Intro to Climate Science
Albedo feedback refers to the process where changes in the Earth's surface reflectivity (albedo) amplify or dampen the effects of climate change. This phenomenon is crucial in understanding how changes in the cryosphere, particularly ice sheets, glaciers, and sea ice, influence global temperatures. When ice melts, it exposes darker surfaces that absorb more sunlight, leading to further warming and additional melting, creating a reinforcing cycle of temperature increase.
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