| |
| | Measurements of UV Radiation |
 | | When expressed on a relative (percentage) basis, the increases in erythemal UV radiation are seen to correlate closely with ozone reductions, whether the latter stem from natural fluctuations and seasonal cycles, or from systematic long-term depletion. |
 | | The corresponding increases in erythemal UV radiation are estimated to be 130%, 22%, 7%, 4%, and 6%, respectively. |
 | | Clouds generally reduce surface UV irradiances, although the magnitude of this effect is highly variable depending on cloud amount and coverage, cloud cell morphology, particle size distributions and phase (water droplets and ice crystals), and possible in-cloud absorbers (esp. tropospheric ozone). |
| www.gcrio.org /UNEP1998/UNEP98p7.html (1910 words) |
|