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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >From Point to Area:Worldwide Assessment of the Representativeness of Monthly Surface Solar Radiation Records
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From Point to Area:Worldwide Assessment of the Representativeness of Monthly Surface Solar Radiation Records

机译:从区域:全球的评估代表性的月面太阳能辐射记录

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The representativeness of surface solar radiation (SSR) point observations is an important issue when using them in combination with gridded data. We conduct a comprehensive near-global (50°S to 55°N) analysis on the representativeness of SSR point observations on the monthly mean time scale. Thereto, we apply the existing concepts of decorrelation lengths (δ), spatial sampling biases (β), and spatial sampling errors (ε) to three high-resolution gridded monthly mean SSR data sets (CLARA, SARAH-P, and SARAH-E) provided by the Satellite Application Facility on Climate Monitoring. While δ quantifies the area for which a point observation is representative, β and ε are uncertainty estimates with respect to the 1-degree reference grid (G). For this grid we find a near-global average δ_G = 3.4°, β_G = 1.4 W/m2, and ε_G = 7.6 W/m~2 with substantial regional differences. Disregarding tropical, mountainous, and some coastal regions, monthly SSR point observations can largely be considered representative of a 1-degree grid. Since ε is an uncorrectable error the total uncertainty when combining point with 1-degree gridded data is roughly 40% higher than the uncertainty of station-based SSR measurements alone if a rigorous bias correction is applied. Cloud cover and terrain data can at maximum explain 50% of the patterns of the representativeness metrics. We apply our methodology to the stations of the Baseline Surface Radiation Network. Overall, this study shows that representativeness is strongly dependent on local conditions and that all three metrics (δ, β, and ε) must be considered for a comprehensive assessment of representativeness.
机译:表面太阳辐射的代表性(SSR)观察是一个很重要的问题当使用他们结合网格数据。我们进行一个全面广泛(50°S55°N)分析SSR的代表性对每月的平均时间规模。解相关长度(δ),空间采样偏见(β),和空间采样错误(ε)三个高分辨率网格每月意味着SSR数据集(SARAH-P,克拉拉和SARAH-E)提供由卫星应用设施气候监控。观察是代表,β和ε不确定性估计对吗1度参考网格(G)。这个网格找到一个全球平均δ_G = 3.4°,β_G = 1.4W / m2,ε_G = 7.6 W / m ~ 2与实质地区差异。山区,和一些沿海地区,每月SSR点观测可以很大程度上被认为是1度网格的代表。总不确定性时无法改正的错误结合与1度网格数据点大约高出40%的不确定性如果一个站SSR单独测量严格的应用偏差纠正。并在最大能解释50%的地形数据模式的代表性指标。我们运用我们的方法的电台基线表面辐射网络。研究表明,代表性强依赖于当地条件,所有三个指标(β,δ、ε)必须被考虑代表性的综合评估。

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