Melting ice sheet: Is it too late? 6 Minute English

69,486 views ใƒป 2020-11-05

BBC Learning English


์•„๋ž˜ ์˜๋ฌธ์ž๋ง‰์„ ๋”๋ธ”ํด๋ฆญํ•˜์‹œ๋ฉด ์˜์ƒ์ด ์žฌ์ƒ๋ฉ๋‹ˆ๋‹ค. ๋ฒˆ์—ญ๋œ ์ž๋ง‰์€ ๊ธฐ๊ณ„ ๋ฒˆ์—ญ๋ฉ๋‹ˆ๋‹ค.

00:08
Hello. This is 6 Minute English from
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์•ˆ๋…•ํ•˜์„ธ์š”. BBC Learning English์˜ 6๋ถ„ ์˜์–ด์ž…๋‹ˆ๋‹ค
00:10
BBC Learning English. I'm Neil.
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. ์ €๋Š” ๋‹์ž…๋‹ˆ๋‹ค.
00:12
And I'm Georgina.
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๊ทธ๋ฆฌ๊ณ  ์ €๋Š” ์กฐ์ง€๋‚˜์ž…๋‹ˆ๋‹ค.
00:13
With no end in sight to the coronavirus
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์ฝ”๋กœ๋‚˜๋ฐ”์ด๋Ÿฌ์Šค ๋Œ€์œ ํ–‰์˜ ๋์ด ๋ณด์ด์ง€ ์•Š๋Š” ์ƒํ™ฉ์—์„œ
00:16
pandemic, many people can't wait for
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๋งŽ์€ ์‚ฌ๋žŒ๋“ค์ด
00:18
the year 2020 to end.
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2020๋…„์ด ๋๋‚˜๊ธฐ๋ฅผ ๊ธฐ๋‹ค๋ฆด ์ˆ˜ ์—†์Šต๋‹ˆ๋‹ค.
00:20
But with the coronavirus dominating
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๊ทธ๋Ÿฌ๋‚˜ ์ฝ”๋กœ๋‚˜ ๋ฐ”์ด๋Ÿฌ์Šค๊ฐ€
00:22
the newspaper headlines, attention
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์‹ ๋ฌธ ํ—ค๋“œ๋ผ์ธ์„ ์ง€๋ฐฐํ•˜๋ฉด์„œ ์กฐ์šฉํžˆ ์•…ํ™”๋˜๊ณ  ์žˆ๋Š”
00:24
has moved away from an equally
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๋˜‘๊ฐ™์ด
00:26
serious global issue which has
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์‹ฌ๊ฐํ•œ ๊ธ€๋กœ๋ฒŒ ๋ฌธ์ œ์ธ
00:28
quietly been getting worse -
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00:30
climate change.
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๊ธฐํ›„ ๋ณ€ํ™”์—์„œ ๊ด€์‹ฌ์ด ์˜ฎ๊ฒจ์กŒ์Šต๋‹ˆ๋‹ค.
00:31
August 2020 saw the hottest
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2020๋…„ 8์›” ์บ˜๋ฆฌํฌ๋‹ˆ์•„ ๋ฐ์Šค๋ฐธ๋ฆฌ๋Š” ์„ญ์”จ
00:34
temperature recorded anywhere
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00:35
in modern times - 54.4 degrees
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54.4๋„๋กœ ํ˜„๋Œ€ ์—ญ์‚ฌ์ƒ ๊ฐ€์žฅ ๋œจ๊ฑฐ์šด ๊ธฐ์˜จ์„ ๊ธฐ๋กํ–ˆ์Šต๋‹ˆ๋‹ค
00:39
Celsius in California's Death Valley.
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.
00:42
The same month also saw record
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๊ฐ™์€ ๋‹ฌ์—๋Š” ๋˜ํ•œ ๊ธฐ๋ก์ ์ธ
00:44
amounts of ice melting into the
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์–‘์˜ ์–ผ์Œ์ด
00:45
oceans around Greenland and the
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๊ทธ๋ฆฐ๋ž€๋“œ์™€ ๋ถ๊ทน ์ฃผ๋ณ€์˜ ๋ฐ”๋‹ค๋กœ ๋…น๋Š” ๊ฒƒ์„ ๋ณด์•˜์Šต๋‹ˆ๋‹ค.
