A systematic review of climate change and water
resources in Sub-Saharan Africa
Benson TURYASINGURA ( bensonturyasingura@gmail.com )
KABALE UNIVERSITY https://orcid.org/0000-0003-1325-4483
Petros Chavula
frica Center of Excellence for Climate Smart Agriculture and Biodiversity Conservation
Hubert Hirwa
China University of Chinese Academy of Sciences
Fatima Sule Mohammed
Kabale University
Natal Ayiga
Kabale University https://orcid.org/0000-0002-7644-2679
Elias Bojago
Wolaita Sodo University https://orcid.org/0000-0002-7235-8760
Brahim Benzougagh7
Mohammed V University https://orcid.org/0000-0002-1787-9678
Hannington Ngabirano
Kabale University
Systematic Review
Keywords: Aquaculture, Pollution, Rainfall, Relationships, Temperature, Variability
Posted Date: November 17th, 2022
DOI: https://doi.org/10.21203/rs.3.rs-2281917/v1
License: This work is licensed under a Creative Commons Attribution 4.0 International License.
Read Full License
A Systematic Review and Meta-analysis of Climate Change and Water
Resources in Sub-Sahara Africa
Benson Turyasingura1*, Petros Chavula2, Hubert Hirwa3, Fatima Sule Mohammed4, Natal
Ayiga5, Elias Bojago6, Brahim Benzougagh7 & Hannington Ngabirano8
1*
Department of Environmental Sciences, Faculty of Agriculture and Environmental Sciences, Kabale
University, P. O. Box 317 Kabale; Collage of Agriculture and Environmental Sciences, Haramaya
University Africa Center of Excellence for Climate Smart Agriculture and Biodiversity
Conservation, PO box 138, Haramaya, Ethiopia; Email: bturyasingura@kab.ac.ug; ORCID ID:
https://orcid.org/0000-0003-1325-4483: Tel No.: +256784580916/+251961951900
2
Collegel of Agriculture and Environmental Sciences Africa Center of Excellence for Climate
Smart Agriculture and Biodiversity Conservation, PO box 138, Haramaya, Ethiopia; E-mail:
petroschavula2@gmail.com
3
Key Laboratory of Ecosystem Network Observation and Modelling, Institute of Geographic
Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
University
of
Chinese
Academy
of
Sciences,
Beijing
100049,
China,
email:
hhirwa2019@igsnrr.ac.cn
4
Faculty of Agriculture and Environmental Sciences, Kabale University, Department of
Environmental
Sciences,
Kabale
University,
PO
box
317,
Kabale;
E-mail:
sumfats2002@gmail.com
5
Faculty of Arts and Social Sciences, Kabale University, Uganda, Department of Social Work
and Social Administration, Kabale, PO box 317, Kabale, Uganda; Email: nayiga@kab.ac.ug or
nayiga1962@gmail.com
6
Department Environmental Science, College of Natural and Computational Sciences, Wolaita
Sodo University, Wolaita Sodo, Ethiopia, Email: eliasboja77@gmail.com ORCID ID:
https://orcid.org/0000-0002-7235-8760
7
Geophysics and Natural Hazards Laboratory, Department of Geomorphology and Geomatics,
Scientific Institute, Mohammed V University in Rabat, Avenue Ibn Batouta, Agdal, PO Box 703,
10106, Rabat-City, Morocco. E-mail: brahim.benzougagh@is.um5.ac.ma; ORCID ID:
https://orcid.org/0000-0002-1787-9678; Tel N°: +212 675 640 655
1
8
Department of Chemistry, Faculty of Science Kabale University, P.O. Box 317, Southern
Division, Kabale, Uganda; Email: hngabirano@kab.ac.ug
*Corresponding Author: (bensonturyasingura@gamil.com/bturyasingura@kab.ac.ug).
ABSTRACT
Variations in precipitation that affect water resources have drawn a lot of attention to climate
change-related water quality issues in recent years. Point and non-point source contaminants
have an impact on water quality due to seasonal rainfall variability, and rainfall events are crucial
in spreading these pollutants. Sub-Saharan Africa has the least stable access to freshwater
supplies. Numerous academics have undertaken extensive research on the connection between
climate change and water resources, yielding significant research findings. However, there is a
dearth of quantitative analysis and thorough evaluation of research accomplishments. The
purpose of the study was to undertake an organized literature review on the topic of examining
the relationship between Sub-Saharan Africa's water resources and climate change. In the first
segment, Vos-Viewer was used to map, study the literature, and identify any gaps in order to
evaluate the impact of rainfall variability on water quality. The adaptation and mitigation
strategies for water availability were described in the second section. This report utilizes the
VOS-Viewer bibliometric software to create a combative network and keyword co-occurrence
map based on the pertinent literature on the topics of climate change and water resources in the
core collection of the Web of Science database and dimension. According to the study's findings,
cooperation networks are not as prominent as research networks between developed and
developing nations. It was also shown that irregular rainfall affects water quality by giving the
water a muddy, acidic, and turbid appearance. According to the assessment, the study's
conclusions suggest that involving all significant parties and adopting strong rules can facilitate
prudent water usage and management. This is crucial for the 884 million people whose survival
depends on surface water resources.
