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首页> 外文期刊>Natural hazards and earth system sciences >Using stochastic space-time models to map extreme precipitation in southern Portugal
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Using stochastic space-time models to map extreme precipitation in southern Portugal

机译:使用随机时空模型绘制葡萄牙南部的极端降水图

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The topographic characteristics and spatial climatic diversity are significant in the South of continental Portugal where the rainfall regime is typically Mediterranean. Direct sequential cosimulation is proposed for mapping an extreme precipitation index in southern Portugal using elevation as auxiliary information. The analysed index (R5D) can be considered a flood indicator because it provides a measure of medium-term precipitation total. The methodology accounts for local data variability and incorporates space-time models that allow capturing long-term trends of extreme precipitation, and local changes in the relationship between elevation and extreme precipitation through time. Annual gridded datasets of the flood indicator are produced from 1940 to 1999 on 800 m x 800 m grids by using the space-time relationship between elevation and the index. Uncertainty evaluations of the proposed scenarios are also produced for each year. The results indicate that the relationship between elevation and extreme precipitation varies locally and has decreased through time over the study region. In wetter years the flood indicator exhibits the highest values in mountainous regions of the South, while in drier years the spatial pattern of extreme precipitation has much less variability over the study region. The uncertainty of extreme precipitation estimates also varies in time and space, and in earlier decades is strongly dependent on the density of the monitoring stations network. The produced maps will be useful in regional and local studies related to climate change, desertification, land and water resources management, hydrological modelling, and flood mitigation planning.
机译:葡萄牙大陆南部的地形特征和空间气候多样性很重要,那里的降雨方式通常为地中海。提出了直接顺序协同模拟方法,以海拔作为辅助信息绘制葡萄牙南部的极端降水指数。可以将分析指数(R5D)视为洪水指标,因为它提供了中期降水总量的度量。该方法考虑了当地数据的变化,并纳入了时空模型,该模型可以捕获极端降水的长期趋势,以及随时间变化的海拔和极端降水之间关系的局部变化。利用海拔和指数之间的时空关系,从1940年至1999年,在800 m x 800 m网格上生成了洪水指示器的年度网格化数据集。每年还会对提议的方案进行不确定性评估。结果表明,在整个研究区域内,海拔和极端降水之间的关系局部变化,并随着时间的推移而减小。在较湿润的年份,洪水指标在南部山区表现出最高的值,而在较干燥的年份,极端降雨的空间格局在研究区域内的变化要小得多。极端降水估计的不确定性也随时间和空间而变化,并且在前几十年中,很大程度上取决于监测站网络的密度。制作的地图将对与气候变化,荒漠化,土地和水资源管理,水文建模以及防洪规划有关的区域和地方研究有用。

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