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Antarctica: The Climate Frontline - SDG Media Zone | 2025 UN Ocean Conference

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Antarctica: The Climate Frontline - SDG Media Zone | 2025 UN Ocean Conference

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0:00

Hello everyone, welcome to the STG media

0:03

zone. We're live from the UN Ocean

0:04

Conference here in Nice, France. Uh the

0:08

next session is with Mr. Ragi Omar,

0:10

international news affairs analyst with

0:13

ITV and he will be connecting with

0:16

Martin Stew, science correspondent who

0:18

is live from Antarctica. Over to you

0:20

guys.

0:20

>> Thank you very much indeed and thanks

0:22

for uh coming. Um this uh session um

0:26

report is called Antarctica, the climate

0:29

front line. Now Antarctica is warming

0:31

fast. In fact, it's 3° hotter, I

0:34

believe, since the 1950s, putting

0:36

wildlife and the global climate at risk.

0:40

It's also home to the Antarctic

0:43

circumpolar current, the only ocean

0:46

current linking all major oceans. Now,

0:49

record low sea ice means that this is

0:52

the latest winter a ship has reached um

0:55

uh Antarctica. Scientists are studying

0:57

melting glacias, nutrient release, and

1:01

underwater tsunamis caused by ice

1:03

breakoffs. Now, ITV News's science team,

1:06

as you were just hearing, joins the

1:08

boat, the RRS

1:11

David Atenburgh, for a month-long

1:13

mission with exclusive access to British

1:16

Antarctic Survey scientists. What

1:18

happens in Antarctica, of course,

1:21

doesn't stay in Antarctica and what

1:23

scientists uncover could shape our

1:25

warming world's future. And I'm

1:27

delighted to say that I'm now joined by

1:28

my colleague Martin Stew. Um Martin,

1:32

just tell us where you are and how your

1:34

journey on the RRS David Asra has gone.

1:38

>> Yeah, hello conference from Antarctica.

1:41

As you say, I am on board the Sir David

1:43

Atenburgh, a research ship run by the

1:45

British Antarctic Survey. It's the UK's

1:48

largest floating laboratory. And we're

1:50

currently 67° south deep with inside the

1:53

Antarctic uh uh circle. And you may be

1:56

able to see behind me a large glacia

2:00

front. This is just one of many places

2:02

uncharted water. We are currently where

2:04

we're having a look. And one thing the

2:05

science have noticed in the last couple

2:07

of hours is that we've been able to get

2:08

much closer to the glasses than we

2:10

thought. And the reason is firstly that

2:13

there's a real lack of sea ice around

2:15

making moving around much easier. But

2:17

secondly, this water is far deeper and

2:20

it always used to be the thought that

2:21

the main melting happening in Antarctica

2:24

was from the atmosphere, from air

2:26

temperatures. What we're seeing

2:27

increasingly is that a lot of that

2:29

warming is coming from the ocean. And

2:32

the fact that this glacia wall sinks

2:34

potentially several hundred meters below

2:36

the ocean just goes to show how much of

2:38

that ice is exposed to the warming ocean

2:41

and how much that is going to impact the

2:43

speeding up of the glacias. It's been an

2:46

incredible trip to get down here. It's

2:47

too dark and too dangerous to fly. So we

2:50

sailed across Drake Passage, one of the

2:52

most dangerous stretches of water with

2:55

huge waves often. [clears throat] And we

2:57

got down here and as we got our first

2:59

glimpse of the continent, it is

3:00

absolutely stunning. You know, you sail

3:02

along and there's penguins swimming

3:04

alongside you, there's seals. And one

3:07

day we counted 115 humpback whales. And

3:10

I think that's a real lesson for the

3:12

topics going on at the conference in

3:14

Nice today because obviously those

3:16

whales were hunted to near oblivion. The

3:18

hunting ban came in, humans took action,

3:21

and now they're coming back. So, it's

3:23

been a real kind of visceral lesson to

3:25

me that actually where we do take

3:28

action, we can make a difference.

3:30

>> And um what else has really surprised

3:32

you and the scientists in terms of your

3:34

journey and what you've seen, Martin?

