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Flood-related extreme precipitation in southwestern Germany: development of a two-dimensional stochastic precipitation model

机译:德国西南部洪水相关的极端降水:发展二维随机降水模型

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摘要

Various fields of application, such as risk assessments of the insurance industry or the design of flood protection systems, require reliable precipitation statistics in high spatial resolution, including estimates for events with high return periods. Observations from point stations, however, lack of spatial representativeness, especially over complex terrain. Current numerical weather models are not capable of running simulations over thousands of years. This paper presents a new method for the stochastic simulation of widespread precipitation based on a linear theory describing orographic precipitation and additional functions that consider synoptically driven rainfall and embedded convection in a simplified way. The model is initialized by various statistical distribution functions describing prevailing atmospheric conditions such as wind vector, moisture content, or stability, estimated from radiosonde observations for a limited sample of observed heavy rainfall events. The model is applied for the stochastic simulation of heavy rainfall over the complex terrain of southwestern Germany. It is shown that the model provides reliable precipitation fields despite its simplicity. The differences between observed and simulated rainfall statistics are small, being of the order of only +/- 10% for return periods of up to 1000 years.
机译:各种应用领域,例如保险业的风险评估或防洪系统的设计,需要高空间分辨率的可靠降水统计数据,包括估计返回期的事件。然而,点站的观察缺乏空间代表性,特别是在复杂的地形上。目前的数值天气模型不能在数千年以上运行模拟。本文提出了一种基于线性理论的广泛沉淀随机仿真的新方法,描述了描述了地形降水的额外函数,以简化的方式考虑概要降雨和嵌入对流。通过各种统计分布函数初始化模型,所述统计分布函数描述普遍的大气条件,例如风向载体,水分含量或稳定性,估计从无线电探测器观察到有限的观察到的大雨事件的样本。该模型适用于德国西南部复杂地形的大量降雨随机模拟。结果表明,尽管其简单性,该模型提供了可靠的降水场。观察和模拟降雨统计之间的差异很小,返回期限为+/- 10%,返回时间高达1000年。

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