00:48
Arctic - huge icebergs breaking
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๊ฑฐ๋Œ€ํ•œ ๋น™์‚ฐ์ด
00:50
away from the edge of the ice
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๋น™์ƒ์˜ ๊ฐ€์žฅ์ž๋ฆฌ์—์„œ ๋–จ์–ด์ ธ ๋‚˜์™€
00:52
sheet - a thick layer of ice which
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00:54
has covered a large area
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00:55
for a long time.
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์˜ค๋žœ ์‹œ๊ฐ„ ๋™์•ˆ ๋„“์€ ์ง€์—ญ์„ ๋ฎ๊ณ  ์žˆ๋Š” ๋‘๊บผ์šด ์–ผ์Œ์ธต์ž…๋‹ˆ๋‹ค.
00:57
Greenland's ice sheet is three
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๊ทธ๋ฆฐ๋ž€๋“œ์˜ ๋น™์ƒ์€
00:59
times the size of Texas and almost
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ํ…์‚ฌ์Šค ํฌ๊ธฐ์˜ 3๋ฐฐ์ด๋ฉฐ
01:01
2 kilometres thick. Locked inside
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๋‘๊ป˜๋Š” ๊ฑฐ์˜ 2km์ž…๋‹ˆ๋‹ค. ์ž ๊ธด ๋‚ด๋ถ€์—๋Š”
01:04
is enough water to raise sea levels
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ํ•ด์ˆ˜๋ฉด์„ 6๋ฏธํ„ฐ ๋†’์ด๊ธฐ์— ์ถฉ๋ถ„ํ•œ ๋ฌผ์ด ์žˆ์Šต๋‹ˆ๋‹ค
01:05
by 6 metres.
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.
01:07
But global heating and melting
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๊ทธ๋Ÿฌ๋‚˜ ์ง€๊ตฌ ์˜จ๋‚œํ™”์™€ ๋…น๋Š”
01:09
polar ice has many scientists
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๊ทน์ง€๋ฐฉ์˜ ์–ผ์Œ์€ ๋งŽ์€ ๊ณผํ•™์ž๋“ค์ด
01:11
asking whether it's now too late
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์ง€๊ธˆ ๋ฉˆ์ถ”๊ธฐ์— ๋„ˆ๋ฌด ๋Šฆ์—ˆ๋Š”์ง€ ๋ฌป๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค
01:12
to stop. Have we have reached the
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. ์šฐ๋ฆฌ๋Š”
01:15
point of no return? In this programme,
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๋Œ์•„์˜ฌ ์ˆ˜ ์—†๋Š” ์ง€์ ์— ๋„๋‹ฌํ–ˆ์Šต๋‹ˆ๊นŒ? ์ด ํ”„๋กœ๊ทธ๋žจ์—์„œ
01:17
we'll looking at the effects of climate
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์šฐ๋ฆฌ๋Š” ๊ธฐํ›„
01:19
change on the Arctic and asking
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๋ณ€ํ™”๊ฐ€ ๋ถ๊ทน์— ๋ฏธ์น˜๋Š” ์˜ํ–ฅ์„ ์‚ดํŽด๋ณด๊ณ 
01:21
if it s too late to change.
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๋ณ€ํ™”ํ•˜๊ธฐ์— ๋„ˆ๋ฌด ๋Šฆ์—ˆ๋Š”์ง€ ์งˆ๋ฌธํ•  ๊ฒƒ์ž…๋‹ˆ๋‹ค.