Keywords: Aquaculture, Pollution, Rainfall, Relationships, Temperature, Variability
2
1. Introduction
Water is life, as life on earth cannot survive without it (Al‐Ghussain, 2019; Zhang et al., 2021;
Frenkel-Pinter et al., 2021). Water resources provide different goods and services like fishing,
eco-tourism, and supply of water for various purposes such as domestic use, irrigation and
drinking (Saturday et al., 2022).
Worldwide, water resources are vulnerable to pollution as a result of their ease of access for
wastewater discharge and pollutants. Besides, complex anthropogenic activities like
urbanization, industrial activities, agricultural activities and sewage discharge and natural
processes like climate change, weathering, precipitation and erosion, affect the quality of water
and little effort have been done. Water contamination is becoming the most serious threats to
human health. It has been estimated that about 80% of all the diseases in mankind are due to one
or another unhealthy aspects of water (Kumar et al., 2018).
Due to climate change, one in three individuals who access securely managed drinking water
(1.9 billion) reside in rural regions (Fisch-Romito, 2021), leaving over 2.1 million people
without access to safe drinking water (UNICEF, 2019; Kong et al., 2020), including over 884
million people (Silva et al., 2020). Unfortunately, weather extremes like heat waves, excessive
rain, droughts, and associated fires, as well as coastal flooding, will have a significant impact on
people's lives, possessions, and environments (McGregor et al., 2005; Gulzar et al., 2021). The
deadliest natural disasters are floods and droughts, which claim lives harm economies, destroy
ecosystems and property worldwide (Wijkman & Timberlake, 2021), thus, affecting water
resources during heavy rainfall.
Water resources are very vital for the local people in Sub-Saharan Africa (SSA) because these
water body areas have wetlands that provide materials for handcrafts (Gopal et al., 2022), fishing
(Onyena & Sam, 2020), and mulching (Milder et al., 2011; Yahaya et al., 2022). Freshwater
resources are vulnerable to climate change and have the potential to be significantly altered, as
evidenced by poor drinking and irrigation water quality, with significant implications for human
societies and ecosystems (Abbasnia et al., 2019; Solangi et al., 2019; Zimmermann & Neu,
2022).
3
In addition, there has been little attention paid to climate change mitigation and adaptation in the
Sub-saharan region, where most people are affected by inadequate drinking water (Grasham et
al., 2019), approximatelly109 million people use unsafe surface water and over 695 million
people still use unimproved facilities (Baye, 2021; Walekhwa et al., 2022) It is estimated that 42
% of the population lack basic water supplies while 72 % lack basic sanitation (Renzaho, 2020).
Approximately 57 % have access to safe drinking water management services (Lord et al., 2021).
Currently, there is insufficient data in Sub-Saharan Africa about the impact of climate change on
water resources”; thus, a gap to fill.
According to Adeyeri (Adeyeri et al., 2020) altering rainfall patterns were noticed in Nigeria
which may affect surface water quality during wet and dry seasons. The status of water supply
and management in Nigeria is complicated because the bulk of the population is poor and must
often travel long distances to obtain potable water for their homes (Gift et al., 2020).
Understanding the dynamic link between rainfall variability and water supply in Sub-Saharan
Africa is crucial for building future water projects (Muringai et al., 2021). In South Africa and
Mozambique, people are fed by surface water or groundwater (Verlicchi & Grillini, 2020).
However, many natural and human-made factors including geochemical processes (Akhtar et al.,
2021), heavy rain, flooding (Du Plessis, 2019), the release of untreated wastewater (from rural
communities) and industrial effluents can pollute water sources.
Ethiopia has surface, underground water, 12 significant stream bowls, 11 freshwater and 9 saline
lakes, 4-hole lakes and more than 12 marshes and wetlands. However, approximately 60 % to 80
% of the populace suffer from waterborne and water-related illnesses (Soboksa et al., 2020).
Around 80 % of the Ethiopia's population and 20 % of the metropolitan population lack access to
safe drinking water during blustery seasons in long periods of dry seasons (Turyasingura &
Chavula, 2022). This is in line with the findings of Benson and Ayiga (2022) who revealed that
some farmers lack good farming methods (climate-smart agricultural) practices, which combat
climate change and its associated problems.
In Tanzania, about 25 % of the population relies altogether on groundwater for drinking
(Alarcón-Herrera et al., 2020). Expanding demand for groundwater has effectively been noted in
East Africa, like in Tanzania, particularly for individuals living in drier areas (Ligate et al.,
2021). As a result, the utilization and nature of groundwater will continue to be critical for the
4
majority of human advancement efforts. Increased rainfall variability has had a significant
impact on the quality of drinking water at both the local and national levels (Bastiancich et al.,
2022).
