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INDEX
Page Title Institut
002-035 MICRO LEVEL VULNERABILITY ASSESSMENT OF ESTUARINE ISLANDS: A CASE STUDY FROM INDIAN SUNDARBAN
Tuhin Ghosh Jadavpur University, India
036-069 ASSESSMENT OF URBAN FLOOD RESILIENCE FOR WATER, SANITATION AND STORM WATER DRAINAGE SECTORS IN TWO CITIES OF INDIA
Sandeep Thakur & Uday Bhonde National Institute of Urban Affairs (NIUA), New Delhi
070-084 IMPACT OF CLIMATE CHANGE ON AGRICULTURAL, METEOROLOGICAL, AND HYDRO-LOGICAL DROUGHTS IN THE CENTRAL HIGHLANDS OF VIETNAM
Dao Nguyen Khoi VNUHCM – University of Science, Vietnam
085-105 ASSESSMENT OF STORM SURGE HAZARD, VULNERABILITY AND RISK OF THE AGRICULTURAL SECTOR IN LEYTE, PHILIPPINES
Engr. Jon H. Gaviola, The Oscar M. Lopez Center
106-119 SELECTING MULTI-FUNCTIONAL GREEN INFRASTRUCTURE TO ENHANCE RESILI-ENCE AGAINST URBAN FLOODS
A. Alves, A. Sanchez, B. Gersonius, Z. Vojinovic UNESCO-IHE, Delft, The Nether-lands
120-155 ADAPTATION TO CLIMATE CHANGE IN AREAS WITH CULTURAL HERITAGE
Z. Vojinovic1, D. Golub1, W. Keerakamolchai1, 2, W. Meesuk1, A. Sanchez Torres1, S. Weesakul 2
1UNESCO-IHE, Delft, The Nether-lands 2Asian Institute of Technology, Pathumthani, Thailand
156-170 WHEN HAZARDS BECOME DISASTERS: THE CASE OF COASTAL FISHING COMMUNI-TIES IN BANGLADESH
Mahmudul Islam, M. Mostafiz, P. Begum Sylhet Agricultural University
171-187 THE USE OF AGENT BASED MODELS FOR CLIMATE CHANGE ADAPTATION AND DE-VELOPMENT OF LARGESCALE EVACUATION STRATEGIES FOR FLOOD RISK MITIGA-TION
Neiler Medina (a) Arlex Sanchez (a) Zoran Vojinovic (a) Alida Alves (a)
(a) UNESCO-IHE, Westvest 7, Delft, Zuid Holland, 2611AX, The Netherlands
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MICRO LEVEL VULNERABILITY ASSESSMENT OF
ESTUARINE ISLANDS: A CASE STUDY FROM
INDIAN SUNDARBAN Tuhin Ghosh
Jadavpur University, India
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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Indian Sundarban• World heritage site
• Largest mangrove patch(4.3%)
• Rich biodiversity- flora, fauna
• 4.6 million population
• 34% under poverty
• 99% rural areas
• Poor access to infrastructure
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Sundarban biodiversity
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Study area
• Three islands- Sagar, Ghoramara
and Mousani
• Western part of Indian Sundarban
Island system
• Extended from 21°37’ North to
21°55’North and 88°2’ East to 88°15’
East
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Sagar Island
Situated under administrative jurisdiction of district South 24 Paraganas of
West Bengal, have 42 mouzas/ villages
Largest among Sundarban Island- area of 245.33 km²
206844 population (Census, 2011)
Ghoramara Island
Situated under administrative jurisdiction of Sagar Block of district South 24
Paraganas of West Bengal
Has an area of 4.4 km² with population 5193 (Census, 2011)
Mousani Island
Mousuni Island is under administrative jurisdiction Namkhana CD Block of West
Bengal, have 4 mouzas/ villages
Covering 29 km² area with population 22073 (Census, 2011)
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Vulnerability context: study islands
• The temperature increase rate has been reported about 0.019˚c with a projected 1 ˚C by the year 2050 (Hazra et al, 2002)
• Sea level rise 1990- 2000: 3.14 mm/year (Hazra et al.,2002)
• Change in river hydrodynamics
• During 1969 to 2009 Indian Sundarban had total landloss of around 210 km2 (Hazra et al, 2013)
• During the last part of decade (2006-2009) : experienced four major cyclones viz. Sidr, Nargis, Bijliand Aila
• Cyclone Aila of 2009 was the most hazardous of the climatic disasters to have recently hit the Sundarban Delta
• High population growth
• Development constraints: road connectivity, access to health services
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Research questions
• What are the trends in physical and anthropogenic changes?
