Intro to Climate Science
Albedo is a measure of how much sunlight is reflected by a surface, expressed as a percentage. Surfaces with high albedo, like ice and snow, reflect most of the incoming solar radiation, while those with low albedo, such as forests or oceans, absorb more sunlight. This concept is crucial in understanding energy balance and how changes in albedo can influence climate, particularly during tipping points and the Earth's energy budget.
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