The proportion of energy mirrored from an object in contrast to the original amount of electricity that struck the object is known as albedo.
A body with an albedo of 1 will reflect all incident solar radiation, while a black body with a value of 0 will absorb all solar radiation. The diffuse representation of solar irradiance out of total sunlight is measured as albedo.
The amount of incoming sunlight that is reflected back into space is known as albedo, which is the reflectivity of the earth. The main factors influencing global albedo are cloud cover and land-based ice cover, particularly in places like Greenland and Antarctica that have substantial ice caps.
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