Flood risk assessment and mapping in Abidjan district using multi-criteria analysis (AHP) model and geoinformation techniques, (cote d’ivoire)
© Danumah et al. 2016
Received: 17 February 2016
Accepted: 11 May 2016
Published: 20 May 2016
Flood is one of the most destructive natural disasters of climate change effects in West Africa. Flood risk occurrence is a combination of natural and anthropogenic factors, which calls for a better understanding of its spatial extent. The aim of this paper is to identify, and map areas of flood risk in Abidjan district.
This work is based on the integration of multi-criteria data including slope, drainage density, type of soil, Isohyet, population density, land use and sewer system density within ArcGIS interface. The resulting AHP flood risk map shows that areas under high and very high flood risk covers 34 % of the study area.
The Analytic Hierarchy Process (AHP) method used as a multi-criteria analysis allowed the integration of several elements under two criteria, hazards and vulnerability, for flood risk assessment and mapping. Results revealed that, Abidjan district is heavily exposed to the risk of flooding. Eight out of thirteen (8/13) municipalities within the district are at a high risk of flooding which calls for decision makers to effectively develop strategies for future flood occurrences within the Abidjan district (South of Côte d’Ivoire).
KeywordsFlood risk Multicriteria analysis Remote sensing Geoinformation techniques Abidjan Cote d’Ivoire
Natural disaster is considered to be the biggest challenge that needs to be examined at global, regional and local scale. Climate change may increase the frequency, magnitude and the seasonality of extreme events such as flood, which means that concurrent flood hazard of importance to urban flood risk management, may occur more frequently in the future (Duan et al. 2015; Huong and Pathirana, 2013; Pedersen et al. 2012). Urbanization is also an important factor to increased flood risk in the cities through increasing runoffs which affect communities’ downstream (Cloke et al. 2013; Duan et al. 2016). Floods are among the most devastating natural hazards in the world, claiming more lives and causing more property damage than any other natural phenomena (Duan et al. 2014; Kebede, 2012; Wang et al. 2011; Forkuo, 2011; Yahaya et al. 2010; Yalcin and Akyurek 2004; Hapuarachchi et al. 2011; Tsakiris, 2014). As a result, floods are one of the greatest challenges to weather prediction (Jeyaseelan, 2003).
In Africa, the situation is very likely to worsen as the intergovernmental panel on climate change (IPCC) has projected higher frequencies and intensities of floods and droughts (IPCC, 2007) for the continent as a consequence of climate change. Floods and flash floods cause loss of life and property damage (Musungu et al. 2012). From 1900 to 2006, floods in Africa killed nearly 20,000 people, and also affected nearly 40 million more, with estimated damages of about 4 billion USD according to the ICSU Regional Office for Africa (2007). Flood is one of the most destructive natural disasters of climate change effects in West Africa (Kouassi et al. 2008). The demands of the growing population and related urbanization lead to severe land use change (Franci et al. 2015) and increasing flood occurrence in West Africa.
Urban floods result from blocked or inadequate storm sewers and are due to increased urbanization (Ajin et al. 2013). Urban areas have high risk of flash flooding due to the presence of large impervious areas and sometimes inefficient drainage system (Chen et al. 2009; Huong and Pathirana, 2013; Sowmya et al. 2015). Several additional phenomena commonly contribute to urban flooding, such as limited conveyance capacity of urban channels and rivers, as well as drains and sewers and infiltration–inflow, and decades of urban development without upgrading of the drainage infrastructure (Pedersen et al. 2012). The rapid growth often results in a poorly planned urbanization making urban populations increasingly vulnerable to floods.
While the primary cause of flooding is excessive rainfall (Kim and Kim, 2014), there are many other causes resulting from human activities such as: land degradation; deforestation of catchment areas; sprawl and increased population density along riverbanks (Prasad et al. 2016; Billi et al. 2015; Mbow et al. 2008; Forkuo, 2013), poor land use planning, zoning, and control of flood plain development; inadequate drainage, particularly in cities, and inadequate management of discharges from river reservoirs.
Hence, assessing and predicting floods risk has become essential to offer appropriate solutions for flood and sustainable environmental management. Flood hazard mapping is a vital component for appropriate land use planning in flood areas and mitigation measures (Bhatt et al. 2014). It provides accessible charts and maps which can be read easily and therefore, facilitates the identification of risk areas by planners and this enable them to prioritize their mitigation efforts (Bapalu and Sinha, 2005; Forkuo, 2011; Wang et al. 2011; Ajin et al. 2013).
