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Analysis of ultraviolet radiation in clear skies in Beijing and its affecting factors

机译:北京晴空紫外线辐射及其影响因素分析

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摘要

Analyzing observational data for solar radiation, meteorological parameters and total ozone concentration during the period of January 1990 to December 1991 in Beijing enabled the development of an empirical method for estimation of UV irradiance (UVI) in clear skies. Predicted values from the model agreed well with observations. The mean relative bias for 24 months was 1.9%. UVI (290-400 ran) in clear sky conditions from 1979 to 1998 was calculated, and its long-term variation showed a declining trend of -3.89%, which was accompanied by a decrease in total O_3 of -5.75%, a decrease in scattering factor (SID, the ratio of solar scattered to direct radiation) of -20.79%, and an increase in water vapor content of +4.76%. It is hypothesized that many substances in the atmosphere, including volatile organic compounds (VOC_S) and their oxidation products, very fine particles and others absorb and/or utilize UV energy. The long-term UVI trends and its main controlling factors in four seasons during the previous 2 decades are discussed, UV energy consumption by atmospheric chemical and photochemical processes, is especially important during summer.
机译:通过分析1990年1月至1991年12月在北京的太阳辐射,气象参数和总臭氧浓度的观测数据,可以开发出一种经验方法来估算晴朗天空中的UV辐照度(UVI)。该模型的预测值与观察值非常吻合。 24个月的平均相对偏倚为1.9%。计算了1979年至1998年晴空条件下的UVI(290-400 ran),其长期变化显示出-3.89%的下降趋势,同时总O_3下降了-5.75%,下降了散射因子(SID,太阳散射与直接辐射的比率)为-20.79%,水蒸气含量增加了+ 4.76%。假设大气中的许多物质,包括挥发性有机化合物(VOC_S)及其氧化产物,非常细的颗粒和其他物质,都会吸收和/或利用紫外线能量。讨论了过去20年中四个季节的长期UVI趋势及其主要控制因素,大气化学和光化学过程产生的UV能量消耗在夏季尤为重要。

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