Abstract

Climate variability and recurrent droughts have caused remarkable strain on water resources in most regions across the globe, with the arid and semi-arid areas being the hardest hit. The impacts have been notable on surface water resources, which are already under threat from massive abstractions due to increased demand, as well as poor conservation and unsustainable land management practices. Drought and climate variability, as well as their associated impacts on water resources, have gained increased attention in recent decades as nations seek to enhance mitigation and adaptation mechanisms. Although the use of satellite technologies has, of late, gained prominence in generating timely and spatially explicit information on drought and climate variability impacts across different regions, they are somewhat hampered by difficulties in detecting drought evolution due to its complex nature, varying scales, the magnitude of its occurrence, and inherent data gaps. Currently, a number of studies have been conducted to monitor and assess the impacts of climate variability and droughts on water resources in sub-Saharan Africa using different remotely sensed and in-situ datasets. This study therefore provides a detailed overview of the progress made in tracking droughts using remote sensing, including its relevance in monitoring climate variability and hydrological drought impacts on surface water resources in sub-Saharan Africa. The paper further discusses traditional and remote sensing methods of monitoring climate variability, hydrological drought, and water resources, tracking their application and key challenges, with a particular emphasis on sub-Saharan Africa. Additionally, characteristics and limitations of various remote sensors, as well as drought and surface water indices, namely, the Standardized Precipitation Index (SPI), Palmer Drought Severity Index (PDSI), Normalized Difference Vegetation (NDVI), Vegetation Condition Index (VCI), and Water Requirement Satisfaction Index (WRSI), Normalized Difference Water Index (NDWI), Modified Normalized Difference Water Index (MNDWI), Land Surface Water Index (LSWI+5), Modified Normalized Difference Water Index (MNDWI+5), Automated Water Extraction Index (shadow) (AWEIsh), and Automated Water Extraction Index (non-shadow) (AWEInsh), and their relevance in climate variability and drought monitoring are discussed. Additionally, key scientific research strides and knowledge gaps for further investigations are highlighted. While progress has been made in advancing the application of remote sensing in water resources, this review indicates the need for further studies on assessing drought and climate variability impacts on water resources, especially in the context of climate change and increased water demand. The results from this study suggests that Landsat-8 and Sentinel-2 satellite data are likely to be best suited to monitor climate variability, hydrological drought, and surface water bodies, due to their availability at relatively low cost, impressive spectral, spatial, and temporal characteristics. The most effective drought and water indices are SPI, PDSI, NDVI, VCI, NDWI, MNDWI, MNDWI+5, AWEIsh, and AWEInsh. Overall, the findings of this study emphasize the increasing role and potential of remote sensing in generating spatially explicit information on drought and climate variability impacts on surface water resources. However, there is a need for future studies to consider spatial data integration techniques, radar data, precipitation, cloud computing, and machine learning or artificial intelligence (AI) techniques to improve on understanding climate and drought impacts on water resources across various scales.

Highlights

  • Drought is a complex, naturally occurring hazard, resulting from climate variability and change, leading to a change in the water balance, due to drastic decreases in precipitation over an extended period of time [1,2,3]

  • Dinku et al [72] compared the performance of Climate Hazards Group Infra-Red Precipitation with Stations (CHIRPS) data, African Rainfall Climatology version 2 (ARC2), and TAMSAT data over Ethiopia, Kenya, Somalia, Uganda, Rwanda, and Tanzania, and the results indicated that CHIRPS had the highest accuracy, but often overestimated precipitation

  • The occurrence of drought is likely to increase, which means the impacts of droughts based on historical, present, and future scenarios need to be analyzed, especially in Africa, which is a data-scarce continent

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Summary

Introduction

Naturally occurring hazard, resulting from climate variability and change, leading to a change in the water balance, due to drastic decreases in precipitation over an extended period of time [1,2,3]. This paper seeks to provide a detailed overview on the progress of remote sensing applications in the monitoring of climate variability and drought impacts on surface water resources in sub-Saharan Africa. Water bodies are vulnerable to climate change and they need accurate, timely, and routine monitoring [26] This will help in determining the onset of drought conditions in order to come up with mitigation and adaptation strategies and avoid loss of lives and crops, and famine [27]. A lot of scientific research work has been conducted to monitor these droughts and associated impacts of climate variability [28,29], knowledge on the advancements in remote sensing applications and data processing techniques, in sub-Saharan Africa, remains poorly documented. To achieve the objective of this work, the paper describes methods used in reviewing and synthesizing relevant literature before identifying key research advancements as well as knowledge gaps warranting further investigations

Literature Search
Remote Sensing Products for Drought and Climate Variability Monitoring
Traditional Drought and Surface Water Body Monitoring Techniques
Remote Sensing Techniques of Drought Monitoring
Key Findings
Future Research Directions and Recommendations
Findings
10. Conclusions
Full Text
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