Flood management is necessary not only because flood imposes huge damages on the society, but for the optimal exploitation of the land and its proper management. This cannot become technically feasible without effective flood hazard and risk maps (Bhatt et al. 2014)
More recently in Cote d’Ivoire, populations have experienced increasingly important phenomena of floods, with its effects such as death, damage to property and population exodus. Heavy rainfall is the main natural hazard which causes loss of many lives; destruction of infrastructures, and the displacement of people during the rainy season in Abidjan. Statistical analysis done in 2013 shows that 26 % of the district of Abidjan is flood risk area and 21, 13, and 15 people died in 2009, 2010, and 2011 respectively due to floods (OCHA, 2013). Also the result indicates that, a total of 80,000 people live in areas that are subject to risk of flooding in the district with 40,000 people in Cocody, 12,500 people in Abobo, 10,000 in Adjame, 9,500 in Yopougon and 8,000 in Attecoube communes (OCHA, 2013). However, the use of multi-criteria evaluation approach to flood risk assessment and mapping in Cote d’Ivoire is still rare (Savane et al. 2003; Saley et al. 2005; Saley et al. 2013). Extreme rainfall data analysis for many years were based on determining break on the times series using some statistical methods such as Pettit and Buishand test (Lubes-Niel et al. 1998), application of Nicholson indices to bring out the wet and dry period in case of rainfall variability and shows general trend and inter-annual behavior (Brou, 2005; Savane et al. 2003; Goula et al. 2006; Kouassi et al. 2008).
Flood risk occurrence is a combination of natural and anthropogenic factors, which means that there is the need for knowledge about spatial extent of flooding areas, using multi data as drivers becomes a potential source for more reliable flood management and mitigation. For all that, Multi-criteria analysis (MCA) approach has become widely used (Wang et al. 2011; Sowmya et al. 2015) to solve complex problems and to assess flood risk. Many methods have been proposed for multi-criteria decision making. Analytic Hierarchy Process (AHP) developed by Saaty (1980) is one of the best known and most widely used MCA approaches (Orencio & Fujii, 2013; Yahaya et al. 2010). AHP is used to solve a broad range of multi-criteria decision-making problems, with the pairwise comparison matrix calculating the weights for each criterion considered (Yalcin, 2008; Orencio & Fujii, 2013; Le Cozannet et al. 2013; Pourghasemi et al. 2014). AHP assumes complete aggregation among several criteria and develops a linear additive model. The uniqueness of applying AHP in different studies helps in modelling situations of uncertainty without losing subjectivity and objectivity of any evaluation measure.
Of late, considerable attention has been given to the use of AHP in natural hazard (earthquake and flood) assessment but more in flood management in various studies: (Savane et al. 2003; Yahaya et al. 2010; Cozannet et al. 2013; Orencio & Fujii, 2013; Saley et al. 2013; Chakraborty and Joshi, 2014; Pourghasemi et al. 2014; Papaioannou et al. 2015; Nejad et al. 2015). It has been shown from these series of papers that AHP has the ability to assess and map flood risk with good accuracy. However, it is based on expert opinions and thus may be subjected to cognitive limitations with uncertainty and subjectivity (Pourghasemi et al. 2014).
The significant research gap identified by this study is that recent scientific work undertaken in the district of Abidjan concentrated on rainfall variability during past and current condition as flood risk drivers within two communes of Abidjan: Attecoube and Abobo (Savane et al. 2003; Hauhouot, 2008). This is a piece-meal approach and does not provide a solution to the problem of flood occurrence within the entire district. Other studies (Kouame et al. 2013; Jourda et al. 2006; Ahoussi et al. 2013) in the district did not directly focus on flood but pointed out the inefficiency of the drainage network and impervious area which are part of the main drivers of floods. However, these studies are fragmented and did not consider the entire district and multi criteria as input to link climate change and flood occurrence, no studies have yet been undertaken to evaluate and map flood risk at Abidjan district level.
The aim of this paper was to identify, and map areas of flood risk based on several factors that are relevant to flood risks in Abidjan district. For this purpose, assessment process of flood risk was conducted under hazard and vulnerability concepts within analytic hierarchy process (AHP) framework.
To the south by the Atlantic Ocean;
In the southwest by the Department of Dabou;
To the west by the Department of Grand Lahou;
To the north by Agboville Department;
In the south-east by the Department of Grand-Bassam;
In the east by the Department of Alepe.
