic legs are huge skis...

:22:10. > :22:14...so each module will be detached from its neighbour then dragged

:22:15. > :22:20.to a new site in the same way it was brought here four years ago.

:22:21. > :22:23.After extensive surveys, a new location has been found 20km

:22:24. > :22:34.away, safely on the other side of the chasm.

:22:35. > :22:46.And there, Halley can continue its work.

:22:47. > :22:49.Before we head home, at the edge of the ice shelf,

:22:50. > :22:51.all the ship's cargo is finally unloaded.

:22:52. > :22:53.These big, red shipping containers we brought down on the Shackleton

:22:54. > :22:55.contain living accommodation - kitchen, bedrooms,

:22:56. > :22:58.bathrooms, working spaces - and they are going to be used

:22:59. > :23:01.to build a temporary camp for the team up at Halley VI.

:23:02. > :23:04.So it's all hands on deck at the moment, the container

:23:05. > :23:08.is being craned out over the ice onto these heavy-duty sledges that

:23:09. > :23:16.will then be dragged all the way up to Halley VI.

:23:17. > :23:20.Once the temporary accommodation is set up, then Halley can be

:23:21. > :24:02.It is a little bit warmer for us across the UK than it was for Pete,

:24:03. > :24:08.but it is still not pleasant across the UK. A lot of cloud around and

:24:09. > :24:09.outbreaks of rain for many. Hints of sunshine