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Why Do Certain Clouds Glow Brightly at Twilight?
为什么某些云层在暮色中会发出明亮光芒?
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Noctilucent clouds form high in the mesosphere, about 80–85 km above Earth’s surface.
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They appear only during summer months near polar regions when sunlight reflects off ice crystals.
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These tiny ice particles grow on meteoric dust that enters our atmosphere from space.
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Unlike lower clouds, noctilucent clouds remain sunlit long after sunset due to their extreme altitude.
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Their electric-blue glow results from scattering of blue wavelengths by nanoscale ice grains.
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Scientists monitor them closely because increasing frequency may signal changes in upper-atmosphere chemistry.
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They are visible only when the Sun is 6–12 degrees below the horizon and the sky is otherwise dark.
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Ground observers must face north in the Northern Hemisphere to spot these delicate, wavy structures.
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Radar and satellite data confirm their composition includes water ice, not frozen carbon dioxide or ammonia.
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Studying them helps us understand how atmospheric gravity waves influence cloud formation far above weather systems.