Machine learning based downscaling of GRACE-estimated groundwater in Central Valley, California

Vibhor Agarwal*, Orhan Akyilmaz, C. K. Shum, Wei Feng, Ting Yi Yang, Ehsan Forootan, Tajdarul Hassan Syed, Umesh K. Haritashya, Metehan Uz

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16 Atıf (Scopus)

Özet

California's Central Valley, one of the most agriculturally productive regions, is also one of the most stressed aquifers in the world due to anthropogenic groundwater over-extraction primarily for irrigation. Groundwater depletion is further exacerbated by climate-driven droughts. Gravity Recovery and Climate Experiment (GRACE) satellite gravimetry has demonstrated the feasibility of quantifying global groundwater storage changes at uniform monthly sampling, though at a coarse resolution and is thus impractical for effective water resources management. Here, we employ the Random Forest machine learning algorithm to establish empirical relationships between GRACE-derived groundwater storage and in situ groundwater level variations over the Central Valley during 2002–2016 and achieved spatial downscaling of GRACE-observed groundwater storage changes from a few hundred km to 5 km. Validations of our modeled groundwater level with in situ groundwater level indicate excellent Nash-Sutcliffe Efficiency coefficients ranging from 0.94 to 0.97. In addition, the secular components of modeled groundwater show good agreements with those of vertical displacements observed by GPS, and CryoSat-2 radar altimetry measurements and is perfectly consistent with findings from previous studies. Our estimated groundwater loss is about 30 km3 from 2002 to 2016, which also agrees well with previous studies in Central Valley. We find the maximum groundwater storage loss rates of −5.7 ± 1.2 km3 yr−1 and -9.8 ± 1.7 km3 yr−1 occurred during the extended drought periods of January 2007–December 2009, and October 2011–September 2015, respectively while Central Valley also experienced groundwater recharges during prolonged flood episodes. The 5-km resolution Central Valley-wide groundwater storage trends reveal that groundwater depletion occurs mostly in southern San Joaquin Valley collocated with severe land subsidence due to aquifer compaction from excessive groundwater over withdrawal.

Orijinal dilİngilizce
Makale numarası161138
DergiScience of the Total Environment
Hacim865
DOI'lar
Yayın durumuYayınlandı - 20 Mar 2023

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Publisher Copyright:
© 2022 Elsevier B.V.

Finansman

Vibhor Agarwal received OSU Fellowship and salary as Teaching Assistant while a PhD student at OSU. Orhan Akyilmaz and Metehan Uz is partially supported by the Scientific and Technological Research Council of Turkey - TÜBİTAK ( 119Y176 ). C.K. Shum is partially supported by NSF 's Partnerships for Innovation Program ( 2044704 ), and NASA 's Earth Surface Interior Focus Area Program ( 80NSSC20K0494 ). Ehsan Forootan is supported by the Danmarks Frie Forskningsfond [ 10.46540/2035-00247B ] under DANSk-LSM project. Vibhor Agarwal received OSU Fellowship and salary as Teaching Assistant while a PhD student at OSU. Orhan Akyilmaz and Metehan Uz is partially supported by the Scientific and Technological Research Council of Turkey - TÜBİTAK (119Y176). C.K. Shum is partially supported by NSF's Partnerships for Innovation Program (2044704), and NASA's Earth Surface Interior Focus Area Program (80NSSC20K0494). Ehsan Forootan is supported by the Danmarks Frie Forskningsfond [10.46540/2035-00247B] under DANSk-LSM project.

FinansörlerFinansör numarası
NASA 's Earth Surface Interior Focus Area Program80NSSC20K0494
NASA's Earth Surface Interior Focus Area Program
National Science Foundation2044704
Türkiye Bilimsel ve Teknolojik Araştırma Kurumu119Y176
Danmarks Frie Forskningsfond

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