UVB is generally defined as the wavelength band from 290-320nm, but it is the band between 290-305 nm that is most important.
The earth’s climate is determined by the amount of solar radiation that strikes the surface.
Factors like the sun’s position, the earth’s rotation, geographic location, the ozone layer, clouds, air-humidity, elevation, environment, etc. influence the intensity of light. Also within the microhabitat the light intensity of both visual and non-visual light varies, depending on the density of the vegetation or geological conditions.
At this time, the sun’s rays have the least distance to travel through the atmosphere and UVB levels are at their highest. In the early morning and late afternoon, the sun’s rays pass through the atmosphere at an angle and their intensity is greatly reduced.
Maps of the UV index for the Northern Hemisphere indicate that the UV index is highest during the summer months (despite the fact that the sun is directly overhead at the Tropic of Cancer only during the Autumnal Equinox).
UV levels in the tropics are very high. High equatorial UV levels are primarily caused by the high angle of the sun, a thinner layer of atmosphere, reduced air pollution, and diminished atmospheric ozone. Ozone is naturally thinner in the tropics compared to the mid- and high-latitudes, so there is less ozone to absorb the UV radiation as it passes through the atmosphere. At higher latitudes the sun is lower in the sky, so UV rays must travel a greater distance through ozone-rich portions of the atmosphere and, in turn, expose those latitudes to less UV radiation. Also, every thousand feet of elevation affects UVB levels by about 3%.
Interested readers should search the internet for “UV index map worldwide”.
UV-B light intensity is usually measured in “milliwatts per square centimeter” (uW/cm2). In an outdoor environment, very large daily variances of exposure to natural UV-B light would be occur due to cloud cover, air pollution, ambient shade, and the time of day. On average for the southern U.S.A., direct summertime sunlight measures about 200 uW/cm2 of UV-B. Tropical sunlight levels may range twice as high. UV radiation output peaks around noon, and about 20-30% of the total daily UV radiation at any point on Earth gets comes between 11 a.m. and 1 p.m. - about 75% between 9 a.m. & 3 p.m.
Natural sunlight has a much higher UV-B irradiance than most commercial lamps. The maximum UV-B irradiance near the equator (solar elevation angle < 25 deg.) under clear, sunny skies, is about 250 µW/cm2.
Measurements from a UV-B lamp cannot be compared directly with readings from sunlight. The spectra of the two light sources are different. The Reptisun 10.0 spectrum has a greater percentage of its UVB in the shorter wavelengths than does sunlight. For example, 30 - 32uW/cm2 from a Reptisun 10.0 lamp is equivalent to approximately 40 – 50 uW/cm2 of sunlight.
Flourescent UV-B tubes supply a diffuse, gentle glow with low intensity visible light, very little heat, and a fairly uniform UV-B gradient, resembling natural UV-B "in the shade" on a sunny day.
Dave Weldon, founder of the South Bay Chameleon Keepers group (Los Angeles) reports:
“[A] … a combination of a 10.0 T-8 Zoo Med Reptisun 48” tube for UVB along with a standard 6500K “grow light” for the plants, all housed in a dual tube aluminum reflector shoplight type fixture … measures a safe and effective 31 uW/cm2 at 16”.”
and,
“[A] … a linear [five month old] Reptisun 10.0 and a 6500K “grow light” [were] mounted in a dual 48” shoplight fixture, lined with reflective aluminum foil to direct … the light …. The Solarmeter 6.2 is held 8.5" away and shows a reading of 30 uW/cm2 … “
http://www.chameleonnews.com/10JulWeldon.html
Intensity vs. distance.
Below is a chart that compares UVB readings from two new Reptisun 5.0 bulbs:
Distance from bulb: Irradiance (measured in uW/cm2)
3" 49/59
6" 24/29
9" 14/18
12" 10/12
15" 7/8
18" 5/6
http://www.beautifuldragons.com/Researchmain.html
UV-B Irradiance from sunlight (SEA = solar elevation angle)
Source of Sunlight
Irradiance of lamp/sunlight in µW/cm
Melbourne, Australia (37.8 S) clear, January 29, maximum irradiance,
Kodiakanal, India (10.14 N) sunny, April,
Miami, Florida (26 N) noon, June 21, summer solstice
Lauder, New Zealand (45 S) clear, December 28, maximum irradiance
Midlands, England (53 N), sunny, July 28, peak intensity
Neuherberg, Germany (48.2 N) clear, July 13
Longyearbyen, Norway (78.2 N), sunny, July 15
Vantaa, Finland (60 N), hazy, sunny, July, noon,
Fort Worth, Texas (32.8 N), shaded, diffuse, March 2, 3 pm,