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Participatory approach for flood risk assessment: the case of Yeumbeul Nord (YN), Dakar, Senegal

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Flooding has emerged lately as a major threat for poor people in the suburban area of Dakar (Senegal), a densely populated area. In this region, flood events are mainly controlled by rainfall intensity and groundwater level fluctuations. To assess flood risk at a neighbourhood level, accurate data on flood extent, exposure and vulnerability is required. The objective of the present study is to obtain these data combining remote sensing data and local knowledge. Field work data were collected through interviews with inhabitants. About 500 respondents were surveyed with the support of a local association and very detailed mapping was carried out to clearly identify elements at risk. Information collected at the household level concerns: 1) socio-economic data, 2) information on the property, 3) flooded houses and 4) strategies of risk reduction. This research demonstrates that local knowledge is an important tool to obtain accurate data useful for understanding flood hazard and vulnerability patterns. It provides quantitative data at the household level that can be used to complement conventional GIS and remote sensing data.
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Reference
Participatory approach for flood risk assessment: the case of
Yeumbeul Nord (YN), Dakar, Senegal
SY, Bocar, et al.
Abstract
Flooding has emerged lately as a major threat for poor people in the suburban area of Dakar
(Senegal), a densely populated area. In this region, flood events are mainly controlled by
rainfall intensity and groundwater level fluctuations. To assess flood risk at a neighbourhood
level, accurate data on flood extent, exposure and vulnerability is required. The objective of
the present study is to obtain these data combining remote sensing data and local knowledge.
Field work data were collected through interviews with inhabitants. About 500 respondents
were surveyed with the support of a local association and very detailed mapping was carried
out to clearly identify elements at risk. Information collected at the household level concerns:
1) socio-economic data, 2) information on the property, 3) flooded houses and 4) strategies of
risk reduction. This research demonstrates that local knowledge is an important tool to obtain
accurate data useful for understanding flood hazard and vulnerability patterns. It provides
quantitative data at the household level that can be used to complement conventional GIS
and remote sensing [...]
SY, Bocar, et al. Participatory approach for flood risk assessment: the case of Yeumbeul Nord
(YN), Dakar, Senegal. WIT Transactions on The Built Environment, 2016, vol. 165, p.
331-342
DOI : 10.2495/UW160291
Available at:
http://archive-ouverte.unige.ch/unige:86254
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Participatory approach for flood risk
assessment: the case of Yeumbeul Nord (YN),
Dakar, Senegal
B. Sy1, C. Frischknecht1, H. Dao2, G. Giuliani4, D. Consuegra1,3,
S. Wade5 & C. Kêdowidé6
1Department of Earth Sciences, University of Geneva, Switzerland
2Department of Geography and Environment,
University of Geneva, Switzerland
3School of Business and Engineering Vaud, Switzerland
4Institute for Environmental Sciences, University of Geneva, Switzerland
5Institute of Earth Sciences, University Cheikh Anta Diop, Senegal
6African Urban Management Institute, Senegal
Abstract
Flooding has emerged lately as a major threat for poor people in the suburban area
of Dakar (Senegal), a densely populated area. In this region, flood events are
mainly controlled by rainfall intensity and groundwater level fluctuations.
To assess flood risk at a neighbourhood level, accurate data on flood extent,
exposure and vulnerability is required. The objective of the present study is to
obtain these data combining remote sensing data and local knowledge. Field work
data were collected through interviews with inhabitants. About 500 respondents
were surveyed with the support of a local association and very detailed mapping
was carried out to clearly identify elements at risk.
Information collected at the household level concerns: 1) socio-economic data,
2) information on the property, 3) flooded houses and 4) strategies of risk
reduction.
This research demonstrates that local knowledge is an important tool to obtain
accurate data useful for understanding flood hazard and vulnerability patterns. It
provides quantitative data at the household level that can be used to complement
conventional GIS and remote sensing data.