Long dry season from December to April;
Long rainy season from May to July;
Short dry season from July to September;
Small rainy season from October to November.
High annual rainfall was recorded in Abidjan district during the period 1960–2012 and ranged from 2800 mm in 1963 to 1020 mm in 1990 with an average of 1910 mm. Generally, in 1960s, the annual rainfall ranged between 2000 and 3000 mm. After 1987, there has been a drop in rainfall and this has oscillated between 1500 and 2200 mm, a reduction of more than 500 mm compared to the 1960s.
Also, observation of highest average monthly rainfall from 1960 to 2014 shows that June and sometimes May are the rainiest month of the District of Abidjan. Secondly, the temperature curve shows that the months of March and April are the hottest months with a monthly average temperature above 27 °C.
Analysis of the annual rainfall and the heavy rainfall month
Data and material
In this study, various basic thematic layers were created from different source including map, field study, satellite image and secondary data based on multi-criteria analysis method. Using ArcGIS, Mapinfo and eCognition software tools, several maps were prepared including slope, soil, rainfall distribution, drainage density, demography, drainage system and urban structure type (land use). The drainage density and administration map were derived from the national center of cartography and remote sensing (CCT) and we extracted them using clip tools. Soil map was digitized based on national soil map done by ORSTOM and validated with field sample using map info software and GIS. The slope map was extracted from Aster DEM with resolution 30 m using spatial analyst tools. The rainfall distribution map was prepared from the national meteorological agency (SODEXAM) using Inverse distance weighted method (IDW). The urban structure types (land use) map was extracted from Spot 5 satellite imagery using eCognition software tools by applying oriented based image analysis. Population data obtained from the National Institute of Statistic (INS) was used to generate the population density map. Sewer system density map was also elaborated based on data collected from field and overlaid with the Water Company sewer system map.
AHP model processing
Breaking a complex unstructured problem down into its component factors
Development of the AHP hierarchy
Paired comparison matrix determined by imposing judgments
Assigning values to subjective judgments and calculate the relative weights of each criteria
Synthesize judgments to determine the priority variables
Check consistency of assessments and judgments
One of the key points in AHP is calculation of consistency ratio (Saaty 1980). If consistency ratio is less of 0.1, then the mentioned matrix can be considered as an acceptable consistency.
However, AHP approach can be summarized in three big levels.
All elements under each criterion were set based on literature and the definition of hazard (physical phenomenon, natural and non- manageable) and vulnerability (degree of susceptibility and exposure due to man-made) concepts that used in this study.
Saaty scale for various elements comparison Saaty (1980)
Judgment of preference
Two factors contribute equally to the objective
Experience and judgment slightly favour one over the other
Experience and judgment strongly important favour one over the other
Very strongly important
Experience and judgment strongly important favour one over the other
The evidence favouring one over the other is of the highest possible validity
2, 4, 6, 8
Intermediate preference between adjacent scales
When compromised is needed
Development and prioritization matrix
determine the eigenvectors (Vp) of each criterion for each item is described in equation 1.
calculate the weighting coefficients (Cp), the formula is given in equation 2.
normalize the matrix by dividing each element by the sum of a column of the column ;
averaging each line to determine the priority vector [C];
multiply each column of the matrix by the priority vector corresponding there to determine the overall priority [D];
Divide each global priority by the priority vector corresponding to it to determine the rational priority [E];
Determine the maximum Eigen value (λmax) by equation 3:
Calculate the consistency index (CI) expressed by equation 4:
Determine the consistency ratio (CR) using equation 5. The ratio of coherence can be interpreted as the probability that the croak is completed in a random manner. In fact, the responses often have a certain degree of incoherence. The AHP method does not require that judgments are consistent or transitive, indeed, Saaty (1980) has defined the value of consistency ratio. In the case where the value of consistency ratio is less than 10 %, the judgment is consistent and when it exceeds 10 %, the assessments may require some revisions.
AHP hazard map
Normalization of hazard matrix
∑ of rows
[D] = [A]* [C]
[E] = [D]/[C]
AHP vulnerability map
Mapping of flood risks
In this study, weight were assigned to the different thematic indicators classes and layers based on their relative influence and contribution to the hazard and vulnerability. The overlay technique was employed to the indicators to determine hazard and vulnerability first of all and by crossing hazard and vulnerability to obtain the goal which is flood risk area identification and zoning. All processes were done in ArcGIS using raster calculator in spatial analyst tools.
