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Observed and modeled changes of the hydrological cycle in Mid-Europe

机译:观察和建模的中欧水文循环改变

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Changes in the hydrological cycle in Mid-Europe have been studied for the last six decades and the next four decades. With particular emphasis on precipitation, and with a sideview to runoff and floods, we use observational data and downscaled climate projections to assess the past changes and to estimate future changes at unprecedented spatial resolution and model ensemble size. Mean decadal precipitation changes were found (by other authors) to have occurred in the second half of the last century, with particular increases in the decades after 1970, in parallel to rising temperatures. The increase is strongest with respect to winter precipitation. Positive trends of runoff are found to predominate in Southern and Western Germany, negative trends in Northeastern Germany. For the near future (up to 2040) moderate increases in mean winter precipitation result from the ensemble modeling, in particular for Northern Germany. There is tendency, statistically less certain, that extreme precipitation and runoff, as well in winter and in summer, and duration of dry spells in summer will increase.
机译:在过去的六十年中,研究了中欧水文周期的变化,并在接下来的四十年里研究过。特别强调降水,并侧视为径流和洪水,我们使用观察数据和较低的气候预测来评估过去的变化,并估计前所未有的空间分辨率和模型整体尺寸的未来变化。在上个世纪下半叶发生(其他作者)(其他作者)(其他作者)发现了平均截止降水变化,在1970年之后的几十年中,与上升的温度平行,特别增加。随着冬季降水的增加,增长最强。德国南部和西部的径流积极趋势占主导地位,德国东北部的负面趋势。对于不久的将来(最多2040),适度的冬季降水量来自集合模型,特别是德国北部。有趋势,统计而言,冬季和夏季以及夏季的极端降水和径流,夏季干旱咒语将增加。

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