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This article in JEQ

  1. Vol. 4 No. 3, p. 285-294
     
    Received: Sept 3, 1974
    Published: July, 1975


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doi:10.2134/jeq1975.00472425000400030001x

Solar Ultraviolet Radiation in Terrestrial Plant Communities1

  1. L. H. Allen,
  2. H. W. Gausman and
  3. W. A. Allen2

Abstract

Abstract

There has been a growing concern that NOx effluents from supersonic or other highflying craft, or chlorofluoromethane refrigerants or aerosol can propellents that diffuse to the stratosphere, could cause a reduction of atmospheric ozone, which would result in a concomitant increase of penetration of solar ultraviolet radiation to the earth's surface with possible biological consequences. Spectral distributions of direct-beam and diffuse solar ultraviolet irradiance at the earth's surface, as a function of stratospheric ozone content and solar elevation angle, have been accurately measured or predicted by other researchers. Our objectives were to couple incident spectra to a plant canopy radiation penetration model to give the redistribution of middle ultraviolet radiation, or UV-B (280–315 nm), within plant canopies. Detailed comparisons were made between two ozone content conditions (0.32 cm, typical for 30° N latitude and 0.24 cm, representing a 25% ozone reduction) with a 60° solar elevation angle.

Predictions of UV-B radiation regimes in plant communities over ranges of architectural or structural characteristics, including erect-leaf, normal-leaf, and horizontal-leaf canopies, were computed. Clumped, random, and regular leaf distributions were modeled, as well as leaf area indices of 2.6, 3.3, and 4.0. Phyloelement optical properties included zero transmissivity and 5% reflectivity. Soil reflectivities of both 5% and 20% were used. Epidermal transmission spectra were used to predict UV-B radiation loads inside leaves.

Predicted penetration of UV-B radiation was much greater in erect-leaf than horizontal-leaf canopies. Upward-directed UV-B irradiance was greater near the ground level than near the top of the canopy.

In conclusion, the model prediction described the range of UV-B radiation regimes to be expected in plant communities under present stratospheric ozone content and under a 25% ozone reduction. Data from these idealized plant communities can be interpolated for other plant canopy types and soil types to predict upward or downward UV-B radiation loads and dosages.

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