The boundary between visible light and ultraviolet begins at around 400 nanometers, and wavelengths smaller than 100 nm are considered X-rays. The earth’s atmosphere absorbs the ultraviolet with very short wavelengths; the shortest ultraviolet wavelengths that reach earth’s surface are about 286 nm.
The spectrum of ultraviolet radiation has been divided in a number of ways:
A division often used by physicists:
Name of Band | Range of Wavelengths |
---|---|
near UV | 400 to 300 nanometers |
middle UV | 300 to 200 nm |
far UV | 200 to 100 nm |
extreme UV | 100 nm to around 40 – 10 nm |
A division based on the radiation’s biological effects¹:
Name of Band | Range of Wavelengths |
---|---|
near UV | 400 to 315 nanometers |
actinic UV | 315 to 200 nm |
vacuum UV | less than 200 nm |
The International Commission on Illumination (the CIE) defined three UV bands², again on the basis of biological effects. This classification is the one encountered in advertisements for sunscreens:
Name of Band | Range of Wavelengths |
---|---|
UV-A | 400 to 315 nanometers |
UV-B | 315 to 280 nm |
UV-C | 280 to 100 nm |
Taking the lower limit of UV-A as 320 nm instead of 315, and the upper limit as 290 instead of 280, is a common practice.
1.
A. F. McKinlay
Ultraviolet radiation: Potential hazards.
In Physics in Medicine and Biology Encyclopedia. Vol. 2
Oxford: Pergamon, 1986.
2.
Commission Internationale de l’Eclairage.
International Lighting Vocabulary. Third Edition.
Publication CIE 17 nr (E-1.1)
Paris: Commission Internationale de l’Eclairage, 1991.
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