分析2000年以后印度拉贾斯坦邦的地下水位和降雨量变化,使用井观测和GRACE数据
Md Moniruzzaman Monir1, Subaran Chandra Sarker1
1Department of Geography and Environmental Science, Begum Rokeya University, Rangpur-5400, Bangladesh.
Heliyon
|February 5, 2024
概括
拉贾斯坦邦的地下水位呈现混合趋势,尽管70%的地区降雨量增加,但地下水位下降了38%. 降雨是这个半干旱地区地下水位的主要驱动因素.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 水资源管理 水资源管理
背景情况:
- 在干旱地区,地下水枯竭是一个关键问题.
- 印度沙漠地区的地下水动态以前没有得到充分的分析.
- 了解地下水与降雨的关系对于环境保护至关重要.
研究的目的:
- 评估2000-2021年拉贾斯坦邦的地下水位 (GWL) 和降雨趋势.
- 分析GWL变化与长期降雨模式之间的关系.
- 在半干旱环境中确定地下水变化的关键驱动因素.
主要方法:
- 从33个地区的921个站点收集了年度GWL和降雨数据.
- 应用了非参数修改的曼-肯德尔和斯皮尔曼rho测试用于趋势分析.
- 利用皮尔森,肯德尔的tau-b和斯皮尔曼对相关性和回归的分析.
主要成果:
- 38%的地区显示显著下降GWL趋势,而49%显示上升趋势.
- 70%的地区呈现降雨量上升趋势,30%的地区呈现稳定趋势.
- 在所有地区观察到GWL深度和降雨量之间的负相关性,其中58%显示中度负相关性.
结论:
- 降雨被认为是拉贾斯坦邦半干旱,干旱地区地下水位的主要影响因素.
- 尽管许多地区降雨量增加,但GWL显著下降突出了复杂的水文相互作用.
- 该研究强调了需要综合水资源管理战略的必要性.
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