Results and discussion
Abidjan district flood risks was evaluated using multi-criteria analysis approach specifically AHP, combining vulnerability and hazard assessment. The flood risk was around 70 % when the study summed moderate, high and very high classes. The analysis shows that 34 % of the study area is flood risk zone, but from critical analysis most of the communal areas are high flood risk areas whiles the low and very low classes are vegetation areas with few population and urbanization. Eight out of thirteen (8/13) municipalities of Abidjan district are at a high risk of flood and therefore need optimal design of technical solutions from society. The reliability of the resulting flood risk map which gives acceptable results is based on input parameters, historical and recorded flood data. Results from the hazard map showed 32 % of the area as high hazard risk with rainfall and slope being the most significant causative factors in flood occurrence. The vulnerability map also showed 24 % of the area as highly vulnerable to flood with population density and land use through urban structure types as relevant factors in flood risk.
Multi-criteria analysis (AHP) adopted for this study within Abidjan district facilitated multi-source data combinations, which constituted a real advantage. The method is based on physical, hydrogeological and anthropogenic parameters. The parameters used in the flood risk map include slope, drainage density, soil, rainfall, system of evacuation, demography and land use which are the combination of hazard and vulnerability require interpolations to allow their crossing. Results indicated that AHP can be used as an efficient method to assess and map flood risk in GIS environment. AHP methodology allowed a better understanding of all the element or indicator contributions in flood process based on weight given to each of them. However, coming from different sources, interpolating and crossing data in GIS at the same resolution are factors of some bias during the processing and analysis. Normalization and weighted steps of these parameters are important to reduce bias and uncertainty in the final result. Also, AHP method shows some failure due to the subjectivity in choosing the value of the indicator weighting from arbitrary judgments of experts (Papaioannou et al. 2015). This weakness is reduced by the consistency ratio test of judgments. Saaty, 1980 provides a consistency ratio threshold which must be less than 10 % to make a coherent judgment. The value of consistency ratio as part of this study is 3 % and the study concludes that, its judgments can be considered coherent.
But the use of other standardization approach such as linear instead of natural break (Jenks) can be improved for map comparison and accuracy assessment purposes. This methodological approach was inspired by various previous work (Saley et al., 2013; Saley et al. 2005; Mbow et al., 2008; Cozannet et al., 2013; Orencio, and Fujii, 2013; Chakraborty and Joshi, 2014; Pourghasemi et al., 2014; Papaioannou et al., 2015; Nejad et al., 2015) and it is clear that the risk of flooding is linked to combined action of many different factors under two criteria: hazard and vulnerability. However, the results can be improved by the development of urban structure types (UST) through oriented based image analysis (OBIA) method using high-resolution images (Ikonos, RapidEye, QuickBird) to raise classification details on urban morphology with good accuracy. Hydrologic modeling in 2D or 3D for efficient processing and management of floods (Zazo et al., 2015) can be added.
The multi-criteria analysis approach used in mapping areas at risk of flood required a combination of hazard map (slope, drainage, soil type and isohyet) and vulnerability map (population, sewer system density and UST). The resulting map indicates that, 34 % of the study area is of high flood risk. In view of the results obtained, the Abidjan district is heavily exposed to the risk of flooding. Thus, this resultant map can serve as a guideline to decision makers for potential anticipatory measures, better land use planning and flood risk management under climate change.
Strict measures needs to be taken concerning the uncontrolled urbanization and the occupation of areas that has proximities of rivers and places of clogged water passages to be implemented by policy makers in order to prevent more significant damages. The identified areas as a high risk require more detailed mapping with the use of high spatial resolution satellite images to constitute a research perspective that can improve and refine the results obtained. This study also put in evidence the reliability and the irrefutable role play by geoinformation techniques in natural disaster assessment which requires the contribution of multi-source data.
We are grateful for the financial support provided by the German Federal Ministry of Education and Research (BMBF) under the auspices of the West African Science Service Centre for Climate Change and Adapted Land Use (WASCAL) project. We are also grateful to the WASCAL GRP-CCLU, Kumasi, Ghana.
JHD collected data from various sources, performed the assessment and drafted the manuscript. BMS, SNO, JS, FKK provided skills development, comments and suggestions during data generation, analysis, and results interpretation. MT provided software and methods guidance to develop urban structure type (UST) classification. AK and LYA helped to draft the manuscript. All authors read and approved the final manuscript.
I declare and certify that this research article is for pure academic purpose. In fact, it is one specific objective of my PhD research. Therefore, there is a non-financial competing interest.
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
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