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Simulation and analysis of the impact of projected climate change on the spatially distributed waterbalance in Thuringia, Germany

机译:对德国图林根州预估的气候变化对空间分布的水平衡影响的模拟和分析

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The impact of projected climate change on the long-term hydrological balance andseasonal variability in the federal German state of Thuringia was assessedand analysed. For this study projected climate data for the scenarios A2 andB1 were used in conjunction with a conceptual hydrological model. Thedownscaled climate data are based on outputs of the general circulation modelECHAM5 and provide synthetic climate time series for a large number ofprecipitation and climate stations in Germany for the time period of 1971 to 2100.These data were used to compute the spatially distributed hydrological quantities,i.e. precipitation, actual evapotranspiration and runoff generation with aconceptual hydrological model. This paper discusses briefly the statisticaldownscaling method and its validation in Thuringia and includes an overviewof the hydrological model. The achieved results show that the projectedclimate conditions in Thuringia follow the general European climate trends –increased temperature, wetter winters, drier summers. But, in terms of thespatial distribution and interannual variability regional differences occur.The analysis showed that the general increase of the winter precipitation ismore distinct in the mid-mountain region and less pronounced in the lowlandwhereas the decrease of summer precipitation is higher in the lowland andless distinct in the mid-mountains. The actual evapotranspiration showed astatewide increase due to higher temperatures which is largest in the summerperiod. The resulting runoff generation in winter was found to increase in themid-mountains and to slightly decrease in the lowland region. In summer andfall a decrease in runoff generation was estimated for the entire area due tolower precipitation and higher evapotranspiration rates. These spatiallydifferentiated results emphasize the need of high resolution climate inputdata and distributed modelling for regional impact analyses.
机译:评估并分析了预计的气候变化对德国联邦图林根州长期水文平衡和季节变化的影响。在本研究中,将情景A2和B1的预估气候数据与概念性水文模型结合使用。缩减后的气候数据基于ECHAM5常规循环模型的输出,并提供了1971年至2100年期间德国大量降水和气候站的合成气候时间序列,这些数据用于计算空间分布的水文量,即概念性水文模型的降水,实际蒸散和径流的产生。本文简要讨论了图林根州的统计缩减方法及其验证,并概述了水文模型。取得的结果表明,图林根州的预计气候条件遵循了欧洲的总体气候趋势,包括温度升高,冬季潮湿,夏季干燥。但是,就空间分布和年际变化而言,存在区域差异。分析表明,冬季降水的总体增加在中部山区更为明显,而在低地则不那么明显,而夏季降水的减少在低地而少则较少在中山地区很独特。实际的蒸散量由于温度升高而在全州范围内增加,夏季期间最大。结果发现,冬季山区的径流增加,而低地地区的径流减少。在夏季和秋季,由于降水减少和蒸散速率较高,估计整个地区的径流产生减少。这些在空间上不同的结果强调了高分辨率气候输入数据和区域影响分析的分布式模型的需求。

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