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Modeling of water balance response to an extreme future scenario in the ?tztal catchment, Austria

机译:奥地利菲茨河谷集水区对极端未来情景的水平衡响应建模

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The aim of the study was to investigate the impact of climate change on thewater balance of the ?tztaler Ache catchment in Tyrol, Austria. For thispurpose the conceptual hydrological model HBV-D REG was applied. First, themodel was calibrated and validated using current observed climate anddischarge data. Second, the calibrated model was applied with reanalysisdata. Third, downscaled climate scenarios from 2010 to 2099 served as inputdata to the HBV-D REG. Thereby two extreme land cover scenarios wereconsidered: for water balance modeling a constant glacier coverage from todayand additionally for runoff simulations a complete loss of glaciered area.The downscaled climate data were generated with the expanded downscalingmethod. Scenario simulations indicated an increase in annual arealtemperature by 3.4 °C and a slight decrease in annual arealprecipitation by 89 mm in the next one hundred years. According to the hydrologicalmodeling, these climate changes caused an increase in evapotranspiration anda decrease in snow coverage. Furthermore model simulations showed an increasein winter and spring runoff, whereas summer runoff was highly sensitive toglacier coverage and decreased with complete loss of glacier coverage.
机译:这项研究的目的是调查气候变化对奥地利蒂罗尔州Ftztaler Ache流域水平衡的影响。为此,应用了概念性水文模型HBV-D REG。首先,使用当前观察到的气候和排放数据对模型进行校准和验证。其次,将校准后的模型与重新分析数据一起应用。第三,2010年至2099年的降尺度气候情景是HBV-D REG的输入数据。因此,考虑了两种极端的土地覆盖情景:从今天开始,为水平衡建模提供恒定的冰川覆盖度,为进行径流模拟,为冰川覆盖的区域完全丧失。缩减的气候数据是通过扩展的缩减规模方法生成的。方案模拟表明,在接下来的一百年中,年平均气温升高了3.4°C,年平均降水量略微下降了89 mm。根据水文模型,这些气候变化导致蒸散量增加,积雪减少。此外,模型模拟表明,冬季和春季径流增加,而夏季径流对冰川覆盖高度敏感,并随着冰川覆盖的完全丧失而减少。

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