James Balog: Time-lapse proof of extreme ice loss

180,808 views ใƒป 2009-09-09

TED


์•„๋ž˜ ์˜๋ฌธ์ž๋ง‰์„ ๋”๋ธ”ํด๋ฆญํ•˜์‹œ๋ฉด ์˜์ƒ์ด ์žฌ์ƒ๋ฉ๋‹ˆ๋‹ค.

๋ฒˆ์—ญ: Seongsu JEONG ๊ฒ€ํ† : Juhyeon Kim
00:18
Most of the time, art and science stare at each other
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๊ทธ๋™์•ˆ ์˜ˆ์ˆ ๊ณผ ๊ณผํ•™์€ ์„œ๋กœ์— ๋Œ€ํ•œ
00:22
across a gulf of mutual incomprehension.
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๋ชฐ์ดํ•ด์— ๊ฐ‡ํ˜€์žˆ์—ˆ์Šต๋‹ˆ๋‹ค.
00:25
There is great confusion when the two look at each other.
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์„œ๋กœ์— ๋Œ€ํ•˜๋Š”๋ฐ ํ˜ผ๋ž€์ด ์žˆ์ฃ .
00:30
Art, of course, looks at the world through the psyche,
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์˜ˆ์ˆ ์€ ์„ธ์ƒ์„ ๋ฐ”๋ผ๋ณผ๋•Œ, ๋งˆ์Œ์ด๋‚˜
00:34
the emotions -- the unconscious at times -- and of course the aesthetic.
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๊ฐ์ •, ๋ฌด์˜์‹, ๋ฏธํ•™ ๊ฐ™์€ ์ธก๋ฉด์—์„œ ๋ฐ”๋ผ๋ด…๋‹ˆ๋‹ค.
00:38
Science tends to look at the world through the rational, the quantitative --
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๋ฐ˜๋ฉด์— ๊ณผํ•™์€ ์„ธ์ƒ์„ ํ•ฉ๋ฆฌ์ ์ด๊ณ  ์ •๋Ÿ‰์ ์œผ๋กœ
00:43
things that can be measured and described --
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์ธก์ •ํ•˜๊ณ  ์„ค๋ช…ํ•  ์ˆ˜ ์žˆ๋Š” ๋Œ€์ƒ์œผ๋กœ ๋ฐ”๋ผ๋ณด๋Š”๋ฐ,
00:46
but it gives art a terrific context of understanding.
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์˜ˆ์ˆ ์ ์ธ ์ง€์‹๊ณผ ์ดํ•ด์— ํ•„์š”ํ•œ ํ›Œ๋ฅญํ•œ ๊ทผ๊ฑฐ๋ฅผ ์ œ๊ณตํ•˜์ฃ .
00:50
In the Extreme Ice Survey,
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์šฐ๋ฆฌ๋Š” ๊ทน์ง€ ๋น™ํ•˜ ํƒ์‚ฌ(EIS)์—์„œ
00:54
we're dedicated to bringing those two parts of human understanding together,
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์˜ˆ์ˆ ๊ณผ ๊ณผํ•™ ๋‘ ์ธก๋ฉด์„ ํ•จ๊ป˜ ํฌ์šฉํ•˜๋ ค๊ณ  ์• ์ผ์Šต๋‹ˆ๋‹ค.
00:59
to merging the art and science
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์˜ˆ์ˆ ๊ณผ ๊ณผํ•™์„ ํ•ฉ์นจ์œผ๋กœ์จ
01:01
to the end of helping us understand nature
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์šฐ๋ฆฌ๊ฐ€ ์ž์—ฐ์„ ์ดํ•ดํ•˜๊ณ 
01:04
and humanity's relationship with nature better.
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์ธ๋ฅ˜์™€ ์ž์—ฐ์˜ ๊ด€๊ณ„๋ฅผ ๊ฐœ์„ ํ•˜๋Š”๋ฐ ๋„์›€์ด ๋˜๋„๋ก ๋ง์ž…๋‹ˆ๋‹ค.
01:08
Specifically, I as a person
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ํŠนํžˆ ํ‰์ƒ์„
01:10
who's been a professional nature photographer my whole adult life,
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์ง์—…์ ์ธ ์ž์—ฐ ์‚ฌ์ง„๊ฐ€๋กœ ์‚ด์•„์˜จ ์ €๋Š”
01:14
am firmly of the belief that photography, video, film
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์‚ฌ์ง„๊ณผ ๋น„๋””์˜ค, ์˜ํ™”๊ฐ€
01:18
have tremendous powers for helping us understand
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์ž์—ฐ์„ ์ดํ•ดํ•˜๊ฒŒ ํ•˜๋Š” ์—„์ฒญ๋‚œ ํž˜์„ ๊ฐ€์ง€๊ณ  ์žˆ๊ณ ,
01:22
and shape the way we think about nature
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์ž์—ฐ์— ๋Œ€ํ•œ, ๋˜ ์ธ๊ฐ„๊ณผ ์ž์—ฐ์˜ ๊ด€๊ณ„์— ๋Œ€ํ•œ
01:25
and about ourselves in relationship to nature.
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์ƒ๊ฐ์„ ํ˜•์„ฑํ•œ๋‹ค๊ณ  ๋ฏฟ์Šต๋‹ˆ๋‹ค.โ„ข
01:28
In this project, we're specifically interested, of course, in ice.
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์šฐ๋ฆฌ๋Š” ์ด ํ”„๋กœ์ ํŠธ์—์„œ ํŠนํžˆ ๋น™ํ•˜์— ๊ด€์‹ฌ์„ ๋‘์—ˆ์Šต๋‹ˆ๋‹ค.
01:32
I'm fascinated by the beauty of it, the mutability of it,
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์ €๋Š” ๋น™ํ•˜์˜ ์•„๋ฆ„๋‹ค์›€๊ณผ ๊ฐ€๋ณ€์„ฑ,
01:36
the malleability of it,
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์œ ์—ฐ์„ฑ, ๊ทธ๋ฆฌ๊ณ 
01:38
and the fabulous shapes in which it can carve itself.
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์Šค์Šค๋กœ ๋นš์–ด๋‚ด๋Š” ๋ฉ‹์ง„ ๋ชจ์–‘์— ๋งค๋ฃŒ๋˜์—ˆ์Šต๋‹ˆ๋‹ค.
01:41
These first images are from Greenland.
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์ด ์ฒซ๋ฒˆ์งธ ์‚ฌ์ง„์€ ๊ทธ๋ฆฐ๋ž€๋“œ์—์„œ ์ฐ์€ ๊ฒƒ์ž…๋‹ˆ๋‹ค.
01:43
But ice has another meaning.
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ํ•˜์ง€๋งŒ ๋น™ํ•˜๋Š” ๋˜ ๋‹ค๋ฅธ ์˜๋ฏธ๋ฅผ ๊ฐ€์ง€๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
01:45
Ice is the canary in the global coal mine.
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๋น™ํ•˜๋Š” '์ง€๊ตฌ'๋ผ๋Š” ํƒ„๊ด‘์— ์žˆ๋Š” ์นด๋‚˜๋ฆฌ์•„์™€ ๊ฐ™์Šต๋‹ˆ๋‹ค.
01:48
It's the place where we can see and touch and hear and feel climate change in action.
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๊ธฐํ›„ ๋ณ€ํ™”๋ฅผ ์ง์ ‘ ๋ณด๊ณ  ๋งŒ์ง€๊ณ  ๋“ฃ๊ณ  ๋Š๋‚„ ์ˆ˜ ์žˆ๋Š” ์žฅ์†Œ์ฃ .
01:54
Climate change is a really abstract thing in most of the world.
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์„ธ๊ณ„ ๋Œ€๋ถ€๋ถ„์€ ๊ธฐํ›„๋ณ€ํ™”๋ฅผ ์ถ”์ƒ์ ์ธ ๊ฒƒ์œผ๋กœ ์ƒ๊ฐํ•ฉ๋‹ˆ๋‹ค.
01:58
Whether or not you believe in it is based on your sense of
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๋ฏฟ๊ฑฐ๋‚˜ ๋ง๊ฑฐ๋‚˜, ์—ฌ๋Ÿฌ๋ถ„์€ ๊ธฐํ›„๋ณ€ํ™”๋ฅผ
02:01
is it raining more or is it raining less?
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๋น„๊ฐ€ ๋” ์˜ค๋Š”์ง€ ๋œ ์˜ค๋Š”์ง€
02:03
Is it getting hotter or is it getting colder?
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๋”์›Œ์ง€๋Š”์ง€ ์ถ”์›Œ์ง€๋Š”์ง€ ํ•˜๋Š” ๊ฐ๊ฐ์ด๋‚˜
02:05
What do the computer models say about this, that and the other thing?
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์ปดํ“จํ„ฐ ๋ชจ๋ธ ๋˜๋Š” ์ธก์ •์น˜์— ๊ทผ๊ฑฐํ•ด ๋Š๋ผ๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
02:10
All of that, strip it away. In the world of the arctic and alpine environments,
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๊ทธ๋Ÿฐ ์ถ”์ƒ์ ์ธ ์ธ์‹์€ ๋ฒ„๋ฆฌ์„ธ์š”. ๊ทน์ง€๋ฐฉ๊ณผ ์‚ฐ์•…์ง€๋Œ€์™€ ๊ฐ™์ด
02:14
where the ice is, it's real and it's present.
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๋น™ํ•˜๊ฐ€ ์žˆ๋Š” ๊ณณ์ด๋ผ๋ฉด ๊ธฐํ›„๋ณ€ํ™”๋Š” ํ˜„์‹ค์ด๊ณ , ์‹ค์ œ๋กœ ์กด์žฌํ•˜๋Š” ๊ฒ๋‹ˆ๋‹ค.
02:17
The changes are happening. They're very visible.
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๋ณ€ํ™”๊ฐ€ ์ผ์–ด๋‚˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค. ๋ˆˆ์œผ๋กœ ๋ณผ ์ˆ˜ ์žˆ์ฃ .
02:20
They're photographable. They're measurable.
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์‚ฌ์ง„์œผ๋กœ ์ฐ์„ ์ˆ˜ ์žˆ๊ณ , ์ธก์ • ๊ฐ€๋Šฅํ•ฉ๋‹ˆ๋‹ค.
02:23
95 percent of the glaciers in the world are retreating or shrinking.
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์ „ ์„ธ๊ณ„ ๋น™ํ•˜์˜ 95ํผ์„ผํŠธ๊ฐ€ ํ›„ํ‡ด, ์ˆ˜์ถ•ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
02:28
That's outside Antarctica.
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์ด๊ณณ์€ ๋‚จ๊ทน์˜ ์™ธ๊ณฝ์ž…๋‹ˆ๋‹ค.
02:30
95 percent of the glaciers in the world are retreating or shrinking,
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์ „ ์„ธ๊ณ„ ๋น™ํ•˜์˜ 95ํผ์„ผํŠธ๊ฐ€ ํ›„ํ‡ด, ์ˆ˜์ถ•ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
02:33
and that's because the precipitation patterns and the temperature patterns are changing.
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๊ฐ•์ˆ˜์™€ ์˜จ๋„ ํŒจํ„ด์ด ๋ณ€ํ•˜๊ณ  ์žˆ๊ธฐ ๋•Œ๋ฌธ์ด์ฃ .
02:37
There is no significant scientific dispute about that.
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์ด ์‚ฌ์‹ค์— ๋Œ€ํ•ด์„œ๋Š” ๊ณผํ•™์ ์œผ๋กœ ์ด๊ฒฌ์ด ์—†์Šต๋‹ˆ๋‹ค.
