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首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >Hydrological impacts of climate change on small ungauged catchments – results from a global climate model–regional climate model–hydrologic model chain
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Hydrological impacts of climate change on small ungauged catchments – results from a global climate model–regional climate model–hydrologic model chain

机译:气候变化对小未凝固集水区的水文影响 - 来自全球气候模型 - 区域气候模型 - 水文模型链的结果

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Climate change is one of the greatest threats currently facing theworld's environment. In Norway, a change in climate will strongly affect thepattern, frequency, and magnitudes of stream flows. However, it ischallenging to quantify to what extent the change will affect the flowpatterns and floods from small rural catchments due to the unavailabilityor inadequacy of hydro-meteorological data for the calibration ofhydrological models and due to the tailoring of methods to a small-scale level. Toprovide meaningful climate impact studies at the level of small catchments,it is therefore beneficial to use high-spatial- and high-temporal-resolutionclimate projections as input to a high-resolution hydrological model. Inthis study, we used such a model chain to assess the impacts of climatechange on the flow patterns and frequency of floods in small ungauged ruralcatchments in western Norway. We used a new high-resolution regional climateprojection, with improved performance regarding the precipitationdistribution, and a regionalized hydrological model (distance distributiondynamics) between a reference period?(1981–2011) and a future period?(2070–2100). The flow-duration curves for all study catchments show more wet periods in the future than during the reference period. The results also show that in the future period, the mean annual flow increases by 16 % to 33 %. The mean annual maximum floods increase by 29 % to 38 %, and floods of 2-?to 200-year return periods increase by 16 % to 43 %. The results are based on the RCP8.5 scenario from a single climate model simulation tailored to the Bergen region in western Norway, and the results should be interpreted in this context. The results should therefore be seen in consideration of other scenarios for the region to address theuncertainty. Nevertheless, the study increases our knowledge and understanding of the hydrological impacts of climate change on smallcatchments in the Bergen area in the western part of Norway.
机译:气候变化是目前世界上最受欢迎的威胁之一。在挪威,气候变化将强烈影响流动流动的图案,频率和大小。然而,由于液态化模型校准的不公平性,因此,它是在多大程度上量化变化会影响来自小型农村集水区的流动图集板和洪水。由于对小规模水平的方法剪裁。 Toprovide有意义的气候影响力在小集水区的水平,因此有利于使用高空间和高颞 - 议程高度预测作为高分辨率水文模型的输入。 Inthis研究,我们使用这种模型链来评估Climatechange对挪威西部小型未凝固的土木发球菌的流动模式和频率的影响。我们使用了一个新的高分辨率区域气候重点,提高了关于沉淀分布的表现,以及参考期之间的区域化水文模型(距离经销率)?(1981-2011)和未来时期?(2070-2100)。所有研究流域的流动持续时间曲线在未来显示比参考周期在未来更多的潮湿时段。结果还表明,在未来期间,平均年流量增加了16%至33%。平均年度最大洪水增加了29%至38%,洪水为2-?到200年的回报期增加了16%至43%。结果基于RCP8.5从挪威西部卑尔根地区量身定制的单一气候模型模拟,结果应在这种情况下解释。因此,考虑到该地区的其他情景来解决该结果以解决该地区的其他情况。然而,该研究提高了我们对挪威西部卑尔根地区的气候变化对气候变化的水文影响的知识和理解。

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