Keywords: flooding risk, P-mapping, P-GIS, Dakar, Yeumbeul Nord (YN).
www.witpress.com, ISSN 1743-3509 (on-line)
WIT Transactions on The Built Environment, Vol 165, ©2016 WIT Press
This paper is part of the Proceedings of the 5 International Conference
th
on Flood Risk Management and Response (FRIAR 2016)
www.witconferences.com
doi:10.2495/UW160291
1 Introduction
Natural disasters caused by natural phenomena, whether geological, hydrological
and climate affect more and more people in the world with floods constituting the
primary cause across the globe (Wang et al. [1]). In the period between 1900 and
2016, there were 910 flood disasters in Africa alone, killing 27,051 people,
affecting 71 million people, and causing 7.9 million USD of economic losses (EM-
DAT [2]). For Senegal itself, in the past 30 years (1980 to 2009 inclusive) over
900,000 people were affected, 45 were killed, and damage costs were estimated to
be more than 142 million USD (Gouvernement du Sénégal [3]). The Dakar region
is the most affected region, where several severe floods occurred in 1989, 1996,
2001, 2005, 2009, and 2012, affecting particularly the suburbs, the 2009 event
being the worst.
Many efforts have been tempted by the Government and local authorities to
deal with and minimize the negative impacts of frequent floods, consisting of
structural (construction of canalization and retention basins) and non-structural
measures (relocation). But flooding within sub-urban of Dakar still represents a
major problem for the local government. And the lack of information on hazard
and vulnerability related to floods does not allow to produce quantitative
assessment on flooding risk, necessary for the implementation of a flood risk
reduction policy and a sustainable development.
Flood risk assessments are usually carried out by three approaches: 1) field
work, 2) remote sensing analysis and/or 3) hydraulic modelling. As such, these
approaches present some specific limitations, related either to the time required to
carry out field work, weather conditions (Brivio et al. [4]) influencing the quality
of satellite images or the lack of images covering the area and the uncertainties on
results obtained by hydraulic modelling (Pappenberger et al. [5]), which is very
sensitive to the accuracy of basic data. Therefore, the main purpose of this study
is to obtain accurate data on flood risk related parameters combining remote
sensing data and local knowledge. As mentioned by Tran et al. [6], local people
have a better understanding of their surroundings and can help identify areas prone
to floods. Moreover, it is also known that local knowledge can improve the
accuracy of data (Dunn [7]). Therefore, a participatory approach has been used
implying participatory mapping (P-mapping) and participatory GIS (P-GIS) in
order to consider and integrate local knowledge on floods.
2 Study area
The area under investigation is the municipal district of Yeumbeul Nord (YN), one
of the 16 municipal districts of the city of Pikine. It is located in the suburbs part of
the capital city Dakar in Senegal (figure 1). The total area of this municipal district
covers about 9 km2 divided into 82 major neighbourhoods (Kêdowi and Cissé
[8]). According to the 2013 census of the National Senegalese Agency for Statistic
and Demography, the total population is about 168,379 inhabitants (ANDS [9]). It
is one of the most populated districts of Senegal, with a population density of
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approximately 18,700 habitants/km2. The study area is characterized by lowlands
with elevations less than 20 m.
Floods occurring in YN are due to the combination of natural (rainfall
variability, groundwater position, topography, hydrology and lithology), and
anthropogenic factors related to uncontrolled urbanization and soil impermeability
(Mbow et al. [10]).
Figure 1: Map of Yeumbeul Nord and the 82 neighbourhoods.
3 Methodology
Acquisition of data related to floods in YN was achieved using remote sensing and
ground based data (figure 2). Satellite data were used to obtain a preliminary land-
use map including the spatial distribution of houses and the spatial distribution of
the 2009 flood extent. Then, information was completed using local spatial
knowledge. This has been achieved through active household survey and
interviews, participatory-mapping and participatory-GIS. The interviews yielded
socio-economics characteristics, physical exposure, flood depth and event
duration, as well as strategies of flood risk reduction applied at the ho usehold level .
In this study, the participatory approach refers to mapping and collecting
information on flooding from the local population. P-mapping helped getting
detailed location of elements at risk and areas of water. Finally, P-GIS was carried
out in order to cross-check results obtained from the remote sensing data,
interviews and P-mapping.
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Figure 2: Chart flow of the data acquisition process.
3.1 Remote sensing data
In order to obtain our first land use map over the study area, we used high
resolution satellite images (January–July, 2015) available on Google Earth®. The
location of different land use categories (infrastructures, agricultural area, water
bodies, etc.) and each house were photo-interpreted and digitized in Google Earth.
We then used Global mapper 15® for the rapid conversion of the KML files into
shapefiles with the reference system UTM (Zone 28N). Finally, we have imported
our preliminary database in ArcGIS 10® where a unique identification number was
attributed for each house.