• What are the key elements of vulnerability in the study area in respect to both
the natural and socio- economic factors?
• What is the extent of social and environmental vulnerabilities in the study
area?
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Data
Primary and secondary data sources:
• Survey data: Direct interviews with
783 households, selected by cluster
random sampling
• Published data: Indian
Meteorological Department;
Directorate of Census, GoI; WWF
• Satellite images: Landsat data
• The data analysis have been done in
two stages
• Stage 1: Trend analysis to get change
pattern as background of
vulnerability analysis
• Stage 2: assessment of actual
scenario along with vulnerability
mapping
Analytical approach
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Climatic Trend analysis
Temperature
(1901 – 2000)
• Average temperature increase: 0.011°C per year
Data source: IMD, Govt. of India
y = 0.0111x + 30.769R² = 0.2178
y = 0.0097x + 21.386R² = 0.1095
y = 0.0104x + 26.078R² = 0.2347
15.00
20.00
25.00
30.00
35.00Ye
ar1
90
1
Year
19
04
Year
19
07
Year
19
10
Year
19
13
Year
19
16
Year
19
19
Year
19
22
Year
19
25
Year
19
28
Year
19
31
Year
19
34
Year
19
37
Year
19
40
Year
19
43
Year
19
46
Year
19
49
Year
19
52
Year
19
55
Year
19
58
Year
19
61
Year
19
64
Year
19
67
Year
19
70
Year
19
73
Year
19
76
Year
19
79
Year
19
82
Year
19
85
Year
19
88
Year
19
91
Year
19
94
Year
19
97
Year
20
00
Tem
pe
ratu
re in
°C
Max
Min
Average
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y = 2.0783x + 1536.9R² = 0.0345
0
500
1000
1500
2000
2500
3000
year
19
01
year
19
04
year
19
07
year
19
10
year
19
13
year
19
16
year
19
19
year
19
22
year
19
25
year
19
28
year
19
31
year
19
34
year
19
37
year
19
40
year
19
43
year
19
46
year
19
49
year
19
52
year
19
55
year
19
58
year
19
61
year
19
64
year
19
67
year
19
70
year
19
73
year
19
76
year
19
79
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82
year
19
85
year
19
88
year
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91
year
19
94
year
19
97
year
20
00
Rai
nfa
ll in
mm
Data Source: IMD, Govt. of India
• Amount of rainfall has increased :rate of 2.08 mm per year (1901 to 2000)• Number of rainy days have decreased implies the increase in intensity of
rainfall.
Rainfall
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Morphological change in study islands(1990 to 2015)
Erosion
• Sagar Island: Erosion rate
estimated 0. 2 km2 per year
• Mousani Island: Considerable
land loss: rate of erosion almost
0.08 km2 per year
• Ghoramara Island: Experienced
huge land loss, maximum loss
between 1975 to 1990
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Island Time window 1990 - 1995 1995 - 2000 2000 - 2005 2005 - 2010 2010 - 2015
Sagar
Erosion in sq km 0.43 9.35 3.8 0.55 5.79
Accretion in sq km 17.13 1.59 0.86 7.56 0.39
Ghoramara
Erosion in sq km 0.11 0.61 0.61 0.09 0.46
Accretion in sq km 0.35 0.00 0.02 0.29 0.05
Mousani
Erosion in sq km 0.18 2.85 0.86 0.42 1.02
Accretion in sq km 2.48 0.05 0.45 1.21 0.37
Erosion/Accretion and Net Land Loss during 1990 to 2015
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y = -0.0187x + 10.873R² = 0.0435
0
10
20
Cyclonic Depression
y = -0.0184x + 5.2625R² = 0.1296
0
5
10
Cyclonic Storm
y = 0.0046x + 1.5533R² = 0.0152
0
2
4
6
8
Severe Cyclonic Storm
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Population growth
• Sagar Island: population growth
of 1.4% per annum in 2011
• Ghoramara Island experienced
little growth, 0.55% per annum
and negative growth rate of -0.08
at 2011
• Mousani Island experienced
population increase at 1%growth
rate per annum in 2011
86769110672
149222180408
206844
2.53.03
1.91.4
0
1
2
3
4
0
50000
100000
150000
200000
250000
year1971 year1981 year1991 year2001 year2011
Gro
wth
rate
Po
pu
lati
on
in
no
.