02:41
It's been observed, it's measured, it's bomb-proof information.
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๊ด€์ธก๋˜๊ณ , ์ธก์ •๋œ ์‚ฌ์‹ค์ž…๋‹ˆ๋‹ค. ๋„๋–ก์—†๋Š” ์ •๋ณด์ด์ฃ .
02:44
And the great irony and tragedy of our time
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๊ทธ๋ฆฌ๊ณ  ์ด ์‹œ๋Œ€์˜ ์—„์ฒญ๋‚œ ์•„์ด๋Ÿฌ๋‹ˆ์ด์ž ๋น„๊ทน์ธ ๊ฒƒ์€
02:46
is that a lot of the general public thinks that science is still arguing about that.
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๋งŽ์€ ๋Œ€์ค‘์ด ์ด ๋ฌธ์ œ๋ฅผ ๊ณผํ•™์ž๋“ค์ด ์•„์ง ๋…ผ์Ÿ์ค‘์ด๋ผ๊ณ  ์ƒ๊ฐํ•˜๋Š” ๊ฒƒ์ž…๋‹ˆ๋‹ค.
02:51
Science is not arguing about that.
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๊ณผํ•™๊ณ„์—์„  ์ด ์‚ฌ์‹ค์— ๋Œ€ํ•ด ๋…ผ์Ÿํ•˜์ง€ ์•Š์Šต๋‹ˆ๋‹ค.
02:53
In these images we see ice from enormous glaciers,
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์ด ์˜์ƒ์—์„œ ์šฐ๋ฆฌ๋Š” ๊ฑฐ๋Œ€ํ•œ ๋น™ํ•˜์—์„œ ๋–จ์–ด์ ธ ๋‚˜๊ฐ„ ์–ผ์Œ์„ ๋ณด๊ฒŒ ๋ฉ๋‹ˆ๋‹ค.
02:58
ice sheets that are hundreds of thousands of years old
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์ˆ˜๋ฐฑ๋…„, ์ˆ˜์ฒœ๋…„์— ๊ฑธ์ณ ์ƒ์„ฑ๋œ ๋น™์ƒ์ด
03:00
breaking up into chunks, and chunk by chunk by chunk,
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์กฐ๊ฐ์กฐ๊ฐ ๋ถ€์„œ์ง‘๋‹ˆ๋‹ค.
03:04
iceberg by iceberg, turning into global sea level rise.
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๋น™์‚ฐ์œผ๋กœ ์ชผ๊ฐœ์ ธ์„œ, ์ง€๊ตฌ์˜ ํ•ด์ˆ˜๋ฉด์ด ์ƒ์Šนํ•ฉ๋‹ˆ๋‹ค.
03:07
So, having seen all of this in the course of a 30-year career,
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์ œ ๊ฒฝ๋ ฅ 30๋…„๋™์•ˆ ์ด๊ฒƒ์„ ๋ณด์•„์™”๋Š”๋ฐ,
03:11
I was still a skeptic about climate change until about 10 years ago,
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10๋…„์ „๋งŒํ•ด๋„ ์ €๋Š” ๊ธฐํ›„ ๋ณ€ํ™”์— ๋Œ€ํ•ด ์˜์‹ฌ์ด ๋งŽ์•˜์Šต๋‹ˆ๋‹ค.
03:14
because I thought the story of climate change was based on computer models.
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๊ธฐํ›„๋ณ€ํ™”๋Š” ์ปดํ“จํ„ฐ ๋ชจ๋ธ์— ๊ทผ๊ฑฐํ•œ ์ด์•ผ๊ธฐ๋ผ๊ณ  ์ƒ๊ฐํ–ˆ์ฃ .
03:20
I hadn't realized it was based on concrete measurements
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๊ทธ๋•Œ๋Š” ๊ธฐํ›„ ๋ณ€ํ™”๊ฐ€ ๊ณ ๊ธฐํ›„ํ•™์˜
03:24
of what the paleoclimates -- the ancient climates -- were,
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๊ตฌ์ฒด์ ์ธ ์ธก๋Ÿ‰๋ฐฉ๋ฒ•์— ๊ทผ๊ฑฐํ•œ ๊ฒƒ์ž„์„ ๋ชฐ๋ž์Šต๋‹ˆ๋‹ค.
03:27
as recorded in the ice sheets, as recorded in deep ocean sediments,
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์ด๋ฅผํ…Œ๋ฉด ๋น™์ƒ์ด๋‚˜ ์‹ฌํ•ด ํ‡ด์ ๋ฌผ์˜ ๊ธฐ๋ก,
03:33
as recorded in lake sediments, tree rings,
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ํ˜ธ์ˆ˜ ํ‡ด์ ๋ฌผ, ๋‚˜์ดํ…Œ์˜ ๊ธฐ๋ก
03:35
and a lot of other ways of measuring temperature.
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๊ทธ๋ฆฌ๊ณ  ์˜จ๋„๋ฅผ ์ธก์ •ํ•˜๋Š” ๋‹ค๋ฅธ ๋งŽ์€ ๋ฐฉ๋ฒ•๋“ค ๋ง์ž…๋‹ˆ๋‹ค.
03:39
When I realized that climate change was real, and it was not based on computer models,
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์ œ๊ฐ€ ๊ธฐํ›„๋ณ€ํ™”๊ฐ€ ์‹ค์ œ๋ผ๋Š”๊ฑธ ๊นจ๋‹ฌ์•˜์„ ๋•Œ, ๊ทธ๊ฒƒ์€ ์ปดํ“จํ„ฐ ๋ชจ๋ธ์— ๊ทผ๊ฑฐํ•œ๊ฒŒ ์•„๋‹ˆ์—ˆ์Šต๋‹ˆ๋‹ค.
03:44
I decided that one day I would do a project
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์–ด๋Š๋‚ , ์ €๋Š” ์‚ฌ์ง„์„ ์ด์šฉํ•ด
03:46
looking at trying to manifest climate change photographically.
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๊ธฐํ›„๋ณ€ํ™”๋ฅผ ์ž…์ฆํ•˜๊ธฐ๋กœ ๊ฒฐ์‹ฌํ–ˆ์Šต๋‹ˆ๋‹ค.
03:50
And that led me to this project.
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๊ทธ๋ฆฌ์„œ ์ด ํ”„๋กœ์ ํŠธ์— ์ฐฉ์ˆ˜ํ–ˆ์ฃ .
03:53
Initially, I was working on a National Geographic assignment --
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์ฒ˜์Œ์—, ์ €๋Š” ๋‚ด์…”๋„ ์ง€์˜ค๊ทธ๋ž˜ํ”ฝ์—์„œ ์ผ์„ ํ•˜๋ฉด์„œ
03:56
conventional, single frame, still photography.
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ํ‰๋ฒ”ํ•˜๊ฒŒ ํ•œ ์žฅ์˜ ์ •์ง€ํ™”๋ฉด์„ ์ฐ์—ˆ์ฃ .
03:58
And one crazy day, I got the idea that I should --
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๊ทธ๋ฆฌ๋˜ ์–ด๋Š๋‚ , ์ €๋Š” ์ผ์„ ๋งˆ์น˜๊ณ ์„œ
04:02
after that assignment was finished --
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์•„์ด๋””์–ด๊ฐ€ ํ•˜๋‚˜ ๋– ์˜ฌ๋ž์Šต๋‹ˆ๋‹ค.
04:04
I got the idea that I should shoot in time-lapse photography,
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์ €์†์ดฌ์˜์œผ๋กœ ์‚ฌ์ง„์„ ์ฐ์–ด๋ณด์ž๋Š” ์•„์ด๋””์–ด์˜€๋Š”๋ฐ,
04:08
that I should station a camera or two at a glacier
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ํ•œ๋‘๊ฐœ์˜ ์นด๋ฉ”๋ผ๋ฅผ ๋น™ํ•˜์— ๊ณ ์ •์‹œ์ผœ๋†“๊ณ 
04:12
and let it shoot every 15 minutes, or every hour or whatever
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15๋ถ„๋งˆ๋‹ค, ๋˜๋Š” ํ•œ์‹œ๊ฐ„๋งˆ๋‹ค, ์ด๋Ÿฐ ์‹์œผ๋กœ ์‚ฌ์ง„์„ ์ดฌ์˜ํ•˜๊ณ 
04:15
and watch the progression of the landscape over time.
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์‹œ๊ฐ„์˜ ํ๋ฆ„์— ๋”ฐ๋ผ ํ’๊ฒฝ์ด ๋ฐ”๋€Œ๋Š” ๊ฒƒ์„ ์ง€์ผœ๋ณด๋Š” ๊ฒ๋‹ˆ๋‹ค.
04:18
Well, within about three weeks,
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์Œ, ์•ฝ 3์ฃผ ๋งŒ์—
04:21
I incautiously turned that idea of a couple of time-lapse cameras
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์ €๋Š” ๋ฌด๋ชจํ•˜๊ฒŒ๋„ 2๋Œ€์˜ ์ €์†์ดฌ์˜์นด๋ฉ”๋ผ๋ฅผ
04:24
into 25 time-lapse cameras.
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25๋Œ€๋กœ ๋Š˜๋ ธ์Šต๋‹ˆ๋‹ค.
04:26
And the next six months of my life were the hardest time in my career,
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๊ทธ ๋‹ค์Œ 6๊ฐœ์›”์€ ์ œ ์ธ์ƒ์—์„œ ๊ฐ€์žฅ ํž˜๋“  ์‹œ๊ฐ„์ด์—ˆ์ฃ .
04:31
trying to design, build and deploy out in the field these 25 time-lapse cameras.
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์ด 25๊ฐœ์˜ ์ €์†์ดฌ์˜ ์นด๋ฉ”๋ผ๋ฅผ ๋””์ž์ธํ•˜๊ณ  ๋งŒ๋“ค์–ด ํ˜„์žฅ์— ๋ฐฐ์น˜ํ•˜๋Š๋ผ๊ตฌ์š”.
04:37
They are powered by the sun. Solar panels power them.
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์ด๊ฒƒ์€ ํƒœ์–‘์ „์ง€ ์นด๋ฉ”๋ผ์—์š”. ํƒœ์–‘ ์ „์ง€ํŒ์ด ์ „๋ ฅ์„ ๊ณต๊ธ‰ํ•ฉ๋‹ˆ๋‹ค.
04:41
Power goes into a battery. There is a custom made computer
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์ „๋ ฅ์ด ๋ฐฐํ„ฐ๋ฆฌ๋กœ ํ˜๋Ÿฌ๊ฐ‘๋‹ˆ๋‹ค. ์ž์ฒด ์ œ์ž‘ํ•œ ์ปดํ“จํ„ฐ๊ฐ€ ์žˆ์–ด์„œ
04:44
that tells the camera when to fire.
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์นด๋ฉ”๋ผ๊ฐ€ ์–ธ์ œ ์ดฌ์˜์„ ํ• ์ง€ ์•Œ๋ ค์ฃผ์ฃ .
04:47
And these cameras are positioned on rocks on the sides of the glaciers,
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๊ทธ๋ฆฌ๊ณ  ์ด ์นด๋ฉ”๋ผ๋Š” ๋น™ํ•˜์˜ ์–‘ ์˜†์— ์žˆ๋Š” ๋ฐ”์œ„์— ์„ค์น˜๋˜์–ด,
04:51
and they look in on the glacier from permanent, bedrock positions,
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๊ณ ์ •๋œ ๊ธฐ๋ฐ˜์•” ์ชฝ์—์„œ ๋น™ํ•˜๋ฅผ ๋ฐ”๋ผ๋ณด๋ฉด์„œ
04:54
and they watch the evolution of the landscape.
