Collaborative Research: Groundwater-surface water interactions in tropical alpine catchments and their influence on sources and stability of water supply during glacial recession

合作研究：热带高山流域地下水与地表水的相互作用及其对冰川衰退期间供水来源和稳定性的影响

• 批准号: 1316432
• 负责人: Bryan Mark
• 金额: $ 26.49万
• 依托单位: Ohio State University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-07-01 至 2018-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1316432&HistoricalAwards=false
• 关键词: Collaborative; Research; Groundwater; surface; water

Alpine watersheds and the ice and snow they contain are one of the most important sources of fresh water in the world, and mountain regions that are dominated by glaciers are especially sensitive to climate change. Melting glaciers in the semi-arid tropics currently provide a large component of annual runoff and buffer highly seasonal precipitation regimes, but ongoing glacier recession is predicted to make alpine runoff smaller in volume and more temporally variable, stressing water resources. Previous research suggests that groundwater aquifers in proglacial catchments are an important storage reservoir during dry seasons, and will likely play a dominant role in streamflow generation under future non-glacierized conditions. Despite their importance, little is known about fundamental hydrogeologic processes governing the interaction of surface water and groundwater in proglacial catchments. The investigators on this grant will study the interactions between surface water and groundwater reservoirs in proglacial meadow landforms in the Andes of Peru, estimate their storage volumes, and quantify contributions to streamflow. The research plan integrates a creative combination of field methods to directly quantify groundwater-surface water interactions (GWSWI) in remote, data-poor glacierized catchments and describe the relative hydrologic influence of groundwater storage and melting glaciers. The objectives of the proposed project are to: (1) measure gains and losses of water between stream channel reaches and groundwater stored in proglacial meadows, moraines, talus slopes, and alluvial fans in wet and dry seasons; (2) measure and map subsurface structures, properties, and water content of meadow aquifers and estimate storage volumes; and (3) determine the impact of GWSWI on surface water chemistry and on hydrochemical mixing models used to estimate glacial melt.The proposed research addresses unknown aspects of proglacial watershed hydrology, and the results will expand the current state of knowledge about groundwater storage and its interaction with surface water resources in tropical glacierized catchments and alpine watersheds. Conclusions from this study could transform alpine hydrologic modeling, which typically ignores or simplifies groundwater storage. The results of the proposed research will be broadly relevant to hydrologists, glaciologists, and physical and human geographers, as well as to water resource managers, development planners, agricultural engineers, municipalities and local governments, indigenous communities, and industrial sectors (hydroelectric and mining). Tropical glacierized mountain ranges are undergoing rapid environmental and demographic shifts and are especially susceptible to climate change and water stress, and this project will contribute to the understanding and prediction of water resources vital to human livelihoods. Education and outreach programs will enhance long-term connections with local community groups, local governments, and Peruvian researchers, and this effort will continue to engage the broader community of water users in the Andes. This project is co-funded by the Hydrologic Sciences and the International Science and Engineering Programs.

高山流域及其所含的冰雪是世界上最重要的淡水来源之一，而以冰川为主的山区对气候变化尤其敏感。在半干旱热带地区融化的冰川目前提供了很大的组成部分，年径流量和缓冲高度季节性降水制度，但持续的冰川衰退预计将使高山径流量更小，更随时间变化，强调水资源。以往的研究表明，在干旱季节，冰前集水区的地下水含水层是一个重要的蓄水池，并可能在未来的非冰川化条件下的径流发电中发挥主导作用。尽管它们的重要性，很少有人知道的基本水文地质过程中的地表水和地下水的相互作用，在冰前集水区。这项研究将研究秘鲁安第斯山脉冰前草甸地貌中地表水和地下水水库之间的相互作用，估计其储存量，并量化对径流的贡献。该研究计划整合了一个创造性的实地方法组合，直接量化远程，数据匮乏的冰川化集水区的地下水-地表水相互作用（GWSWI），并描述地下水储存和冰川融化的相对水文影响。该项目的目标是：（1）测量雨季和旱季河流河道河段与冰前草甸、冰碛、岩屑坡和冲积扇中储存的地下水之间的水量增减;（2）测量和绘制草甸含水层的地下结构、性质和含水量，并估计储存量;以及（3）确定GWSWI对地表水化学和用于估计冰川融化的水化学混合模型的影响。拟议的研究涉及冰前流域水文学的未知方面，研究结果将扩大目前关于热带冰川流域和高山流域地下水储存及其与地表水资源相互作用的知识。这项研究的结论可以改变高山水文模型，通常忽略或简化地下水储存。拟议研究的结果将与水文学家、冰川学家、自然地理学家和人文地理学家以及水资源管理人员、发展规划人员、农业工程师、市政当局和地方政府、土著社区和工业部门（水电和采矿）广泛相关。热带冰川山脉正在经历环境和人口的迅速变化，特别容易受到气候变化和水资源紧张的影响，该项目将有助于了解和预测对人类生计至关重要的水资源。教育和推广计划将加强与当地社区团体、地方政府和秘鲁研究人员的长期联系，这一努力将继续吸引安第斯山脉更广泛的用水者社区。该项目由水文科学和国际科学与工程计划共同资助。