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WHAT IS AN AURORA? - Contenido educativo
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Every second, one million tons of matter is blasted from the sun at a velocity of one million miles per hour.
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And it's on a collision course with Earth.
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But don't worry, this isn't the opening of a new Michael Bay movie.
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This is the journey of the polar lights.
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The northern and southern lights, also known as the aurora borealis and aurora australis respectively,
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occur when high-energy particles from the sun collide with neutral atoms in our atmosphere.
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The energy emitted from this crash produces a spectacle of light that mankind has marveled at for centuries.
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But the particle's journey isn't just as simple as leaving the sun and arriving at Earth.
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Like any cross-country road trip, there's a big detour, and nobody asks for directions.
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Let's track this intergalactic voyage by focusing on three main points of their journey.
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Leaving the sun, making a pit stop in the Earth's magnetic fields, and arriving at the atmosphere above our heads.
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The protons and electrons creating the northern lights depart from the sun's corona.
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The corona is the outermost layer of the sun's atmosphere and is one of the hottest regions.
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Its intense heat causes the sun's hydrogen and helium atoms to vibrate and shake off protons and electrons,
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as if they were stripping off layers on a hot, sunny day.
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Impatient and finally behind the wheel,
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these freak protons and electrons move too fast to be contained by the sun's gravity
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and group together as plasma, an electrically charged gas.
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They travel away from the Sun as a constant gale of plasma, known as the solar wind.
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However, the Earth prevents the solar wind from traveling straight into the planet by setting up a detour, the magnetosphere.
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The magnetosphere is formed by the Earth's magnetic currents and shields our planet from the solar winds by sending out the particles around the Earth.
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Their opportunity to continue the journey down to the atmosphere comes when the magnetosphere is overwhelmed by a new wave of travelers.
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This event is coronal mass ejection, and it occurs when the Sun shoots out a massive ball of plasma into the solar wind.
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When one of these coronal mass ejections collides with Earth, it overpowers the magnetosphere and creates a magnetic storm.
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The heavy storm stresses the magnetosphere until it suddenly snaps back, like an overstretched elastic band, flinging some of the detoured particles towards Earth.
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The retracting band of the magnetic field guides them down to the aurora ovals,
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which are the locations of the northern and southern lights.
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After traveling 93 million miles across the galaxy,
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the sun's particles finally produce their dazzling light show with the help of some friends.
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Twenty to two hundred miles above the surface,
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the electrons and protons meet up with oxygen and nitrogen atoms,
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and they sure are happy to see each other.
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The sun's particles high-five the atoms,
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atoms, giving their energy to the Earth's neutral oxygen and nitrogen atoms.
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When the atoms in the atmosphere are contacted by the particles, they get excited and emit
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photons.
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Photons are small bursts of energy in the form of light.
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The colors that appear in the sky depend on the wavelength of the atom's photon.
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Excited oxygen atoms are responsible for the green and red colors, whereas excited nitrogen
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atoms produce blue and deep red hues.
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The collection of these interactions is what creates the northern and southern lights.
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Polar lights are best seen on clear nights in regions close to the magnetic north and
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south poles.
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Nighttime is ideal because the aurora is much dimmer than sunlight and cannot be seen in
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daytime.
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Remember to look up at the sky and read up on the sun's energy patterns, specifically
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sunspots and solar flares, as these will be good guides for predicting the auroras.
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- Subido por:
- Alicia M.
- Licencia:
- Dominio público
- Visualizaciones:
- 58
- Fecha:
- 1 de abril de 2021 - 18:03
- Visibilidad:
- Público
- Centro:
- IES LA SENDA
- Duración:
- 04′ 09″
- Relación de aspecto:
- 1.78:1
- Resolución:
- 1920x1080 píxeles
- Tamaño:
- 110.21 MBytes