Uganda’s Vision 2040 promises general use and safe access to drinking water for all Ugandans
(Odokonyero et al., 2020). Water resources in SSA provide water for domestic use, irrigation,
car, and motorcycle washing. However, the faster-growing population in amalgamation with the
agricultural activities (Benson & Ayiga, 2022), in the water catchment areas has had a substantial
adverse impact on water quality and the ecosystem (Alex et al., 2021).
In addition, people have historically resided close to freshwater bodies because of the advantages
to health and wellbeing, both in Uganda (Saturday et al., 2021), and elsewhere in the world
(Hotez, 2021). Within three kilometers of a freshwater body, more than 50% of people on earth
reside (Panhwar et al., 2022). Nevertheless, rising population, intensive farming methods, and
infrastructure improvements have increased the level of external nutrient loading in the last
remaining natural freshwater systems, leading to unsustainable water extraction. As a result,
considerable changes in the physical and chemical properties of freshwater bodies have taken
place, frequently exhibiting a noticeable transition from the state of clear water to that of
turbidity.
Although several studies have been undertaken on the impact of rainfall variability on water
resources (Bwire et al., 2020), data on the implications of seasonal and yearly rainfall variability
on rural water supply systems is still missing. As a result, the purpose of this paper is to
investigate the relationship between climate change and water resources in Sub-Saharan Africa
to facilitate adaptation, mitigation, and water management practices to reduce water
contamination and achieve a sustainable environment. This understanding underpins the
development of measures to protect the water from further deterioration in quality, thereby
protecting the population relying on this resource as well as the environment. It was guided by
the following specific objectives, namely: to assess the effect of rainfall variability on the
physicochemical water quality parameters (turbidity, temperature, calcium, magnesium,
phosphates, pH, and electrical conductivity); and to determine the adaptation and mitigation
measures for water availability in Africa.
5
The study's argument is that growing human activity on lake borders and islands, which has the
ability to change the water's physical characteristics, puts the ecosystem services provided by
those resources at danger. However, it is unknown whether or not studies on the relationship
between climate change and water resources have been conducted to ascertain whether or not
human activities have had an impact on the water quality. By evaluating the meta-analysis of
climate change and water resources in sub-Saharan Africa, the suggested seeks to close.
2. Method
The SSA comprises two-thirds of the land area of the continent or around 24 million square
kilometres and world’s area most susceptible to climate change (Junk et al., 2013). Natural
disasters are becoming more frequent and more intense, and the geography of the area is
dramatically changing, impacting water resources (Van Aalst, 2006). Nearly 60 % of the
population of SSA live in rural regions and rely heavily on water supplies for drinking, industrial
usage, and agricultural purposes (Fróna et al., 2019). The population of SSA increased from 490
million in 1990 to 1 billion (or around 14 % of the world's population) in 2015, at a growth rate
of 2.7 % (Fenta et al., 2020). With over 190 million inhabitants, Nigeria is the most populous
nation in Africa; Ethiopia is the second with over 100 million (Olowe, 2021). Although water
resources are essential to people's livelihoods, this dependence is most apparent in developing
nations like those in SSA, where the majority of the population is impoverished and heavily
dependent on natural resources.
6
Figure 1: Study area map showing regions of Sub-Saharan Africa, (2022).
Source: Google reviews
The purpose of the study was to undertake an organised literature evaluation on the relationship
between Sub-Saharan Africa's water resources and climate change. Using Vos-viewer software
to map and review the literature and detect existing gaps, the first portion set out to determine the
effects of rainfall variability on water quality. The adaptation and mitigation strategies for water
availability were described in the second section. The scientific research conducted in SSA that
is primarily focused on climate change and water resources is the subject of this study. Using the
keywords "Climate-Change" AND "Water resources," searches were conducted in the Web of
Science (WOS) and Scopus databases to find the data. Based on the results of the initial search,
70 papers were selected for this study from a total search of 687. In addition, 20 papers from
WOS and 50 publications from Scopus were found relevant for this study, papers were selected
and discussed in the following, the review focuses on the effects of rainfall variability on water
quality, the adaptation and mitigation measures for water availability, from (1945-2022).
7
2.1 Climate Change and Water Resources in Uganda
Reduced stream flows in important catchments, lower recharging of groundwater, reduced
inflows to water storages, or intensified droughts are all consequences of rising temperatures and
reduced rainfall (Mahmo od et al., 2016), raising competition for water among sectors (Stoerk et
al., 2020). Changes in surface runoff and groundwater flows in shallow aquifers are examples of
hydrological processes linked to climate change, with implications for permanent and seasonal
water bodies like lakes and reservoirs hence, affecting its quality for example river Rwizi in
Mbarara district have been affected due to agricultural activities which leads to soil erosion
during rainfall thus, affecting aquatic species (Ojok et al., 2017).
