albedo

American  

[al-bee-doh] / ælˈbi doʊ /

noun

plural

albedos

1. Astronomy. the ratio of the light reflected by a planet or satellite to that received by it.

2. Meteorology. such a ratio for any part of the earth's surface or atmosphere.

3. pith.

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albedo British  

/ ælˈbiːdəʊ /

noun

1. the ratio of the intensity of light reflected from an object, such as a planet, to that of the light it receives from the sun

2. physics the probability that a neutron passing through a surface will return through that surface

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albedo Scientific  

/ ăl-bē′dō /

1. The fraction of the total light striking a surface that gets reflected from that surface. An object that has a high albedo (near 1) is very bright; an object that has a low albedo (near 0) is dark. The Earth's albedo is about 0.37. The Moon's is about 0.12.

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Etymology

Origin of albedo

First recorded in 1855–60; from Late Latin albēdō “white (color), whiteness,” equivalent to alb(us) “white” + -ēdō noun suffix; torpedo

Explanation

Albedo refers to how reflective and bright something is. Snow has a high albedo, which is why skiers wear sunglasses and sunscreen. Technically speaking, the albedo of an object is a ratio. It compares the amount of light hitting the surface of the object to the amount of light that gets reflected back. The more light reflected, the higher the albedo. Scientists often use this word in reference to the surfaces of planets and other reflective objects in the night sky. Albedo comes from a Latin word for “white.”

Example Sentences

"Water vapor does not affect the albedo of Earth, so it did not affect our analysis of the magnitude of the aerosol forcing."

From Salon • Feb. 6, 2025

In order to calculate the potential effects of this reduced albedo, the researchers applied an established energy budget model capable of mimicking the temperature response of complex climate models.

From Science Daily • Dec. 5, 2024

Other potential outcomes include reductions in albedo — or the amount of light reflected by the ice — which would accelerate human-caused warming by creating an amplifying feedback loop.

From Los Angeles Times • Mar. 5, 2024

The loss of ice affects land surface temperatures because of albedo, which is the measure of how reflective a surface is.

From Science Daily • Feb. 13, 2024

In technical terms, the albedo of the moon is .07, which means that it bounces back only 7 percent of the light striking it, absorbing the other 93 percent.

From "Flying to the Moon: An Astronaut's Story" by Michael Collins