• Sorted by Date • Sorted by Last Name of First Author •
Amazirh, Abdelhakim, Ouassanouan, Youness, Bouimouass, Houssne, Baba, Mohamed Wassim, Bouras, El Houssaine, Rafik, Abdellatif, Benkirane, Myriam, Hajhouji, Youssef, Ablila, Youness, and Chehbouni, Abdelghani, 2024. Remote Sensing-Based Multiscale Analysis of Total and Groundwater Storage Dynamics over Semi-Arid North African Basins. Remote Sensing, 16(19):3698, doi:10.3390/rs16193698.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2024RemS...16.3698A,
author = {{Amazirh}, Abdelhakim and {Ouassanouan}, Youness and {Bouimouass}, Houssne and {Baba}, Mohamed Wassim and {Bouras}, El Houssaine and {Rafik}, Abdellatif and {Benkirane}, Myriam and {Hajhouji}, Youssef and {Ablila}, Youness and {Chehbouni}, Abdelghani},
title = "{Remote Sensing-Based Multiscale Analysis of Total and Groundwater Storage Dynamics over Semi-Arid North African Basins}",
journal = {Remote Sensing},
keywords = {groundwater dynamics, GRACE, ERA5-Land, Mediterranean regions, water balance},
year = 2024,
month = oct,
volume = {16},
number = {19},
eid = {3698},
pages = {3698},
abstract = "{This study evaluates the use of remote sensing data to improve the
understanding of groundwater resources in climate-sensitive
regions with limited data availability and increasing
agricultural water demands. The research focuses on estimating
groundwater reserve dynamics in two major river basins in
Morocco, characterized by significant local variability. The
study employs data from Gravity Recovery and Climate Experiment
satellite (GRACE) and ERA5-Land reanalysis. Two GRACE
terrestrial water storage (TWS) products, CSR Mascon and JPL
Mascon (RL06), were analyzed, along with auxiliary datasets
generated from ERA5-Land, including precipitation,
evapotranspiration, and surface runoff. The results show that
both GRACE TWS products exhibit strong correlations with
groundwater reserves, with correlation coefficients reaching up
to 0.96 in the Oum Er-rbia River Basin and 0.95 in the Tensift
River Basin (TRB). The root mean square errors (RMSE) were 0.99
cm and 0.88 cm, respectively. GRACE-derived groundwater storage
(GWS) demonstrated a moderate correlation with observed
groundwater levels in OERRB (R = 0.59, RMSE = 0.82), but a
weaker correlation in TRB (R = 0.30, RMSE = 1.01). On the other
hand, ERA5-Land-derived GWS showed a stronger correlation with
groundwater levels in OERRB (R = 0.72, RMSE = 0.51) and a
moderate correlation in TRB (R = 0.63, RMSE = 0.59). The
findings suggest that ERA5-Land may provide more accurate
assessments of groundwater storage anomalies, particularly in
regions with significant local-scale variability in land and
water use. High-resolution datasets like ERA5-land are,
therefore, more recommended for addressing local-scale
heterogeneity in regions with contrasted complexities in
groundwater storage characteristics.}",
doi = {10.3390/rs16193698},
adsurl = {https://ui.adsabs.harvard.edu/abs/2024RemS...16.3698A},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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