4163 43364972 5,236 5193
0.41
1.4
0.52
-0.08
-0.5
0
0.5
1
1.5
0
1000
2000
3000
4000
5000
6000
year1971 year1981 year1991 year2001 year2011
Po
pu
lati
on
in
no
1014812639
16803
2001322073
2.2
2.9
1.8
0.98
0
0.5
1
1.5
2
2.5
3
3.5
0
5000
10000
15000
20000
25000
year1971 year1981 year1991 year2001 year2011
Po
pu
lati
on
in
no
.
Sagar Island
Ghoramara Island
Mousani Island
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Crop productivity
Production decreased due to salinization of soil, fertilizer and labour cost, non-marketing of the produce, etc.
y = -5.2645x + 701.54
400
500
600
700
800
2000-01 2001-02 2002-03 2003-04 2004-05 2006-07 2007-08 2008-09 2009-10 2010-11 2011-12
Pad
dy p
rod
. In
‘0
00
to
nn
es
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Vulnerability assessment
• Vulnerability= f (exposure, sensitivity, adaptive capacity)
• Risk depends on the exposure of the system and adaptive capacity
of the system reduces the risk from threats.
• Residual Threat = Adaptive capacity – Risk
• Residual threat determine the extent of vulnerability
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• Composite Vulnerability Index: assessment based on both physical and
socio- economic variables
• Assessment done following the methodology developed by Ramakrishna
Mission in 2009 and report prepared by Hazra et. al., 2013.
• Normalization of variable by percentage
• Ranking as high- medium- low
Vulnerability assessment methodology (1)
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• The geometric mean of different vulnerability classes with rank has been
derived to assess mouza level Vulnerability Rank (VR) -
VR= 7√V1*V2*V3……..V7
• Vulnerability maps of study islands have been prepared separately in
interactive GIS platform.
• Finally overlying the maps to get Composite vulnerable zones or ‘hot spot’
mouzas
Vulnerability assessment methodology (2)
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Erosion
• Vulnerable mouzas: Ghoramara, Baliara,
Radhakrishnapur, Chandipur,
Chemaguri
• Low: < 0.04 Km2 land loss per year
Moderate: 0.041 to 0.08 Km2
High: >0.081 Km2 per year
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• 33% household are severely being
affected by erosion
• Loss of land, Homestead, livelihood
Severe Impact Moderate Impact No Impact
Impact of erosion on local inhabitants
0 5 10 15 20 25
land
homestead
livelihood
%of households
Types of Loss Due to Erosion
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House structure
• Low- <40% kachcha house,
moderate- 41- 70% kachcha, high-
71% kachcha houses
• Sapkhali (50%), Kusumtala (44%),
Ghoramara (43%): most vulnerable to
damage during storms and coastal
flooding.