The flood extent of the 2009 event has been obtained by comparing a reference
high resolution satellite image before the flood (March 11) and after (October 14)
obtained in Google Earth using its historical satellite dataset.
The Google Earth high-resolution imagery archive remains a largely
unexploited resource for the analysis and description of the Earth’s land surface
(Potere [11]). The high-resolution images (2.5 m resolution) used in this analysis
come from Digital Globe’s (e.g. Quick Bird—Ikonos) satellites.
It can be seen in figure 3 that some areas are covered with clouds causing a
partial loss of information.
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Figure 3: Free Google Earth® images used for flood extent mapping.
3.2 Household survey
Interviews were carried out on the basis of a questionnaire developed specifically
for this study. It consisted of five main sections: 1) respondent’s characteristics,
2) information on the property, 3) flooded houses, 4) socio-economic data and
5) strategies for flood risk reduction. The target of the interview was the household
head and when the household head was not available, the spouse or a person
having memories of the floods was surveyed. The questionnaires were conducted
by teams composed of young adults from the local associationRéseau
d’Information d’Education de Communication maternité de Yeumbeul” and the
students from the Institute of Earth Sciences at the University of Dakar and each
team was attributed to a specific neighbourhood for a total of 54. They were trained
before going to the field.
Moreover, the questionnaire was first administrated in a test study lasting one
day and implying 50 households. Feedback obtained from these participants and
from the investigators allowed to ensure that wording was comprehensible
and added other aspects not taken into account. In view of the low levels of
education of respondents and the high illiteracy rate, the interviewers were called
to translate the French version to the most widely spoken language in Senegal the
Wolof. Each survey lasted 30 to 45mn during which the respondents actively
interact with the investigators. Finally, 502 households were surveyed (figure 4).
In complement to the interviews, the respondents also provided information on
the water depth affecting their house during the past flood events, when possible.
With a handled GPS and the support of a paper map showing the details of each
investigated neighbourhood, investigators were instructed to identify the house on
the map and take GPS coordinates for cross checking.
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Figure 4: Distribution of the surveyed households.
3.3 Participatory mapping and participatory GIS
The P-mapping was carried out in the 82 neighbourhoods with the support of the
local association and the householders interviewed. These local representatives
brought their knowledge at three levels of the dataset. The first level was to verify
the accuracy of the preliminary land-use map obtained with remote sensing data.
The second level concerns the precise mapping of areas of water (lake, outlet,
retention basin) and the third level was to achieve a detailed survey of important
infrastructures of the area (e.g. health centres, schools, recreation areas, public
service etc.). Handled GPSs, and mobile GIS were used to carry out the detailed
mapping of the key infrastructures and water bodies. In complement to the update
of the land use map, the data obtained on each household were combined with the
GIS database existing on houses. To do this, the information gathered in the
household survey was included into ArcGis 10® by joining the excel sheet
containing the survey data and the initial GIS layer of houses based on a common
identifier which was the name of the houses (each house had the same name in the
Excel sheet and the initial database). This operation was carried out with the help
of the interviewers in order to make sure that the merging of the two datasets was
correctly done.
4 Results
4.1 Land use
The resulting land-use map of the study area was obtained from remote sensing
data and then verified with the local teams and improved by integrating local
knowledge. The result shows 7 major land cover types: forest, agriculture,
buildings, infrastructures, water bodies, livestock farming, and recreation (figure
5). The area used for buildings and infrastructure is the largest with about 47%.
The other including roads, canalisations and the nature were estimated about 33%.
Water bodies were estimated about 10%. The proportion of agriculture land is
5.8%. Forest accounts for 3.6%. The percentage of recreation area is 0.56 and
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livestock farming is 0.48 (table 1). This classification shows that the study area is
highly urbanized.
Figure 5: Land-use map.
Table 1: Land-use classes.
4.2 Flood extent
Figure 6 presents the flood extent of the 2009 event based on remote sensing
analysis and the flood extent that might have really occurred if we integrate the
places highlighted by the household interviews for this event. This result
demonstrates that household surveys can contribute to improve data provided by
remote sensing, when the images is covered by clouds and also yield more accurate
information.
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Figure 6: Flood extent based on remote sensing and P-mapping.
4.3 Flood depth and flood duration
During the survey, respondents were asked to show the depth reached by flood
events and to describe the duration. Based on this information, we can see
(figure 7) that the flood depth, independently of the event, varies from 0.2m to 1m,
Figure 7: Spatial distribution of flood depths.