3:38

>> Well, that sea ice thing really, I mean,

3:40

less so the scientists than some of the

3:42

sailors on board. I was talking to one

3:44

guy, his he's been sailing on British

3:46

Antarctic survey ships for 39 years. His

3:48

father did the same before him. and he

3:51

was stood out on deck in a t-shirt in

3:54

June sailing through a stretch which

3:57

would and should have been

3:59

[clears throat] completely frozen shut

4:00

and he was you know gobsmacked really

4:04

that it was open and available to sail

4:06

through at this time if if nothing is a

4:09

more visceral sense of the fact that our

4:10

ch climate is changing it has been that

4:13

and there's lots of things that

4:14

scientists are looking at as you alluded

4:16

to one of them is to do with underwater

4:19

tsunamis and Two of the scientists are

4:21

on board, you're going to hear from

4:22

later on in this session. Six years ago,

4:25

they were stood and they looked at a

4:28

glacia and they saw it carve in front of

4:29

them is where the ice falls into the

4:30

ocean. Somewhere between 3 and 20

4:33

million tons of ice fell into the ocean

4:36

in front of them. That obviously caused

4:37

waves on the surface, but it causes this

4:39

mixing underneath the ocean. And that's

4:42

what they've been studying. And lo and

4:44

behold, when we were on the ship this

4:46

time, we were stood up on the bridge at

4:49

night in the winter when you do not

4:51

really expect carving to be happening.

4:52

And they saw exactly the same glacia

4:54

carve again. Now, it wasn't as much for

4:58

ice falling ocean this time, but it's

5:00

perhaps more worrying that it's

5:02

happening in the winter. So, the fact

5:04

they're able to gather data in these

5:06

winter months that they never normally

5:07

can could potentially be invaluable. And

5:10

Martin, you're there because we are

5:12

doing a special week's reporting on the

5:16

Antarctic and on uh the climate crisis

5:19

as it affects oceans. Now, tell us about

5:21

it and introduce a a segment of your

5:24

report for us, please.

5:27

>> Yeah, absolutely. So, it's a a unique

5:28

opportunity to be on this ship and we

5:30

wanted to give viewers across the UK

5:33

and the world digitally as much of a

5:36

sense of how this climate is changing.

5:38

So, we've got climate stories. We've

5:40

also got stories looking at wildlife.

5:42

We've got stories of hope as well.

5:43

Species like those whales rebounding

5:46

back. We're trying to capture exactly

5:48

what goes on and just how challenging it

5:50

is to do science down here. That's going

5:53

to be played out across the next two

5:55

weeks. I've got a colleague in the

5:57

Bahamas looking at how the sea level

5:58

rises triggered by glasses like the one

6:01

behind me will be impacting places like

6:04

that. not to mention coverage in the UK

6:07

to see the impacts at home as well. So,

6:11

the first report I'm going to show you

6:12

is the lead package which is going to be

6:14

playing tonight and after that I've got

6:16

a Q&A session with two of the scientists

6:18

on board where I pose to them some of

6:21

the questions which uh university

6:23

students have sent in to the UN. So, I

6:25

hope you enjoy this report.

6:30

Sunrise 11 a.m. Our first glimpse of

6:34

Antarctica. A frozen wilderness warming

6:38

before our eyes.

6:41

No British ship has sailed here at this

6:43

time of year since Shackleton's

6:45

Endurance. That was crushed by ice.

6:51

Now we glide through almost open water.

6:55

We shouldn't be able to make this

6:56

journey. The very fact we can in

6:59

midpolar winter is a warning shot across

7:02

the boughs from mother nature.

7:05

>> Gee, aren't you going to be cold?

7:06

>> Just a little bit.

7:07

>> Bosen Dave has been making this journey

7:10

for 39 years. Never this late in the

7:13

winter.

7:15

>> What do you think it says about how much

7:16

this place is changing the fact we're

7:18

making this journey in June

7:20

>> in global warming kind of thing? It's

7:22

pretty Yeah, it's pretty unusual. That's

7:25

what I mean.

7:26

I don't I wouldn't believe we'd be down

7:28

here at this time.

7:29

>> We sail through a sheltered stretch

7:31

called the Gullet, unencumbered by the

7:34

sea ice, which would have made this

7:35

route to Rother almost impossible in the

7:38

past. The bay next to the British

7:41

Antarctic Survey Station used to be

7:44

frozen by now. Compared to 30 years ago,

7:48

there is now 1.5 million square

7:51

kilometers less sea ice than there used

7:53

to be at this time of the year. That

7:55

equates to an area six times the size of

7:58

the UK.