01:23
And learning some of the related
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๊ทธ๋ฆฌ๊ณ  ๊ด€๋ จ
01:25
vocabulary too. Now, Georgina,
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์–ดํœ˜๋„ ๋ฐฐ์›Œ์š”. ์ž, ์กฐ์ง€๋‚˜,
01:27
you mentioned record levels of
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๋‹น์‹ ์€ ๋ถ๊ทน์—์„œ ๊ธฐ๋ก์ ์ธ ์ˆ˜์ค€์˜ ์–ผ์Œ์ด ๋…น๋Š”๋‹ค๊ณ  ์–ธ๊ธ‰ํ–ˆ์ง€๋งŒ
01:29
ice melt in the North Pole but
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01:30
the scale is hard to take in. The
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๊ทธ ๊ทœ๋ชจ๋Š” ๋ฐ›์•„๋“ค์ด๊ธฐ ์–ด๋ ต์Šต๋‹ˆ๋‹ค. ๊ทธ
01:33
amounts are so big they're
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์–‘์€ ๋„ˆ๋ฌด ์ปค์„œ ๊ธฐ๊ฐ€ํ†ค
01:34
measured in gigatonnes - that's
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๋‹จ์œ„๋กœ ์ธก์ •๋ฉ๋‹ˆ๋‹ค. ์ฆ‰,
01:36
a billion metric tonnes.
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10์–ต ๋ฏธํ„ฐํ†ค์ž…๋‹ˆ๋‹ค. 1km x 1km x 1km ํฌ๊ธฐ์˜
01:39
Imagine a giant ice cube
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๊ฑฐ๋Œ€ํ•œ ์–ผ์Œ ์กฐ๊ฐ์„ ์ƒ์ƒํ•ด ๋ณด์‹ญ์‹œ์˜ค
01:41
1 kilometre by 1 kilometre
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01:43
by 1 kilometre.
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.
01:45
So my quiz question is this:
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์ œ ํ€ด์ฆˆ ์งˆ๋ฌธ์€ ์ด๊ฒƒ์ž…๋‹ˆ๋‹ค. ๋งค๋…„
01:47
how many gigatonnes of ice
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์–ผ๋งˆ๋‚˜ ๋งŽ์€ ๊ธฐ๊ฐ€ํ†ค์˜ ์–ผ์Œ์ด
01:49
are now melting into the ocean
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๋ฐ”๋‹ค๋กœ ๋…น๊ณ  ์žˆ์Šต๋‹ˆ๊นŒ
01:50
every year? Is it: a) 450 gigatonnes?,
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? a) 450๊ธฐ๊ฐ€ํ†ค์ž…๋‹ˆ๊นŒ,
01:55
b) 500 gigatonnes?, or
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b) 500๊ธฐ๊ฐ€ํ†ค์ž…๋‹ˆ๊นŒ,
01:57
c) 550 gigatonnes?
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c) 550๊ธฐ๊ฐ€ํ†ค์ž…๋‹ˆ๊นŒ?
01:59
I'll take a guess at b)
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b)
02:01
500 gigatonnes.
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500๊ธฐ๊ฐ€ํ†ค์„ ์ถ”์ธกํ•˜๊ฒ ์Šต๋‹ˆ๋‹ค.
02:04
OK, Georgina, we'll find out
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์ข‹์•„์š”, ์กฐ์ง€๋‚˜, ๋‚˜์ค‘์— ์•Œ์•„๋ณผ๊ฒŒ์š”
02:05
later. Now, glaciologist Michalea
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. ํ˜„์žฌ ๋น™ํ•˜ํ•™์ž์ธ Michalea
02:09
King has been monitoring the
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King์€
02:11
melting of Arctic ice by satellite.
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์œ„์„ฑ์œผ๋กœ ๋ถ๊ทน ์–ผ์Œ์ด ๋…น๋Š” ๊ฒƒ์„ ๋ชจ๋‹ˆํ„ฐ๋งํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
02:13
Here she is answering a question
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์—ฌ๊ธฐ์—์„œ ๊ทธ๋…€๋Š” ๋น™์ƒ์˜ ํŒŒ๊ดด๊ฐ€ ์ด์ œ ํ”ผํ•  ์ˆ˜ ์—†๋Š”์ง€์— ๋Œ€ํ•œ
02:15
from BBC World Service programme,
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BBC World Service ํ”„๋กœ๊ทธ๋žจ์ธ
02:17
Science in Action, on whether the
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Science in Action์˜ ์งˆ๋ฌธ์— ๋‹ตํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
02:19
destruction of the ice sheet is
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02:21
now unavoidable:
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02:23
If we were to say ... define a
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02:26
tipping point as a shift from
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02:27
one stable dynamic state to
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02:30
another, this certainly meets
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02:32
that criteria, because we're
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02:35
seeing now that the ice sheet
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02:36
was more or less in balance prior
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02:38
to 2000 where the amount of ice
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2000๋…„ ์ด์ „์—๋Š” ๋น™ํ•˜์—์„œ ํ˜๋Ÿฌ๋‚˜์˜จ ์–ผ์Œ์˜ ์–‘์ด
02:41
being drained from the glaciers
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02:42
was approximately equal to
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02:44
what we are gaining on the
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02:45
surface via snow every year.
