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Improving pan-European hydrological simulation of extreme events through statistical bias correction of RCM-driven climate simulations

机译:通过RCM驱动的气候模拟的统计偏差修正来改善极端事件的泛欧水文模拟

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In this work we asses the benefits of removing bias in climate forcing data used for hydrological climate change impact assessment at pan-European scale, with emphasis on floods. Climate simulations from the HIRHAM5-ECHAM5 model driven by the SRES-A1B emission scenario are corrected for bias using a histogram equalization method. As target for the bias correction we employ gridded interpolated observations of precipitation, average, minimum, and maximum temperature from the E-OBS data set. Bias removal transfer functions are derived for the control period 1961-1990. These are subsequently used to correct the climate simulations for the control period, and, under the assumption of a stationary error model, for the future time window 2071-2100. Validation against E-OBS climatology in the control period shows that the correction method performs successfully in removing bias in average and extreme statistics relevant for flood simulation over the majority of the European domain in all seasons. This translates into considerably improved simulations with the hydrological model of observed average and extreme river discharges at a majority of 554 validation river stations across Europe. Probabilities of extreme events derived employing extreme value techniques are also more closely reproduced. Results indicate that projections of future flood hazard in Europe based on uncorrected climate simulations, both in terms of their magnitude and recurrence interval, are likely subject to large errors. Notwithstanding the inherent limitations of the large-scale approach used herein, this study strongly advocates the removal of bias in climate simulations prior to their use in hydrological impact assessment.
机译:在这项工作中,我们评估了消除在用于泛欧范围的水文气候变化影响评估所用的气候强迫数据中偏见的好处,重点是洪水。使用直方图均衡方法对由SRES-A1B排放情景驱动的HIRHAM5-ECHAM5模型进行的气候模拟进行了校正。作为偏差校正的目标,我们从E-OBS数据集中采用了网格插值的降水,平均,最低和最高温度的观测值。偏差去除传递函数是在1961-1990年控制期间得出的。随后将这些用于校正控制时段内的气候模拟,并在固定误差模型的假设下,校正未来时间窗口2071-2100。在控制期内针对E-OBS气候的验证表明,该校正方法成功地消除了整个季节内大部分欧洲地区洪水模拟相关的平均和极端统计数据中的偏差。这可以转化为对欧洲大部分554个验证河流站的观测平均和极端河流流量的水文模型进行的改进的模拟。使用极端价值技术得出的极端事件的概率也可以更精确地再现。结果表明,基于未校正的气候模拟,就其强度和复发间隔而言,对欧洲未来洪灾危害的预测可能会出现较大误差。尽管本文使用的大规模方法存在固有局限性,但本研究强烈主张在将气候模拟用于水文影响评估之前,应消除气候模拟中的偏差。

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