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Drought indices revisited – improving and testing of drought indices in a simulation of the last two millennia for Europe

机译:重新审视干旱指数–通过模拟欧洲近两千年来改进和测试干旱指数

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Over the past decades, different drought indices have been suggested in the literature. This study tackles the problem of how to characterize droughts by defining a framework and proposing a generalized family of drought indices that is flexible regarding the use of different hydrological fluxes in the water balance. The sensitivity of various indices and its skill to represent drought conditions is evaluated using a regional model simulation for Europe spanning the last two millennia as test bed. The framework combines an exponentially damped memory with a normalization method based on quantile mapping. Both approaches are more robust and physically meaningful compared to the existing methods used to define drought indices. Still, the framework is flexible with respect to hydrological fluxes used for the water balance, enabling users to adapt the index formulation to the data availability of different locations. Based on it, indices using different hydrological fluxes in the water balance are compared with each other showing that a drought index considering only precipitation in the water balance is sufficient for western to central Europe. In the Mediterranean, temperature effects via evapotranspiration rather than potential evapotranspiration, need to be considered to produce meaningful indices representative of water deficit. In addition, our results indicate that in north-eastern Europe and Scandinavia, snow and run-off effects need to be considered simultaneously in the index definition to obtain accurate results.
机译:在过去的几十年中,文献中提出了不同的干旱指数。这项研究解决了如何通过定义框架和提出一个广义的干旱指数系列来表征干旱的问题,该系列干旱指数在水平衡中使用不同的水文通量方面具有灵活性。使用针对过去两千年的欧洲区域模型模拟,评估了各种指数的敏感性及其代表干旱状况的技巧。该框架将指数阻尼的内存与基于分位数映射的规范化方法结合在一起。与用于定义干旱指数的现有方法相比,这两种方法都更加健壮且在物理上有意义。尽管如此,该框架在用于水平衡的水文通量方面还是很灵活的,使用户能够使索引公式适应不同位置的数据可用性。在此基础上,将水平衡中使用不同水文通量的指标进行了相互比较,表明仅考虑水平衡中的降水量的干旱指标就足以满足西欧和中欧的需求。在地中海地区,需要考虑通过蒸散而不是潜在的蒸散引起的温度影响,以产生代表缺水的有意义的指数。另外,我们的结果表明,在北欧和斯堪的纳维亚半岛,为了获得准确的结果,需要在指数定义中同时考虑降雪和径流影响。

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