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๋งค๋…„ ๋ˆˆ์„ ํ†ตํ•ด ํ‘œ๋ฉด์—์„œ ์–ป๋Š” ์–‘๊ณผ ๊ฑฐ์˜ ๊ฐ™์•˜์Šต๋‹ˆ๋‹ค. ๋…„๋„.
02:49
Ice is made from snow falling on
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์–ผ์Œ์€ ๊ทธ๋ฆฐ๋ž€๋“œ์˜ ๋น™ํ•˜์— ๋–จ์–ด์ง€๋Š” ๋ˆˆ์œผ๋กœ ๋งŒ๋“ค์–ด์ง‘๋‹ˆ๋‹ค.
02:51
Greenland's glaciers - large,
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ํฌ๊ณ 
02:52
slow-moving masses of ice.
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๋Š๋ฆฌ๊ฒŒ ์›€์ง์ด๋Š” ์–ผ์Œ ๋ฉ์–ด๋ฆฌ์ž…๋‹ˆ๋‹ค.
02:55
At the same time though, ice is
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๊ทธ๋Ÿฌ๋‚˜ ๋™์‹œ์— ์–ผ์Œ
02:56
also lost through melting.
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๋„ ๋…น์œผ๋ฉด์„œ ์†์‹ค๋ฉ๋‹ˆ๋‹ค. ์–ผ์Œ์„ ๋งŒ๋“ค๊ณ  ๋…น์ด๋Š”
02:58
These two processes of
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์ด ๋‘ ๊ฐ€์ง€ ๊ณผ์ •์€ ์„œ๋กœ
03:00
making and melting ice kept
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03:02
the ice level in balance - having
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03:04
different parts or elements
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๋‹ค๋ฅธ ๋ถ€๋ถ„์ด๋‚˜ ์š”์†Œ๋ฅผ
03:05
arranged in the correct
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์˜ฌ๋ฐ”๋ฅธ
03:07
proportions. Essentially the
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๋น„์œจ๋กœ ๋ฐฐ์—ดํ•˜์—ฌ ์–ผ์Œ ๋†’์ด์˜ ๊ท ํ˜•์„ ์œ ์ง€ํ–ˆ์Šต๋‹ˆ๋‹ค. ๋ณธ์งˆ์ ์œผ๋กœ
03:09
melting ice was replaced
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๋…น๋Š” ์–ผ์Œ์€
03:10
by newly frozen ice.
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์ƒˆ๋กœ ์–ผ์–ด๋ถ™์€ ์–ผ์Œ์œผ๋กœ ๋Œ€์ฒด๋˜์—ˆ์Šต๋‹ˆ๋‹ค.
03:12
But now, the glaciers are
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๊ทธ๋Ÿฌ๋‚˜ ์ด์ œ ๋น™ํ•˜๋Š”
03:14
shrinking faster than new ice
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์ƒˆ๋กœ์šด ์–ผ์Œ์ด ์Œ“์ด๋Š” ๊ฒƒ๋ณด๋‹ค ๋” ๋นจ๋ฆฌ ์ค„์–ด๋“ค๊ณ 
03:16
is being accumulated and the
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์žˆ์œผ๋ฉฐ ์ƒํ™ฉ์€
03:17
situation may have reached
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03:19
a tipping point - the time at
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์ „ํ™˜์ , ์ฆ‰
03:21
which a change or an effect
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๋ณ€ํ™”๋‚˜ ์˜ํ–ฅ์„
03:22
cannot be stopped.
