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Comparison of the effectiveness of four Budyko-based methods in attributing long-term changes in actual evapotranspiration

机译:比较四种基于Budyko的方法对实际蒸散量的长期变化进行归因的有效性

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摘要

The responses of hydrological processes to climate change and anthropogenic influence have received significant attention over the past few decades. Several Budyko-based methods have been widely used to attribute hydrological variations and identify the extent of variation due to climate change and human activities. However, the accuracy of various methods has rarely been compared. This study employed four Budyko-based methods, namely the total differential method, complementary method, extrapolation method, and decomposition method, to attribute the changes in actual evapotranspiration in 13 basins in China’s Loess Plateau. We compared their performances and analysed factors that contribute to the differences in attribution results yielded by the various methods. The results showed that the total differential, complementary, and decomposition methods presented similar estimates of the contributions of climate change and human activities. However, the extrapolation method showed a large deviation in the contribution of human activities. The error of the extrapolation method was the largest, followed by that of the two-stage total differential method. The complementary method and decomposition method exhibited negligible errors.
机译:在过去的几十年中,水文过程对气候变化和人为影响的反应受到了极大的关注。几种基于Budyko的方法已被广泛用于归因于水文变化并确定由于气候变化和人类活动造成的变化程度。但是,很少比较各种方法的准确性。这项研究采用了四种基于Budyko的方法,即总微分法,互补法,外推法和分解法,来归因于中国黄土高原13个盆地的实际蒸散量的变化。我们比较了他们的表现,并分析了各种方法导致的归因结果差异的因素。结果表明,总的差异,补充和分解方法对气候变化和人类活动的贡献具有相似的估计。但是,外推法在人类活动的贡献上显示出很大的偏差。外推法的误差最大,其次是两阶段总微分法的误差。互补法和分解法的误差可忽略不计。

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