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Electrification
• Low- <10% left electrification, moderate- 11-
30%, high- more than 31% left electrification
• Most of the villages don’t have electric
connection
• Few mouzas of Sagar have grid connection
since 2011
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Population density
• Low- less than 900 persons/ Km2, high-
greater than 1301 persons/ Km2 area,
moderate- 901- 1300 persons per Km2
area
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Education achievement level
• Low- more than 41% adult
educational attainment, high- less
than 20% attainment, moderate-
rest (21- 40)
• Lack of alternate skill and low
educational attainment leads to
more vulnerable situation
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Level of sanitation
Low: more than 81% houses having
good sanitation
High: less than 50% houses having good
sanitation
Moderate: rest (51- 80)
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• Only around 40% of population is employed- major share unemployment
• Female work participation is very low around 25%
• Decreasing productivity- less profit in agriculture
• Increasing poverty
• Shift to daily labour- quick money; out migration
• Increasing income inequality
• 38%, 37% and 25% surveyed families of Sagar Island, Ghoramara Island andMousuni Island are under below poverty level respectively
Economic status
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0
10
20
30
40
50
60
70
80
90
100
0 10 20 30 40 50 60 70 80 90 100
Cu
mu
lati
ve P
erce
nta
ge o
f M
on
thly
In
com
e
Cumulative Percentage of Total Income
Gini Coefficient- 0.22
0
10
20
30
40
50
60
70
80
90
100
0 10 20 30 40 50 60 70 80 90 100
Cu
mu
lati
ve P
erce
nta
ge o
f M
on
thly
In
com
e
Cumulative Percentage of Total Income
Gini Coefficient: 0.18
Lorenz curve & Gini- coefficient showing income inequality among surveyed mouzas of
Sagar Block Mousani Island
Striking income inequality has been found in study islands
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Low: < 50% BPL families
Moderate: 51- 65% BPL families
High: > 66% BPL families
• BPL families- average income, assets
considered
Poverty
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Estimation of composite vulnerability
• Composite vulnerability map of 27
surveyed mouzas
• Ghoramara highly vulnerable
• Sapkhali, Baliara, Shibpur mouzas are
also closer to highly vulnerable
condition
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Delta in distress!!
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Conclusion & recommendations
• 21% mouzas highly vulnerable to erosion
• Social vulnerability is higher among the surveyed villages
• Educational attainment is lacking for 46% mouzas
• 21% mouzas need immediate economic assistance
• Around 66% mouzas are standing at the edge of vulnerability
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Recommendations (1)
• Regular maintenance of embankment in the coastal villages
• Proper warning and evacuation plan for cyclone
• Planned housing structure: Ghoramara, Sapkhali, Kusumtala
• Expansion of non- conventional source of energy to meet the deficiency: tidal energy, wind energy, solar energy
• Night school, vocational training, technical schools for adults; involvement of school children of locality
• Raising awareness about sanitation; monitoring and upgrading sanitation condition from gram panchayat
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Recommendations (2)
• Initiatives from local authority to give prior attention to economically
vulnerable mouzas to reduce poverty
• Reduction of income inequality: stable occupation; labour law for informal
sectors
• Focus on traditional practices- improve productivity through climate-
resilient agricultural practices
• Stakeholder participation
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Thank you for your kind patience
Questions please????
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ASSESSMENT OF URBAN FLOOD RESILIENCE
FOR WATER, SANITATION AND STORM WATER
DRAINAGE SECTORS IN TWO CITIES OF INDIA
Sandeep Thakur & Uday Bhonde,
National Institute of Urban Affairs (NIUA), New Delhi
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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Yellow area – flood prone
Physiography of India and locations of important cities
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13
29
9
4,3
44
17
,13
0
55
,44
0
1
10
100
1,000
10,000
100,000
I V X XI XII - outlay
Exp
en
dit
ure
on
flo
od
m
anag
em
en
t (i
n c
rore
)
Five Year Plan
1,0
94 1
7,5
09
19
,49
0
6,0
47
0
5,000
10,000
15,000
20,000
25,000
2008 2009 2010 2011
Dam
age
to
pu
blic
uti
litie
s (i
n c
rore
)
Year
1951 2012
Sources: Planning commission & central water Commission reports
Flood Expenditure in India
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Climate change threats
• Long term trends indicates 5-8% increase in rainfall at upper catchments
• Short duration (24/hrs.) rainy days are increasing chances of urban flooding
• Threats on infrastructure like storage reservoirs, water supply, transportation already indicated in national reports
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Year Urban Flooding2000 Mumbai, Chennai, Bangalore Kolkata, Hyderabad
2001 Ahmadabad, Bhubaneswar, Thane, Mumbai
2002 Delhi
2003 Delhi, Ahmadabad, Vadodara
2004 Chennai
2005 About 10 cities; Mumbai was the worst affected.
2006 Number of affected cities rose to 22. Surat was the worst affected.
Vishakhapatnam airport was inundated for more than 10 days.
