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Detection of long-term trends in monthly hydro-climatic series of Colombia through Empirical Mode Decomposition

机译:通过经验模式分解检测哥伦比亚每月水文气候系列的长期趋势

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We test for the existence of long-term trends in 25- to 50-year long series of monthly rainfall, average river discharges, and minimum air temperatures in Colombia. The Empirical Mode Decomposition method is used as a mathematical filter to decompose a given time series into a finite number of intrinsic mode functions, assuming the coexistence of different frequency oscillatory modes in the series, and that the residual captures the likely existing long-term trends. The Mann-Kendall test for autocorrelated data is used to assess the statistical significance of the identified trends, and the Sen test is used to quantify their magnitudes. Results show that 62 % of river discharge series exhibit significant decreasing trends between 0.01-1.92 m (3) s (-1) per year, which are highly consistent downstream albeit with different ratios between the trend magnitudes and mean discharges. Most minimum temperature series (87 %) exhibit increasing trends (0.01-0.08 A degrees Cyr (-1)). Results for precipitation series are inconclusive owing to the mixing between increasing trends (41 %, between 0.1-7.0 mm yr (-1)) and decreasing trends (44 %, between 0.1-7.4 mm yr (-1)), with no clear-cut geographical pattern, except for the increasing trend identified along the Pacific region, consistent with the increasing trend identified in the strength of the Choc low-level wind jet off the Pacific coast of Colombia, an important moisture source of continental precipitation. Our results contribute to discerning between signals of climate change and climate variability in tropical South America.
机译:我们测试了哥伦比亚25至50年的长期降雨序列,长期平均河流量和最低气温的长期趋势是否存在。经验模式分解方法用作数学过滤器,以将给定的时间序列分解为有限数量的本征模式函数,假设该序列中不同频率的振荡模式共存,并且残差捕获了可能存在的长期趋势。进行自相关数据的Mann-Kendall检验用于评估已识别趋势的统计显着性,Sen检验用于量化其趋势。结果表明,有62%的河流流量在每年0.01-1.92 m(3)s(-1)之间显示出显着的下降趋势,这是高度一致的下游,尽管趋势量和平均流量之间的比率不同。大多数最低温度序列(87%)呈现上升趋势(0.01-0.08 A摄氏度(-1))。由于上升趋势(41%,在0.1-7.4 mm yr(-1)之间)和下降趋势(44%,在0.1-7.4 mm yr(-1)之间)之间的混合,降水序列的结果尚无定论。的地理格局,除了沿太平洋区域确定的增加趋势外,与确定为哥伦比亚大陆沿海重要水分源的哥伦比亚太平洋沿岸的Choc低空喷气机强度确定的增长趋势一致。我们的结果有助于辨别南美热带地区的气候变化信号与气候变异性。

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