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albedo

[al-bee-doh]

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.



albedo

/ 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

“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

albedo

  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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Word History and Origins

Origin of albedo1

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

Origin of albedo1

C19: from Church Latin: whiteness, from Latin albus white
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Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

"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

Planetary albedo describes the percentage of incoming solar radiation that is reflected back into space after all interactions with the atmosphere and the surface of the Earth.

Even in these locations, however, albedo changes are likely to offset the net climate benefit by at least 20 percent in around two-thirds of cases.

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.

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

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Al-Battanialbedometer