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Spatial and temporal patterns as well as major influencing factors of global and diffuse Horizontal Irradiance over China: 1960-2014

机译:1960-2014年全球水平和弥散水平辐照度的时空格局及主要影响因素

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Global Horizontal Irradiance (GHI) on Earth is a central element of climate systems. With changes in the climate and regional development, the patterns and influencing factors of GHI, in addition to presenting global consistency, are increasingly showing regional particularities. Based on data for GHI, Diffuse Horizontal Irradiance (DHI) and potential impact factors (geographical position, elevation, cloud cover, water vapor, and ground atmospheric transparency related variables) from 1960 to 2014 in China, we analyzed the pattern and major influencing factors of GHI and DHI. The results showed that the major influencing factors of the GHI spatial pattern were the total cloud cover (TCC) and relative humidity (RH) in China. Dividing all of China into two regions, the major factors were the water vapor pressure (WVP) in the northern region and TCC in the southern region. And we divided the GHI and DHI data into two periods (1960-1987 and 1988-2014) due to global dimming and brightening observed in China in the late 1980s. The temporal GHI showed that 31 of 58 decreased significantly with an average decreasing rate of 95 MJ 10 yr(-1) during the periods of 1960-2014 and 49 of 76 stations decreased significantly with an rate of 342 MJ 10 y(r-)1 during 1960-1987, whereas 57 of 88 stations did not change and 24 stations increased significantly with an rate of 201 MJ 10 yr(-1) during the period of 1988-2014. The temporal DHI showed that 40 of 61sites did not change significantly from 1960 to 1987. The major influencing factors for temporal changes of GHI in nine typical cities from 1960 to 2013 were as follows: air quality-related variables in super cities, sandstorms and wind in desert oasis cities, clouds in cities with good air quality, and a low cloud amount (LCA) and annual fog days (FD) in Chengdu. Overall, we identified characteristics of GHI and DHI based on global climate change and regional urban development and found that the spatial characteristics of GHI results for China are consistent with global trends, whereas the spatial characteristics of DHI and temporal characteristics of GHI and DHI have changed significantly and exhibit these measurable trends due to strong regional influences of changing cloud amounts, water vapor, and air quality.
机译:地球上的全球水平辐照度(GHI)是气候系统的核心要素。随着气候和区域发展的变化,GHI的模式和影响因素除了表现出全球一致性外,还越来越显示出区域特殊性。基于1960年至2014年中国GHI,漫射水平辐照度(DHI)以及潜在影响因素(地理位置,海拔,云量,水汽和地面大气透明度相关变量)的数据,我们分析了模式和主要影响因素GHI和DHI。结果表明,中国GHI空间格局的主要影响因素是总云量(TCC)和相对湿度(RH)。将整个中国分为两个地区,主要因素是北部地区的水蒸气压(WVP)和南部地区的TCC。由于1980年代后期在中国观测到的全球变暗和变亮,我们将GHI和DHI数据分为两个时期(1960-1987年和1988-2014年)。时间GHI显示1960-2014年期间58个中的31个显着下降,平均下降速率为95 MJ 10 yr(-1),76个站中的49个显着下降,下降速率为342 MJ 10 y(r-)在1960-1987年期间为1个,而在1988-2014年期间88个站点中的57个未发生变化,而24个站点则以201 MJ 10 yr(-1)的速率显着增加。 DHI的时间变化表明,从1960年到1987年,有61个站点中的40个站点​​没有显着变化。1960年至2013年的9个典型城市中,GHI的时空变化的主要影响因素如下:超级城市中与空气质量有关的变量,沙尘暴和风在沙漠绿洲城市中,空气质量良好的城市中的云,而成都的云量(LCA)和年雾天(FD)低。总体而言,我们根据全球气候变化和区域城市发展确定了GHI和DHI的特征,发现中国的GHI结果的空间特征与全球趋势一致,而DHI的空间特征以及GHI和DHI的时间特征已经改变由于云量,水蒸气和空气质量变化的强烈区域影响,这些变化趋势显着并显示出这些可测量的趋势。

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