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ํ’๊ฒฝ์˜ ๋ณ€ํ™”๋ฅผ ๊ด€์ฐฐํ•˜์ฃ .
04:57
We just had a number of cameras out on the Greenland Ice Sheet.
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์ด์ œ ๊ทธ๋ฆฐ๋ž€๋“œ ๋น™์ƒ์„ ๊ด€์ฐฐํ•˜๋Š” ์ˆ˜๋งŽ์€ ์นด๋ฉ”๋ผ๊ฐ€ ์žˆ์Šต๋‹ˆ๋‹ค.
05:00
We actually drilled holes into the ice, way deep down below the thawing level,
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์šฐ๋ฆฌ๋Š” ํ•ด๋น™์ด ์ผ์–ด๋‚˜๋Š” ๊นŠ์ด๊นŒ์ง€ ์–ผ์Œ์— ๊ตฌ๋ฉ์„ ๋šซ์–ด์„œ
05:05
and had some cameras out there for the past month and a half or so.
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์ง€๋‚œ ํ•œ๋‹ฌ ๋ฐ˜ ๋™์•ˆ ๊ทธ๊ณณ์— ์นด๋ฉ”๋ผ๋ฅผ ์„ค์น˜ํ–ˆ์Šต๋‹ˆ๋‹ค.
05:08
Actually, there's still a camera out there right now.
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์‚ฌ์‹ค, ์ง€๊ธˆ๋„ ๊ฑฐ๊ธฐ์— ์นด๋ฉ”๋ผ๊ฐ€ ์žˆ์–ด์š”.
05:10
In any case, the cameras shoot roughly every hour.
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์–ด์จŒ๋“  ์ด ์นด๋ฉ”๋ผ๋“ค์€ ๋Œ€๋žต ๋งค์‹œ๊ฐ„๋งˆ๋‹ค, ๋˜๋Š” 30๋ถ„๋งˆ๋‹ค
05:13
Some of them shoot every half hour, every 15 minutes, every five minutes.
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15๋ถ„๋งˆ๋‹ค, 5๋ถ„๋งˆ๋‹ค ์‚ฌ์ง„์„ ์ดฌ์˜ํ•ฉ๋‹ˆ๋‹ค.
05:17
Here's a time lapse of one of the time-lapse units being made.
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์ด ์žฅ๋ฉด์€ ์ €์†์ดฌ์˜ ์žฅ๋น„ ์ œ์ž‘ ๊ณผ์ •์„ ์ €์†์ดฌ์˜ํ•œ ๊ฒ๋‹ˆ๋‹ค.
05:20
(Laughter)
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(์›ƒ์Œ)
05:22
I personally obsessed about every nut, bolt and washer in these crazy things.
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์ €๋Š” ์ด ์žฅ๋น„ ์•ˆ์˜ ๋ณผํŠธ์™€ ๋„ˆํŠธ, ์™€์…” ํ•˜๋‚˜ํ•˜๋‚˜์— ๋งค๋‹ฌ๋ ธ์Šต๋‹ˆ๋‹ค.
05:26
I spent half my life at our local hardware store
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์ด ๊ธฐ๊ณ„๋ฅผ ์ฒ˜์Œ ๋งŒ๋“ค ๋•Œ ์ˆ˜๊ฐœ์›”๋™์•ˆ
05:28
during the months when we built these units originally.
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๋™๋„ค ์ฒ ๋ฌผ์ ์—์„œ ๋Œ€๋ถ€๋ถ„ ์‹œ๊ฐ„์„ ๋ณด๋ƒˆ์ฃ .
05:33
We're working in most of the major glaciated regions of the northern hemisphere.
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์ €ํฌ๋Š” ๋ถ๋ฐ˜๊ตฌ์˜ ์ฃผ์š” ๋น™ํ•˜ ์ง€์—ญ ๋Œ€๋ถ€๋ถ„์—์„œ ์ž‘์—…ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
05:39
Our time-lapse units are in Alaska, the Rockies, Greenland and Iceland,
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์ €์†์ดฌ์˜ ์นด๋ฉ”๋ผ๊ฐ€ ์•Œ๋ž˜์Šค์นด, ๋กํ‚ค์‚ฐ๋งฅ, ๊ทธ๋ฆฐ๋ž€๋“œ, ๊ทธ๋ฆฌ๊ณ  ์•„์ด์Šฌ๋ž€๋“œ ์ง€์—ญ์— ์„ค์น˜๋˜์–ด ์žˆ์Šต๋‹ˆ๋‹ค.
05:43
and we have repeat photography positions,
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๋ฐ˜๋ณตํ•ด์„œ ์‚ฌ์ง„์„ ์ฐ๋Š” ์žฅ์†Œ๋„ ์žˆ๋Š”๋ฐ,
05:45
that is places we just visit on an annual basis,
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์ €ํฌ๊ฐ€ ๋งค๋…„ ๋‹จ์œ„๋กœ ๋ฐฉ๋ฌธํ•˜๋Š”
05:48
in British Columbia, the Alps and Bolivia.
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๋ธŒ๋ฆฌํ‹ฐ์‰ฌ ์ฝœ๋Ÿผ๋น„์•„, ์•Œํ”„์Šค์™€ ๋ณผ๋ฆฌ๋น„์•„ ๊ฐ™์€ ๊ณณ์ด์ฃ .
05:51
It's a big undertaking. I stand here before you tonight
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์‹ค๋กœ ์—„์ฒญ๋‚œ ์ž‘์—…์ด์ฃ . ์ €๋Š” ์˜ค๋Š˜๋ฐค ์ด ์ž๋ฆฌ์—
05:53
as an ambassador for my whole team.
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์ œ ๋ชจ๋“  ํŒ€์›๋“ค์„ ๋Œ€ํ‘œํ•ด ์—ฌ๋Ÿฌ๋ถ„ ์•ž์— ์„ฐ์Šต๋‹ˆ๋‹ค.
05:56
There's a lot of people working on this right now.
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์ง€๊ธˆ ์ด์ˆœ๊ฐ„์—๋„ ๋งŽ์€ ์‚ฌ๋žŒ๋“ค์ด ์ด ์ผ์„ ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
05:58
We've got 33 cameras out this moment.
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์ €ํฌ๋Š” ํ˜„์žฌ 33๊ฐœ์˜ ์นด๋ฉ”๋ผ๋ฅผ ์‚ฌ์šฉํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
06:01
We just had 33 cameras shoot about half an hour ago
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33๋Œ€์˜ ์นด๋ฉ”๋ผ๊ฐ€ ์•ฝ 30๋ถ„ ์ „์— ์‚ฌ์ง„์„ ์ดฌ์˜ํ–ˆ์Šต๋‹ˆ๋‹ค.
06:05
all across the northern hemisphere, watching what's happened.
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๋ถ๋ฐ˜๊ตฌ ๊ฐ์ง€์—์„œ, ๋ฌด์Šจ ์ผ์ด ์ผ์–ด๋‚ฌ๋Š”์ง€ ์ง€์ผœ๋ณด๊ณ  ์žˆ์ฃ .
06:08
And we've spent a lot of time in the field. It's been a fantastic amount of work.
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์ €ํฌ๋Š” ํ˜„์žฅ์—์„œ ๋งŽ์€ ์‹œ๊ฐ„์„ ๋ณด๋ƒˆ์Šต๋‹ˆ๋‹ค. ์ •๋ง ๊ต‰์žฅํ•œ ์–‘์˜ ์ž‘์—…์ด์ฃ .
06:12
We've been out for two and a half years,
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์šฐ๋ฆฌ๋Š” 2๋…„๋ฐ˜๋™์•ˆ ๋Œ์•„๋‹ค๋…”๊ณ ,
06:14
and we've got about another two and a half years yet to go.
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๋˜ 2๋…„๋ฐ˜์ด ๋” ๋‚จ์•˜์Šต๋‹ˆ๋‹ค.
06:16
That's only half our job.
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์ด๊ฑด ์ €ํฌ ์ž‘์—…์˜ ์ ˆ๋ฐ˜์ด๊ตฌ์š”.
06:18
The other half of our job is to tell the story to the global public.
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๋‹ค๋ฅธ ์ ˆ๋ฐ˜์€ ์ „ ์„ธ๊ณ„ ๋Œ€์ค‘๋“ค์—๊ฒŒ ์ด์•ผ๊ธฐ๋ฅผ ๋“ค๋ ค์ฃผ๋Š” ์ผ์ž…๋‹ˆ๋‹ค.
06:22
You know, scientists have collected this kind of information
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์•„์‹œ๋‹ค์‹œํ”ผ, ๊ณผํ•™์ž๋“ค์€ ์ด๋Ÿฐ ๋ฅ˜์˜ ์ •๋ณด๋“ค์„
06:27
off and on over the years, but a lot of it stays within the science community.
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์ˆ˜๋…„์— ๊ฑธ์ณ ์ˆ˜์ง‘ํ•ด ์™”์ง€๋งŒ, ๊ทธ ์ •๋ณด๋Š” ๊ณผํ•™๊ณ„ ์•ˆ์—์„œ ๋จธ๋ฌผ๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
06:32
Similarly, a lot of art projects stay in the art community,
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๋งˆ์ฐฌ๊ฐ€์ง€๋กœ, ๋งŽ์€ ์˜ˆ์ˆ ํ”„๋กœ์ ํŠธ๋„ ์˜ˆ์ˆ ๊ณ„ ์•ˆ์—๋งŒ ๋จธ๋ฌผ๋Ÿฌ ์žˆ์ฃ .
06:36
and I feel very much a responsibility through mechanisms like TED,
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๊ทธ๋ž˜์„œ ์ €๋Š” ์ด ์‚ฌ์ง„์„ ๊ฐ€์ง€๊ณ  TED์™€ ๊ฐ™์€ ๋งค์ปค๋‹ˆ์ฆ˜์ด๋‚˜
06:42
and like our relationship with the Obama White House,
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์˜ค๋ฐ”๋งˆ์˜ ๋ฐฑ์•…๊ด€์ด๋‚˜
06:45
with the Senate, with John Kerry, to influence policy
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์กด ์บ๋ฆฌ ์ƒ์›์˜์› ๋“ฑ์„ ํ†ตํ•ด ๋  ์ˆ˜ ์žˆ๋Š” ํ•œ
06:49
as much as possible with these pictures as well.
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์ •์ฑ…์— ๋งŽ์€ ์˜ํ–ฅ์„ ์ฃผ์–ด์•ผ ํ•œ๋‹ค๋Š” ์ฑ…์ž„๊ฐ์„ ๋Š๋‚๋‹ˆ๋‹ค.
06:51
We've done films. We've done books. We have more coming.
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์ €ํฌ๋Š” ์‚ฌ์ง„์„ ์ฐ์—ˆ์Šต๋‹ˆ๋‹ค. ์ฑ…์„ ์ถœ๊ฐ„ํ–ˆ์Šต๋‹ˆ๋‹ค. ํ•  ์ผ์ด ๋” ์žˆ์Šต๋‹ˆ๋‹ค.
06:55
We have a site on Google Earth
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์ €ํฌ๋Š” ๊ตฌ๊ธ€ ์–ด์Šค์— ์‚ฌ์ดํŠธ๊ฐ€ ์žˆ์Šต๋‹ˆ๋‹ค.
06:57
that Google Earth was generous enough to give us,
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์นœ์ ˆํ•˜๊ฒŒ๋„ ๊ตฌ๊ธ€ ์–ด์Šค๊ฐ€ ์ €ํฌ์—๊ฒŒ ์ œ๊ณตํ•ด์ฃผ์—ˆ์ฃ .
