
Clouds, air pollution, haze and elevation all have affects
on the amount of ultraviolet (UV) radiation reaching the surface.
UV radiation reaches the surface as a sum of its direct component
(normal to the sun) and its diffuse component (from all directions).
UV radiation reaches the top of the troposphere in mostly
its direct component. This is because there are few molecules
to scatter the radiation. Decreases in UV radiation intensity
has resulted due to absorption by ozone. Once the UV radiation
reaches the troposphere it encounters much greater numbers
of scattering air molecules and dust. Below are how UV radiation
is affected by:
Elevation:
In the troposphere, air molecules and dust increase as the
UV radiation travels from the stratosphere to the troposphere.
The further down in to the atmosphere UV radiation travels,
the more the direct component is reduced and the more the
diffuse component is increased. As more UV radiation is scattered,
the smaller the amount that reaches the surface. As a result,
there is more UV radiation at higher elevations than at lower
elevations.
Clouds:
Made up of millions of water droplets, clouds can transmit,
reflect and scatter UV radiation. The amount of each is dependant
upon the thickness of the cloud and its morphology. Generally,
the larger and thicker the cloud is the lesser amount of UV
radiation that is transmitted. UV radiation can and does reflect
off the sides of towering cumulus clouds. Such conditions
result in actual enhancements of surface UV radiation.
Dust/Haze:
These two conditions act on UV radiation the same way. They
both scatter UV radiation. Enough UV radiation is scattered
that on hazy or dusty days there is less UV radiation reaching
the surface than would otherwise be there on a clear day.
Air
Pollution/Smog: This encompasses many greenhouse gases.
Emissions from traffic and manufacturing plants form smog
as UV radiation and heat cause the necessary chemical reactions
to take place. As a result, the amounts of UV radiation reaching
the surface is smaller under these conditions.
Return
to UV Index

Last
Updated September 2, 1997 by Craig
S. Long
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