RAPID: Field investigation to collect snow, debris flow and sediment deposition and the glacier-melt induced peak flows and landslide in the Chamoli region, Uttarakhand, India

RAPID：在印度北阿坎德邦查莫利地区收集积雪、泥石流和沉积物以及冰川融化引起的洪峰和山体滑坡的现场调查

• 批准号: 2127775
• 负责人: Venkataramana Sridhar
• 金额: $ 2.5万
• 依托单位: Virginia Polytechnic Institute and State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-04-01 至 2023-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2127775&HistoricalAwards=false
• 关键词: RAPID; Field; investigation; collect; snow

On 7 Feb 2021, a cataclysmic flood triggered cascading events near Chamoli, in the state of Uttarakhand in the Himalayan range of India, resulting in washing away of a bridge and cutting off villages near the border areas of China. About 15 km downstream of the avalanche location, the Rishi Ganga Hydroelectric project was washed off and the National Thermal Power Corporation (NTPC) Tapovan project was also damaged. The cause of this glacier melt-induced landslide and flooding is suspected to have links to global warming and glacial retreat. The data to be collected for this project will inform whether this natural disaster was triggered by snowpack and glacial melt versus land-use change and deforestation, or a combination of these factors, that cause devastating landslides and floods in the ecologically fragile, headwater region of the Ganges. Understanding hydrologic and geomorphic processes in high-altitude environments is essential to closely evaluate if human-induced changes are contributing to extreme events. Improvements in our ability to predict glacial outburst/landslide/flooding events in high elevation, glaciated areas such as the Himalayan region has potential to mitigate impacts of future disasters.Changing climate and deforestation are impacting hydrological processes in the high elevation regions of the Himalayan range. Climate change is causing glacial retreat and changes in snowpack dynamics, while deforestation and land use change are modifying snow energy budgets and soil moisture dynamics. These impacts are compounded by one another and may result in extreme flood events. The data to be collected for this project will inform gaps in knowledge on snowmelt runoff and soil moisture dynamics and landslide vulnerability in the hillslopes of the Himalayan Range. The time-bound perishable data will be valuable for identifying the mass of snow and volume of runoff, as well as understanding the hydrological and landslide processes associated with this extreme event. The proposed RAPID project leverages a unique opportunity to collect information at the site in collaboration with the Indian Institute of Technology, Roorkee (IITR), which is located within 200 miles of the site. This proposal is co-funded by the Hydrologic Sciences and Geomorphology & Land-use Dynamics programs, as well as the Division of Earth Sciences.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.

2021 年 2 月 7 日，一场特大洪水在印度喜马拉雅山脉北阿坎德邦查莫利附近引发连环事件，导致一座桥梁被冲毁，中国边境地区附近的村庄被切断。雪崩地点下游约15公里处，Rishi Ganga水力发电项目被冲毁，国家热电公司（NTPC）Tapovan项目也遭到破坏。冰川融化引发的山体滑坡和洪水的原因被怀疑与全球变暖和冰川退缩有关。该项目收集的数据将表明这场自然灾害是否是由积雪和冰川融化、土地利用变化和森林砍伐引发的，还是这些因素的组合，导致生态脆弱的源头地区发生毁灭性的山体滑坡和洪水。恒河。了解高海拔环境中的水文和地貌过程对于密切评估人类引起的变化是否导致极端事件至关重要。提高我们预测喜马拉雅地区等高海拔冰川地区冰川爆发/滑坡/洪水事件的能力，有可能减轻未来灾害的影响。气候变化和森林砍伐正在影响喜马拉雅山脉高海拔地区的水文过程。气候变化正在导致冰川退缩和积雪动态变化，而森林砍伐和土地利用变化正在改变雪能预算和土壤湿度动态。这些影响相互叠加，可能导致极端洪水事件。该项目收集的数据将弥补有关喜马拉雅山脉山坡融雪径流、土壤湿度动态和滑坡脆弱性的知识空白。有时间限制的易腐烂数据对于确定降雪量和径流量以及了解与这一极端事件相关的水文和山体滑坡过程非常有价值。拟议的 RAPID 项目与距该地点 200 英里范围内的印度鲁尔基理工学院 (IITR) 合作，利用独特的机会在该地点收集信息。该提案由水文科学、地貌学和土地利用动力学项目以及地球科学部共同资助。该奖项反映了 NSF 的法定使命，并通过利用基金会的智力优势和更广泛的评估进行评估，认为值得支持。影响审查标准。