Empirical studies on the effects of climate on water resources has been documented as climate
change can impact on water supplies by causing greater surface temperatures, melting of snow
and glaciers, rising sea levels due to droughts and floods, changes in rainfall frequency and
distribution, river drying, water bodies receding, landslides, and cyclones are some of the
potential effects of climate change on Uganda's water resources (Yakubu et al., 2012). For
example, on October 1, 2019, the water level in Lake Victoria steadily rose from 12 meters to its
current level of 13.32 meters as of April 30, 2020. The level has increased by 1.32 meters in just
6 months, and it is only 0.08 meters below the greatest level ever observed. This was due to
heavy rains that caused rivers and lakes in several parts of Uganda to rise over the limits below
which no settlements or development should take place. This had previously occurred between
1961 and 1964, as well as between 1996 and 1998.
Drought has an impact on the quality of fresh water, according to Khalid et al. (2020), from the
shortage of water to the concentration of toxins in the streams. Drought leads people to use
contaminated water for themselves, their crops (which affects productivity) and their animals,
resulting in crop wilting and low yield rates. In addition, Kanungu district faced the problem of
drought to the extent that people almost eat spear grass due to shortage of food. As a result,
farmers in Uganda must be trained on flood management and correct water management
methods such as tree planting to limit runoffs, with trees acting as carbon sinks as part of the
third pillar of climate wise agriculture, which attempts to reduce greenhouse gas emissions.
8
Rainfall is a seasonal phenomenon with significant inter-annual fluctuation due to climate
changes, extreme climate events, changes in the duration of continuous rain or no rain spells, and
the overall amount of water supplied during each wet spell (Rani et al., 2021). As a result, all of
these parameters are dependent on the characteristics of the watershed and its geographic
location in Uganda, where rainfall is the norm.
The relationship between precipitation and the microbiological quality of lakes such as Mutanda,
Victoria, Kyoga in Uganda is complicated, involving a complex interplay between the type of
water supply and its management (Howard et al., 2016). Unfortunately, rapid and unplanned
urbanization, poor sanitation, erosion, and a lack of upkeep of water catchment regions all
contribute to climate change vulnerability (Maskey et al., 2020). As a result, the infrastructural
and environmental changes, the study timeframe (yearly, season, or day to day), and the rainfall
patterns are all factors to consider (Ogunsanya Dr. et al., 2014).
Local weather, climatic change, and hydrologic conditions, according to (Vinçon-Leite and
Casenave, 2019), are examples of elements that affect water quality in Uganda, nutrient loads,
and eutrophication of water bodies. Rainfall fluctuation promotes cyanobacteria dominance,
exacerbates eutrophication, and affects the stability of lake features such as physical, chemical,
and bacteriological stability, as well as the availability of nutrients.
2.2 Effects of Rainfall Variability on Water Quality
This study considered water quality parameters that affect drinking water standards as per
(Apha., 1976), resulting from human activities that lead to climate change. For example, cutting
down forests for agriculture causes emissions and releases the carbon stored in trees; this leads to
global warming and climate change as greenhouse gas emissions blanket the earth by trapping
the sun’s heat. Water quality parameters that affect drinking water in this study include turbidity,
temperature, calcium, magnesium, phosphates, pH, and electrical conductivity.
2.2.1 Turbidity
According to Ojok et al. (2017), the mean turbidity was higher in the rainy season as compared
to the dry season. Because of soil erosion in the prepared agricultural areas with a loose top layer
of soil, turbidity measurements were greater during the wet season. Particles in the river water
9
could have come from debris swept in by the wind and rain. Variation in turbidity was also
influenced by increased agricultural land usage and built-up intensity in the river watershed at
the start of the rainy season (Mbaye et al., 2015). Furthermore, because the increased water
volume in water bodies may be attributable to resuspended bottom sediments due to high water
flow rates, this is critical to this review paper because it is an indicator of the effect of seasonal
rainfall variability on water quality.
Waithaka et al. (2020) found that water quality metrics during the rainy season had a higher
mean than their similar values during the dry season. He concluded that temporal precipitation
inconsistency significantly affects the pH, turbidity, dissolved oxygen, thermal conductivity, and
total dissolved solids of water ecology. Therefore, this research needs to make combined water
resource management based on what was found to ease water quality among people.
2.2.2 Temperature
According to Fujisaki-Manome et al. (2020), the minimum water temperatures in the winter were
near freezing for all five lakes, with minimum daily values ranging from 0.3° C (Lake Erie) to
2.3° C (Lake Superior) and (Lake Ontario). However, in 2015, there was an uncertain warming
in Lake Superior, Lake Huron, and Lake Erie from late April to early May. He found that the
direct effects of precipitation (snow or rain) on the water surface temperature were rather small
when compared to seasonal fluctuations in water surface temperature. Large snowstorms brought
direct snowfall to open water areas, which were then cooled by the release of latent heat from the
melting snow. Hence, SSA is the region most affected by the increase in temperature.
