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The dependence of global and diffuse PAR radiation components on sky conditions at Athens, Greece.

机译:希腊雅典的整体和漫射PAR辐射分量对天空条件的依赖性。

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The interrelationship between broadband solar components, global (RS) and diffuse (Rd) and the photosynthetic photon flux density components, global (QP) and diffuse (QPd), is investigated using a 2-year data archive obtained at Athens, Greece. These data are used to determine temporal variability of the ratios (QP/RS) and (QPd/Rd) and their dependence on sky conditions. The seasonal variation of the ratios obtained from hourly data ranges from 2.006+or-0.032 (winter) to 1.989+or-0.028 micro mol J-1 (summer) with an annual mean of 1.995+or-0.032 micro mol J-1 for (QP/RS) and from 2.298+or-0.27 (winter) to 2.538+or-0.22 micro mol J-1 (summer) with an annual mean of 2.434+or-0.26 micro mol J-1 for (QPd/Rd). The hourly ratio (QP/RS) increased from 1.982+or-0.025 to 2.106+or-0.029 micro mol J-1 as sky conditions changed from clear to overcast; whereas the ratio (QPd/Rd) decreased from 2.556+or-0.27 to 2.422+or-0.24 micro mol J-1 as sky conditions changed from clear to overcast skies. The seasonal daily ratio patterns are presented and discussed through clearness index kt (the ratio of the global-to-extraterrestrial solar radiation). Finally, the relationship between the spectral diffuse fraction kdP (the ratio of diffuse PAR-to-global PAR radiation) and the clearness index ktP (the ratio of global PAR-to-extraterrestrial solar PAR) is established for the Athens atmosphere..
机译:使用在希腊雅典获得的2年数据档案,研究了宽带太阳能分量全局(RS)和扩散(Rd)与光合光子通量密度分量全局(QP)和扩散(QPd)之间的相互关系。这些数据用于确定比率(QP / RS)和(QPd / Rd)的时间变化及其对天空条件的依赖性。从每小时数据获得的比率的季节变化范围从2.006+或-0.032(冬季)到1.989+或-0.028 micro mol J-1(夏季),年度平均值为1.995+或-0.032 micro mol J-1。 (QP / RS),从2.298+或-0.27(冬季)到2.538+或-0.22 micro mol J-1(夏季),年平均(QPd / Rd)为2.434+或-0.26 micro mol J-1 。当天空条件从晴朗变为阴天时,小时比率(QP / RS)从1.982+或-0.025微摩尔J-1增加到2.106+或-0.029 micro mol J-1。而当天空条件从晴朗的天空变为阴天时,比率(QPd / Rd)从2.556+或-0.27降低到2.422+或-0.24 micro mol J-1。通过清除指数kt(全球与外星太阳辐射之比)介绍并讨论了季节性日比模式。最后,建立雅典大气层的光谱扩散分数kdP(扩散PAR与全球PAR辐射之比)与净度指数ktP(全球PAR与地球外太阳PAR之比)之间的关系。

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