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Simulation and classification of the impacts of projected climate change on flow regimes in the arid Hexi Corridor of Northwest China

机译:中国西北干旱河西走廊预测气候变化对流态影响的模拟与分类

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摘要

Traditional assessment approaches of climate change on flow regimes usually focus on flow magnitude and cannot capture the overall variation of flow regimes (e.g., variability, frequency, duration, timing, and rating). The Hexi Corridor, which is a typical arid and semiarid region in Northwest China, was selected as the study area. Streamflows were simulated by an integrated water system model in a historical period (1985-2005) and three future periods (2030s, 2050s, and 2070s). Twenty-nine global climate models were picked from the Coupled Model Intercomparison Project Phase 5 based on projection performance, and the high (RCP85) and intermediate (RCP45) ranges of Representative Concentration Pathways were selected for future scenario analysis. All the streamflows were characterized in detail by flow regime metrics, including the magnitude, variability, and frequency of the overall flow events. The regional impacts of climate change were assessed and clustered into several similar spatial patterns. Results showed that the projected climate change would sensibly increase the magnitudes of average and low flows (75th percentile), as well as the frequencies of low and high flows (25th percentile), but decrease the flow variability. By contrast, it would not sensibly change the magnitude of high-flow events. The flow regime variations of all scenarios and periods were clustered into three robust classes (highly, moderately, and slightly impacted classes) in the entire region. The flow regimes would be highly and moderately impacted in the middle stream and downstream with large-sized and semidesert catchments but slightly impacted in the upper and middle streams with small-sized and montane vegetation catchments. The impacted classes will sensibly vary at most stations in different future periods because of the spatial differences of climate change. This study would provide scientific support to implement the integrated adaptive water resource management for climate change at regional scales in the arid Hexi Corridor.
机译:传统的基于流态的气候变化评估方法通常关注流的大小,无法捕获流态的整体变化(例如,可变性,频率,持续时间,时间和等级)。河西走廊是中国西北地区典型的干旱和半干旱地区,被选为研究区域。在一个历史时期(1985-2005年)和三个未来时期(2030年代,2050年代和2070年代),通过综合水系统模型对流量进行了模拟。根据预测性能,从耦合模型比较项目第5阶段中选取了29个全球气候模型,并选择了代表集中路径的高(RCP85)和中(RCP45)范围进行未来的情景分析。所有流量均通过流量状态指标进行详细描述,包括总体流量事件的大小,可变性和频率。对气候变化的区域影响进行了评估,并归纳为几种类似的空间格局。结果表明,预计的气候变化将合理地增加平均流量和低流量(第75个百分位数)的大小,以及高流量和低流量(第25个百分位数)的频率,但会减小流量的可变性。相比之下,它不会明智地改变高流量事件的大小。在整个区域中,所有情景和时段的流态变化都被分为三个鲁棒类别(高,中和轻微受影响的类别)。在大型和半荒漠集水区的中游和下游,水流状况将受到中等程度的影响,而在小型和山地植被集水区的上游和中游,水流状况将受到轻微影响。由于气候变化的空间差异,在不同的未来时期内,大多数电台的受影响类别将明智地变化。这项研究将为在干旱的河西走廊实施区域尺度的气候变化综合适应水资源管理提供科学支持。

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