2.2.3 Calcium
Calcium is essential for both plant and animal bone, nervous system, and cell development
(Kozisek, 2020). The majority of this is obtained by food; drinking water accounts for 50–300
mg per day, depending on the hardness of the water and assuming a daily intake of 2 L. Ca is
non-toxic in food and water. Many metals are less hazardous to aquatic life when there is enough
calcium in the water. As a result, the presence of calcium in water is advantageous, and no Ca
restrictions have been set to safeguard human or aquatic health (Dinaol, 2015).
10
The total hardness of Triveni Lake, according to Khan (Ahmad et al., 2020), ranged from (69.33
to 193.67) mL. Minimum values were reported during the monsoon in the Harsal dam, ranging
from (83.8 to 178) mL. Sulfates, calcium chlorides, and magnesium chlorides are all included in
total hardness. The study concluded that the most common ions in natural water are bicarbonates,
which are primarily related to calcium, to a lesser degree with magnesium, and even less with
sodium.
2.2.4 Magnesium
Magnesium is required for the development of bones and cells in both plants and animals (Ben &
Morgan, 2017). Manganese in water sources gives beverages an unpleasant flavour and stains
sanitary ware and laundry at concentrations greater than 0.1 mL. High quantities are possible due
to reducing circumstances in groundwater and some lakes and reservoirs; up to 1.3 mL in neutral
water and 9.6 mL in acidic water (Shyamala et al., 2008). Manganese in drinking water, like
iron, can develop deposits in the distribution system for lake water users in the area. According
to Mbura (Mbura, 2018), during the dry season, the mean magnesium and calcium ions in
groundwater were 59.1 mL and 130.1 mL, respectively, and during the rainy season, 67.5 mL
and 143.5 mL. The mean magnesium levels were within the guidelines. However, the calcium
levels were determined to be greater than the guidelines for drinking water (Sila, 2019). In
addition, there was a statistically significant difference (p=0.05) in the mean magnesium and
calcium levels in the dry and wet seasons. The research location's high levels of calcium ions
were related to the geology of the area, which consists of limestone with high calcium levels
(Schoeman, 1951). This could potentially be the result of rainwater with magnesium and calcium
ions replenishing the aquifer.
2.2.5 Phosphates
According to Ouma Ouma et al. (2016), study results in the Lake Victoria catchment suggested
0.15-1.04 and 1.17-2.23 mL in the dry and wet seasons, respectively; (Ontumbi et al., 2015)
study in the Sosiani River, Kenya, indicated (0.010-0.018 and 0.750-1.160 mL) in the dry and
wet seasons, respectively. Phosphate levels were found to be high during the wet season due to a
high rate of decomposition of organic materials, as well as run-off, surface catchment, and
contact between the water and sediments from dead plants and animals at the river's bottom
11
(Ouma et al., 2016). He concluded that the river's slow and shallow water is due to the overflow
of discharge from residential areas and sewers.
2.2.6 pH
This is a measure for detecting whether water is acidic or basic. The pH scale runs from 0 to 14,
with 7 indicating neutral, less than 7 acidic, and greater than 7 abase (Tian et al., 2017; Wilbera
et al., 2020). Pollution can alter the pH of water, causing harm to aquatic animals and plants.
Acid deposition degrades the water quality of lakes and streams by reducing pH levels (raising
acidity) and diminishing acid-neutralizing capacity as a result of industrial pollutants
(Papadaskalopoulou et al., 2015). In the aquatic environment, dissolved sulphur with a positive
factor loading is produced by the oxidation of organic and inorganic sulphur compounds. He
concluded that seasonal fluctuations in sulphur were caused by variations in the rate and intensity
of weathering as well as rainfall variability. He found that home wastewater, agricultural runoff,
industrial effluents, and natural hydrologic processes were the main causes of water
contamination. Iron, chemical oxygen demand, and pH (rain season) levels at every research site
were higher than the permitted upper limit for surface water. Because of variations in rainfall,
some sites have more manganese, biochemical oxygen demand, and total dissolved solids than is
permitted.
2.2.7 Electrical Conductivity
According to Alex et al. (2021), Lake Bunyonyi, Uganda's Electrical Conductivity (EC)
measurements did not exceed the WHO's 2500 Siemens per centimetre maximum permissible
limits, as stated in international national drinking water standards and guidelines. Because of
this, the study's conclusions accurately stated that Lake Bunyonyi's water is not strongly ionized
and has a low ionic concentration. The study concluded that while the low EC values at Nyombe
station suggest an unpolluted aquatic environment, the high EC values at Harutinda station may
be caused by pollution from Crater Bay Cottages and Lake Bunyonyi Overland camp.
The study's electrical conductivity findings, according to Wilbera and Kasangaki (Wilbera et al.,
2020), suggested a relative amount of ions present in water. The river Rwimi has the highest EC
(162.831.41 Siemens per cm) compared to the rivers Nyamwamba and Mubuku (146.501.93
Siemens per cm and 103.061.37 Siemens per cm, respectively) in Uganda. The study concluded
12
that the highest EC at Rwimi was due to the use of agricultural and fertilizers, as well as the
discharge of home effluents related to the intake of sewage water; hence, litter.