07:00
and so forth, because we feel very much the need to tell this story,
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์ด ๋ชจ๋“ ๊ฒŒ ์ด ์ด์•ผ๊ธฐ๋ฅผ ์ „ํ•ด์•ผ ํ•  ํ•„์š”์„ฑ์„ ๊ฐ„์ ˆํžˆ ๋Š๋ผ๊ธฐ ๋•Œ๋ฌธ์ด๋ฉฐ,
07:04
because it is such an immediate evidence of ongoing climate change right now.
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๋ฐ”๋กœ ์ง€๊ธˆ ์ง„ํ–‰๋˜๊ณ  ์žˆ๋Š” ๊ธฐํ›„ ๋ณ€ํ™”์— ๋Œ€ํ•œ ์ฆ‰๊ฐ์ ์ธ ์ฆ๊ฑฐ์ด๊ธฐ ๋•Œ๋ฌธ์ž…๋‹ˆ๋‹ค.
07:11
Now, one bit of science before we get into the visuals.
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์ด์ œ, ์‚ฌ์ง„์„ ๋ณด์‹œ๊ธฐ ์ „์— ๊ณผํ•™ ์ด์•ผ๊ธฐ ํ•œ๋งˆ๋”” ํ•˜์ฃ .
07:14
If everybody in the developed world understood this graph,
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์„ ์ง„๊ตญ์˜ ๋ชจ๋“  ์‚ฌ๋žŒ๋“ค์ด ์ด ๊ทธ๋ž˜ํ”„๋ฅผ ์ดํ•ดํ•œ๋‹ค๋ฉด,
07:18
and emblazoned it on the inside of their foreheads,
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๊ทธ๋ฆฌ๊ณ  ์ด ๊ทธ๋ž˜ํ”„๋ฅผ ๋จธ๋ฆฌ ์†์— ์ƒˆ๊ฒจ๋„ฃ๋Š”๋‹ค๋ฉด
07:21
there would be no further societal argument about climate change
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๊ธฐํ›„๋ณ€ํ™”์— ๋Œ€ํ•œ ์‚ฌํšŒ์  ๋…ผ์Ÿ์€ ๋” ์ด์ƒ ์ƒ๊ธฐ์ง€ ์•Š์„ ๊ฒ๋‹ˆ๋‹ค.
07:25
because this is the story that counts.
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์™œ๋ƒํ•˜๋ฉด ์ด๊ฑด ์ค‘์š”ํ•œ ์‚ฌ์•ˆ์ด๋‹ˆ๊น์š”.
07:28
Everything else you hear is just propaganda and confusion.
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์ด๋ฐ–์— ์—ฌ๋Ÿฌ๋ถ„์ด ๋“ฃ๋Š” ๊ฒƒ๋“ค์€ ๋‹จ์ง€ ์„ ์ „์ด๊ณ  ํ˜ผ๋™์ผ ๋ฟ์ž…๋‹ˆ๋‹ค.
07:32
Key issues: this is a 400,000 year record.
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ํ•ต์‹ฌ์€ ์ด๊ฒƒ์ž…๋‹ˆ๋‹ค: ์ด ๊ทธ๋ž˜ํ”„๋Š” 40๋งŒ๋…„ ๋™์•ˆ์˜ ๊ธฐ๋ก์ž…๋‹ˆ๋‹ค.
07:35
This exact same pattern is seen going back now
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์ด๊ฒƒ๊ณผ ์™„์ „ํžˆ ๋™์ผํ•œ ํŒจํ„ด์ด
07:37
almost a million years before our current time.
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์ง€๊ธˆ ์‹œ๋Œ€๋กœ๋ถ€ํ„ฐ ์•ฝ 100๋งŒ๋…„ ์ „์—๋„ ๋‚˜ํƒ€๋‚ฉ๋‹ˆ๋‹ค.
07:40
And several things are important.
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๋˜ํ•œ ๋ช‡๊ฐ€์ง€ ์ค‘์š”ํ•œ ์ ์ด ์žˆ์Šต๋‹ˆ๋‹ค.
07:43
Number one: temperature and carbon dioxide in the atmosphere
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์ฒซ์งธ: ์˜จ๋„์™€ ๋Œ€๊ธฐ์ค‘์˜ ์ด์‚ฐํ™”ํƒ„์†Œ๋Š”
07:46
go up and down basically in sync.
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๊ธฐ๋ณธ์ ์œผ๋กœ ํ•จ๊ป˜ ์ฆ๊ฐ€ํ•˜๊ณ  ๊ฐ์†Œํ•œ๋‹ค๋Š” ๊ฒƒ์ž…๋‹ˆ๋‹ค.
07:48
You can see that from the orange line and the blue line.
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์˜ค๋ Œ์ง€์ƒ‰๊ณผ ํŒŒ๋ž€์ƒ‰ ์„ ์œผ๋กœ ํ™•์ธํ•˜์‹ค ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
07:51
Nature naturally has allowed carbon dioxide to go up to 280 parts per million.
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์ž์—ฐ์€ ์ด์‚ฐํ™”ํƒ„์†Œ์˜ ๋†๋„๋ฅผ ์ตœ๋Œ€ 280ppm๊นŒ์ง€ ํ—ˆ์šฉํ•ด์™”์Šต๋‹ˆ๋‹ค.
07:58
That's the natural cycle.
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์ด๊ฒƒ์ด ์ž์—ฐ์ˆœํ™˜์ž…๋‹ˆ๋‹ค.
08:00
Goes up to 280 and then drops
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280ppm๊นŒ์ง€ ์ฆ๊ฐ€ํ•œ ํ›„ ๋–จ์–ด์ง‘๋‹ˆ๋‹ค.
08:02
for various reasons that aren't important to discuss right here.
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๋‹ค์–‘ํ•œ ์ด์œ ๊ฐ€ ์žˆ์ง€๋งŒ ์ง€๊ธˆ ๋…ผ์˜ํ• ๋งŒํผ ์ค‘์š”ํ•œ๊ฑด ์•„๋‹ˆ๊ณ ,
08:05
But 280 is the peak.
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์–ด์จŒ๋“  280ppm์ด ์ตœ๋Œ€์น˜ ์ž…๋‹ˆ๋‹ค.
08:07
Right now, if you look at the top right part of that graph,
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๋ฐ”๋กœ ์ง€๊ธˆ, ์—ฌ๋Ÿฌ๋ถ„์ด ์ด ๊ทธ๋ž˜ํ”„์˜ ์šฐ์ธก ์ƒ๋‹จ์„ ๋ณด์‹œ๋ฉด
08:10
we're at 385 parts per million.
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ํ˜„์žฌ๋Š” 385ppm ์ด๋ผ๋Š”๊ฑธ ์•„์‹ค ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
08:12
We are way, way outside the normal, natural variability.
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์šฐ๋ฆฌ๋Š” ์ •์ƒ์ ์ธ ์ž์—ฐ ๋ณ€๋™์„ฑ์—์„œ ๋ฒ—์–ด๋‚˜ ์žˆ์Šต๋‹ˆ๋‹ค.
08:17
Earth is having a fever.
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์ง€๊ตฌ๋Š” ์—ด๋ณ‘์„ ์•“๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
08:19
In the past hundred years, the temperature of the Earth
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์ง€๋‚œ 100๋…„๋™์•ˆ ์ง€๊ตฌ์˜ ์˜จ๋„๋Š”
08:22
has gone up 1.3 degrees Fahrenheit, .75 degrees Celsius,
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ํ™”์”จ 1.3๋„, ์„ญ์”จ 0.75๋„ ์ƒ์Šนํ–ˆ๊ณ 
08:27
and it's going to keep going up
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๊ณ„์† ์ƒ์Šนํ•˜๋ ค ํ•˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
08:29
because we keep dumping fossil fuels into the atmosphere.
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์šฐ๋ฆฌ๊ฐ€ ๋Œ€๊ธฐ์ค‘์— ํ™”์„์—ฐ๋ฃŒ๋ฅผ ๊ณ„์† ์Ÿ์•„๋ถ“๊ณ  ์žˆ๊ธฐ ๋•Œ๋ฌธ์ด์ฃ .
08:32
At the rate of about two and a half parts per million per year.
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๋งค๋…„ 2.5ppm์˜ ์†๋„๋กœ ๋ง์ž…๋‹ˆ๋‹ค.
08:35
It's been a remorseless, steady increase.
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๊ฐˆ์ˆ˜๋ก ์‹ฌํ•ด์ง€๋ฉฐ, ๊พธ์ค€ํžˆ ์ฆ๊ฐ€ํ•ฉ๋‹ˆ๋‹ค.
08:38
We have to turn that around.
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์šฐ๋ฆฌ๋Š” ์ด ์ถ”์„ธ๋ฅผ ๋Œ๋ ค์•ผ ํ•ฉ๋‹ˆ๋‹ค.
08:40
That's the crux, and someday I hope to emblazon that
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์ด๊ฒƒ์ด ๊ฐ€์žฅ ์ค‘์š”ํ•œ ๋ถ€๋ถ„์ž…๋‹ˆ๋‹ค. ์–ธ์  ๊ฐ€ ์ €๋Š” ์ด๊ฑธ
08:43
across Times Square in New York and a lot of other places.
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๋‰ด์š• ํƒ€์ž„์Šคํ€˜์–ด์™€ ๊ทธ์™ธ ๋งŽ์€ ์žฅ์†Œ์— ์ƒˆ๊ฒจ๋„ฃ์—ˆ์œผ๋ฉด ํ•ฉ๋‹ˆ๋‹ค.
08:46
But anyway, off to the world of ice.
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์•„๋ฌดํŠผ, ์–ผ์Œ์˜ ์„ธ๊ณ„๋กœ ๋‹ค์‹œ ๋Œ์•„์˜ค๊ฒ ์Šต๋‹ˆ๋‹ค.
08:48
We're now at the Columbia Glacier in Alaska.
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์•Œ๋ž˜์Šค์นด์˜ ์ปฌ๋Ÿผ๋น„์•„ ๋น™ํ•˜๋ฅผ ๋ณด๊ณ  ๊ณ„์‹ญ๋‹ˆ๋‹ค.
08:50
This is a view of what's called the calving face.
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'๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด'์ด๋ผ๊ณ  ๋ถ€๋ฅด๋Š” ๋ถ€๋ถ„์˜ ์‚ฌ์ง„์ž…๋‹ˆ๋‹ค.
08:53
This is what one of our cameras saw over the course of a few months.
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์ด ์˜์ƒ์€ ์ €ํฌ ์นด๋ฉ”๋ผ ํ•˜๋‚˜๊ฐ€ ๋ช‡๊ฐœ์›”์— ๊ฑธ์ณ ์ดฌ์˜ํ•œ ๊ฒƒ์ž…๋‹ˆ๋‹ค.
08:56
You see the glacier flowing in from the right,
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๋ณด์„ธ์š”. ๋น™ํ•˜๊ฐ€ ์˜ค๋ฅธ์ชฝ์—์„œ ํ˜๋Ÿฌ์™€์„œ
09:00
dropping off into the sea, camera shooting every hour.
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๋ฐ”๋‹ค ์†์œผ๋กœ ๋น ์ ธ ๋‚˜๊ฐ‘๋‹ˆ๋‹ค. ์นด๋ฉ”๋ผ๊ฐ€ ๋งค์‹œ๊ฐ„ ์ดฌ์˜ํ•ฉ๋‹ˆ๋‹ค.
