Assessing impacts of climate variability and land use/land cover change on the water balance components in the Sahel using Earth observations and hydrological modelling

Journal Article (2023)
Author(s)

Ali Bennour (Chinese Academy of Sciences, Commissariat Regional au Development Agricole)

Li Jia (Chinese Academy of Sciences)

Massimo Menenti (TU Delft - Optical and Laser Remote Sensing, Chinese Academy of Sciences)

Chaolei Zheng (Chinese Academy of Sciences)

Yelong Zeng (Chinese Academy of Sciences)

Beatrice Asenso Barnieh (University of Energy and Natural Resources, Chinese Academy of Sciences)

Min Jiang (Chinese Academy of Sciences)

Research Group
Optical and Laser Remote Sensing
DOI related publication
https://doi.org/10.1016/j.ejrh.2023.101370
More Info
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Publication Year
2023
Language
English
Research Group
Optical and Laser Remote Sensing
Volume number
47
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Abstract

Study region: Senegal river (SRB), Niger river (NRB), and Lake Chad basins (LCB). Study focus: We investigated the impacts of land use/land cover change (LULC) and climate variability on the water balance components from 1990 to 2020. We applied the Soil and Water Assessment Tool (SWAT) coupled with remote sensing retrievals of actual evapotranspiration (ETa) and surface soil moisture (SSM). To separate the impacts of the two aforementioned factors, two numerical experiments were designed: (i) climate variability effects by applying frozen LULC while changing the climate; (ii) LULC change impacts by applying frozen climate while changing LULC. New hydrological insights for the region: Overall, at the basin level, the results indicated that climate variability had the dominant role in increasing groundwater recharge, surface runoff, groundwater return flow and lateral flow in LCB and SRB. These increases triggered the recovery of lake area and higher water table in LCB and increased in SRB streamflow, while water scarcity increased in NRB. In contrast, the separate effect of LULC change, specifically natural vegetation expansion, increased actual ET and decreased the surface runoff, which could be a reason for lake area depletion in LCB and decreasing SRB and NRB streamflow. At the sub-basin level, LULC change, i.e. a gain in cropland and urban areas at the expense of forests in some sub-basins in NRB, led to a local increase in surface runoff. This implies a better redistribution of water in downstream and compensates the deficit in surface runoff caused by natural vegetation expansion in some other catchments. These changes, simultaneously with high intensity and long-duration precipitation, may increase the likelihood of inundation in some small catchments in the Niger river basin. These outcomes give useful hydrological insights into water and land management by emphasizing the crucial role of water recycling.