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Water Resources Adaptation to Global Changes: Risk Management through Sustainable Infrastructure Planning and Management

机译:水资源适应全球变化:通过可持续基础设施规划和管理风险管​​理

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Global changes due to climatic variations, demographic changes and economic development, have impacts on the quality and quantity of potable and irrigation source waters. Internal and external climatic forcings, for example, redistribute precipitation seasonally and spatially in the temperate contiguous United States. This change is expressed in hydrologic periodicity, dry and wet period switching frequency, and the change in maximum rainfall intensity. Spatially, the long-term change is shown by increased precipitation in the eastern U.S., flash floods in the lower Mississippi River basin, and intensified droughts in the Great Plain and Southwestern states, and the southern California. In Florida and other coastal areas, greater degrees of salt water intrusion to productive aquifers could materialize due to predicted rise in sea levels. Data mining of historical hydrologic records has shown the existence of these regional patterns. The results are in general agreement with the published general circulation model outputs. In addition, water usage has changed with time and water demand has been redistributed spatially as population centers shifted in the past decades. Quantitative impact analysis focusing on water availability and demand changes is important to risk management and adaptive infrastructure development at various watershed scales. In this approach, adaptive engineering techniques and management methods can be proposed for each relatively homogeneous hydrologic region. Examples include water reuse in the water-stressed Florida, the Great Plain states and California, salt-water intrusion mitigation in Florida and coastal areas, adaptive hydrological engineering in the eastern U.S., Ohio River valley, and lower Mississippi River basin. These results are discussed to highlight the importance of engineering factors (e.g., design storms, groundwater level control) in adaptation of water infrastructure planning and management.
机译:由于气候变化,人口变化和经济发展导致的全球变化对饮用和灌溉源水域的质量和数量产生影响。例如,内部和外部气候强制,例如,在温带连续的美国季节性和空间上重新分配降水。这种变化以水文周期性,干燥和潮湿的时段开关频率表示,以及最大降雨强度的变化。在空间上,长期改变通过较低的密西西比河流域中的闪蒸洪水增加,并在伟大的平原和西南国家和南加州的加剧干旱。在佛罗里达和其他沿海地区,由于海平面预测的预测,富含含水层的盐水侵入程度更大。历史水文记录的数据挖掘表明存在这些区域模式。结果与已发表的一般循环模型输出一致。此外,随着时间的推移,随着时间的推移,水需求随着时间的推移而改变了水需求,随着人口中心在过去的几十年里转移。关注水可用性和需求变化的定量影响分析对于各种流域尺度的风险管理和适应性基础设施发展是重要的。在这种方法中,可以针对每个相对均匀的水文区域提出自适应工程技术和管理方法。实例包括在佛罗里达州的水力强调,佛罗里达州的大型州和加利福尼亚州和加利福尼亚州的盐水侵入缓解,在美国东部,俄亥俄州河谷和较低的密西西比河流域中的自适应水文工程。讨论了这些结果以突出工程因素(例如,设计风暴,地下水位控制)适应水基础设施规划和管理的重要性。

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