쉐도잉 연습: What causes avalanches, and can you survive them? - Simon Trautman - YouTube로 영어 말하기 배우기

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In February 2012, pro skier Elyse Saugstad was carving through the slopes of the Cascade Mountains when a crack formed in the snowpack above her.
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In February 2012, pro skier Elyse Saugstad was carving through the slopes of the Cascade Mountains when a crack formed in the snowpack above her.
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Before she was fully engulfed by a 5,000-ton wall of snow, Elyse heard “AVALANCHE!” just in time to react with a lifesaving maneuver.
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So, how could she survive this crushing snow surge?
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Avalanches are the rapid descension of snow, ice, rock, or a combination of these down a slope.
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They can be destructive natural disasters and personal tragedies: in the United States alone, avalanches kill an average of 27 people annually.
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These alpine nightmares don’t just awaken out of nowhere; they need three specific conditions.
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First, the mountain needs to have the right slope, typically between 30 and 45 degrees.
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This is shallow enough to allow snow to build up on the slope, yet steep enough to provide enough potential energy for movement.
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Second, they typically need a layer of sturdy snow deposited over a weak or unstable layer, or what’s sometimes called “something over nothing.” Take the Cascade Mountain avalanche, where recent heavy storms deposited a nearly 1-meter-deep slab of fresh snow.
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Below this sat a thin layer of surface hoar.
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These are delicate, feathery ice crystals that form when water vapor in the air rapidly freezes on the surface of snow, almost like dew in the wintertime.
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Finally, avalanches need a trigger, something to collapse the weak layer and put the snow in motion.
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A trigger can be natural, such as heavy snowfall, strong winds, rainfall, or even other avalanches.
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Or they can be human-caused, like the surface impact of skiers or snowmobilers.
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Since fractures can propagate quickly through the snowpack, triggers can originate hundreds of meters away— upstream, downstream, or even adjacent to the avalanche’s path.
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Once in motion, how quickly an avalanche moves depends on the slope’s steepness, its exposure or vegetation cover, terrain roughness, and the type and amount of snow involved.
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For example, dry, light, and loosely bonded snow tends to travel fast, forming a powder cloud as it moves.
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In contrast, wet snow avalanches, caused by water moving through the snowpack, travel more slowly but are much denser and can be particularly destructive.
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Larger avalanches can travel more than 160 kilometers per hour, breaking trees, destroying buildings, and burying roadways.
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In 1970, one particularly massive avalanche consisting of 50 to 100 million cubic meters of glacial ice, snow, mud, and rock reached speeds of over 300 kilometers per hour.
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This avalanche proved to be the deadliest in history, engulfing an entire Peruvian town and killing 18,000 people.
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Avalanches aren't always this large, but even smaller ones can be dangerous for anyone caught in their path.
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As snow rushes downhill, it can behave like both a solid and a liquid, making its movement difficult to predict.
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At the fastest-moving front, surface snow moves faster than the snow beneath, pulling victims deep into the snowpack and scattering them across wide areas, making rescue difficult.
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Once an avalanche slows, the snow loses its fluid-like properties and compacts, leaving victims immobilized and unable to escape on their own.
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For these reasons, the best way to survive an avalanche is to avoid one altogether.
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Thankfully, at most ski resorts, parks, and even highways, avalanche workers mitigate risk by continuously monitoring the weather, stability of the snowpack, and human activity.
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If a threat is detected, they'll close terrain and may even intentionally trigger a controlled avalanche with explosives or artillery.
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However, there are regions where avalanche risk is not actively mitigated, known as the backcountry.
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Here, you are responsible for managing your own risk.
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Local avalanche centers provide avalanche forecasts, and anyone entering the backcountry should understand them, be properly trained, and carry essential rescue gear.
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And ultimately, in high-hazard terrain, there's no way to completely eliminate risk.
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The group at the Cascade Mountains consisted of highly experienced skiers.
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Yet the area was very exposed, and following a large storm, the avalanche danger forecast was elevated.
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In the end, three skiers lost their lives.
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But not Elyse, as she was able to deploy an inflatable airbag.
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These devices are imperfect and a last line of defense, yet can keep a victim closer to the surface, improving their chance of rescue should disaster strike.

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이 수업에 대하여

이번 수업에서는 눈사태에 대해 배우고, 생존 방법에 대한 이야기를 통해 영어 실력을 키워볼 것입니다. 수업을 통해 눈사태가 어떻게 발생하는지, 그 위험성을 줄이기 위한 예방 조치에 대해 이해할 수 있습니다. 이러한 과정에서 관련 어휘와 표현을 익히며, 유튜브 영어 공부에 큰 도움이 될 것입니다.

핵심 어휘 및 구문

  • 눈사태 (avalanche) - 눈, 얼음, 바위 등이 경사의 아래로 급속히 내려오는 현상
  • 구조 (rescue) - 위험에 처한 사람을 구하는 행위
  • 위험 (danger) - 위험한 상황이나 조건
  • 적극적인 사고 방지 (active mitigation) - 사고를 미연에 방지하기 위한 활동
  • 예방 조치 (preventive measures) - 사고를 예방하기 위한 방법
  • 법적 책임 (responsibility) - 특정 상황에서 해야 할 일이나 의무
  • 구조 장비 (rescue gear) - 구조를 위한 장비나 도구
  • 지형 (terrain) - 산악 지역이나 지형의 특성

연습 팁

이번 영상에서는 주제와 관련된 정보가 빠르게 제공됩니다. 쉐도잉 연습을 할 때는 영상의 속도에 맞춰 발음을 따라하는 것이 중요합니다. 빠른 발음에 익숙해지기 위해, 처음에는 낮은 속도로 시작하고 점차 속도를 높여가는 방법이 효과적입니다. 'shadow speech' 방식을 사용하여 자주 듣는 구문을 반복하면 자연스럽게 영어 발음 교정이 이루어질 것입니다. 또한, 영상의 감정과 톤을 소리내어 따라서 말해보면 문맥을 이해하는 데 도움이 됩니다. 영어 쉐도잉을 통해 자연스러운 발음을 기를 수 있으며, 이는 결국 대화 능력을 향상시키는 데 큰 도움이 됩니다.

쉐도잉이란? 영어 실력을 빠르게 키우는 과학적 방법

쉐도잉(Shadowing)은 원래 전문 통역사 훈련을 위해 개발된 언어 학습 기법으로, 다언어 학자인 Dr. Alexander Arguelles에 의해 대중화된 방법입니다. 핵심 원리는 간단하지만 매우 강력합니다: 원어민의 영어를 들으면서 1~2초의 짧은 지연으로 즉시 소리 내어 따라 말하는 것——마치 '그림자(shadow)'처럼 화자를 따라가는 것입니다. 문법 공부나 수동적인 청취와 달리, 쉐도잉은 뇌와 입 근육이 동시에 실시간으로 영어를 처리하고 재현하도록 훈련합니다. 연구에 따르면 이 방법은 발음 정확도, 억양, 리듬, 연음, 청취력, 말하기 유창성을 크게 향상시킵니다. IELTS 스피킹 준비와 자연스러운 영어 소통을 원하는 분들에게 특히 효과적입니다.

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