Abstract. Solar ultraviolet-B
(280-320 nm) spectral irradiance and total shortwave radiation
were measured along an arctic-alpine life zone gradient from the
Arctic (70°N) at sea level to equatorial latitudes at high
elevations above sea level. This series of measurements portrays
the radiant flux to be anticipated during periods of maximum annual
solar radiation. Along this arctic-alpine gradient, maximum daily
total shortwave irradiance varies only by a factor of 1.6 and
total daily shortwave radiation by less than 15% for cloudless
conditions. In contrast, the maximum integrated effective UV-B
irradiance can vary by a full order of magnitude and by seven-fold
for total daily effective radiation. The steep UV-B radiation
gradient is the result of a natural latitudinal gradient in total
atmospheric ozone column thickness, prevailing solar angles at
different latitudes, elevation above sea level, and an optical
amplification effect, which results from a combination of highly
wavelength-dependent radiation attenuation in the atmosphere and
the pronounced wavelength dependence of biological action spectra.
Forty to 70% of the solar UV-B flux is in the form of scattered
radiation. Because of the large proportion of diffuse UV-B radiation,
steeply inclined foliage would still receive a sizable fraction
of the global UV-B irradiance in most situations. Snow cover
can add substantially to the radiation load.
This research was supported by grants from the National Science
Foundation (DEB-7622381) and the National Aeronautics and Space Administration (NAS-9-14871).