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Albedo is an indicator of how much incident radiation, such as sunlight, is reflected by the Earth's surface or the surface of an object. It is typically expressed as a dimensionless value between 0 and 1, or as a percentage (%), where higher values indicate higher reflectivity and lower values indicate greater absorption of energy. For example, fresh snow has a very high albedo, reflecting most sunlight. In contrast, forests, oceans, and asphalt pavements have relatively low albedo, absorbing more energy. Albedo is a key physical quantity significantly involved in Earth's energy balance and climate system, and is utilized in many fields including climate science, environmental research, remote sensing, and urban climatology.
2026-03-27 07:42:00
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