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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Decadal variability of surface incident solar radiation over China: Observations, satellite retrievals, and reanalyses
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Decadal variability of surface incident solar radiation over China: Observations, satellite retrievals, and reanalyses

机译:中国地面入射太阳辐射的年代际变率:观测,卫星检索和再分析

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Existing studies have shown that observed surface incident solar radiation (Rs) over China may have important inhomogeneity issues. This study provides metadata and reference data to homogenize observed Rs, from which the decadal variability of Rs over China can be accurately derived. From 1958 to 1990, diffuse solar radiation (Rsdif) and direct solar radiation (Rsdir) were measured separately, and Rs was calculated as their sum. The pyranometers used to measure Rsdif had a strong sensitivity drift problem, which introduced a spurious decreasing trend into the observed Rsdif and Rs data, whereas the observed Rsdir did not suffer from this sensitivity drift problem. From 1990 to 1993, instruments and measurement methods were replaced and measuring stations were restructured in China, which introduced an abrupt increase in the observed Rs. Intercomparisons between observation-based and model-based Rs performed in this research show that sunshine duration (SunDu)-derived Rs is of high quality and can be used as reference data to homogenize observed Rs data. The homogenized and adjusted data of observed Rs combines the advantages of observed Rs in quantifying hourly to monthly variability and SunDu-derived Rs in depicting decadal variability and trend. Rs averaged over 105 stations in China decreased at -2.9 W m~(-2) per decade from 1961 to 1990 and remained stable afterward. This decadal variability is confirmed by the observed Rsdir and diurnal temperature ranges, and can be reproduced by high-quality Earth System Models. However, neither satellite retrievals nor reanalyses can accurately reproduce such decadal variability over China.
机译:现有研究表明,在中国观察到的地面入射太阳辐射(Rs)可能存在重要的不均匀性问题。这项研究提供了元数据和参考数据,以使观测到的Rs均匀化,从而可以准确得出中国Rs的年代际变化。从1958年到1990年,分别测量了散射太阳辐射(Rsdif)和直接太阳辐射(Rsdir),并计算了Rs作为它们的总和。用于测量Rsdif的日射强度计具有很强的灵敏度漂移问题,这向观察到的Rsdif和Rs数据中引入了虚假的下降趋势,而观测到的Rsdir则没有此灵敏度漂移问题。从1990年到1993年,在中国更换了仪器和测量方法,并重组了测量站,这使观测到的Rs突然增加。在这项研究中进行的基于观测的Rs与基于模型的Rs之间的比较表明,源自阳光持续时间(SunDu)的Rs具有较高的质量,可以用作均化观测Rs数据的参考数据。观测值Rs的均质化和调整后的数据结合了观测值Rs在每小时到每月的变异性定量方面的优势以及SunDu派生的Rs在描述年代际变化性和趋势方面的优势。从1961年到1990年,中国平均超过105个台站的Rs在每十年下降-2.9 W m〜(-2),此后保持稳定。年代际变化可以通过观测到的Rsdir和昼夜温度范围得到确认,并且可以通过高质量的地球系统模型来再现。但是,无论是卫星检索还是再分析都不能准确地再现出中国的年代际变化。

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