What does albedo measure?

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Albedo measures the reflectivity of a surface, specifically defined as the ratio of electromagnetic radiation that is reflected by a surface to the total amount of radiation that is incident upon it. This means that when sunlight or other forms of radiation strike a surface, albedo quantifies how much of that energy is bounced back into space versus how much is absorbed.

For example, surfaces like ice and snow have high albedo because they reflect a significant portion of incoming solar radiation, while darker surfaces, like forests or oceans, have lower albedo as they absorb more energy. Understanding albedo is crucial in fields like climatology and environmental science, as it influences temperature regulation, climate change, and even weather patterns. In contrast, the measurement of temperature, the amount of energy absorbed, or atmospheric thickness relates to different scientific concepts which do not directly correspond to the definition of albedo.

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