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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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UV radiation: balancing risks and benefits.

Richard L McKenzie1, J Ben Liley, Lars Olof Björn

  • 1National Institute of Water & Atmospheric Research (NIWA), Lauder, Central Otago, New Zealand. r.mckenzie@niwa.co.nz

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Summary

Vitamin D production from UV radiation varies more with time and location than sunburning UV. An algorithm helps optimize UV exposure for vitamin D synthesis while minimizing skin damage risks.

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Area of Science:

  • Environmental science
  • Human health
  • Photobiology

Background:

  • Ultraviolet (UV) radiation plays a dual role in human health, contributing to both skin damage and vitamin D synthesis.
  • Understanding the variations in UV exposure is crucial for public health recommendations.

Purpose of the Study:

  • To analyze diurnal, seasonal, and latitudinal variations in UV-a health risks (erythemally weighted) and benefits (vitamin D-weighted).
  • To investigate the relationship between UV-a for skin damage and vitamin D production.
  • To develop an algorithm for optimizing UV exposure for vitamin D synthesis using the UV index.

Main Methods:

  • Utilized action spectra from the International Commission on Illumination.
  • Examined variations in erythemally weighted UV and vitamin D-weighted UV.
  • Developed and applied an algorithm to correlate vitamin D production with the UV index.

Main Results:

  • Vitamin D-weighted UV shows greater variability with ozone and solar zenith angle compared to erythemally weighted UV.
  • Optimal vitamin D synthesis at mid-latitudes in summer requires ~1 minute of full body exposure, while skin damage occurs after ~15 minutes.
  • Vitamin D production in winter at mid-latitudes may require larger skin exposure than typically considered, questioning current action spectra.

Conclusions:

  • The variability of vitamin D-weighted UV is more pronounced than erythemally weighted UV.
  • An algorithm is presented to guide the public in balancing UV exposure for vitamin D benefits and skin damage risks.
  • Further research is needed to validate the action spectrum for vitamin D production, especially concerning wintertime exposure at mid-latitudes.