2007 Number of affected cities rose to 35. Kolkata was the worst affected.
2008 Jamshedpur, Mumbai, Hyderabad were worst affected.
2009 Delhi, Mumbai, Kurnool
2010 Delhi, Guwahati, Ahmadabad, Leh, Mumbai
2015 Chennai, Mumbai
2016 Gurgaon, Bhopal, Nashik, Guwahati (NE states, MP, Gujarat, Bihar, UP, WB,
Rajasthan)
Source: various web resources
Highlighted impacts Of urban flooding particularly on economy
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Flood Resilience
• The United Nations International Strategy for Disaster Reduction (UNISDR) defines resilience as “an ability of a system, community or society exposed to hazards to resist, absorb, accommodate and recover from the effects of a hazard in a timely and efficient manner, including through the preservation and restoration of its essential basic structures and functions” (https://www.unisdr.org/we/inform/terminology#letter-r).
• Term “resilience” is now widely referred particularly in natural hazard risk reduction and climate change adaptations programmes.
• Use of term has become prominent post year 2005 (Serre D., & Barroca, B.,2013)
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Flood Resilience – Benchmark studiesCORFU - 2007 (EU)
CIRIA - 2010 (UK)
USEPA- 2014 (USA)
ZFRA- 2014 (Zurich)
• Aerts, J. et.al. (2014) estimated Cost of Flood Resilience in coastal megacity of New York for different strategies.
• Three strategies were proposed to make coastal areas flood resilient viz. • measures to enhance building codes in NY city, a non-structural approach • different structural measures like levee barriers, beach nourishment in coastal areas of city and • hybrid approach which combines building codes measures, and barrier construction only for very
high risk areas as per probabilistic hazard estimation.• Interesting policy recommendations like collection of US$10 resilience fees from tourists
(50million/year) visiting city to recover an investment in building resilience measures are proposed in the study.
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Flood Resilience - India• Disaster Management Act – 2005, formed Nat.DM. Authority
• NDMA – 2008 - flood resilience guidelines
• NDMA – 2010 – urban flood resilience guidelines
2005 2016..Improved
• In India, understanding of resilience (urban flood) is limited and now increasingly used by academia and development sector.
• Especially, the term is frequently used post climate change and natural hazard studies carried out by national agencies (MoEF, NDMA) under resilience programmes and with support from international donors.
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Flood resilience and national missions of India• Atal Mission for Rejuvenation and Urban Transformation (AMRUT)
• Swachh Bharat Mission (SBM) to improve urban infrastructure and sanitation conditions in Indian cities.
• Smart cities mission
• All programmes under Ministry of Urban Development, Govt. of India
This research study aimed to propose broad framework to measure cost of urban flood resilience which would be useful to city officials in preparing projects in WSS sectors under such missions.
It is anticipated that by incorporating the resilience dimension for future WSS projects with some cost details; damages to critical infrastructure would be minimized and services will be less affected during urban floods by achieving some degree of urban flood resilience (http://smartcities.gov.in/ )
Urban areas (cities) are playing vital role in economic growth of country as their share in gross domestic product (GDP) is increasing. High Powered Expert Committee (HPEC) indicated that it is expected to be 75% by 2030 (HPEC, 2011) in India. Thus, any adverse impact on urban economy due to natural or manmade disasters directly affects economy of India
http://amrut.gov.in/http://www.swachhbharaturban.in/sbm/home/
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Aim & ObjectivesStudies/research in India on climate change impacts in urban areas have emphasised on risk
profiling, vulnerability assessment of population & service sectors and then recommends suitableadaptation/resilience options. However, there are limited information on financial aspects ofresilience particularly of WSS sectors.