According to Alex et al. (2021), the nutrient and ammonia readings at Akampene (M2) and
Heissesero (L1) stations were 0.070.01 mL and 0.130.07 mL, respectively. The Total Nitrogen
concentrations at Nyombe (U1) and Rugarambiro (L2) stations were 1.0 0.7 mL and 2.9 2.1 mL,
respectively.
Table 1: Searching the Web of Science (WOS) and Scopus databases using "ClimateChange" AND "Water resources."
Search Platform
Papers from Scopus databases
Papers from WOS
Papers selected in this study
Total
Total no. of used papers
67
40
107
107
Total no. of articles reviewed
287
360
687
687 Papers reviewed
Figure 2: Flowchart for the selection of literature.
Total Number of publications = 107
Scopus
Web of
databases
Science
67 papers
40 papers
Total number
of articles
reviewed
Excluded
687 articles
20 papers
107 papers were used in this study
The flow chart in Figure 2 provides a detailed description. It was confirmed that every search
result was exactly on the topic of climate change and water resources in SSA. The total number
13
of articles reviewed was six hundred eighty-seven. Twenty-five papers were obtained from the
Scopus database, fifty papers from the Web of Science, and around 20 papers were excluded
from this study because they were outside of the search topic and specific objectives. This was
justified for this study to reduce bias in the analysed data and to ease data collection.
Publication in each Country
Figure 3 shows that the number of articles published in the USA, Canada, and Brazil is greater
than 100, which is much more than in other nations. These three countries were responsible for
31.84 per cent, 19.9 per cent, and 18.15 per cent of all publications in this field, respectively. As
a result, linkages between nodes are many and intricate, suggesting that various nations
frequently engage in cooperative relationships. The United States is positioned near the leading
edge of a few nodes in Figure 3, which also suggests that the node holds a significant position
within the network structure.
Figure 3: Publication per country.
Author Analysis
The most frequently published authors were identified and analysed to classify the 687 articles
that are part of the sample. From this analysis, the topics arising more often in the analysed area
stand out. The map represented in Figure 4 groups the authors into four clusters with different
14
colours. This map highlights, further, that climate change and water resources seem to be the
direction the research is taking and where new research opportunities might be arising.
Figure 4: Network Analysis of the author’s trends.
15
Figure 5: Density visualization of the author’s trends.
2.3 Adaptation and Mitigation Measures for Water Availability
2.3.1 Adaptive Measures
To create practical and effective adaptation and mitigation strategies for Africa, it is necessary to
use an interdisciplinary and holistic strategy that involves policymakers, academics,
practitioners, and the public and private sectors (Turyasingura et al., 2022). There are numerous
immediate and long-term implications of climate change on the water on ecosystems and
communities in African nations, ranging from economic and social effects to health and food
shortages, all of which threaten the survival of many African regions (Fuso Nerini et al., 2019).
Vulnerability, on the other hand, differs depending on individual countries’ geographical
location and their ability to mitigate or adapt to changes (Thomas et al., 2019). As a result,
rethinking climate change adaptation on Africa's water resources to adapt to these changes
includes, but is not limited to, water availability through an integrated approach based on African
countries' cooperation; water resource sustainability through efficient management, the creation
of a new supportive network, and a strong African movement of young people and women to
16
assist throughout the implementation of adaptive activities to increase diversity resilience to
withstand with the adverse effects of climate change (Turyasingura et al., 2022). Mitigation
actions focused on the reinforcement of strong institutions and infrastructure in Africa should
also be encouraged (Fuso Nerini et al., 2019).
2.3.2 Integrative Approach to adapt to Continental water Resources Crisis
An integrated strategy for the water resources crisis is a bilateral and international collaboration
between countries, particularly African countries, to address the issue of shared water (M. Fan et
al., 2020). This includes not just cooperation, but also binding agreements, the construction of a
water climate information network among African countries, the use of technology, and effective
communication. This enables countries to consider each other's needs, benefits, advantages, and
disadvantages, as well as cooperation, to solve and gain collectively the outcomes of water
utilization.
Collaboration, depending on the degree of negotiation of every country sharing the same rivers.
Cooperation between countries could provide several benefits, including access to clean water
and the prevention of water pollution (Grech-Madin et al., 2018). The usage of dirty water, on
the other hand, has all the negative repercussions on public health. For example, because of a
lack of bilateral cooperation between the two nations, the river Kasai in the Democratic Republic
of the Congo (DRC) is receiving filthy water from Angola's river (Blessing, 2018).
The water climate information platform is crucial for Africa, and most importantly for local,
regional and continental collaboration specifically when the resources are shared by several
nations (Daron, 2018). Water is a resource that affects every area of the economy, it can be
viewed as a source of collaboration and progress, and hence peace and stability in Africa
(Zougmoré et al., 2018).
