下降的地下水及其在甘河流沿线的影响,使用了 Sentinel-1,GRACE,水位和降雨数据的综合数据
Ashwani Raju1, Ramesh P Singh2, Praveen Kumar Kannojiya3
1Remote Sensing & GIS Lab., Department of Geology, Institute of Science, Banaras Hindu University, Varanasi 221005, Uttar Pradesh, India; School of Life and Environmental Sciences, Schmid College of Science and Technology, Chapman University, Orange, CA-92866, United States.
The Science of the total environment
|February 15, 2024
概括
印度印度河平原的地下水枯竭正在导致土地沉降. 这项研究将水气候变化和城市化与瓦拉纳西的水资源短缺和沉降土地联系起来.
科学领域:
- 地球和环境科学 地球和环境科学
- 水文学的水文学
- 地质物理学 地质物理学
背景情况:
- 印度-河流平原 (IGP) 面临水资源短缺,原因是气候变化和人口密度高.
- 城市地区的地下水密集吸收导致土地沉降,威胁基础设施.
研究的目的:
- 调查瓦拉纳西的地下水位,水气候变量和土地沉降之间的关系.
- 评估城市化对水文应力和表面变形的影响.
主要方法:
- 使用的Sentinel-1 (2017-2023),GRACE (2003-2023),地下水位 (1998-2023) 和降水量 (2002-2023) 的数据.
- 分析了时空变化和长期水文反应.
主要成果:
- 观察到连续的地下水耗尽 (14.6 ± 5.6 毫米/年) 与降水变化有关.
- 鉴定了地下水储存的非线性趋势,原因是气候变化和水的吸收,特别是在干旱期间.
- 在甘河沿岸测量土地沉降 (∼2-8毫米/年),与储能减少和城市化相关.
结论:
- 城市化显著增加了水文压力,并导致甘中部平原的土地沉降.
- 地下水位数据证实了水气候变量和沉降之间的联系.
- 调查结果强调,在气候变化影响的背景下,需要将这些见解纳入水资源管理战略.
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