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Figure 8: Spatial distribution of flood duration.
with an average of 0.5m, whereas the flood duration (figure 8) ranges from
< 1 day to 365 days. Such a long duration is probably due to the lack of means for
water evacuation and the existence of topographic depressions (Mbow et al. [10]).
But the usual water duration is between 0 and 7 days.
4.4 Socio-economic characteristics of the household survey
Table 2 summarizes the general demographic and social characteristics of the 502
households included in our sample. The majority of the respondents were women
(67%). Among the respondents 41% were the owner of the house and 59% were
not. Respondents were distributed among the following categories: 25% were the
head of household, 36% were the spouse of head of household and 39% other were
in general the most knowledgeable person in terms of flooding. The average
number of persons per household is 13. The average of number of women per
household was 6. The average number of disabled was 1. The average number of
children per household was 5. The age of the respondents varies from 15 to 87 and
the average is 44 years old.
The analysis of household head education shows that 27% of the household
head were illiterate, 18% had primary school level, and 14% had secondary school
level, 6% had university level and 32% had received another type of education.
The average monthly income per household in YN is 435 USD.
4.5 Information on the physical exposure
The survey revealed key information on the 502 households related to date of
construction, the ownership, the type of construction materials and the structure as
well as the price of the land. Results show that 12% of the houses were built
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Table 2: Respondent’s characteristics.
between 1970 and 1980, 40% between 1981 and 2002 and 14% between 2003 and
2015. 65% of the surveyed households were living in their own houses, 20% were
occupied by lodger and 15% by both owner and lodger. A majority of 88% of the
surveyed houses were residential and 12% were mixed residential and workplace.
Almost all houses were built in cement and 34% of the interior courtyards
consist of cement, 29% of sand and finally 27% are in tile. More than 91% of the
surveyed houses have a foundation and 2% do not know if there is or not. 67% of
surveyed houses had cracks. 17% of surveyed houses were having the ground floor
lower than the road.
The land surface occupied by houses varies from about 100 m2 to more than
300 m2. In terms of land price one third (36%) costs less than 2000 USD (approx.
1FCFA= 500 USD), 13% varies between 2001USD and 6000 USD, 6% between
60001 USD and 12000 USD and 7% above 12000 USD. 34% of respondents do
not know the land price of their house and 4% didn’t want to answer.
Among the 502 houses included in the surveyed, 209 were at least once flooded
(figure 9). Most of surveyed houses were flooded in 2005, 2009, and 2012.
Figure 9: Number of events per house.
4.6 Local strategies for flood risk reduction
The household survey reveals the variety of local strategies put in place for flood
risk mitigation. They can be classified in structural and non-structural measures as
summarized in table 3.
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Table 3: Flood risk mitigation.
5 Discussion and conclusion
This study illustrated how the combined use of remote sensing data and local
knowledge manages to capture key elements on flood hazard (the magnitude of
flood: flood depth, flood duration), elements at risk (houses, critical
infrastructures), vulnerability (socio-economic and physical vulnerability at the
household level) as well as local strategies for flood risk reduction.
The innovative contribution of our investigation in comparison with previous
works, such as Canevari-Luzardo et al. [12] and Musungu et al. [13] is the size of
the survey, 502 households, and the level of details obtained on each flood risk
parameters, in particular, detailed information on flood hazard. Moreover, we
demonstrated how local knowledge can complement the use of remote sensing
analysis, aspect that wasn’t integrated in Canevari-Luzardo et al. [12] and
Musungu et al. [13].
Although the participatory approach allowed us to improve the analysis of
satellite images, it has some limitations. The local population can give inaccurate
information, especially in terms of hazard mapping and spatial perception (Haynes
et al. [14]). However in our study, we used neighbourhood scale paper maps,
handled GPS and mobile SIG, therefore increasing the accuracy of mapping as
already noticed by Canevari-Luzardo et al. [12]. In order to acquire high quality
data, interviewers were trained, we organized a test study to ensure wording was
comprehensible and we used the local language to avoid misunderstanding.
However, the stability of the responses was not tested and it could be interesting
to do so, in particular regarding flood events and their intensity.
In conclusion, our integration of local knowledge together with remote sensing
shows that this can improve data, when satellite images are covered by clouds and
also yield new or more accurate information in terms of hazard intensity, exposure
and location of key infrastructures. Our approach is an alternative to the use of
expensive high-resolution satellite images, when financial resources are scarce or
when images are not available on the study area. While this study focuses on flood
risk assessment, this approach could be replicated for different risks in other
contexts.
