Color Temperature Chart

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Color TemperaTure and Color rendering
There are two standard measurements for the color characteristics of light: “color rendering index” (CRI), a term used to
describe the extent to which an artificial light source is able to render the true color of objects as seen by natural outdoor
sunlight which has a CRI of 100, and “color temperature”, which expresses the color appearance of the light itself.
Color rendering index: Incandescent is used as the base reference of 100 CRI. Compact fluorescent lamps are graded
at 82-86 CRI, which is considered high quality color rendering. CRI is a more important consideration for retail lighting
design than it is for office lighting.
Any CRI rating of 80 or above is considered high and indicates that the source has good color properties. Incandescent
lamps and daylight have a CRI of 100, the highest possible CRI. The higher the CRI of the light source, the “truer” it
renders color.
Color Temperature: Refers to the way color groups are perceived – the psychological impact of lighting. Color
temperature is how cool or warm the light source appears.
The color temperature of a light source is a numerical measurement of its color appearance. This temperature is based
on the principle that any object will emit light if it is heated to a high enough temperature and that the color of that light will
shift in a predictable manner as the temperature is increased. This system is based on the color changes of a black metal
as it is heated from a cold black to a white hot state. As the temperature increases, the color would shift gradually from red
to orange to yellow to white and finally to a blue white. Color temperature is measured in degrees Kelvin (K). Colors and
light sources from the red/orange/yellow side of the spectrum are described as warm (incandescents) and those toward
the blue end are referred to as cool (natural daylight).
The sun, for example, rises at approximately 1800 Kelvin and changes from red to orange to yellow and to white as it
rises to over 5000 Kelvin at high noon. It then goes back down the scale as it sets.

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