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Spatiotemporal variability analysis of diffuse radiation in China during 1981a??2010

机译:1981a—2010年中国漫射辐射的时空变化分析

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Solar radiation is the primary driver of terrestrial plant photosynthesis and the diffuse component can enhance canopy light use efficiency (LUE), which in turn influences the carbon balance of terrestrial ecosystems. In this study we calculated the spatial data of diffuse radiation in China from 1981 to 2010, using a radiation decomposition model and spatial interpolation method based on observational data. Furthermore, we explored the spatiotemporal characteristics of diffuse radiation using GIS and trend analysis techniques. The results show the following: (1) The spatial patterns of perennial average of annual diffuse radiation during 1981a??2010 are complex and inhomogeneous in China, generally lower in the north and higher in the south and west. The perennial average ranges from 1730.20 to 3064.41 MJ msupa??2/sup yrsupa??1/sup across the whole country. (2) There is an increasing trend of annual diffuse radiation in China from 1981 to 2010 on the whole, with mean increasing amplitude of 7.03 MJ msupa??2/sup yrsupa??1/sup per decade. Whereas a significant downtrend was observed in the first 10 years, distinct anomalies in 1982, 1983, 1991 and 1992 occurred due to the eruptions of El Chinchon and Pinatubo. (3) The spatial distribution of the temporal variability of diffuse radiation showed significant regional heterogeneity in addition to the seasonal differences. Northwestern China has the most evident downtrend, with highest decreasing rate of 6% per decade, while the Tibetan Plateau has the most evident uptrend, with highest increasing rate of up to 9% per decade. Such quantitative spatiotemporal characteristics of diffuse radiation are essential in regional scale modeling of terrestrial carbon dynamics.
机译:太阳辐射是陆地植物光合作用的主要驱动力,扩散成分可以提高冠层光的利用效率(LUE),进而影响陆地生态系统的碳平衡。在这项研究中,我们使用辐射分解模型和基于观测数据的空间插值方法,计算了1981年至2010年中国漫射辐射的空间数据。此外,我们使用GIS和趋势分析技术探索了散射辐射的时空特征。结果表明:(1)中国1981a—2010年年平均漫辐射的常年空间格局在中国较为复杂且不均匀,一般在北部较低,在南部和西部较高。全国的多年平均水平在1730.20到3064.41 MJ m a ?? 2 yr a ?? 1 之间。 (2)从1981年到2010年,中国的年漫辐射总体上呈上升趋势,平均幅度增加7.03 MJ m a ?? 2 yr a ?? 1 < / sup>每十年。尽管在最初的十年中观察到了明显的下降趋势,但由于El Chinchon和Pinatubo的爆发,在1982、1983、1991和1992年出现了明显的异常。 (3)散射辐射的时间变化的空间分布除季节差异外还表现出显着的区域异质性。中国西北地区的下降趋势最为明显,下降幅度最高,为每十年6%,而青藏高原的上升趋势最为明显,上升幅度最高,为每十年9%。扩散辐射的这种定量时空特性在地面碳动力学的区域尺度建模中至关重要。

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