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๋ฉˆ์ถœ ์ˆ˜ ์—†๋Š” ์‹œ์ ์— ๋„๋‹ฌํ–ˆ์„ ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
03:24
So, does this mean that global
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๊ทธ๋ ‡๋‹ค๋ฉด ์ด๊ฒƒ์€ ์ธ๊ฐ„์ด ๋Œ€๊ธฐ ์ค‘์œผ๋กœ ๋ฐฐ์ถœํ•˜๋Š” ์˜จ์‹ค ๊ฐ€์Šค์˜ ์–‘๊ณผ๋Š” ๋ณ„๊ฐœ๋กœ ์ง€๊ตฌ
03:26
heating and ice melting are now
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์˜จ๋‚œํ™”์™€ ์–ผ์Œ ์œตํ•ด๊ฐ€
03:28
running automatically, separate
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์ž๋™์œผ๋กœ ์ง„ํ–‰๋˜๊ณ  ์žˆ๋‹ค๋Š” ์˜๋ฏธ์ž…๋‹ˆ๊นŒ
03:29
from the amount of greenhouse
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03:31
gases humans are pumping into
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03:32
the atmosphere? And does that
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? ๊ทธ๋ฆฌ๊ณ  ๊ทธ๊ฒƒ์€ ํ–‰์„ฑ์„ ํฌ๊ธฐ
03:34
mean should just give up on
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ํ•ด์•ผ ํ•œ๋‹ค๋Š” ๊ฒƒ์„ ์˜๋ฏธํ•ฉ๋‹ˆ๊นŒ
03:36
the planet?
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?
03:37
In fact, the situation is far from
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์‚ฌ์‹ค
03:39
simple, as Michalea King explains
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Michalea King์ด
03:41
here to BBC World Service programme,
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BBC World Service ํ”„๋กœ๊ทธ๋žจ์ธ
03:43
Science in Action:
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Science in Action์—์„œ ์„ค๋ช…ํ•œ ๊ฒƒ์ฒ˜๋Ÿผ ์ƒํ™ฉ์€ ๋‹จ์ˆœํ•˜์ง€ ์•Š์Šต๋‹ˆ๋‹ค.
03:46
We can definitely control the rate of
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03:49
mass loss, so it's definitely not a
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03:52
'throw your hands up' and jus
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03:54
not do anything about it - give up
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๊ทธ๊ฒƒ์— ๋Œ€ํ•ด ๋ฌด์—‡์ด๋“  -
03:56
on the ice sheet kind of situation -
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๋น™์ƒ ์ข…๋ฅ˜์˜ ์ƒํ™ฉ์„ ํฌ๊ธฐํ•˜์‹ญ์‹œ์˜ค -
03:57
that's certainly not the message
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๊ทธ๊ฒƒ์€ ํ™•์‹คํžˆ
03:59
I want to send... but it does seem
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๋‚ด๊ฐ€ ๋ณด๋‚ด๊ณ  ์‹ถ์€ ๋ฉ”์‹œ์ง€๊ฐ€ ์•„๋‹™๋‹ˆ๋‹ค... ํ•˜์ง€๋งŒ
04:01
likely that we will continue to lose
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์šฐ๋ฆฌ๋Š” ๊ณ„์†ํ•ด์„œ
04:03
mass... but of course, a slow rate
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์งˆ๋Ÿ‰์„ ์žƒ์„ ๊ฒƒ ๊ฐ™์Šต๋‹ˆ๋‹ค... ํ•˜์ง€๋งŒ ๋ฌผ๋ก  ๋Š๋ฆฐ ์†๋„
04:06
of mass loss is highly preferred
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์˜ ์งˆ๋Ÿ‰ ์†์‹ค์€
04:08
to large annual losses every year.
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๋งค๋…„ ํฐ ์—ฐ๊ฐ„ ์†์‹ค๋ณด๋‹ค ์„ ํ˜ธ๋ฉ๋‹ˆ๋‹ค.