09:03
If you look in the middle background,
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๊ฐ€์šด๋ฐ ๋ฐฐ๊ฒฝ์„ ๋ณด์‹œ๋ฉด
09:05
you can see the calving face bobbing up and down like a yo-yo.
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๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์ด '์š”์š”'์ฒ˜๋Ÿผ ์ผ๋ ๊ฑฐ๋ฆฌ๋Š”๊ฑธ ๋ณผ ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
09:09
That means that glacier's floating and it's unstable,
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์ด๊ฑด ๋น™ํ•˜๊ฐ€ ๋ถˆ์•ˆ์ •ํ•˜๊ฒŒ ๋ฌผ ์œ„์— ๋– ์žˆ๋‹ค๋Š” ๋œป์ด๊ณ ,
09:12
and you're about to see the consequences of that floating.
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๊ทธ๋ ‡๊ฒŒ ๋– ๋‹ค๋‹Œ ๊ฒฐ๊ณผ๋ฅผ ์ด์ œ ์—ฌ๋Ÿฌ๋ถ„์€ ๋ณด์‹ค ๊ฒ๋‹ˆ๋‹ค.
09:15
To give you a little bit of a sense of scale,
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๊ทœ๋ชจ๋ฅผ ์ง์ž‘ํ•˜์‹ค ์ˆ˜ ์žˆ๋„๋ก ํ•œ๋งˆ๋”” ๋ง๋ถ™์ด์ž๋ฉด
09:18
that calving face in this picture
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์ด ์‚ฌ์ง„์˜ ๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์€
09:20
is about 325 feet tall. That's 32 stories.
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๋†’์ด๊ฐ€ 325ํ”ผํŠธ(99m)์ž…๋‹ˆ๋‹ค. 32์ธต ๊ฑด๋ฌผ ๋†’์ด์ฃ .
09:25
This is not a little cliff. This is like a major office building in an urban center.
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์กฐ๊ทธ๋งˆํ•œ ์ ˆ๋ฒฝ์ด ์•„๋‹™๋‹ˆ๋‹ค. ๋„์‹ฌ ๊ฐ€์šด๋ฐ ์žˆ๋Š” ์ปค๋‹ค๋ž€ ๋นŒ๋”ฉ ํฌ๊ธฐ์ฃ .
09:30
The calving face is the wall where the visible ice breaks off,
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๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์€ ๋ˆˆ์— ๋ณด์ด๋Š” ์–ผ์Œ์ด ๊นจ์ ธ๋‚˜๊ฐ€๋Š” ๋ฒฝ๋ฉด์ž…๋‹ˆ๋‹ค.
09:35
but in fact, it goes down below sea level another couple thousand feet.
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์‚ฌ์‹ค์ƒ ์ด๊ฒƒ์€ ํ•ด์ˆ˜๋ฉด ์•„๋ž˜ 2์ฒœ์—ฌํ”ผํŠธ(6๋ฐฑ์—ฌm) ์ •๋„๊นŒ์ง€ ๋ป—์–ด ์žˆ์Šต๋‹ˆ๋‹ค.
09:40
So there's a wall of ice a couple thousand feet deep
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๊ทธ๋Ÿฌ๋‹ˆ๊นŒ 2์ฒœ์—ฌํ”ผํŠธ(6๋ฐฑ์—ฌm) ๊นŠ์ด์˜ ๋น™๋ฒฝ์ด ์žˆ๋Š”๋ฐ
09:44
going down to bedrock if the glacier's grounded on bedrock,
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๋น™ํ•˜๊ฐ€ ๊ธฐ๋ฐ˜์•” ์œ„์— ๋†“์—ฌ์žˆ๋‹ค๋ฉด ๊ธฐ๋ฐ˜์•”๊นŒ์ง€ ๋‹ฟ์•„์žˆ๊ณ ,
09:48
and floating if it isn't.
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๊ทธ๋ ‡์ง€ ์•Š๋‹ค๋ฉด ๋ฌผ ์œ„์— ๋– ์žˆ๋Š” ์ƒํƒœ์ฃ .
09:52
Here's what Columbia's done. This is in south central Alaska.
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์ด๊ฒƒ์€ ์ปฌ๋Ÿผ๋น„์•„ ๋น™ํ•˜์—์„œ ์ผ์–ด๋‚œ ์ผ์ž…๋‹ˆ๋‹ค. ์•Œ๋ž˜์Šค์นด ์ค‘๋‚จ๋ถ€ ์ง€์—ญ์ž…๋‹ˆ๋‹ค.
09:56
This was an aerial picture I did one day in June three years ago.
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์ด๊ฒƒ์€ 3๋…„์ „ 6์›”์— ์ฐ์€ ํ•ญ๊ณต์‚ฌ์ง„์ž…๋‹ˆ๋‹ค.
10:01
This is an aerial picture we did this year.
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์ด๊ฒƒ์€ ์˜ฌํ•ด ์ฐ์€ ํ•ญ๊ณต์‚ฌ์ง„ ์ž…๋‹ˆ๋‹ค.
10:04
That's the retreat of this glacier.
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๋น™ํ•˜๊ฐ€ ํ›„ํ‡ดํ•œ ๊ฒƒ์ž…๋‹ˆ๋‹ค.
10:07
The main stem, the main flow of the glacier is coming from the right
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๋น™ํ•˜์˜ ๋ณธ๋ฅ˜๊ฐ€ ์˜ค๋ฅธ์ชฝ์—์„œ๋ถ€ํ„ฐ ํ˜๋Ÿฌ์˜ค๊ณ  ์žˆ๋Š”๋ฐ
10:11
and it's going very rapidly up that stem.
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๊ทธ ์ค„๊ธฐ ์ƒ๋ฅ˜๋กœ ๋น ๋ฅด๊ฒŒ ์˜ฌ๋ผ๊ฐ€๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
10:14
We're going to be up there in just a few more weeks,
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์ €ํฌ๋Š” ๋ช‡ ์ฃผ ๋‚ด์— ์ €๊ณณ์„ ๋ฐฉ๋ฌธํ•  ์˜ˆ์ •์ธ๋ฐ,
10:18
and we expect that it's probably retreated another half a mile,
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์•„๋งˆ๋„ 0.5๋งˆ์ผ(์•ฝ800m) ์ •๋„ ๋” ํ›„ํ‡ดํ–ˆ์„ ๊ฑธ๋กœ ์˜ˆ์ƒํ•ฉ๋‹ˆ๋‹ค.
10:21
but if I got there and discovered that it had collapsed
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ํ•˜์ง€๋งŒ ์ €๊ณณ์— ๋„์ฐฉํ•ด์„œ, ๋น™ํ•˜๊ฐ€ ๋ถ•๊ดด๋˜๊ณ 
10:24
and it was five miles further back, I wouldn't be the least bit surprised.
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5๋งˆ์ผ(8km) ๋” ํ›„ํ‡ดํ–ˆ๋‹ค๋Š”๊ฑธ ๋ฐœ๊ฒฌํ•˜๋”๋ผ๋„ ์ „ํ˜€ ๋†€๋ผ์ง€ ์•Š์„ ๊ฒ๋‹ˆ๋‹ค.
10:29
Now it's really hard to grasp the scale of these places,
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์ด์ œ ์ด๋Ÿฐ ๊ณณ์˜ ๊ทœ๋ชจ๋ฅผ ๊ฐ€๋Š ํ•˜๊ธฐ๊ฐ€ ๋งค์šฐ ์–ด๋ ต์Šต๋‹ˆ๋‹ค.
10:32
because as the glaciers --
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์™œ๋ƒ๋ฉด ๋น™ํ•˜๋Š” --
10:34
one of the things is that places like Alaska and Greenland are huge,
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์•Œ๋ž˜์Šค์นด๋‚˜ ๊ทธ๋ฆฐ๋ž€๋“œ ๊ฐ™์€ ๊ณณ์˜ ๋น™ํ•˜๊ฐ€ ๊ฑฐ๋Œ€ํ•˜๋‹ค๋Š” ์ ๋„ ์žˆ์ง€๋งŒ,
10:37
they're not normal landscapes --
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๋น™ํ•˜๋Š” ํ‰๋ฒ”ํ•œ ํ’๊ฒฝ์ด ์•„๋‹™๋‹ˆ๋‹ค.--
10:39
but as the glaciers are retreating, they're also deflating,
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ํ›„ํ‡ดํ•˜๋ฉด์„œ ๋™์‹œ์— ์ˆ˜์ถ•ํ•˜๊ณ  ์žˆ๊ฑฐ๋“ ์š”.
10:43
like air is being let out of a balloon.
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๋งˆ์น˜ ํ’์„ ์—์„œ ๋ฐ”๋žŒ์ด ๋น ์ ธ๋‚˜๊ฐ€๋“ฏ์ด ๋ง์ž…๋‹ˆ๋‹ค.
10:46
And so, there are features on this landscape.
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๊ทธ๋ž˜์„œ ์ด ํ’๊ฒฝ์—๋Š” ํŠน์ง•์ด ์žˆ์Šต๋‹ˆ๋‹ค
10:49
There's a ridge right in the middle of the picture, up above where that arrow comes in,
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์‚ฌ์ง„ ๊ฐ€์šด๋ฐ์˜ ์˜ค๋ฅธ์ชฝ, ํ™”์‚ดํ‘œ๋กœ ๊ฐ€๋ฆฌํ‚จ ๋ถ€๋ถ„์— ์‚ฐ๋“ฑ์„ฑ์ด๊ฐ€ ์žˆ์Šต๋‹ˆ๋‹ค.
10:53
that shows you that a little bit.
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์ด๊ฑธ ๋ณด์‹œ๋ฉด ์ข€ ์ดํ•ด๊ฐ€ ๋˜์‹คํ…๋ฐ์š”,
10:55
There's a marker line called the trim line
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๋นจ๊ฐ„์ƒ‰์œผ๋กœ ๊ทธ๋ฆฐ ๋ถ€๋ถ„์—
10:58
above our little red illustration there.
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ํ…Œ๋‘๋ฆฌ์„  ํ‘œ์‹œ๊ฐ€ ๋ณด์ด์ฃ .
11:02
This is something no self-respecting photographer would ever do --
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์ž์กด์‹ฌ ์žˆ๋Š” ์‚ฌ์ง„๊ฐ€๋ผ๋ฉด ์ด๋ ‡๊ฒŒ ํ•˜์ง€ ์•Š๊ฒ ์ฃ .
11:04
you put some cheesy illustration on your shot, right? --
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์ €๊ธ‰ํ•œ ๊ทธ๋ฆผ์„ ์‚ฌ์ง„ ์œ„์— ๋ง๋Œ€๋Š”๊ฑฐ ๋ง์ด์—์š”.
11:07
and yet you have to do it sometimes to narrate these points.
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ํ•˜์ง€๋งŒ ๊ฐ€๋”์€ ์š”์ ์„ ์„ค๋ช…ํ•˜๊ธฐ ์œ„ํ•ด ์ด๋ž˜์•ผ ํ•˜์ฃ .
11:11
But, in any case, the deflation of this glacier since 1984
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์–ด์จŒ๋“ , 1984๋…„๋ถ€ํ„ฐ ์ด ๋น™ํ•˜๊ฐ€ ์ˆ˜์ถ•๋œ ํฌ๊ธฐ๋Š”
11:15
has been higher than the Eiffel Tower, higher than the Empire State Building.
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์—ํŽ ํƒ‘๋ณด๋‹ค ํฌ๊ณ , ์— ํŒŒ์ด์–ด ์Šคํ…Œ์ดํŠธ ๋นŒ๋”ฉ๋ณด๋‹ค ํฝ๋‹ˆ๋‹ค.
