• Sorted by Date • Sorted by Last Name of First Author •
Barbosa, Sergio A., Jones, Norman L., Williams, Gustavious P., Teklu, Henok, Yidana, Sandow M., Pulla, Sarva T., Sanchez, Jorge Luis, Nelson, E. James, Ames, Daniel P., and Miller, A. Woodruff, 2025. A multi-source approach to groundwater storage and recharge assessment in the Volta Basin. Science of the Total Environment, 1001:180421, doi:10.1016/j.scitotenv.2025.180421.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025ScTEn100180421B,
author = {{Barbosa}, Sergio A. and {Jones}, Norman L. and {Williams}, Gustavious P. and {Teklu}, Henok and {Yidana}, Sandow M. and {Pulla}, Sarva T. and {Sanchez}, Jorge Luis and {Nelson}, E. James and {Ames}, Daniel P. and {Miller}, A. Woodruff},
title = "{A multi-source approach to groundwater storage and recharge assessment in the Volta Basin}",
journal = {Science of the Total Environment},
keywords = {Earth observations, GRACE, Groundwater, Recharge estimation, Surface water{\textendash}groundwater interaction, Volta Basin},
year = 2025,
month = oct,
volume = {1001},
eid = {180421},
pages = {180421},
abstract = "{Assessing groundwater storage changes is important in semiarid regions
such as the Volta Basin in sub-Saharan Africa but can be
challenging due to data scarcity. This study presents a multi-
source approach combining NASA's Gravity Recovery and Climate
Experiment (GRACE) mission data, Climate Hazards group Infrared
Precipitation with Stations (CHIRPS) precipitation data, the new
Global Land Data Assimilation System (GLDAS) v2.2 CLSM
groundwater storage anomaly dataset, traditional non-groundwater
terrestrial water storage components from GLDAS v2.1, and
Copernicus satellite data for surface water dynamics to analyze
groundwater storage changes and recharge rates in the Volta
Basin. Our study reveals: (1) A small change in groundwater
storage from 2002 to 2012, followed by a significant increase
from 2012 to 2022; (2) A total groundwater increase of
approximately 30 cubic kilometers or about 10 cm of liquid water
equivalent over the entire study period; (3) Water storage in
the basin is dominated by fluctuations in Lake Volta, which
accounts for {\ensuremath{\sim}}50 \% of terrestrial water
storage; (4) Groundwater recharge rates estimated using the
Water Table Fluctuation Method on GRACE- and GLDAS-derived data,
aligned with values from monitoring wells and previous studies;
(5) The GLDAS v2.2 dataset exhibits similar seasonal trends with
periodic peaks and troughs, yet the amplitude of anomalies from
GLDAS are larger compared to the GRACE dataset; and (6)
Groundwater recharge shows a weak correlation with extreme
precipitation events, suggesting more water percolates rather
than evaporates during such events. However, other factors,
including land use changes and agricultural practices, may also
impact groundwater storage and recharge.}",
doi = {10.1016/j.scitotenv.2025.180421},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025ScTEn100180421B},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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