04:12
Michalea thinks that changes in
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Michalea๋Š”
04:14
human activity can still slow the
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์ธ๊ฐ„ ํ™œ๋™์˜ ๋ณ€ํ™”๊ฐ€ ์—ฌ์ „ํžˆ
04:16
rate - or speed at which something
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์–ด๋–ค ์ผ์ด
04:18
happens, in this case the speed of
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์ผ์–ด๋‚˜๋Š” ์†๋„, ์ฆ‰
04:20
Greenland's ice sheet melting.
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๊ทธ๋ฆฐ๋ž€๋“œ์˜ ๋น™์ƒ์ด ๋…น๋Š” ์†๋„๋ฅผ ๋Šฆ์ถœ ์ˆ˜ ์žˆ๋‹ค๊ณ  ์ƒ๊ฐํ•ฉ๋‹ˆ๋‹ค.
04:23
She's convinced it's not too late
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๊ทธ๋…€๋Š” ์ง€๊ตฌ๋ฅผ ๊ตฌํ•˜๊ธฐ ์œ„ํ•ด ์ง‘๋‹จ ํ–‰๋™์„ ์ทจํ•˜๊ธฐ์— ๋„ˆ๋ฌด ๋Šฆ์ง€ ์•Š์•˜๋‹ค๊ณ  ํ™•์‹ ํ•˜๋ฏ€๋กœ
04:24
for collective action to save the
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04:26
planet, so it's not yet time to
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์•„์ง
04:28
'throw your hands up' - an idiom
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'์†์„ ์œ„๋กœ ๋ป—์„' ๋•Œ๊ฐ€ ์•„๋‹™๋‹ˆ๋‹ค
04:30
meaning to show frustration and
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04:32
despair when a situation becomes
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04:34
so bad that you give up or submit.
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.
04:37
It's a positive message but one
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๊ทธ๊ฒƒ์€ ๊ธ์ •์ ์ธ ๋ฉ”์‹œ์ง€์ด์ง€๋งŒ ๋„ˆ๋ฌด ๋Šฆ๊ธฐ
04:38
which calls for everyone to do
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04:40
what they can before it really
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์ „์— ๋ชจ๋‘๊ฐ€ ํ•  ์ˆ˜ ์žˆ๋Š” ์ผ์„ ํ•˜๋„๋ก ์š”๊ตฌํ•˜๋Š” ๋ฉ”์‹œ์ง€์ž…๋‹ˆ๋‹ค
04:42
is too late.
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.
04:43
Because the rate of ice melt is
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์–ผ์Œ์ด ๋…น๋Š” ์†๋„๊ฐ€
04:45
still increasing, right, Neil?
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์—ฌ์ „ํžˆ ์ฆ๊ฐ€ํ•˜๊ณ  ์žˆ๊ธฐ ๋•Œ๋ฌธ์ด์ฃ , ๋‹?
04:47
Yes, that s right - in fact, that
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๋„ค, ๋งž์Šต๋‹ˆ๋‹ค. ์‚ฌ์‹ค
04:48
was my quiz question, Georgina...
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์ œ ํ€ด์ฆˆ ์งˆ๋ฌธ์ด์—ˆ์Šต๋‹ˆ๋‹ค, Georgina...
04:50
do you remember?
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๊ธฐ์–ต๋‚˜์„ธ์š”?
04:51
Yes, you asked me how many
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์˜ˆ,
04:53
gigatonnes of Greenland's ice sheet
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๊ทธ๋ฆฐ๋ž€๋“œ ๋น™์ƒ์ด
04:55
are now melting every year. I said
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๋งค๋…„ ๋ช‡ ๊ธฐ๊ฐ€ํ†ค์”ฉ ๋…น๊ณ  ์žˆ๋Š”์ง€ ๋ฌผ์—ˆ์Šต๋‹ˆ๋‹ค. ๋‚˜๋Š”
04:58
b) 500 gigatonnes.
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b) 500๊ธฐ๊ฐ€ํ†ค์ด๋ผ๊ณ  ๋งํ–ˆ๋‹ค.
