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.
书籍暂未推出简体中文版——当前显示英文版。
Earth and Space Sciences · 术语表
什么是 Ice–albedo feedback?
又称: ice--albedo feedback