Ultraviolet radiation (UVR) during passage through the layer of
ozone in the stratosphere mostly absorbed by ozone, so the UVA and UVB rays
that reach the earth's surface becomes less. UVC photolysis interact with
oxygen produces ozone. this is because the biological effects of ultraviolet B
radiation is greater than ultraviolet A radiation, so the concentration of pan
environmentalists and environmental epidemiology is devoted to observing UVB
from time to time, although the percentage of ultraviolet A radiation is much
higher when compared with a ratio of 95% UVB and 5%. Ultraviolet radiation
reaches the earth's surface depends on latitude, altitude and the presence of
cloud or aerosol particles. Area near the equator, have the highest intensity
when compared to the northern and southern hemispher. The presence of clouds and air pollution (in the form of smoke or
water vapor particles), can lower the UVB. The influence of clouds on the
irradiation of the spiral can be approximated by a factor F: F = 1 to 0.056 C.
C is the total cloud index which ranges between 00-10. Value of 10
for thick clouds covering the sky completely. For dense clouds, ultraviolet radiation down to 44% for
direct radiation. The
estimated reduction in ultraviolet B radiation (UVB) because the cloud based on satellite measurements of backscattering with UVB which is 30% at 60 ° latitude, 10% at 20 ° and 20% on the equator. The relative intensities of ultra-violet B radiation from time to
time is not fixed, the maximum at noon (12.00) and minimum in the morning and
afternoon (at 06.00 and 19.00).
European population is estimated to have exposure to UVB radiation
ranges between 210-390 MED, depending on the type of work (outside / inside the
room).
The estimated annual doses of UVB from some activities
Activities
|
Annual doses of UVB (MED)
|
Working outdoors
(including exposure of on the weekend)
Working
indoors
(including exposure of on the weekend)
2
weeks vacation in the Mediterranean
Sunbathing on the beach 15 hours
|
270
90
100
20
|
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