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Elameen, Ayman M., Jin, Shuanggen, and Sarfo, Isaac, 2025. Runoff Dynamics and Its Regime Changes in the Major River Basins of Africa From GRACE and GRACE-FO Observations. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 18:22891–22926, doi:10.1109/JSTARS.2025.3601672.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025IJSTA..1822891E,
author = {{Elameen}, Ayman M. and {Jin}, Shuanggen and {Sarfo}, Isaac},
title = "{Runoff Dynamics and Its Regime Changes in the Major River Basins of Africa From GRACE and GRACE-FO Observations}",
journal = {IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing},
keywords = {Africa, climate change, gravity recovery and climate experiment (GRACE)/GRACE follow-on (GRACE-FO), major river basins, runoff},
year = 2025,
month = jan,
volume = {18},
pages = {22891-22926},
abstract = "{The major African basins supply freshwater to around 0.5 billion people,
while monitoring runoff fluctuations in these basins is still
challenging due to limited in-situ data and high costs.
Hydrologic models are widely used for this purpose, but they
have certain drawbacks with larger uncertainty and low accuracy
in poorly gauged basins. This study attempts to address this
issue by using Gravity Recovery and Climate Experiment
(GRACE)/GRACE Follow-On (GRACE-FO) satellite measurements and
remote sensing data to estimate runoff changes in five major
African basins from 2003 to 2019. Moreover, a comprehensive
framework was developed to quantify interannual and intraannual
runoff regimes and their changes from the perspectives of
magnitude, variability, and duration. Results showed that runoff
changes estimated from GRACE/GRACE-FO in the major African
basins were in good alignment with those from the Global Land
Data Assimilation System, European Centre for Medium-Range
Weather Forecasts Reanalysis 5, and Soil Conservation Service-
Curve Number. Seasonal runoff increased in the Nile (0.12 to
0.46 mm/a, p < 0.05) and Congo (0.52 to 0.76 mm/a, p < 0.05)
basins during 20032019, while it was decreased in the Zambezi (1
to 0.34 mm/a, p < 0.05) and Orange (0.54 to 0.24 mm/a, p < 0.05)
basins during the same period. Further in-depth analysis showed
that the impacts of climate change in the study area were the
primary contributors to changes in runoff. Monthly runoff in the
Nile, Congo, and Niger basins showed an increase in magnitude,
duration, and variability. In contrast, the Zambezi and Orange
basins experienced a decrease in runoff magnitude, along with
reduced variability and duration. In addition, large-scale
atmospheric circulations, such as El-Nino Southern Oscillation
Index and Indian Ocean Dipole, have been found to be associated
with changes in runoff within the study area, as demonstrated by
correlation and wavelet analysis. Our findings provided valuable
insights into long-term runoff changes in major African basins
and enhanced the understanding of hydrologic processes in poorly
gauged regions.}",
doi = {10.1109/JSTARS.2025.3601672},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025IJSTA..1822891E},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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