05:00
And you were correct! In fact, some
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๊ทธ๋ฆฌ๊ณ  ๋‹น์‹ ์ด ๋งž์•˜์Šต๋‹ˆ๋‹ค! ์‚ฌ์‹ค,
05:03
of these giant ice cubes are like
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์ด ๊ฑฐ๋Œ€ํ•œ ์–ผ์Œ ์กฐ๊ฐ ์ค‘ ์ผ๋ถ€๋Š”
05:05
small towns, almost a kilometre tall!
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๊ฑฐ์˜ 1km ๋†’์ด์˜ ์ž‘์€ ๋งˆ์„๊ณผ ๊ฐ™์Šต๋‹ˆ๋‹ค!
05:08
So there's still work to be done.
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๊ทธ๋ž˜์„œ ์•„์ง ํ•ด์•ผ ํ•  ์ผ์ด ์žˆ์Šต๋‹ˆ๋‹ค.
05:10
In this programme, we've been
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์ด ํ”„๋กœ๊ทธ๋žจ์—์„œ ์šฐ๋ฆฌ๋Š”
05:11
looking at the rate - or speed -
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05:13
of ice melt in Greenland's ice
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05:15
sheet - the thick layer of ice
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05:17
covering a large area of the Arctic.
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๋ถ๊ทน์˜ ๋„“์€ ์ง€์—ญ์„ ๋ฎ๊ณ  ์žˆ๋Š” ๋‘๊บผ์šด ์–ผ์Œ์ธต์ธ ๊ทธ๋ฆฐ๋ž€๋“œ์˜ ๋น™์ƒ์—์„œ ์–ผ์Œ์ด ๋…น๋Š” ์†๋„ ๋˜๋Š” ์†๋„๋ฅผ ์‚ดํŽด๋ณด์•˜์Šต๋‹ˆ๋‹ค.
05:20
Previously, the melting ice was
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์ด์ „์—๋Š” ๋…น๋Š” ์–ผ์Œ์ด ๋น™ํ•˜
05:21
replaced by newly formed ice on
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์— ์ƒˆ๋กœ ํ˜•์„ฑ๋œ ์–ผ์Œ, ์ฆ‰ ๋Š๋ฆฌ๊ฒŒ ์›€์ง์ด๋Š”
05:23
glaciers - large masses of
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ํฐ ๋ฉ์–ด๋ฆฌ์˜
05:25
slow-moving ice. This kept the
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์–ผ์Œ์œผ๋กœ ๋Œ€์ฒด๋˜์—ˆ์Šต๋‹ˆ๋‹ค. ์ด๊ฒƒ์€
05:28
Arctic in balance having
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05:29
different elements arranged
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์„œ๋กœ ๋‹ค๋ฅธ ์š”์†Œ๊ฐ€
05:31
in proportion.
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๋น„๋ก€ํ•˜์—ฌ ๋ฐฐ์—ด๋˜์–ด ๋ถ๊ทน์˜ ๊ท ํ˜•์„ ์œ ์ง€ํ–ˆ์Šต๋‹ˆ๋‹ค.
05:32
But the effects of global
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๊ทธ๋Ÿฌ๋‚˜ ์ง€๊ตฌ ์˜จ๋‚œํ™”์˜ ์˜ํ–ฅ์œผ๋กœ ํ‹ฐํ•‘ ํฌ์ธํŠธ๋ผ๊ณ  ํ•˜๋Š”
05:34
heating have brought us
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05:35
close to a point of no return,
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๋˜๋Œ๋ฆด ์ˆ˜ ์—†๋Š” ์ง€์ , ์ฆ‰
05:36
called a tipping point - the
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05:38
time at which a change or an
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๋ณ€ํ™”๋‚˜
05:40
effect cannot be stopped.
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์˜ํ–ฅ์„ ๋ฉˆ์ถœ ์ˆ˜ ์—†๋Š” ์‹œ์ ์— ๊ฐ€๊นŒ์›Œ์กŒ์Šต๋‹ˆ๋‹ค.
