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Slusser, C. Booth, and T. Lucas, Several-fold enhancement of biologically effective ultravio let radiation levels at McMurdo Station Antarctica during the 1990 ozone "hole," Geophys. Res. , 19, 1013-1016, 1992. United Nations Environment Programme, Environmental effects panel report, 64 pp. plus 3 appendices, New York, 1989. Urbach, F. , The biological effects of increased ultraviolet radiation: An update, Photochem. Photobiol, 50, 439-580, 1989. U. S. , Washington, D. C, 1993. Watson, R. , Present state of knowledge of the upper atmosphere 1988: An assessment report, NASA Publ.
Apparent noon for 4 days during this transient event are presented in Table 4. Note that the broadband integrated irradiances (400-600 nm) for these days vary by only 10%, but that the highest UV exposure varies by 100%. SUMMARY A monitoring network for measuring UV irradiance in polar regions has been successfully established by the National Science Foundation/United States Antarctic Program. The network provides hourly, high-resolution measurements of the spectral distribution of irradiance whenever the Sun is above the horizon.
The parameterization is given by Green et al . The scale is normalized as presented in the original publications. pyronometer (model PSP with WG7 hemisphere) and a UV radiometer (model TUVR), both from the Eppley Laboratory, Newport, Rhode Island). These sensors pro vide backup information that can be used to track instru ment stability and operation and may also be used to normalize the scanning data for time-dependent changes in atmospheric conditions and system responsivity. EXAMPLES OF NETWORK DATA Data scans are conducted on an hourly basis when the Sun is above the horizon and on a reduced schedule at night to monitor instrument stability.
Measurements of Delayed Neutron Parameters [U-235, Np-237]