Improving crop-specific groundwater use estimation in the Mississippi Alluvial Plain: Implications for integrated remote sensing and machine learning approaches in data-scarce regions

被引:2
|
作者
Majumdar, Sayantan [1 ,4 ]
Smith, Ryan G. [2 ]
Hasan, Md Fahim [2 ]
Wilson, Jordan L. [3 ]
White, Vincent E. [3 ]
Bristow, Emilia L. [3 ]
Rigby, J. R. [3 ]
Kress, Wade H. [3 ]
Painter, Jaime A. [3 ]
机构
[1] Desert Res Inst, Reno, NV USA
[2] Colorado State Univ, Ft Collins, CO USA
[3] US Geol Survey, Catonsville, MD USA
[4] Desert Res Inst, Div Hydrol Sci, 2215 Raggio Pkwy, Reno, NV 89512 USA
基金
美国国家科学基金会;
关键词
Groundwater; Remote sensing; Machine learning; Regression; Irrigation; Estimation; Geospatial; UNITED-STATES; SATELLITE; SUSTAINABILITY; PRECIPITATION; IRRIGATION; AGRICULTURE; DEPLETION; AQUIFER; STORAGE; FUTURE;
D O I
10.1016/j.ejrh.2024.101674
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study region: The Mississippi Alluvial Plain (MAP) in the United States (US). Study focus: Understanding local-scale groundwater use, a critical component of the water budget, is necessary for implementing sustainable water management practices. The MAP is one of the most productive agricultural regions in the US and extracts more than 11 km3/year for irrigation activities. Consequently, groundwater-level declines in the MAP region pose a substantial challenge to water sustainability, and hence, we need reliable groundwater pumping monitoring solutions to manage this resource appropriately. New hydrological insights for the region: We incorporate remote sensing datasets and machine learning to improve an existing lookup table-based model of groundwater use previously developed by the U.S. Geological Survey (USGS). Here, we employ Distributed Random Forests, an ensemble machine learning algorithm to predict annual and monthly groundwater use (2014-2020) throughout this region at 1-km resolution, using pumping data from existing flowmeters in the Mississippi Delta. Our model compares favorably with the existing USGS model, with higher R2 (0.51 compared to 0.42 in the previous model), and lower root mean square error (RMSE) and mean absolute error (MAE)- 0.14 m and 0.09 m, respectively in our model, compared to 0.15 m and 0.1 m in the previous model. Therefore, this work advances our ability to predict groundwater use in regions with scarce or limited in-situ groundwater withdrawal data availability.
引用
收藏
页数:21
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