EAR-Climate: Acquisition of hydrometric equipment to support undergraduate training and research on glacier lake outburst floods in southeast Alaska

EAR-Climate：采购水文测量设备，以支持阿拉斯加东南部冰川湖溃决洪水的本科生培训和研究

• 批准号: 2141243
• 负责人: Sonia Nagorski
• 金额: $ 7.77万
• 依托单位: University of Alaska Southeast Juneau Campus
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-04-15 至 2023-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2141243&HistoricalAwards=false
• 关键词: EAR; Climate; Acquisition; hydrometric; equipment

As glaciers melt each summer and recede over the years due to the warming climate, the chemical nature of their meltwater changes. Studying the physical and chemical characteristics of the meltwater released from glaciers is important because it directly affects the quality of downstream lakes, streams, and coastal marine zones. The Coastal Mountains of southeast Alaska are experiencing some of the highest glacial melt rates on Earth. As the glaciers shrink, they leave behind newly formed landscapes and waterbodies such as lakes collecting water in front of the glacier (proglacial lakes) and lakes on the edges of glaciers that are dammed by the glacier ice (glacially dammed lakes). Such lakes can trap sediment, nutrients, carbon, and other elements, preventing them from moving downstream. Additionally, glacially dammed lakes can suddenly release massive outbursts of water if their ice dam fails, creating flooding hazards and sending a surge of sediment and dissolved chemicals downstream. With thousands of glaciers currently receding in Alaska, it is critical to characterize and quantify the ongoing changes in glacierized watersheds and to better understand their ecological impacts. We will track the quantity and quality of water and sediment moving through and out of a glacially dammed lake and a proglacial lake in southeast Alaska using the acoustic doppler velocimeter and other equipment acquired through this project. In doing so, we will involve and train undergraduate students from the University of Alaska Southeast and the local high school, helping to equip the next generation of earth scientists with the skills and tools they need to address glacier change, hydrologic dynamics, Earth surface processes, and natural hazards.Climate change has triggered glaciers in the Coastal Mountain of Alaska to recede at some of the highest rates on Earth. Increased glacier mass loss is causing the growth of (1) proglacial lakes that can dramatically alter sediment and chemical export from watersheds and of (2) glacially-dammed lakes, which can produce hazardous glacial lake outburst floods (GLOFs) and release a large pulse of biogeochemical elements and sediment to downstream ecosystems. Understanding the storage and release of carbon, water, sediment, and metals such as mercury in and through these glacier-associated lakes is important for explaining how glacier retreat and ensuing landscape change will affect current and future chemical and sediment fluxes. As warming continues and glaciers further diminish, the changing physical and chemical outputs from glaciated watersheds will have implications for recipient aquatic ecosystems, including food web structure and productivity, availability of contaminants, organic carbon burial in coastal sediments, CO2 outgassing to the atmosphere, and the seasonal timing and intensity of coastal ocean acidification. In this project, we will monitor the hydrometric impacts of glacial change in southeast Alaska by acquiring an Accoustic Doppler Velocity meter, water quality sondes, and a multi-probe water quality meter for use in the glacierized Mendenhall watershed in Juneau, Alaska. The hydrometric instruments will be used to train undergraduate students through class labs and research assistantships at the University of Alaska Southeast, which is a small, Alaska-native serving, undergraduate university, and to engage local high school students. The instruments will allow us to further develop a research program aimed at understanding the dynamics and consequences of glacier melt and GLOFs on sediment and chemical export to the highly productive coastal watersheds of southeast Alaska.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

由于气候变暖，每年夏天冰川都会融化并逐渐消退，其融水的化学性质也会发生变化。研究冰川释放的融水的物理和化学特征非常重要，因为它直接影响下游湖泊、溪流和沿海海洋区域的质量。阿拉斯加东南部的沿海山脉正在经历地球上最高的冰川融化速度。随着冰川的缩小，它们留下了新形成的景观和水体，例如在冰川前积水的湖泊（前冰川湖）和冰川边缘被冰川冰拦住的湖泊（冰川堰塞湖）。这些湖泊可以捕获沉积物、营养物、碳和其他元素，阻止它们向下游移动。此外，如果冰坝失效，冰川堰塞湖可能会突然释放大量水，造成洪水危险，并向下游输送大量沉积物和溶解的化学物质。目前阿拉斯加有数千座冰川正在消退，因此表征和量化冰川流域的持续变化并更好地了解其生态影响至关重要。我们将使用声学多普勒测速仪和通过该项目获得的其他设备来跟踪阿拉斯加东南部冰川堰塞湖和前冰川湖进出的水和沉积物的数量和质量。为此，我们将邀请并培训来自阿拉斯加东南大学和当地高中的本科生，帮助下一代地球科学家掌握解决冰川变化、水文动力学、地球表面过程所需的技能和工具和自然灾害。气候变化已导致阿拉斯加沿海山区的冰川以地球上最高的速度消退。冰川质量损失的增加导致 (1) 冰川前湖的增长，可以极大地改变流域的沉积物和化学物质的输出，以及 (2) 冰川堰塞湖的增长，这可以产生危险的冰川湖溃决洪水 (GLOF) 并释放大量脉冲生物地球化学元素和沉积物对下游生态系统的影响。了解这些与冰川相关的湖泊中和通过这些冰川相关湖泊的碳、水、沉积物和汞等金属的储存和释放对于解释冰川退缩和随之而来的景观变化将如何影响当前和未来的化学和沉积物通量非常重要。随着变暖的持续和冰川的进一步减少，冰川流域物理和化学输出的变化将对受体水生生态系统产生影响，包括食物网结构和生产力、污染物的可用性、沿海沉积物中的有机碳埋藏、二氧化碳排放到大气中，以及沿海海洋酸化的季节时间和强度。在该项目中，我们将通过购买声学多普勒速度计、水质探空仪和多探头水质计来监测阿拉斯加东南部冰川变化对水文测量的影响，用于阿拉斯加朱诺冰川覆盖的门登霍尔流域。水文测量仪器将用于通过阿拉斯加东南大学（阿拉斯加东南大学）的课堂实验室和研究助学金来培训本科生，并吸引当地高中生，该大学是一所小型的阿拉斯加本地服务本科大学。这些仪器将使我们能够进一步开发一项研究计划，旨在了解冰川融化和 GLOF 对阿拉斯加东南部高产沿海流域的沉积物和化学品出口的动态和后果。该奖项反映了 NSF 的法定使命，并被认为是值得的通过使用基金会的智力优势和更广泛的影响审查标准进行评估来提供支持。