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342 Urban Water Systems and Floods
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... Với sự gia tăng của các thiết bị di động, công nghệ web 2.0, KHCĐ được áp dụng ngày càng phổ biến để cung cấp thông tin bổ sung và có giá trị trong lĩnh vực thủy văn -tài nguyên nước. Phần này, bài báo sẽ cung cấp một số thông tin chi tiết về cách cộng đồng khoa học đã đóng góp trong lĩnh vực này, được tổng hợp như trong Bảng 1. [45] x Yeumbeul Nord (Senegal) [46] Độ sâu ngập x x Pijnacker (Hà Lan) [47] x x Lưu vực Haltwhistle Burn (Anh) [21] Vận tốc dòng chảy x x Ardèche river (Pháp) [22] Thời gian ngập x Yeumbeul Nord (Senegal) [46] Theo dõi hạn hán, đánh giá rủi ro hạn ...
... Với sự gia tăng của các thiết bị di động, công nghệ web 2.0, KHCĐ được áp dụng ngày càng phổ biến để cung cấp thông tin bổ sung và có giá trị trong lĩnh vực thủy văn -tài nguyên nước. Phần này, bài báo sẽ cung cấp một số thông tin chi tiết về cách cộng đồng khoa học đã đóng góp trong lĩnh vực này, được tổng hợp như trong Bảng 1. [45] x Yeumbeul Nord (Senegal) [46] Độ sâu ngập x x Pijnacker (Hà Lan) [47] x x Lưu vực Haltwhistle Burn (Anh) [21] Vận tốc dòng chảy x x Ardèche river (Pháp) [22] Thời gian ngập x Yeumbeul Nord (Senegal) [46] Theo dõi hạn hán, đánh giá rủi ro hạn ...
... Đôi khi, tại thời điểm xảy ra các trận mưa lũ, người tham gia không thu thập thông tin vì lý do an toàn [22]. Trong những năm gần đây, ứng dụng KHCĐ trong thu thập các dữ liệu về lũ lụt khá phổ biến ở nhiều châu lục khác nhau [21,45,46]. Điều này, trái ngược với bài toán đánh giá rủi ro hạn, đây vẫn là những chủ đề tiềm năng trong tương lai. ...
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Quản lý tài nguyên nước hiệu quả yêu cầu tính sẵn có, cập nhật của dữ liệu về các đại lượng thủy văn. Tuy nhiên, nhiều khu vực trên thế giới đối mặt với việc thiếu dữ liệu, thông tin liên quan do khó khăn về mặt tài chính. Khoa học cộng đồng (citizen science) là phong trào toàn cầu đang phát triển nhanh chóng, có khả năng liên kết các nhà khoa học, nhà nghiên cứu trẻ và sự tham gia của cộng đồng trong việc thu thập và chia sẻ các thông tin khoa học. Ngoài ra, trong những năm gần đây, sự phát triển của công nghệ di động, kỹ thuật phân tích và xử lý dữ liệu cũng như các phương pháp truyền tải thông tin và tri thức, mở ra những cơ hội mới cho khoa học cộng đồng. Bài báo này trình bày tổng quan tình hình áp dụng khoa học cộng đồng và điện thoại thông minh trong lĩnh vực thủy văn - tài nguyên nước trên thế giới, và hiện trạng áp dụng ở Việt Nam. Qua đó, thấy được những tiềm năng áp dụng phương pháp mới để thu thập, quan trắc, điều tra và giám sát Tài nguyên nước, nhất là việc sử dụng các ứng dụng thu thập dữ liệu. Efficient water resources management requires data availability and update about the hydrology aspect. However, many areas worldwide are facing unavailable data, scattered information due to financial constraints. “Citizen science” is a rapidly developing global movement that links these themes of scientists, young researchers, and participatory involvement in scientific data monitoring and sharing. On the other hand, mobile technology, data analyzing and processing, and communication methods of news and knowledge have paved the way to citizen science development in recent. This paper will review the utilization of citizen science and smartphones in hydrology and water resource and the current situation in Viet Nam. Thereby, it reveals the great potential of this approach in collecting, monitoring water resources, especially data collection app use.