05:41
The situation is serious but
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์ƒํ™ฉ์€ ์‹ฌ๊ฐํ•˜์ง€๋งŒ
05:43
there's still time to take action
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05:45
and not simply throw your
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๋‹จ์ˆœํžˆ
05:46
hands up - show frustration and
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์†์„ ์œ„๋กœ ๋˜์ง€๋Š” ๊ฒƒ์ด ์•„๋‹ˆ๋ผ ์กฐ์น˜๋ฅผ ์ทจํ•  ์‹œ๊ฐ„์ด ์•„์ง ๋‚จ์•„ ์žˆ์Šต๋‹ˆ๋‹ค.
05:48
despair when you want to give up.
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ํฌ๊ธฐํ•˜๊ณ  ์‹ถ์„ ๋•Œ ์ขŒ์ ˆ๊ณผ ์ ˆ๋ง์„ ๋ณด์—ฌ์ฃผ์‹ญ์‹œ์˜ค.
05:50
That's all for this programme, but if
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์ด๊ฒƒ์ด ์ด ํ”„๋กœ๊ทธ๋žจ์˜ ์ „๋ถ€์ž…๋‹ˆ๋‹ค. ๊ทธ๋Ÿฌ๋‚˜
05:52
you want to find out more about
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05:53
climate change and Greenland's ice
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๊ธฐํ›„ ๋ณ€ํ™”์™€ ๊ทธ๋ฆฐ๋ž€๋“œ์˜
05:55
sheets, search BBC's Science in
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๋น™์ƒ์— ๋Œ€ํ•ด ๋” ์•Œ๊ณ  ์‹ถ๋‹ค๋ฉด BBC์˜ ๊ณผํ•™
05:57
Action website.
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์‹ค์ฒœ ์›น์‚ฌ์ดํŠธ๋ฅผ ๊ฒ€์ƒ‰ํ•˜์‹ญ์‹œ์˜ค.
05:58
And for more trending topics
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๊ทธ๋ฆฌ๊ณ  ๋” ๋งŽ์€ ์ธ๊ธฐ ์ฃผ์ œ
05:59
and useful vocabulary, remember
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์™€ ์œ ์šฉํ•œ ์–ดํœ˜๋ฅผ ๋ณด๋ ค๋ฉด
06:01
to join us again soon at 6 Minute
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๊ณง 6 Minute English์— ๋‹ค์‹œ ์ฐธ์—ฌํ•˜์„ธ์š”
06:03
English. Bye for now!
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. ์ง€๊ธˆ์€ ์•ˆ๋…•!
06:05
Goodbye!
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์•ˆ๋…•ํžˆ ๊ฐ€์„ธ์š”!
์ด ์›น์‚ฌ์ดํŠธ ์ •๋ณด

์ด ์‚ฌ์ดํŠธ๋Š” ์˜์–ด ํ•™์Šต์— ์œ ์šฉํ•œ YouTube ๋™์˜์ƒ์„ ์†Œ๊ฐœํ•ฉ๋‹ˆ๋‹ค. ์ „ ์„ธ๊ณ„ ์ตœ๊ณ ์˜ ์„ ์ƒ๋‹˜๋“ค์ด ๊ฐ€๋ฅด์น˜๋Š” ์˜์–ด ์ˆ˜์—…์„ ๋ณด๊ฒŒ ๋  ๊ฒƒ์ž…๋‹ˆ๋‹ค. ๊ฐ ๋™์˜์ƒ ํŽ˜์ด์ง€์— ํ‘œ์‹œ๋˜๋Š” ์˜์–ด ์ž๋ง‰์„ ๋”๋ธ” ํด๋ฆญํ•˜๋ฉด ๊ทธ๊ณณ์—์„œ ๋™์˜์ƒ์ด ์žฌ์ƒ๋ฉ๋‹ˆ๋‹ค. ๋น„๋””์˜ค ์žฌ์ƒ์— ๋งž์ถฐ ์ž๋ง‰์ด ์Šคํฌ๋กค๋ฉ๋‹ˆ๋‹ค. ์˜๊ฒฌ์ด๋‚˜ ์š”์ฒญ์ด ์žˆ๋Š” ๊ฒฝ์šฐ ์ด ๋ฌธ์˜ ์–‘์‹์„ ์‚ฌ์šฉํ•˜์—ฌ ๋ฌธ์˜ํ•˜์‹ญ์‹œ์˜ค.

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