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首页> 外文期刊>Water resources research >Stochastic downscaling of precipitation to high-resolution scenarios in orographically complex regions: 1. Model evaluation
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Stochastic downscaling of precipitation to high-resolution scenarios in orographically complex regions: 1. Model evaluation

机译:地形复杂区域中降水的随机降尺度到高分辨率场景:1.模型评估

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摘要

[1] The simulation of space-time precipitation has been studied since the late 1980s. However, there are still many open issues concerning the most appropriate approach to simulate it, specially in highly heterogeneous areas, such as in mountain environments. For this reason, we present here a comprehensive investigation of the Space-Time Neyman-Scott Rectangular Pulses model, with the purpose of analyzing its performance in a challenging Alpine environment of Switzerland and identifying weaknesses that can drive future improvements. The results point at the suitability of the model in reproducing not only the basic statistics at different temporal aggregations, but also the more challenging distributional and scaling properties. The intrinsic stationarity of the model in space, induced by the parameter estimation procedure, poses occasional limitations with regard to the accurate simulation of the variability of the observed climate characteristics, which are strongly influenced by local microclimates. However, the model is able, even in the complex Alpine environment, to preserve the spatial patterns observed in the actual precipitation process. The study allowed (ⅰ) to conclude about the robustness of the model and its suitability for multisite downscaling of precipitation estimated from climate model simulations, as reported in the companion paper, and (ⅱ) to put in evidence some limitations that require further consideration to improve space-time rainfall generation.
机译:[1]自1980年代以来一直研究时空降水的模拟。但是,关于最合适的模拟方法仍然存在许多悬而未决的问题,特别是在高度异构的地区,例如山区环境中。因此,在此我们对时空Neyman-Scott矩形脉冲模型进行全面研究,目的是分析其在瑞士充满挑战的高山环境中的性能,并找出可以推动未来改进的弱点。结果表明,该模型不仅适用于再现不同时间聚合的基本统计信息,而且适用于更具挑战性的分布和缩放属性。由参数估计程序引起的模型在空间中的固有平稳性,偶尔会给精确模拟观测到的气候特征的可变性带来局限性,这受到局部微气候的强烈影响。但是,即使在复杂的高山环境中,该模型也能够保留实际降水过程中观察到的空间格局。该研究使(ⅰ)可以得出该模型的稳健性及其对气候模型模拟估计的降水多站点降尺度的适用性的结论,以及(ⅱ)提出一些需要进一步考虑的局限性证据改善时空降雨的产生。

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  • 来源
    《Water resources research》 |2014年第1期|540-561|共22页
  • 作者

    R. Bordoy; P. Burlando;

  • 作者单位

    Institute of Environmental Engineering, ETH Zurich, HIF CO 46.6, Schafmattstrasse 6, CH-8093 Zurich, Switzerland;

    Institute of Environmental Engineering, ETH Zurich, Zurich, Switzerland;

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  • 正文语种 eng
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