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Transboundary Climate Change Effects on the Hydrologic Regime in the Rio Conchos Basin

机译:跨界气候变化对里奥康乔斯盆地水文状况的影响

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This paper presents results about potential effects of climate change on the hydrology and water resources in the Rio Conehos basin, with special emphasis on the transboundary water treaty signed between the US and Mexico in 1944. The Rio Conchos watershed, the main tributary of the lower portion of the bi-national Rio Grande/Bravo basin, is located in Chihuahua State in northern Mexico. The most relevant problem in the basin is the frequent occurrence of long drought periods, such as those that occurred in 1950s, 1960s, and the most recent from 1992 to 2003. Coupled with increased water demand and low irrigation efficiencies, the competition for water resources is high on both sides of the border. This paper reports on part of an assessment of expected climate change impacts in the basin. The methodology includes: 1) developing a model that represents the hydrological behavior of the basin; 2) analyzing downscaled climate data from five General Circulation Models (GCMs), for emission scenarios A2 and A1B; 3) simulating the basin under these climate change scenarios; 4) assessing the impacts of climate change on the hydrology and water resources in the basin; and 5) simulating and evaluating water management scenarios that could be used to adapt to the expected climate impacts in the coming decades. Some results from tasks (1) and (2) are reported here. These indicate a negative trend of precipitation in the area over the next few decades. Consequently, streamflow is projected to be lower by more than 18% at the basin outlet (Ojinaga station at the confluence with the Rio Grande) for scenario A2. Moreover, seasonal runoff analysis shows that winter and summer flows will be reduced more than 25% by the end of the century. Trend analysis also indicates negative trends over time. In addition, the change in runoff concentration and periodicity was explored in this research.
机译:本文介绍了气候变化对里约科尼奥斯河盆地水文学和水资源的潜在影响的结果,特别着重于1944年美国和墨西哥之间签署的跨界水条约。里约康科斯分水岭是下游的主要支流两国之间的里奥格兰德/布拉沃盆地的一部分位于墨西哥北部的奇瓦瓦州。流域中最相关的问题是长期干旱时期的频繁发生,例如1950年代,1960年代以及1992年至2003年的最近时期。加上水资源需求增加和灌溉效率低下,水资源竞争加剧在边界的两边都很高。本文报告了该盆地对气候变化的预期影响评估的一部分。该方法包括:1)建立代表流域水文行为的模型; 2)针对排放情景A2和A1B,分析来自五个通用循环模型(GCM)的降尺度气候数据; 3)在这些气候变化情景下模拟流域; 4)评估气候变化对流域水文和水资源的影响; 5)模拟和评估水资源管理方案,以适应未来几十年的预期气候影响。此处报告了任务(1)和(2)的一些结果。这些表明未来几十年该地区的降水呈负趋势。因此,对于方案A2,流域出口(与里奥格兰德河交汇处的Ojinaga站)的流量预计将降低18%以上。此外,季节性径流分析表明,到本世纪末,冬季和夏季的流量将减少25%以上。趋势分析还显示了一段时间内的负面趋势。此外,本研究探讨了径流浓度和周期性的变化。

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