Higher albedo refers to the increased reflectivity of a surface, meaning it reflects a larger proportion of incoming sunlight rather than absorbing it. Surfaces with high albedo, such as ice, snow, and certain types of clouds, can contribute to cooling effects in the environment, as they reduce the amount of heat absorbed by the Earth. In contrast, surfaces with low albedo, like forests or oceans, absorb more sunlight, leading to warmer temperatures. Changes in albedo can significantly impact climate and weather patterns.
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