... For example, several studies have reconstructed past floods using either water depths and velocity retrieved from texts, pictures and videos uploaded to social media platforms (see review by Assumpção et al. 2018)) or flood duration derived using interviews (e.g. Sy et al. 2016). Data retrieved from communities may require extensive pre-processing and are susceptible to errors since they are reported by non-experts (e.g. ...
... Focussing on field visits, several researchers have integrated face-to-face interviews for the collection of post-event observations and subsequent application for past flood reconstruction using a GIS approach (e.g. Poser and Dransch 2010;Singh 2014;Sy et al. 2016Sy et al. , 2020. A recent advancement in mapping past floods in typical data-scarce regions using interviews was carried out by Sy et al. (2020) in Yeumbeul North, Senegal. ...
... In particular, it extends the application of interview data from methods using GIS to map past flood events (e.g. Poser and Dransch 2010; Singh 2014; Sy et al. 2016Sy et al. , 2020 to a method using a hydrodynamic model. In such a way, the physical and dynamic characteristic of past flood events can also be represented. ...
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The scarcity of model input and calibration data has limited efforts in reconstructing scenarios of past floods in many regions globally. Recently, the number of studies that use distributed post-flood observation data collected throughout flood-affected communities (e.g. face-to-face interviews) are increasing. However, a systematic method that applies such data for hydrodynamic modelling of past floods in locations without hydrological is lacking. In this study, we developed a method for reconstructing plausible scenarios of past flood events in data-scarce regions by applying flood observation data collected through field interviews to a hydrodynamic model (CAESAR-Lisflood). We tested the method using 300 spatially distributed flood depths and duration data collected using questionnaires on five river reaches after the 2017 flood event in Suleja and Tafa region, Nigeria. A stepwise process that aims to minimize the error between modelled and observed flood depth and duration at the locations of interviewed households was implemented. Results from the reconstructed flood depth scenario produced an error of ± 0.61 m for all observed and modelled locations and lie in the range of error produced by studies using comparable hydrodynamic models. The study demonstrates the potential of utilizing interview data for hydrodynamic modelling applications in data-scarce regions to support regional flood risk assessment. Furthermore, the method can provide flow depths and durations at houses without observations, which is useful input data for physical vulnerability assessment to complement disaster risk reduction efforts.
... There are some data required to provide an overview of the problems and conditions associated with the research location before conducting participatory mapping (Bizimana & Schilling 2010;Kienberger 2014:269-275;Sy et al. 2016), such as: ...
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This article discusses the reliability of flood inundation information that is obtained from participatory mapping. The commonly applied method to map flood inundation requires both direct and interpretive measurement data based on remote sensing images. Such assessments have limited availability of data; as a result, participatory mapping has become the solution. A number of studies have conducted participatory mapping to obtain flood hazard information in areas with limited sources of data, however, there has been little discussion about its reliability. This research conducted participatory flood inundation mapping by involving local leaders as respondents. The mental map drawn by the local leaders was digitised to obtain a shapefile format map. The information obtained from the semistructured interview was then included in the geographic information system (GIS) data as attributes. The obtained information was compared with the field data to determine its quality. A literature study was then conducted to discuss how the participatory mapping could support managing a disaster. Information obtained through participatory mapping can be effectively applied to disaster management because of its precise location information, lower cost and less time-consuming nature. The reliability of the information has weak accuracy of quantitative data; however, it has advantages in terms of qualitative data, especially in the detailed descriptions of flood information. In the future, participatory mapping should rely on integrating the perspectives of cross-disciplinary researchers, a comprehensive study of multidisciplinary knowledge and level of understanding of the stakeholders
... Les voies d'écoulement s'éloignent désormais des formes géomorphologiques originelles et déplacent la vulnérabilité vers d'autres zones qui étaient moins exposées. A Dakar, les inondations constituent une préoccupation majeure comme en témoignent les différentes actions visant à minimiser leurs impacts négatifs et à renforcer la résilience au moyen de politiques de réduction du risque (Bottazzi et al., 2018 ;Cissé & Mendy, 2018 ;Schaer et al., 2017 ;Sy et al., 2016). ...