8:01

>> The retreat in sea ice is linked to the

8:03

warming of the ocean and that's

8:06

something that we know us humans are

8:07

doing. So there's a a direct signal

8:10

there of our activity. Um the

8:12

implications of this are climatic in

8:15

that um it affects how reflective the

8:18

surface of the planet is. So the

8:20

planet's now absorbing more heat from

8:22

the sun than it used to. It also removes

8:24

a protective barrier from around

8:26

Antarctica and can actually contribute

8:28

to the destabilization

8:30

of the ice sheets.

8:31

>> That's what's happened to the Sheldon

8:33

glacia. Without ice acting like a cork,

8:36

it's collapsing into the sea, retreating

8:40

several kilometers and creating this

8:42

entire bay which used to look like land.

8:47

Back on board, Mike and his colleague

8:49

Rianan revisit a different glacia they

8:52

saw carve three million tons of ice in

8:55

the summer six years ago.

8:58

>> Unbelievably, they film it happening

9:01

again.

9:02

>> Oh my god. This time at night in the

9:05

winter.

9:06

>> That's That's disaster from underneath.

9:09

>> To stand there and see it directly in

9:10

front of us was incredible. It was

9:13

really unexpected. It really hit home

9:15

that we're seeing some rapid changes to

9:17

the region and we don't know what the

9:18

consequences of that will be.

9:21

>> The theory is ice collapse on this scale

9:24

causes underwater tsunamis.

9:26

>> So I'm going to switch this one on so it

9:28

>> the team are monitoring water samples to

9:31

understand how those waves release heat,

9:34

carbon, and nutrients into the

9:36

environment, not to mention huge amounts

9:39

of fresh water. Latest modeling shows

9:42

even in the unlikely case we can cap

9:45

global warming to 1 and a half degrees,

9:48

melting polar ice will push sea levels

9:51

up by a centimeter a year come the end

9:53

of the century. A rate fast enough to

9:56

tangibly affect our children's lives.

10:00

Hello Nice, from Antarctica. We're stood

10:03

on the peninsula, one of the warmest

10:05

parts of this frozen continent, which is

10:08

changing so rapidly before our eyes.

10:10

We've sailed down the latest in the

10:12

season the British Antarctic Survey have

10:14

ever done. And I'm with some top

10:15

scientists, including to my left,

10:17

Rihanna Jones, who specializes in

10:19

understanding the differences or the way

10:21

that biology and chemistries interact

10:23

within the ocean, and Mike Meredith, who

10:26

is an oceanographer, a climate

10:27

scientist, and a lead author for the

10:29

IPCC. We've got some questions that have

10:31

been sent in. one if you could help me

10:33

answer some of them. The first one comes

10:35

from uh Niha. She says, "What role do

10:37

Antarctic ocean ecosystems play in

10:39

absorbing carbon and how might that

10:42

change as the region warms?"

10:44

>> That's a great question, Niha. Thank

10:45

you. Um so the Antarctic Ocean, the

10:47

Southern Ocean that surrounds Antarctica

10:49

is globally an integral region for

10:52

carbon storage. So the ocean absorbs the

10:55

humanmade atmospheric carbon long term

10:57

for us. does us a climatic favor. In

10:59

fact, and as we see climate warming

11:02

continue, the oceans warm and the

11:04

atmosphere warm, what we're seeing is

11:06

huge changes in the region. What this

11:08

means is, for example, sea ice decline,

11:11

uh, this changes the potentially changes

11:13

the potential for the southern ocean to

11:15

store this carbon forest. And it was

11:17

explained to me, tell me if I've got

11:19

this wrong, but the the less sea ice

11:21

there is, and I think that there's about

11:22

a million square kilometers less sea ice

11:24

now than there was 30 years ago, that

11:27

exposes more of the ocean to wind, which

11:29

whips and stirs things up, and that can

11:31

release carbon and heat. Is that right?

11:33

>> Yes, that's right. So, the deep ocean is

11:35

where most of this carbon is stored. And

11:37

so, as you physically change how the the

11:40

ocean mixes and the ocean cycles, you

11:42

can release some of this carbon from the

11:43

deep ocean back into the atmosphere. and

11:45

the ocean stops being such an effective

11:47

sink for that atmospheric carbon.