However, based on the experience of shared rivers polluted by mining companies, the platform
would face numerous challenges, including structural corruption, impunity culture, influence
peddling, and conflicts of interests (Dandison, 2021), all of which would require the involvement
of impartial international courts to effectively combat.
As a result, international cooperation would improve not just the quality but also the availability
of water for everyone (Shah et al., 2018). It would improve Africa's economy and development
17
by facilitating trade and prudent management of water resources. Non-binding agreements are
one of the most difficult aspects of the integrated approach to getting African countries to
collaborate based on transboundary rivers or lakes. Africa has 94 international water agreements
for cooperation and management of shared water resources, but none of them is in use (Hirwa et
al., 2022). As a result, legally enforceable agreements are useful for enforcing cooperation
between transboundary countries (Schmeier & Vogel, 2018).
Technological initiatives can also help African countries cooperate more effectively both within
and outside of their borders. Traditional and modern water harvesting techniques, water
conservation and storage, and better water recycling and reuse are all approaches that have been
combined (Bolt, 2019). One of the most essential adaptation requirements has been identified as
the significance of building on traditional knowledge relating to water harvesting and utilization
(Vyas & Nath, 2021). As a result, Africans who have a traditional approach to dealing with
climate change issues such as drought and flooding should be bolstered by new and modern
technology to address water scarcity and rainfall availability.
2.3.3 Integrated Water Resources Management and Infrastructure
This is linked to the principles of Integrated Water Resources Management (IWRM), which are
essential for the effective and efficient management of water resources (in both current and
future climates) and must be facilitated by appropriate policies and institutional frameworks (AlJawad et al., 2019). These tactics should be carefully adjusted to the realities of existing
institutional arrangements, local people's livelihood plans, and the current low levels of
infrastructural development.
New and retrofitted water infrastructure, such as surface reservoirs, multipurpose dams, soil
moisture conservation techniques, natural wetlands, rainwater harvesting for storage, rainwater
harvesting for infiltration, urban green spaces, conjunctive use of surface and groundwater,
managed aquifer charge, and source water, is listed as a priority for adaptation action in over 68
per cent of all Nationally Determined Contributions (NDCs) (Wang et al., 2019).
2.3.4 Water harvesting
18
Water harvesting is the process of collecting rainfall directly from the sky (Tu et al., 2018).
Rainwater can be collected and stored for immediate consumption or returned into the
groundwater system. Rain is the first form of water in the hydrological cycle that humans are
aware of, making it a key supply of water for humanity. Rainwater harvesting entails absorbing
runoff from rooftops, catchment runoff, seasonal floodwaters from local streams, and watershed
management (Bennett & Barton, 2018). Therefore, there is need for rain water harvesting in
Uganda especially Kigezi and Northern regions to keep water during dry seasons for both
domestic use and irrigation to increase productivity as shown in (Figure 6).
Figure 6: Conceptual sketch of rooftop rainwater harvesting system
Source: http://www.eng.warwick.ac.uk/DTU/rainwa.
2.3.5 Other Adaptive Measures
Wetland ecosystems should be conserved, maintained, or rehabilitated. Wetlands are important
for adaptation because they act as a buffer against floods and other extreme weather events, as
well as purifying water (J. Fan et al., 2021). Drought resistance and water scarcity can both be
improved by co-management, which allows a region's overall water storage capacity to be
increased (Zarei et al., 2020).
19
Protection water efficiency and demand management are two issues that need to be addressed.
Progressive pricing, hydrological zoning, water licensing and permits, shifting usage from peak
to off-peak periods, and water conservation requirements in building codes are all examples of
water conservation measures (Stip et al., 2019). Seawater desalination, solar water distillation,
fog harvesting, inter-basin transfers, groundwater prospecting and extraction, boreholes and tube
wells, and water recycling and reuse are examples of alternative water sources (Conca, 2021).
Integrated watershed management: Watersheds are natural environmental and land management
units that influence a country's overall health. Poor ecosystem management in watersheds has
resulted in and will continue to result in reduced watershed functioning, which in sensitive areas
can lead to ecosystem collapse (Pourghasemi et al., 2020).
If appropriate policies are enacted, watershed management is often successful. Watershed
management necessitates the use of the three "Ps": planning, partnership, and stakeholder
participation (Karambelkar & Gerlak, 2020). Public-private partnerships are becoming a more
typical strategy to increase management success. This bring these two sectors together to work
toward a common goal, allowing each to benefit from the skills and resources of the other to
more effectively fulfil management goals. Watershed management is mainly based on the study
of watersheds, which is a branch of hydrology that analyses the effects of vegetation and land
management on water quality, erosion, and sedimentation (Ranjan et al., 2020). Many
environmental and natural resource management decisions are being predicated on watershed
management concepts to increase diversity resilience, as it is becoming increasingly clear that
land management decisions cannot be undertaken in isolation (Turyasingura, Mwanjalolo, &
Ayiga, 2022).