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In recent decades, African cities have been exposed to a series of floods related to rapid urbanisation, intensification of heavy rainfall and failure of the storm drainage systems. Predicting these floods is a major challenge, and requires accurate and legible mapping of surface runoff. This study, carried out in the urban periphery of Dakar, aims to propose a calculation method for locating the overflows of the drainage network on the scale of the conurbation, with calculation times compatible with real time. After briefly describing the method, the article shows how to integrate the various urban objects modifying the drainage directions or the flow characteristics (buildings, collectors, retention basins), and to restore the drainage topology at a fine scale (5 m). The method is described by presenting the algorithms used or developed, illustrated by examples. These algorithms are operational in the ATHYS software and its Vicair module. This article will be completed later by a description of the hydrological and hydraulic modelling associated with this topology.
... It is most often difficult to prove that the cause is water. Some [14] believe that the problem affects more the vulnerable and poor populations of the disadvantaged neighborhoods, while the flooded SONUCI neighborhood in Niamey is rather a symbol of an economic success story of the 1980s. ...
... However, several attempts have been made in recent years to apply citizen science and local knowledge in the field of flood hazard assessment (Assumpção et al. 2018, See 2019, either during flood response or in the near real-time mapping of flooding events (Eilander et al. 2016, Wan et al. 2014. For example, Sy et al. (2016) researched flood risk at the neighborhood level with surveys (500 respondents). They did participatory mapping and collected information at the household level to consider and integrate local knowledge on floods. ...
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This study addresses the pressing need for flood extent and exposure information in data-scarce and vulnerable regions, with a specific focus on West Africa, particularly Senegal. Leveraging the Google Earth Engine (GEE) platform and integrating data from the Sentinel-1 SAR, Global Surface Water, HydroSHEDS, the Global Human Settlement Layer, and MODIS land cover type, our primary objective is to delineate the extent of flooding and compare this with flooding for a one-in-a-hundred-year flood event, offering a comprehensive assessment of exposure during the period from July to October 2022 across Senegal’s 14 regions. The findings underscore a total inundation area of 2951 square kilometers, impacting 782,681 people, 238 square kilometers of urbanized area, and 21 square kilometers of farmland. Notably, August witnessed the largest flood extent, reaching 780 square kilometers, accounting for 0.40% of the country’s land area. Other regions, including Saint-Louis, Ziguinchor, Fatick, and Matam, experienced varying extents of flooding, with the data for August showing a 1.34% overlap with flooding for a one-in-a-hundred-year flood event derived from hydrological and hydraulic modeling. This low percentage reveals the distinct purpose and nature of the two approaches (remote sensing and modeling), as well as their complementarity. In terms of flood exposure, October emerges as the most critical month, affecting 281,406 people (1.56% of the population). The Dakar, Diourbel, Thiès, and Saint-Louis regions bore substantial impacts, affecting 437,025; 171,537; 115,552; and 77,501 people, respectively. These findings emphasize the imperative for comprehensive disaster preparation and mitigation efforts. This study provides a crucial national-scale perspective to guide Senegal’s authorities in formulating effective flood management, intervention, and adaptation strategies.
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This study addresses the pressing need for flood extent and exposure information in data-scarce and vulnerable regions, with a specific focus on West Africa, particularly Senegal. Leveraging the Google Earth Engine (GEE) platform and integrating data from Sentinel-1 SAR, Global Surface Water, HydroSHEDS, Global Human Layer Settlement, and MODIS Land Cover, our primary ob-jective is to delineate flood extents and compare them with centennial flood-prone areas, offering a comprehensive assessment of exposure during the period from July to October 2022 across Sen-egal's 14 regions. The findings underscore a total inundation area of 2 951 square kilometers, impacting 297 142 people, 175 square kilometers of urban and 16 square kilometers of crops. Notably, August wit-nessed the largest flooded areas, reaching 780 square kilometers, constituting 0.40% of the coun-try's surface. Subsequent regions, including Saint-Louis, Ziguinchor, Fatick, and Matam, experi-enced varying extents of flooding, with August data showing a 1.34% overall overlap compared to centennial flood-prone areas derived from hydrological and hydraulic modeling. This low per-centage reveals the distinct purposes and natures of the two approaches (remote sensing and modeling), as well as their complementarity. Turning to flood exposure, August emerges as the most critical month, affecting 76 595 people (0.43% of the total population). Dakar, Diourbel, Thiès, and Saint-Louis regions bore substantial impacts, affecting 100 707, 57 648, 31 579, and 26 581 people, respectively. These findings emphasize the imperative for comprehensive disaster preparedness and mitigation efforts. The study provides a crucial national-scale perspective to guide Senegal's authorities in formulating effective flood management, intervention, and adaptation strategies.
Chapter
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