11:49

>> Great. Thank you. My next question is uh

11:51

from Jay Whitney from the University of

11:53

Arizona. How does climate change affect

11:55

food resources available for the ocean?

11:58

We've seen some seals out there this

11:59

morning, haven't we?

12:00

>> Yes. So, the uh southern ocean, this

12:02

this ocean we are at right now is a

12:04

highly productive region across the food

12:06

web and that is driven from bottomup uh

12:08

processes. What that means is the ocean

12:11

is nutrient-rich. It's foodrich for the

12:14

photosynthesizing plants of the ocean,

12:15

phytolanton. And these phytolankton

12:18

support the whole food web. So they feed

12:20

the krill, the plankton. And the krill

12:22

are a keystone species for the region.

12:24

They feed animals up the food web such

12:26

as the seals we've seen there this

12:27

morning. Whales that we saw here

12:29

yesterday. And all of these animals are

12:31

at risk from a changing climate.

12:33

>> And one of the you just had a paper

12:35

published to do with nutrients and

12:38

glasses. Is that right?

12:39

>> Yes. Yeah. What we're seeing is as uh

12:41

glacias and ice sheets continue to melt

12:43

and discharge fresh water into the

12:45

ocean, that changes how the ocean itself

12:47

is physically cycling the chem the

12:50

chemistry of the ocean, the nutrient

12:51

supply, and potentially that will have

12:53

impacts again on those primary

12:55

producers, photosynthesizers, and up the

12:57

food web.

12:58

>> Great. Thank you, Mike. I think this

12:59

next one may be for you. Um, how do you

13:02

prepare for unexpected weather events or

13:04

ice conditions while at sea in

13:06

Antarctica? And how does it affect your

13:08

ability to gather data? That's from uh

13:10

Kayla Wrl from Cornell University.

13:12

>> Yeah, it's a great question. Um, working

13:14

in the Antarctic, you can be exposed to

13:16

quite hostile conditions. Um, there are

13:19

very powerful storms here. You've got to

13:21

navigate the ice. Uh, sometimes you've

13:24

got to cope with 24-hour darkness, which

13:25

we're going to be dealing with pretty

13:27

soon. Um, you got to be prepared for

13:29

this. Um, the way you do that is by a

13:33

lot of advance planning.

13:35

>> That's the ship's horn.

13:36

>> That's the ship's horn. [laughter]

13:38

um you've got to have flexibility built

13:40

into your plans um so you can adapt as

13:43

you go um and still get the signs that

13:45

you need to uh delivered. A key thing

13:48

there is to have very robust facilities

13:51

available to you like the ship the Sir

13:53

David Atenburgh which is a very powerful

13:56

very capable ice breaker so it can cope

13:58

with what the Antarctic throws at us uh

14:00

and still get the measurements we need.

14:02

I guess it's contingency after

14:03

contingency. If that breaks, we've got

14:05

plan B and C and D because you can't get

14:07

people out of here, can you? Sometimes,

14:08

>> sometimes not. Um, so you got to be

14:10

self-sufficient. You got to be prepared

14:12

to look after yourselves while you're

14:13

here. You got to have plans out to plan

14:15

zed and beyond. Um, but we've got a lot

14:17

of experience of doing that. So,

14:19

typically, you know, we do get the

14:20

science, we do get the measurements that

14:22

we need.

14:22

>> Great. And one of the final questions

14:24

here, what is an arising issue that

14:26

scientists and marine sciences or

14:28

environmental policy should look at? Uh

14:30

that's from EL Emily Conception from

14:32

East Carolina University.

