Engelsen Ola, Brustad Magritt, Aksnes Lage, Lund Eiliv
Norwegian Institute for Air Research (NILU), Tromsø, Norway.
Photochem Photobiol. 2005 Nov-Dec;81(6):1287-90. doi: 10.1562/2004-11-19-RN-375.
Vitamin D production in human skin occurs only when incident UV radiation exceeds a certain threshold. From simulations of UV irradiances worldwide and throughout the year, we have studied the dependency of the extent and duration of cutaneous vitamin D production in terms of latitude, time, total ozone, clouds, aerosols, surface reflectivity and altitude. For clear atmospheric conditions, no cutaneous vitamin D production occurs at 51 degrees latitude and higher during some periods of the year. At 70 degrees latitude, vitamin D synthesis can be absent for 5 months. Clouds, aerosols and thick ozone events reduce the duration of vitamin D synthesis considerably, and can suppress vitamin D synthesis completely even at the equator. A web page allowing the computation of the duration of cutaneous vitamin D production worldwide throughout the year, for various atmospheric and surface conditions, is available on the Internet at http://zardoz.nilu.no/~olaeng/fastrt/VitD.html and http://zardoz.nilu.no/~olaeng/fastrt/VitD-ez.html. The computational methodology is outlined here.
人体皮肤中的维生素D仅在入射紫外线辐射超过一定阈值时才会产生。通过对全球全年紫外线辐照度的模拟,我们从纬度、时间、总臭氧、云层、气溶胶、地表反射率和海拔高度等方面研究了皮肤维生素D产生的范围和持续时间的依赖性。在晴朗的大气条件下,一年中的某些时期,纬度51度及以上地区不会产生皮肤维生素D。在纬度70度地区,维生素D合成可能会有5个月的缺失。云层、气溶胶和厚臭氧事件会显著缩短维生素D合成的持续时间,甚至在赤道地区也可能完全抑制维生素D的合成。互联网上有一个网页(http://zardoz.nilu.no/~olaeng/fastrt/VitD.html和http://zardoz.nilu.no/~olaeng/fastrt/VitD-ez.html),可根据各种大气和地表条件计算全球全年皮肤维生素D产生的持续时间。这里概述了计算方法。