2.4 Mitigation Measures
Water availability is a difficult issue in Africa that necessitates strong institutions, infrastructure,
and technology for successful water management, whether transboundary or within the country
(Ngene et al., 2021). Most technology-driven climate change mitigation strategies necessitate
investing in reducing emissions from water infrastructures, such as drinking water supply, waste
and stormwater treatment, and water pumping for agriculture and other purposes. Different water
20
and sanitation-related mitigation techniques should be considered for planning and management
processes in this context (Otingi, 2019).
Infrastructure is one of the most significant problems, as are strong institutions to address the
issue of water availability, a specific program to fund and change the mindset of leaders, and the
battle against other concerns such as corruption and impunity for this approach to succeed.
Infrastructure, for example, will help to distribute water in the Sud-Sahara region using new
technologies such as irrigation systems for large rivers such as the Congo River and other rivers,
as well as manage water that falls into the sea internally to avoid waste and maximize water
availability for African people, lands, and local communities (Baylouny & Klingseis, 2018).
The greatest way to prepare for climate change in the extraction, delivery, and treatment of water
is to invest more across Africa in water infrastructure to boost the positive functions and
decrease the negative impacts of water. Nature-based solutions (NBS) are a critical way to go
beyond business as usual to address many of the world's water concerns while also providing
additional advantages that are critical to all elements of sustainable development (Alpízar et al.,
2020). NBS use or mimic natural processes to increase water availability (for example, soil
moisture retention or groundwater recharge), improve water quality (for example, natural and
constructed wetlands), and reduce the risks associated with water-related disasters and climate
change.
3. Implications for the Future Research
This report suggests that county governments develop a strategic plan for water quality
management based on priorities that reflect an awareness of the economic and social
implications of contaminated water. Specific procedures for delivering community-level drinking
water monitoring capabilities should be devised.
A regulatory framework with a combination of acceptable water quality objectives and effluent
management is required. This will be crucial for the 2.1 million people with no access to safe
drinking water, of which more than 884 million individuals have no basic drinking water
services and who rely on surface water to survive. By incorporating both traditional and modern
21
expertise, like water harvesting techniques, water conservation and storage, and improved water
recycling and reuse, the continent's adaptive capacity to climate change will be enhanced.
The management of surface and groundwater, irrigation systems, the continuum system of water
storage reservoirs, infrastructure for water transportation, efficient supply chains for both
agriculture and drinking water, and assurance of water availability, sanitation, access, and
utilization should all be improved. To develop both small-scale and large-scale water
infrastructure, increasing capital investment in water resource management across Africa is the
best adaptation strategy.
4. Conclusion and Recommendations
Based on the findings of several reviewers, it has been determined that seasonal rainfall
unpredictability brought on by climate change has an overall negative impact on the quality of
water in various water bodies. The fact that the mean values for certain of the physicochemical
variables under consideration fell within the WHO's acceptable limits for drinking water and
recreational waters, respectively, provides further evidence for this. This is demonstrated by the
evaluated sample values for temperature, magnesium, pH, DO, turbidity, EC, nitrites, nitrates,
and ammonia that were below the acceptable limits and may not pose a threat to the health of
either people or aquatic life. As a result, even while the measured physicochemical parameters
showed notable temporal variations, dramatic variances were observed in several of the study
stations/areas. The results of this investigation showed that pH, turbidity, dissolved oxygen,
thermal conductivity, and calcium are all considerably impacted by climate change. To discuss
the future of sustainable food production in the face of climate change and variability in the
current and future centuries, complex and multidisciplinary solutions involving all stakeholders
are required at the local, national, regional, and global levels. These stakeholders include
researchers, policymakers, the private sector, national government, international agencies, FAO,
World Bank, donors, World Food Program, men, women, and youth. Climate change has an
impact on water, the food chain, and the food environment; it is a multidisciplinary issue that
necessitates a multidisciplinary approach to designing and implementing potential solutions. Coauthor-ship is needed to increase publications and improve the water resources in SSA.
22
The following are recommendations to African policymakers and NGOs based on the study's
findings. Strategies are required, which necessitate various resources such as financial and
human resources, as well as political support for the projects. Local and national governments
should consider policies and programs to address the local government's lack of financial and
human resources.
In the face of climate change, African planners should seriously consider integrating and
institutionalizing adaptation with development initiatives. It should not be an afterthought or an
add-on. Based on the background and literature assessment, there is currently minimal proof of
this, leaving a gap to fill. Long-term policies that satisfy local developmental goals and handle
water resource management problems should be implemented, with the government and NGOs
playing a key role. This will ensure that, despite the uncertainty of future climate projections,
local governments have the necessary adaptive resilience in place to ensure that the communities
they serve have adequate clean water to meet their developmental needs.
ACKNOWLEDGEMENTS
Each author has provided permission for the results of this research study to be published.
Conflict of Interest
The authors state that they have no competing interests in the publication of this research.
Conflict of Interest
Data is available at the request of the author.
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