14:35

>> Uh well, one of the most important

14:36

things we're beginning to understand

14:38

about Antarctica is how rapidly and

14:40

dramatically it can change. You know, we

14:43

develop a scientific understanding, but

14:45

Antarctica continues to surprise us. It

14:48

continues to throw things at us that we

14:49

just hadn't predicted. Um the loss of

14:52

sea ice about a decade ago is a prime

14:54

example of that. uh but also we're

14:56

seeing uh ice being lost from glacias at

14:58

increasingly rapid rates. We can pass

15:01

tipping points uh in which the system

15:04

shifts to an entirely different way of

15:05

working and what we really need to do is

15:08

understand more about where those

15:10

tipping points are, how close we are to

15:12

them and be able to better predict what

15:14

happens once we go past them. Uh that's

15:17

really important understanding because

15:18

that then feeds into policy for setting

15:21

climate uh initiatives uh fisheries

15:24

policy uh marine protected areas all the

15:27

policy domains to try and protect

15:28

Antarctica protect the world uh it comes

15:31

down to trying to get that that

15:33

understanding better

15:34

>> and scale is a massive thing. You were

15:36

telling me that this project you're

15:37

working at the moment called Polo Mint

15:38

was inspired when you saw Glacia carve

15:42

into the ocean and we've just seen the

15:44

terrible pictures from Switzerland of a

15:46

whole village being wiped out by

15:48

something similar happening. But what we

15:50

sort of looked on a small scale

15:51

Antarctica, but it was exactly the same

15:53

size as that event in Switzerland. So

15:55

we're talking about really big impacts

15:57

here, aren't we?

15:58

>> We are. I mean Antarctica is is a really

16:00

big continent and different parts of it

16:02

behave differently. Um but some of the

16:05

changes, some of some of the very sudden

16:07

events you can see like collapsing

16:08

glaciers, like collapsing ice sheets, uh

16:11

very significant huge amounts of ice

16:13

being discharged very very suddenly and

16:15

everything can change. Um and things

16:17

like the terrible event in Switzerland,

16:19

you know, they really bring it home uh

16:21

the actual magnitude of what we're

16:23

seeing here in Antarctica by putting it

16:25

alongside things that people can relate

16:27

to such as settlements, villages, and so

16:29

on. And I've been interested sailing

16:30

down with you guys that there's no doubt

16:33

in your minds that there is serious

16:35

change of foot. It is not going in the

16:37

right direction. But also it's not too

16:39

late. There are some options. And I was

16:41

struck because it's the 40th anniversary

16:42

of the discovery of the hole in the

16:43

ozone layer which was found by your bass

16:46

predecessors discovered down in

16:48

Antarctica. So are you hopeful that the

16:51

science here if policy makers listen to

16:54

the science we can still make a

16:55

difference and make a change?

16:57

>> Absolutely we can. I mean, you're

16:58

absolutely right that, you know, in

17:01

terms of climate change, we're not where

17:02

we want to be. We need more action. We

17:04

need better action. Uh we need much more

17:07

accelerated progress at the policy

17:08

scale. Uh that has to be informed by

17:11

science, which is what we're down here

17:13

doing now. Um but there's still cause

17:16

for hope. Um it isn't game over yet. We

17:19

can still avoid the worst case

17:21

scenarios, the worst um impacts that

17:23

climate change can throw at us. What we

17:26

need to do is really push hard now um

17:29

because the sooner we get the action

17:30

needed um the more we can save in terms

17:33

of the lives and livelihoods around the

17:34

world that are going to be affected by

17:36

it.

17:36

>> Well, I think you couldn't have summed

17:37

it up better. Uh Mike Rian, thank you

17:40

very much and um thank you for having us

17:42

uh in the conference. I hope it all goes

17:44

well.

17:48

>> Great. Thank you very much indeed

17:50

everyone and thank you to Martin and

17:52

everyone on the boat with him. And

17:54

that's the end of the session. Thanks

17:56

for attending.

Interactive Summary

The video discusses the concerning rate at which Antarctica is warming, highlighting that it is 3°C hotter since the 1950s. This warming poses risks to wildlife and the global climate. Scientists are actively studying melting glaciers, nutrient release, and underwater tsunamis caused by ice breakoffs. A significant observation is that warming is increasingly coming from the ocean, not just the atmosphere, as evidenced by glaciers sinking hundreds of meters below the ocean surface. The lack of sea ice is making navigation easier but is a clear sign of climate change. The video also touches upon the recovery of whale populations after hunting bans as a sign of hope and the potential for positive change when action is taken. Scientists are facing challenges in gathering data due to harsh conditions, but are equipped with advanced research vessels and contingency plans. The importance of understanding tipping points in Antarctica's climate system is emphasized for informing policy decisions. The discussion concludes on a hopeful note, suggesting that while more action is needed, it is not too late to avoid the worst-case scenarios of climate change.

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