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Albedo (/ æ l ˈ b iː d oʊ / al-BEE-doh; from Latin albedo 'whiteness') is the fraction of sunlight that is diffusely reflected by a body. It is measured on a scale from 0 (corresponding to a black body that absorbs all incident radiation) to 1 (corresponding to a body that reflects all incident radiation).
A list of 'effects' that have been noticed in the field of psychology. [clarification needed] Ambiguity effect;
Citrinitas, or sometimes xanthosis, [1] is a term given by alchemists to "yellowness." It is one of the four major stages of the alchemical magnum opus.In alchemical philosophy, citrinitas stood for the dawning of the "solar light" inherent in one's being, and that the reflective "lunar or soul light" was no longer necessary.
In alchemy, albedo, or leucosis, is the second of the four major stages of the Magnum Opus, along with nigredo, citrinitas and rubedo. [1] It is a Latinicized term meaning "whiteness". Following the chaos or massa confusa of the nigredo stage, the alchemist undertakes a purification in albedo, which is literally referred to as ablutio – the ...
In psychology, libido (/ l ɪ ˈ b iː d oʊ /; from Latin libīdō 'desire') is psychic drive or energy, usually conceived of as sexual in nature, but sometimes conceived of as including other forms of desire. [1] The term libido was originally developed by Sigmund Freud, the pioneering originator of psychoanalysis.
Cloud albedo is a measure of the albedo or reflectivity of a cloud. Clouds regulate the amount of solar radiation absorbed by a planet and its solar surface irradiance . Generally, increased cloud cover correlates to a higher albedo and a lower absorption of solar energy .
For Carl Jung, "the rediscovery of the principles of alchemy came to be an important part of my work as a pioneer of psychology". [3] As a student of alchemy, he (and his followers) "compared the 'black work' of the alchemists (the nigredo) with the often highly critical involvement experienced by the ego, until it accepts the new equilibrium brought about by the creation of the self."
Ice–albedo feedback also has a smaller, but still notable effect on the global temperatures. Arctic sea ice decline between 1979 and 2011 is estimated to have been responsible for 0.21 watts per square meter (W/m 2 ) of radiative forcing , which is equivalent to a quarter of radiative forcing from CO 2 [ 13 ] increases over the same period.