1961-2018年挪威月降水序列的均一化

Q2 Earth and Planetary Sciences
Elinah Khasandi Kuya, H. M. Gjelten, O. E. Tveito
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引用次数: 6

摘要

摘要分析的主要目标是建立一个高质量的降水参考数据集,该数据集既一致又均匀,用于计算新的标准气候常态(1991-2020)。采用气候均质化方法检测了1961-2018年挪威325个降水序列的非均质性。同质性测试的结果发现,325个系列中有29%存在不同质性,然而,在与元数据结合并进行调整后,只有25%被归类为不同质。降水计的重新安置和自动化是挪威系列中所有不均匀性的主要原因,分别解释了所有检测到的中断的71%和12%。结果进一步显示了将元数据合并到自动检测的不均匀性中的好处。线性趋势分析显示,1961-2018年期间,除秋季呈下降趋势外,其他季节均呈上升趋势。均匀性分析得到了一个58年325个月降水的均匀数据集,其区域时间变异性和空间相干性优于非均匀化序列。该数据集在解释大尺度气候变化方面更为可靠,并被用于计算挪威的新气候常态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Homogenization of Norwegian monthly precipitation series for the period 1961–2018
Abstract. The primary goal of the analysis was to establish a high-quality precipitation reference dataset, which is both consistent and homogeneous, for calculation of the new standard climate normals (1991–2020). Climatol homogenization method was applied to detect inhomogeneities in 325 Norwegian precipitation series, during the period 1961–2018. Results from homogeneity testing found inhomogeneities in 29 % of the 325 series, however, only 25 % were classified as inhomogeneous after conferring with metadata and therefore adjusted. Relocation of the precipitation gauge and automation were the main causes of all the inhomogeneities in the Norwegian series, explaining 71 % and 12 % respectively of all detected breaks. Results further showed benefits of incorporating metadata to the automatically detected inhomogeneities. Linear trend analysis showed increasing trends in the period 1961–2018 except in autumn where a decreasing trend was observed. The homogeneity analysis produced a 58-year long homogenous dataset for 325 monthly precipitation sums with regional temporal variability and spatial coherence that is better than that of non-homogenized series. The dataset is more reliable in explaining the large-scale climate variations and was used to calculate the new climate normals in Norway.
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来源期刊
Advances in Science and Research
Advances in Science and Research Earth and Planetary Sciences-Geophysics
CiteScore
4.10
自引率
0.00%
发文量
13
审稿时长
22 weeks
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