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Obscured Overcast Sky Radiance Distributions for Ultraviolet and Photosynthetically Active Radiation

机译:紫外线和光合有效辐射的阴暗天空辐射度分布

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Sky radiance measurements in the wavelength bands of ultraviolet-B (0.28-0.32 μm), ultraviolet-A (0.32-0.40 μm); and photosynthetically active radiation (0.40-0.70 μm) were made under obscured overcast skies in a rural area. Radiance distributionswere modeled for seven measuromentscans with solar zenith angles varying from 19°to 49°. For the seven scans, the atmospheric transmittance of photosynthetically active photon flux density varied from 0.16 to 0.25. The corresponding fraction of cloud-free sky photosynthetically active photon flux density ranged from 0.21 to 0.32. The corresponding fraction of ultraviolet-B cloud-free sky irradiance was between 0.20 and 0.34, with typically lower fractions of cloud-free sky irradiance in the ultraviolet-B than in the photosynthetically active photon flux density. The sky radiance was modeled from the ensembled measurements according to the standard overcast sky radiance distribution for each of the wavelength bands. Although the ultraviolet wave bandshad slightly greater normalized radiance at the zenith and smaller radiance at the horizon than has been found for the photosynthetically active radiation wave band, the differences between the photosynthetically active radiation and the ultraviolet-A and ultraviolet-B radiance distributions were not statistically significant. Therefore, the authors concluded that the normalized obscured overcast sky radiance distribution for all three wave bands could be satisfactorily described by the standard overcast sky model of the photosynthetically active radiation distribution.
机译:在紫外线B(0.28-0.32μm),紫外线A(0.32-0.40μm)的波长带中的天空辐射测量;在农村阴暗的天空下进行了光合有效辐射(0.40-0.70μm)。对七个太阳辐射天平扫描(太阳天顶角从19°到49°不等)的辐射测量建模。对于这七个扫描,光合作用的光子通量密度的大气透射率在0.16到0.25之间变化。无云的天空光合有效光子通量密度的相应分数在0.21到0.32之间。紫外线-B的无云天空辐照度的相应分数在0.20和0.34之间,紫外线-B中的无云的天空辐照度的分数通常比光合有效光子通量密度低。根据每个波段的标准阴暗天空辐射度分布,根据集合的测量结果对天空辐射度进行建模。尽管紫外光带的天顶归一化辐射比水平光辐射要大一些,而地平线上的辐射带却比光合有效辐射波段要小一些,但光合有效辐射与紫外线A和紫外线B辐射分布之间的差异并不大。具有统计意义。因此,作者得出的结论是,通过光合作用有效辐射分布的标准阴天模型,可以令人满意地描述所有三个波段的归一化模糊阴天辐射度分布。

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