11:20
A tremendous amount of ice has been let out of these valleys
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์—„์ฒญ๋‚œ ์–‘์˜ ์–ผ์Œ์ด ์ด ๊ณ„๊ณก์—์„œ ๋ฐฐ์ถœ๋˜์—ˆ์œผ๋ฉฐ
11:23
as it's retreated and deflated, gone back up valley.
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๋น™ํ•˜๋Š” ํ›„ํ‡ดํ•˜๊ณ  ์ˆ˜์ถ•ํ•˜๋ฉด์„œ ๊ณ„๊ณก ์œ„์ชฝ์œผ๋กœ ์ด๋™ํ•ฉ๋‹ˆ๋‹ค.
11:28
These changes in the alpine world are accelerating.
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์‚ฐ์•…์ง€๋Œ€์—์„œ ์ด๋Ÿฌํ•œ ๋ณ€ํ™”๋Š” ๊ฐ€์†ํ™”๋˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
11:31
It's not static.
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๊ณ ์ •๋˜์–ด ์žˆ์ง€ ์•Š์•„์š”.
11:33
Particularly in the world of sea ice,
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ํŠนํžˆ, ๋ฐ”๋‹ค์— ์žˆ๋Š” ๋น™ํ•˜์—์„œ๋Š” ๋ง์ด์ฃ .
11:36
the rate of natural change is outstripping predictions of just a few years ago,
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์ž์—ฐ์˜ ๋ณ€ํ™” ์†๋„๋Š” ๋ช‡๋…„ ์ „์— ์˜ˆ์ธกํ–ˆ๋˜ ๊ฒƒ์„ ๋›ฐ์–ด๋„˜๊ณ  ์žˆ๊ณ 
11:40
and the processes either are accelerating
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๋ณ€ํ™”๊ณผ์ •์ด ๊ฐ€์†๋˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
11:43
or the predictions were too low to begin with.
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๊ทธ๊ฒŒ ์•„๋‹ˆ๋ฉด ์ฒ˜์Œ์˜ ์˜ˆ์ƒ์น˜๊ฐ€ ๋„ˆ๋ฌด ๋‚ฎ์•˜์ฃ .
11:45
But in any case, there are big, big changes happening as we speak.
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์–ด์จŒ๊ฑฐ๋‚˜, ์šฐ๋ฆฌ๊ฐ€ ๋งํ•œ ์ปค๋‹ค๋ž€ ๋ณ€ํ™”๊ฐ€ ์ผ์–ด๋‚˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
11:50
So, here's another time-lapse shot of Columbia.
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์ž, ์—ฌ๊ธฐ ์ฝœ๋กฌ๋น„์•„๋ฅผ ์ €์† ์ดฌ์˜ํ•œ ๋‹ค๋ฅธ ์žฅ๋ฉด์ž…๋‹ˆ๋‹ค.
11:54
And you see where it ended in these various spring days,
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๋ณด์‹œ๋‹ค์‹œํ”ผ ์ด ์ €์†์ดฌ์˜์€ 6์›”, 5์›”, 10์›” ๋“ฑ
11:57
June, May, then October.
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๋”ฐ๋œปํ•œ ๋‚ ์— ๋๋‚ฌ์Šต๋‹ˆ๋‹ค.
11:59
Now we turn on our time lapse.
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์ด์ œ ์ €์†์ดฌ์˜ ์˜์ƒ์„ ๋ณด์‹œ๊ฒ ์Šต๋‹ˆ๋‹ค.
12:01
This camera was shooting every hour.
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์ด ์นด๋ฉ”๋ผ๋Š” ๋งค์‹œ๊ฐ„๋งˆ๋‹ค ์‚ฌ์ง„์„ ์ดฌ์˜ํ–ˆ์Šต๋‹ˆ๋‹ค.
12:03
Geologic process in action here.
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์ง€์งˆํ•™์  ํ™œ๋™์ด ์ผ์–ด๋‚˜๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
12:05
And everybody says, well don't they advance in the winter time?
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๋งŽ์€ ๋ถ„๋“ค์ด, ๋น™ํ•˜๊ฐ€ ๊ฒจ์šธ์—๋Š” ์•ž์œผ๋กœ ๋‚˜์˜ค์ง€ ์•Š๋Š๋ƒ๊ณ  ๋งํ•ฉ๋‹ˆ๋‹ค.
12:08
No. It was retreating through the winter because it's an unhealthy glacier.
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์•„๋‹ˆ์˜ค. ์ด ๋น™ํ•˜๋Š” ๊ฒจ์šธ์—๋„ ํ›„ํ‡ดํ–ˆ์Šต๋‹ˆ๋‹ค. ์ƒํƒœ๊ฐ€ ์ข‹์ง€์•Š์œผ๋‹ˆ๊นŒ์š”.
12:11
Finally catches up to itself, it advances.
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๋งˆ์นจ๋‚ด ์•ž์œผ๋กœ ์ „์ง„ํ•ด ์› ์ƒํƒœ๋ฅผ ๋”ฐ๋ผ์žก์Šต๋‹ˆ๋‹ค.
12:18
And you can look at these pictures over and over again
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์—ฌ๋Ÿฌ๋ถ„์€ ์ด ๊ทธ๋ฆผ์„ ๋ฐ˜๋ณตํ•ด์„œ ์—ฌ๋Ÿฌ๋ฒˆ ๋ณด์‹ค ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
12:20
because there's such a strange, bizarre fascination in seeing
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์ด ์žฅ๋ฉด๋“ค์€ ๋ณด๊ณ  ์žˆ์œผ๋ฉด ๋‚ฏ์„ค๊ณ , ๊ธฐ๋ฌ˜ํ•˜๊ฒŒ ๋งค๋ฃŒ๋˜๊ธฐ ๋•Œ๋ฌธ์ด์ฃ .
12:24
these things you don't normally get to see come alive.
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์ด ์žฅ๋ฉด๋“ค์€ ๋ณดํ†ต์€ ์ด๋ ‡๊ฒŒ ์ƒ์ƒํ•˜๊ฒŒ ๋ณผ ์ˆ˜ ์žˆ๋Š”๊ฑด ์•„๋‹ˆ์ฃ .
12:27
We've been talking about "seeing is believing "
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์šฐ๋ฆฌ๋Š” "๋ฐฑ๋ฌธ์ด ๋ถˆ์—ฌ์ผ๊ฒฌ"์ด๋ผ ๋งํ•ด์™”๊ณ 
12:29
and seeing the unseen at TED Global.
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๋ณด์ด์ง€ ์•Š์•˜๋˜ ๊ฒƒ์„ TED Global์—์„œ ๋ณด๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
12:32
That's what you see with these cameras.
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๋ฐ”๋กœ ์ด ์นด๋ฉ”๋ผ๋ฅผ ํ†ตํ•ด ๋ณด๋Š” ๊ฒƒ์ž…๋‹ˆ๋‹ค.
12:35
The images make the invisible visible.
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์ด ์‚ฌ์ง„๋“ค์€ ๋ณด์ด์ง€ ์•Š๋˜ ๊ฒƒ์„ ๋ณด์—ฌ์ค๋‹ˆ๋‹ค.
12:42
These huge crevasses open up.
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๊ฑฐ๋Œ€ํ•œ ํ‹ˆ์ด ์—ด๋ ธ์Šต๋‹ˆ๋‹ค.
12:44
These great ice islands break off --
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์ด ์ปค๋‹ค๋ž€ ์–ผ์Œ ์„ฌ์ด ๋–จ์–ด์ ธ ๋‚˜๊ฐ‘๋‹ˆ๋‹ค.
12:47
and now watch this.
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์ž ์—ฌ๊ธฐ๋ฅผ ๋ณด์„ธ์š”.
12:49
This has been the springtime this year --
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์˜ฌํ•ด ๋ด„์—
12:57
a huge collapse. That happened in about a month,
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์ปค๋‹ค๋ž€ ๋ถ•๊ดด๊ฐ€ ์žˆ์—ˆ์Šต๋‹ˆ๋‹ค. ์•ฝ ํ•œ๋‹ฌ๋งŒ์—
12:59
the loss of all that ice.
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์–ผ์Œ์ด ๋‹ค ์‚ฌ๋ผ์กŒ์Šต๋‹ˆ๋‹ค.
13:11
So that's where we started three years ago,
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๊ทธ๋Ÿฌ๋‹ˆ๊นŒ ์šฐ๋ฆฌ๊ฐ€ 3๋…„์ „์— ์ดฌ์˜์„ ์‹œ์ž‘ํ•œ ๊ณณ์œผ๋กœ,
13:13
way out on the left, and that's where we were a few months ago, the
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๋น™ํ•˜๊ฐ€ ์™ผ์ชฝ์œผ๋กœ ํ˜๋Ÿฌ๋‚˜๊ฐ€๋Š” ์ €๊ณณ์€ ์šฐ๋ฆฌ๊ฐ€ ๋ช‡๋‹ฌ ์ „์—
13:15
last time we went into Columbia.
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๋งˆ์ง€๋ง‰์œผ๋กœ ์ฝœ๋กฌ๋น„์•„์— ๊ฐ”๋˜ ๊ณณ์ž…๋‹ˆ๋‹ค.
13:18
To give you a feeling for the scale of the retreat,
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ํ›„ํ‡ด์˜ ๊ทœ๋ชจ๋ฅผ ๊ฐ€๋Š ํ•˜์‹ค ์ˆ˜ ์žˆ๋„๋ก
13:20
we did another cheesy illustration,
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๋˜๋‹ค์‹œ ์ €๊ธ‰ํ•œ ๊ทธ๋ฆผ์„ ๋„ฃ์–ด๋ดค์Šต๋‹ˆ๋‹ค.
13:22
with British double-decker buses.
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์˜๊ตญ์˜ ์ด์ธต๋ฒ„์Šค ๊ทธ๋ฆผ์ž…๋‹ˆ๋‹ค.
13:25
If you line up 295 of those nose to tail, that's about how far back that was.
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295๋Œ€๋ฅผ ์ค„์ค„์ด ์„ธ์›Œ๋†“์€ ๊ฑฐ๋ฆฌ๋งŒํผ ๋’ค๋กœ ๋ฐ€๋ ค๋‚ฌ์Šต๋‹ˆ๋‹ค.
13:30
It's a long way.
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์•„์ฃผ ๊ธด ๊ฑฐ๋ฆฌ์ง€์š”.
13:35
On up to Iceland.
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์•„์ด์Šฌ๋žœ๋“œ๋กœ ๊ฐ€๋ณด๊ฒ ์Šต๋‹ˆ๋‹ค.
13:37
One of my favorite glaciers, the Sรณlheimajรถkull.
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์ œ๊ฐ€ ๊ฐ€์žฅ ์ข‹์•„ํ•˜๋Š” ๋น™ํ•˜์ธ ์†”ํ•˜์ด๋งˆ์กฐ์ฟจ์ž…๋‹ˆ๋‹ค.
13:43
And here, if you watch, you can see the terminus retreating.
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์—ฌ๊ธธ ๋ณด์‹œ๋ฉด ๋ ์„ ์ด ํ›„ํ‡ดํ•˜๊ณ 
13:46
You can see this river being formed.
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๊ฐ•์ด ํ˜•์„ฑ๋˜๋Š”๊ฒƒ์„ ๋ณด์‹ค ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
13:48
You can see it deflating.
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์ค„์–ด๋“œ๋Š”๊ฒƒ๋„ ๋ณด์‹ค ์ˆ˜ ์žˆ์ฃ .
13:56
Without the photographic process, you would never see this. This is invisible.
