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Earth and Space Sciences · 术语表

什么是 Ice–albedo feedback?

又称: ice--albedo feedback

Definition 18.8 University Earth and Space Sciences — Year 2 · 第 18 章 — The Precambrian Earth

The ice–albedo feedback is the amplification of a change of temperature by the change of snow and ice cover it causes: cooling extends the ice, which raises the planet’s albedo, reduces the sunlight absorbed and cools the planet further; warming works the other way. It is a positive feedback.

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