Institute of Biogeochemistry and Pollutant Dynamics (IBP), Department of Environmental Systems Science, ETH Zurich, 8092Zurich, Switzerland.
Environ Sci Technol. 2023 Feb 14;57(6):2682-2690. doi: 10.1021/acs.est.2c07359. Epub 2023 Feb 3.
Photochemical reactions in surface waters play important roles in element cycling and in the removal of organic contaminants, among other processes. A central environmental variable affecting photochemical processes in surface waters is the incoming solar irradiance, as this initiates these processes. However, clear-sky incident irradiance spectra are often used when evaluating the fate of aquatic contaminants, leading to an overestimation of contaminant decay rates due to photochemical transformation. In this work, incident irradiance satellite data were used to develop global-scale non-clear-sky correction factors for commonly used reference irradiance spectra. Non-clear-sky conditions can decrease incident irradiance by over 90% depending on the geographic location and time of the year, with latitudes above 40°N being most heavily affected by seasons. The impact of non-clear-sky conditions on contaminant half-lives was illustrated in a case study of triclosan in lake Greifensee, which showed a 39% increase in the triclosan half-life over the course of a year under non-clear-sky conditions. A global annual average correction factor of 0.76 was determined as an approximate way to account for non-clear-sky conditions. The correction factors are developed at monthly and seasonal resolutions for every location on the globe between 70°N and 60°S at a 4 km spatial resolution and can be used by researchers, practitioners, and regulators who need improved estimates of incident irradiance.
光化学反应在地表水中扮演着重要的角色,不仅参与元素循环,还能去除有机污染物等。影响地表水中光化学过程的一个关键环境变量是入射太阳辐射,因为它会引发这些过程。然而,在评估水生污染物的命运时,通常会使用晴空入射辐照度光谱,这导致污染物衰减率被高估,因为存在光化学转化。在这项工作中,我们使用入射辐照度卫星数据为常用参考辐照度光谱开发了全球范围的非晴空校正因子。非晴空条件会导致入射辐照度降低超过 90%,具体取决于地理位置和一年中的时间,北纬 40 度以上地区受季节影响最大。非晴空条件对污染物半衰期的影响在 Greifensee 湖三氯生的案例研究中得到了说明,结果表明,在非晴空条件下,三氯生的半衰期在一年中增加了 39%。确定了全球年平均校正因子为 0.76,这是一种近似方法,可以用来考虑非晴空条件。校正因子以每月和季节性分辨率开发,适用于全球北纬 70 度至南纬 60 度之间每个地点,空间分辨率为 4 公里,可以供需要改进入射辐照度估计的研究人员、从业者和监管机构使用。