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์‚ฌ์ง„ ์ž‘์—… ์—†์ด๋Š” ์ด๋Ÿฐ ๊ฒƒ์„ ์ ˆ๋Œ€ ๋ณผ ์ˆ˜ ์—†์Šต๋‹ˆ๋‹ค. ๋ณด์ด์ง€ ์•Š๋Š” ๊ฒƒ๋“ค์ด์ฃ .
14:00
You can stand up there your whole life and you would never see this,
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์ €๊ธฐ์— ํ‰์ƒ ์„œ์žˆ๋”๋ผ๋„ ์ด๋Ÿฐ๊ฑด ๋ณผ ์ˆ˜ ์—†์ง€๋งŒ,
14:03
but the camera records it.
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์นด๋ฉ”๋ผ๋Š” ์ด๊ฑธ ๊ธฐ๋กํ•ฉ๋‹ˆ๋‹ค.
14:09
So we wind time backwards now.
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์ด์ œ ์‹œ๊ฐ„์„ ๋’ค๋กœ ๋˜๋Œ๋ ค๋ณด๊ฒ ์Šต๋‹ˆ๋‹ค.
14:13
We go back a couple years in time.
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๋‘์–ดํ•ด ์ „์œผ๋กœ ๋Œ์•„๊ฐ‘๋‹ˆ๋‹ค.
14:15
That's where it started.
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์—ฌ๊ธฐ๊ฐ€ ์‹œ์ž‘์ ์ž…๋‹ˆ๋‹ค.
14:23
That's where it ended a few months ago.
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์—ฌ๊ธฐ๊ฐ€ ๋ช‡๋‹ฌ ์ „์— ๋๋‚œ ์ง€์ ์ž…๋‹ˆ๋‹ค.
14:28
And on up to Greenland.
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๊ทธ๋ฆฐ๋ž€๋“œ๋กœ ๊ฐ€๋ด…์‹œ๋‹ค.
14:31
The smaller the ice mass, the faster it responds to climate.
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์–ผ์Œ ๋ฉ์–ด๋ฆฌ๊ฐ€ ์ž‘์„์ˆ˜๋ก, ๊ธฐํ›„์— ๋” ๋นจ๋ฆฌ ๋ฐ˜์‘ํ•˜์ฃ .
14:35
Greenland took a little while to start reacting
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๊ทธ๋ฆฐ๋ž€๋“œ๊ฐ€ ์ง€๋‚œ ์„ธ๊ธฐ์˜ ๊ธฐํ›„ ์˜จ๋‚œํ™”์— ๋ฐ˜์‘ํ•˜๋Š”๋ฐ๋Š”
14:38
to the warming climate of the past century,
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์•ฝ๊ฐ„์˜ ์‹œ๊ฐ„์ด ๊ฑธ๋ ธ์Šต๋‹ˆ๋‹ค๋งŒ,
14:41
but it really started galloping along about 20 years ago.
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์•ฝ20๋…„ ์ „๋ถ€ํ„ฐ๋Š” ๊ธ‰์†ํžˆ ์ง„ํ–‰๋˜๊ธฐ ์‹œ์ž‘ํ–ˆ์Šต๋‹ˆ๋‹ค.
14:45
And there's been a tremendous increase in the temperature up there.
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๋˜ํ•œ ์ด ์ง€์—ญ์˜ ์˜จ๋„ ์ƒ์Šน์ด ์–ด๋งˆ์–ด๋งˆ ํ–ˆ์Šต๋‹ˆ๋‹ค.
14:48
It's a big place. That's all ice.
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์ด๊ณณ์€ ๊ฑฐ๋Œ€ํ•œ ์ง€์—ญ์ž…๋‹ˆ๋‹ค. ์ „๋ถ€ ์–ผ์Œ์ด์ฃ .
14:50
All those colors are ice and it goes up to about two miles thick,
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์ƒ‰๊น”๋กœ ํ‘œ์‹œํ•œ ๋ชจ๋“  ์ง€์—ญ์ด ์–ผ์Œ์ด๊ณ , ๋‘๊ป˜๊ฐ€ ์•ฝ 2๋งˆ์ผ(3.2km)์ด๋‚˜ ๋ฉ๋‹ˆ๋‹ค.
14:54
just a gigantic dome that comes in from the coast and rises in the middle.
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ํ•ด์•ˆ๊ฐ€์—์„œ ์‹œ์ž‘ํ•ด ์ค‘์•™๋ถ€๊ฐ€ ์†Ÿ์•„์˜ค๋ฅธ ๊ฑฐ๋Œ€ํ•œ ๋”์ฒ˜๋Ÿผ ์ƒ๊ฒผ์ฃ .
14:58
The one glacier up in Greenland
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์ด๊ฑด ๊ทธ๋ฆฐ๋ž€๋“œ์— ์žˆ๋Š” ๋น™ํ•˜์ค‘ ํ•˜๋‚˜์ธ๋ฐ,
15:00
that puts more ice into the global ocean
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๋ถ๋ฐ˜๊ตฌ์˜ ๋‹ค๋ฅธ ๋น™ํ•˜๋ฅผ ๋‹ค ํ•ฉ์นœ ๊ฒƒ๋ณด๋‹ค
15:02
than all the other glaciers in the northern hemisphere combined
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๋” ๋งŽ์€ ์–‘์˜ ์–ผ์Œ์„ ๋ฐฐ์ถœํ•ฉ๋‹ˆ๋‹ค.
15:05
is the Ilulissat Glacier.
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์ผ๋ฃจ๋ฆฌ์‚ฟ ๋น™ํ•˜์ž…๋‹ˆ๋‹ค.
15:07
We have some cameras on the south edge of the Ilulissat,
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์ผ๋ฃจ๋ฆฌ์‚ฟ ๋น™ํ•˜์˜ ๋‚จ์ชฝ ๋์— ์นด๋ฉ”๋ผ๋ฅผ ๋ช‡ ๋Œ€ ์„ค์น˜ํ•˜์—ฌ
15:10
watching the calving face as it goes through this dramatic retreat.
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๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์ด ๊ทน์ ์œผ๋กœ ํ›„ํ‡ดํ•˜๋Š” ๋ชจ์Šต์„ ๊ด€์ฐฐํ–ˆ์Šต๋‹ˆ๋‹ค.
15:14
Here's a two-year record of what that looks like.
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2๋…„๋™์•ˆ ์–ด๋–ป๊ฒŒ ๋ณ€ํ–ˆ๋Š”์ง€ ๊ธฐ๋กํ•œ๊ฒŒ ์—ฌ๊ธฐ ์žˆ์Šต๋‹ˆ๋‹ค.
15:16
Helicopter in front of the calving face for scale, quickly dwarfed.
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ํ—ฌ๋ฆฌ์ฝฅํ„ฐ๊ฐ€ ๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด ์•ž์— ์žˆ์œผ๋‹ˆ, ๊ฐ‘์ž๊ธฐ ์™œ์†Œํ•ด์ง€๋Š”๊ตฐ์š”.
15:21
The calving face is four and a half miles across,
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๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์€ ๊ฐ€๋กœ ๊ธธ์ด๊ฐ€ 4.5๋งˆ์ผ(7.2km)์ธ๋ฐ,
15:23
and in this shot, as we pull back, you're only seeing about a mile and a half.
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์ด ์‚ฌ์ง„์€ ์ตœ๋Œ€ํ•œ ์คŒ-์•„์›ƒ ํ–ˆ์ง€๋งŒ 1.5๋งˆ์ผ(2.4km) ์ •๋„๋งŒ ๋ณด์ž…๋‹ˆ๋‹ค.
15:26
So, imagine how big this is
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๊ทธ๋Ÿฌ๋‹ˆ ์–ผ๋งˆ๋‚˜ ๊ฑฐ๋Œ€ํ•œ ๋น™ํ•˜์ธ์ง€
15:28
and how much ice is charging out.
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๋˜ ์–ผ๋งˆ๋‚˜ ๋งŽ์€ ์–ผ์Œ์ด ๋ฐฉ์ถœ๋˜๊ณ  ์žˆ๋Š”์ง€ ์ƒ์ƒํ•ด๋ณด์„ธ์š”.
15:30
The interior of Greenland is to the right.
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๊ทธ๋ฆฐ๋ž€๋“œ ๋‚ด๋ฅ™์€ ์‚ฌ์ง„์˜ ์˜ค๋ฅธ์ชฝ ๋ถ€๋ถ„์ž…๋‹ˆ๋‹ค.
15:32
It's flowing out to the Atlantic Ocean on the left.
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์™ผ์ชฝ์˜ ๋Œ€์„œ์–‘์„ ํ–ฅํ•ด ํ˜๋Ÿฌ๋‚ด๋ ค๊ฐ€๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
15:35
Icebergs, many, many, many, many times the size of this building, are roaring out to sea.
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์ด ๊ฑด๋ฌผ๋ณด๋‹ค ๋ช‡๋ฐฐ๋Š” ๋” ํฐ ๋น™์‚ฐ๋“ค์ด ๋ฐ”๋‹ค๋ฅผ ํ–ฅํ•ด ์šธ๋ถ€์ง–๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
15:41
We just downloaded these pictures a couple weeks ago,
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์ด ์‚ฌ์ง„๋“ค์€ 2์ฃผ์ฏค ์ „์— ๋‹ค์šด๋กœ๋“œ ๋ฐ›์€ ๊ฒ๋‹ˆ๋‹ค.
15:43
as you can see. June 25th,
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๋ณด๋‹ค์‹œํ”ผ 6์›” 25์ผ์—,
15:47
monster calving events happened.
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๊ฑฐ๋Œ€ํ•œ ๋น™ํ•˜ ๋ถ„๋ฆฌ ํ˜„์ƒ์ด ์ผ์–ด๋‚ฌ์Šต๋‹ˆ๋‹ค.
15:49
I'll show you one of those in a second.
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๊ทธ ์ค‘ ํ•˜๋‚˜๋ฅผ ๊ธˆ๋ฐฉ ๋ณด์—ฌ๋“œ๋ฆฌ๊ฒ ์Šต๋‹ˆ๋‹ค.
15:51
This glacier has doubled its flow speed in the past 15 years.
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์ด ๋น™ํ•˜๋Š” ์ง€๋‚œ 15๋…„๋™์•ˆ ์œ ์†์ด 2๋ฐฐ๋กœ ์ฆ๊ฐ€ํ–ˆ์Šต๋‹ˆ๋‹ค.
15:56
It now goes at 125 feet a day, dumping all this ice into the ocean.
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์ง€๊ธˆ์€ ํ•˜๋ฃจ์— 125ํ”ผํŠธ(38m)์˜ ์†๋„๋กœ ์›€์ง์ด๋ฉฐ, ์–ผ์Œ์„ ๋ฐ”๋‹ค์— ๋น ๋œจ๋ฆฌ๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
16:01
It tends to go in these pulses, about every three days,
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์•ฝ 3์ผ๋งˆ๋‹ค ์–ผ์Œ์ด ๋–จ์–ด์ ธ ๋‚˜๊ฐ€๋Š” ํŽธ์ธ๋ฐ,
16:03
but on average, 125 feet a day,
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ํ‰๊ท ์„ ๋‚ด๋ฉด ํ•˜๋ฃจ์— 125ํ”ผํŠธ(38m)์ด๊ณ 
16:05
twice the rate it did 20 years ago.
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20๋…„์ „๋ณด๋‹ค 2๋ฐฐ์ฃ .
16:09
Okay. We had a team out watching this glacier,
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๋„ค. ์ด ๋น™ํ•˜๋ฅผ ๊ด€์ฐฐํ•˜๋Š” ํŒ€์ด ์žˆ์–ด์„œ
16:13
and we recorded the biggest calving event that's ever been put on film.
