Albedo
This is called the "albedo." It is the ratio of reflected light compared to incident light, and depends on the surface material and its condition (e.g. snow, grassland).
The reflection of a celestial body is called "albedo," which is a measure of how much light is reflected by a surface. A high albedo means that the surface reflects a lot of light, while a low albedo means that the surface absorbs more light. Albedo can vary depending on the composition and texture of the celestial body's surface.
Albedo. The albedo of the Earth is 0.367. When Vangelis released his album, Albedo 0.39, that was what the albedo of Earth was in 1976.
The albedo of the Earth's surface is the fraction of solar radiation that is reflected back into space. It is a measure of how reflective a surface is, with higher albedo values indicating more reflection and less absorption of sunlight by the surface. Land surfaces, ice, and clouds generally have higher albedo values, while oceans and forests have lower albedo values.
Low albedo indicates that a surface has a lower ability to reflect sunlight. This means that the surface absorbs more sunlight and heats up more quickly compared to a surface with a higher albedo.
albedo
Albedo is the measure of reflectivity of a surface - the higher the albedo, the more sunlight is reflected and less is absorbed, leading to lower surface temperatures. Surfaces with low albedo absorb more sunlight and heat up faster, whereas surfaces with high albedo reflect more sunlight and stay cooler.
Charcoal has the lowest albedo. Albedo is the reflectivity of light from a surface.
Albedo is a measure of reflectivity; it is a measure of the percentage of light reflected from a surface. A perfect mirror would have an albedo of 1, while white snow has an albedo of about 0.9. Charcoal has an albedo of about 0.04.An albedo higher than 1 is impossible.
A high albedo indicates that a surface has a strong ability to reflect sunlight.
Albedo refers to the reflectivity of a surface. Surfaces with high albedo reflect more solar radiation back into space, which can cool the Earth's surface and lower temperatures. Surfaces with low albedo absorb more solar radiation, leading to warming of the Earth's surface.