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์—ฌ์ง€๊ป ๋…นํ™”ํ•œ ๊ฒƒ ์ค‘ ์ตœ๋Œ€์˜ ๋น™ํ•˜ ๋ถ„๋ฆฌ ์žฅ๋ฉด์„ ๊ธฐ๋กํ–ˆ์Šต๋‹ˆ๋‹ค.
16:16
We had nine cameras going.
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9๊ฐœ์˜ ์นด๋ฉ”๋ผ๋ฅผ ๊ฐ€๋™ํ•˜๊ณ  ์žˆ๋Š”๋ฐ์š”.
16:18
This is what a couple of the cameras saw.
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์ด๊ฒƒ์€ ๋‘์–ด๊ฐœ์˜ ์นด๋ฉ”๋ผ๊ฐ€ ๋ณธ ์žฅ๋ฉด์ž…๋‹ˆ๋‹ค.
16:22
A 400-foot-tall calving face breaking off.
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400ํ”ผํŠธ(120m) ๋†’์ด์˜ ๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์ด ๋–จ์–ด์ ธ ๋‚˜๊ฐ‘๋‹ˆ๋‹ค.
16:26
Huge icebergs rolling over.
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๊ฑฐ๋Œ€ํ•œ ๋น™์‚ฐ์ด ๋’ค์ง‘ํž™๋‹ˆ๋‹ค.
17:13
Okay, how big was that? It's hard to get it.
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์–ผ๋งˆ๋‚˜ ํฐ ๋…€์„์ด์—ˆ์„๊นŒ์š”? ๊ฐ์ด ์ž˜ ์•ˆ์˜ค์‹ค ๊ฒ๋‹ˆ๋‹ค.
17:16
So an illustration again, gives you a feeling for scale.
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ํฌ๊ธฐ๋ฅผ ์‹ค๊ฐํ•˜์‹ค ์ˆ˜ ์žˆ๊ฒŒ ๋˜ ๋‹ค์‹œ ๊ทธ๋ฆผ์„ ๊ทธ๋ ค๋ดค์Šต๋‹ˆ๋‹ค.
17:19
A mile of retreat in 75 minutes
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[๋Œ€๋žต] 75๋ถ„๋™์•ˆ 1๋งˆ์ผ(1.6km) ํ›„ํ‡ดํ•ฉ๋‹ˆ๋‹ค.
17:22
across the calving face, in that particular event, three miles wide.
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ํญ์ด 3๋งˆ์ผ(4.8km)์ธ ์ € ํŠน์ • ๊ตฌ๋ฉ์˜ ๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์„ ๋”ฐ๋ผ์„œ ๋ง์ด์ฃ .
17:26
The block was three-fifths of a mile deep,
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์ด ๋ฉ์–ด๋ฆฌ๋Š” 5๋ถ„์˜ 3๋งˆ์ผ(960m) ๊นŠ์ด์ด๊ณ ,
17:28
and if you compare the expanse of the calving face
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์ด ๋ถ„๋ฆฌ๋น™ํ•˜๋ฉด์˜ ๊ด‘ํ™œํ•จ์„ ๋Ÿฐ๋˜์˜ ํƒ€์›Œ๋ธŒ๋ฆฌ์ง€๋ž‘ ๋น„๊ตํ•˜์ž๋ฉด
17:31
to the Tower Bridge in London, about 20 bridges wide.
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๊ทธ ํญ์ด ํƒ€์›Œ๋ธŒ๋ฆฌ์ง€ ์•ฝ 20๊ฐœ์— ๋‹ฌํ•ฉ๋‹ˆ๋‹ค.
17:34
Or if you take an American reference, to the U.S. Capitol Building
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๋ฏธ๊ตญ ๊ฒƒ์œผ๋กœ ์ฐธ์กฐํ•˜์ž๋ฉด, ๋ฏธ ๊ตญํšŒ์˜์‚ฌ๋‹น ๊ฑด๋ฌผ์„ ๊ฐ€์ ธ์™”์„๋•Œ
17:38
and you pack 3,000 Capitol Buildings into that block,
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์ € ๋ฉ์–ด๋ฆฌ ์•ˆ์— ๊ตญํšŒ์˜์‚ฌ๋‹น์„ 3000๊ฐœ ์ง‘์–ด๋„ฃ์„ ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
17:42
it would be equivalent to how large that block was.
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์ € ์–ผ์Œ๋ฉ์–ด๋ฆฌ์˜ ํฌ๊ธฐ๋Š” ๊ทธ ์ •๋„ ๋  ๊ฒ๋‹ˆ๋‹ค.
17:47
75 minutes.
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์ด ๋ชจ๋“ ๊ฒŒ 75๋ถ„ ๋งŒ์— ์ผ์–ด๋‚ฌ์Šต๋‹ˆ๋‹ค.
17:51
Now I've come to the conclusion
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์ด์ œ ๊ฒฐ๋ก ์— ๋‹ค๋‹ค๋ž์Šต๋‹ˆ๋‹ค.
17:53
after spending a lot of time in this climate change world
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๊ธฐํ›„ ๋ณ€ํ™”์— ๋Œ€ํ•ด ๋ฐฐ์šฐ๋Š๋ผ ๋งŽ์€ ์‹œ๊ฐ„์„ ๋ณด๋ƒˆ๋Š”๋ฐ์š”.
17:56
that we don't have a problem of economics, technology and public policy.
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์šฐ๋ฆฌ๋Š” ๊ฒฝ์ œ, ๊ธฐ์ˆ , ์ •์ฑ…์  ๋ฌธ์ œ๋ฅผ ์•ˆ๊ณ  ์žˆ๋Š” ๊ฒƒ์ด ์•„๋‹ˆ๋ผ
18:00
We have a problem of perception.
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์ธ์‹์˜ ๋ฌธ์ œ๋ฅผ ๊ฐ€์ง€๊ณ  ์žˆ์Šต๋‹ˆ๋‹ค.
18:03
The policy and the economics and the technology are serious enough issues,
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์ •์น˜, ๊ฒฝ์ œ, ๊ธฐ์ˆ ๋„ ์‹ฌ๊ฐํ•œ ๋ฌธ์ œ์ž…๋‹ˆ๋‹ค๋งŒ
18:06
but we actually can deal with them.
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์šฐ๋ฆฌ๋Š” ์ด๋ฅผ ํ•ด๊ฒฐํ•  ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค.
18:08
I'm certain that we can.
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๊ทธ๋Ÿด ๊ฑฐ๋ผ๊ณ  ํ™•์‹ ํ•ฉ๋‹ˆ๋‹ค.
18:11
But what we have is a perception problem
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ํ•˜์ง€๋งŒ ์šฐ๋ฆฌ์—๊ฒ ์ธ์‹์˜ ๋ฌธ์ œ๊ฐ€ ์žˆ์Šต๋‹ˆ๋‹ค.
18:13
because not enough people really get it yet.
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์ด๊ฑธ ์•„์‹œ๋Š” ๋ถ„๋“ค์ด ์•„์ง ์ถฉ๋ถ„์น˜ ์•Š์Šต๋‹ˆ๋‹ค.
18:17
You're an elite audience. You get it.
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์—ฌ๋Ÿฌ๋ถ„์€ ์—˜๋ฆฌํŠธ๋“ค์ด๊ณ , ์ด๊ฑธ ์•„์‹œ์ฃ .
18:19
Fortunately, a lot of the political leaders in the major countries of the world
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๋‹คํ–‰ํžˆ๋„, ์„ธ๊ณ„ ์ฃผ์š” ๊ตญ๊ฐ€๋“ค์˜ ์ •์น˜ ์ง€๋„์ž๋“ค์€
18:23
are an elite audience that for the most part gets it now.
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์—˜๋ฆฌํŠธ๋“ค์ด๋ผ์„œ ๋Œ€๋ถ€๋ถ„ ์ด ๋ฌธ์ œ๋ฅผ ์ดํ•ดํ•ฉ๋‹ˆ๋‹ค.
18:27
But we still need to bring a lot of people along with us.
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ํ•˜์ง€๋งŒ ์•„์ง๋„ ์šฐ๋ฆฌ๋Š” ๋งŽ์€ ์‚ฌ๋žŒ๋“ค์„ ๋Œ์–ด๋ชจ์•„์•ผ ํ•ฉ๋‹ˆ๋‹ค.
18:30
And that's where I think organizations like TED,
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๊ทธ๋ž˜์„œ ์ „ TED๋‚˜ ๊ทน์ง€ ๋น™ํ•˜ ํƒ์‚ฌ(EIS) ๊ฐ™์€ ์กฐ์ง์ด
18:34
like the Extreme Ice Survey can have a terrific impact
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์‚ฌ๋žŒ์˜ ์ธ์‹์— ์ง€๋Œ€ํ•œ ์˜ํ–ฅ์„ ๋ผ์น˜๊ณ 
18:37
on human perception and bring us along.
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์šฐ๋ฆฌ์™€ ํ•จ๊ป˜ ํ•  ๊ฑฐ๋ผ๊ณ  ์ƒ๊ฐํ•ฉ๋‹ˆ๋‹ค.
18:40
Because I believe we have an opportunity right now.
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์ง€๊ธˆ์€ ๊ธฐํšŒ๊ฐ€ ์žˆ๋‹ค๊ณ  ๋ฏฟ์Šต๋‹ˆ๋‹ค.
18:42
We are nearly on the edge of a crisis,
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์šฐ๋ฆฌ๋Š” ์œ„๊ธฐ์˜ ๋ฒผ๋ž‘ ๋์— ๊ฑฐ์˜ ๋‹ค๋‹ค๋ž์ง€๋งŒ,
18:45
but we still have an opportunity to face the greatest challenge
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์šฐ๋ฆฌ ์„ธ๋Œ€์™€ ์šฐ๋ฆฌ ์„ธ๊ธฐ์˜ ๊ฐ€์žฅ ๋Œ€๋‹จํ•œ ๋„์ „์—
18:49
of our generation and, in fact, of our century.
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๋งž์„ค ๊ธฐํšŒ๊ฐ€ ์•„์ง ์žˆ์Šต๋‹ˆ๋‹ค.
18:52
This is a terrific, terrific call to arms
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์ด๊ฒƒ์€ ์†Œ์ง‘ ๋ช…๋ น์ž…๋‹ˆ๋‹ค.
18:56
to do the right thing for ourselves and for the future.
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์Šค์Šค๋กœ์™€ ๋ฏธ๋ž˜๋ฅผ ์œ„ํ•ด ์˜ณ์€ ์ผ์„ ํ•˜์ž๋Š” ๊ฑฐ์ฃ .
18:59
I hope that we have the wisdom to let the angels of our better nature
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์ด ์ƒํ™ฉ์—์„œ ์šฐ๋ฆฌ ๋ณธ์„ฑ์— ๊นƒ๋“  ๋ณด๋‹ค ์„ ๋Ÿ‰ํ•œ ์ฒœ์‚ฌ๊ฐ€ ๋‚˜ํƒ€๋‚˜๊ธฐ๋ฅผ,
19:02
rise to the occasion and do what needs to be done. Thank you.
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๋˜ํ•œ ํ•ด์•ผ ํ•  ์ผ์„ ํ•˜๋Š” ์ง€ํ˜œ๋ฅผ ๊ฐ€์ง€๊ธธ ๋ฐ”๋ž๋‹ˆ๋‹ค. ๊ฐ์‚ฌํ•ฉ๋‹ˆ๋‹ค.
19:06
(Applause)
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(๋ฐ•์ˆ˜)
์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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