• Therefore, important aim of this article is ,
• To highlight status of urban flood resilience in general and particularly of WSS sectors in two select cities in India namely Guwahati and Vishakhapatnam
• The specific objectives are ,
• To discuss gaps in WSS infrastructure, associated challenges and how the gap influences flood resilience in selected cities
• To appraise WSS infrastructure, institutional set up and financial status in study cities from flood resilience perspective
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Infrastructure: Gap assessment, emergency plans, innovative technologies, new infrastructurearrangements, retrofitting, relocation plans
Institutions: Good governance, roles and responsibilities, enforcement of laws, devolution of powers, bye-laws, skilled staff, capacity building and training
Finance : Revenue receipts/expenditure, grants (centre, state), loans (international institutes)
Urban Floor Resilience
WSS Sectors
Framework to test urban flood resilience
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Guwahati
Vishakhapatnam
Indo-Gangetic PlainDesert
Himalaya Highlands
Coastal Plains
This is part of research study whereinFour cities were studied
Two cities are discussed in this article
Guwahati – NE hilly terrainVishakhapatnam – SE coastal plain
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Profile of study cities
• Guwahati, North East Hilly terrain has an average annual rainfall 1,600 mm
• Severe urban flooding since 1980
• Vishakhapatnam, South Eastern Coastal Plain has an average annual rainfall 1,200 mm
• Urban flooding during HUDHUD Cyclone, 2014
• Vulnerable to cyclone, storm surges, sea level rise, tsunami
• Both cities have saucer/bowl shape, due to typical topographical set both cites are vulnerable to urban flooding
Cost of Inaction to Public Utilities:-
• Guwahati – Rs. 224 crore (US$35 million) in two years (2014-15)
• Vishakapatnam – Rs. 255 crore (US$40 million) in single extreme event of Hudhudcyclone (2014)
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Flood vulnerability
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Guwahati, Assam - Baseline
• As per Census 2011, population living in the city was 957,352 (~1.2 million now considering Urban Agglomeration).
• In 2012, slum population residing in slums noted was 139,000 (14%)
• Decadal growth rate – 19%
• GMC area - 216 sq.km., GMDA -262 sq.km.
• Master plan available for 2021
1890 19672010
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DEEPOR BEEL
BRAHMAPUTRA RIVER
BASISTHA RIVER
PAMOHI RIVER
FATASIL HILL
UNIVERSITY HILL
SILAPAHAR
NILACHALHILL
NARKASURHILL
SONAIGHULIHILL
JAPORIGOG HILL
UDAIGIRIHILL RAMCHAI
HILL
KHAGHULIHILL
NARENGIHILL BURAGOSAIN
HILL
RANI RESERVEHILL
KHANAPARARESERVEHILL
KALIHILL
CONTOURS
WATER BODY
NATURAL DRAINAGES
RAILWAYLINE
LEGEND
AIRPORT
NATIONAL HIGHWAY
MAJOR ROADS
Meghalaya Plateau
Slope direction – South to north
N
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Courtesy : GMDA
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Primary reasons of urban flooding
• High rainfall in river catchment areas of southern plateau
• Backflow of flood water from Brahmaputra river – ultimate discharge
• Reduction in carrying capacities of local rivers/drainage with high silt load from deforested hills
• Degradation of natural wetland areas and local water bodies
• Poor sanitation conditions in city – no sewerage infrastructure
• Increased paved areas in the city with urbanization
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Urban flooding impacts
• Shifting of water intake barges in Brahmaputra River
•Damage to water supply infrastructure in hills
• Silt load in septic tanks - overflow
• Submergence of hand pumps and bore wells in flood water
•Water-borne diseases risk
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City Sector Planning Infrastructure Institutions Finance Implementation/O&M
Guwahati
Water Good Poor Very Poor Good Very Poor
Sewage Poor Very Poor Very Poor Very Poor Very Poor
Solid waste Average Poor Good Average Average
Storm water Good Poor Very Poor Good Poor
Appraisal of Guwahati for urban flood resilience
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Current approach - More engineering
Courtesy : GMDA
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Current approach – cont.
Courtesy : GMDA
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Conclusions• 18 Automatic Weather Stations for the City
• EWS & Alarm System for Disaster preparedness
• Drainage Design on basis of Peak Discharge
• SoP for city agencies
Overall –
• Guwahati has started towards achieving resilience as ..
Initiatives of storm water drainage and some resilient measure like raising power supply transformers,
New technologies for de-silting city drains are seen on ground
Short term duration measures have relieved from the urban flooding in 2015-16 Courtesy : GMDA
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Vishakhapatnam, Andhra Pradesh - Baseline
• As per Census 2011, population living in the city was 1.8 million (~2.0 million now considering Urban Agglomeration).
• Slum population 0.56 million (30%) highest in India
• There are 741 slums in the city out of that 286 are notified and 455 non-notified slums.
• Decadal growth rate – 19%
• GVMC – 566.95 sq.km.
• VUDA - 1701sq.km. covering entire GVMC area
• Master plan available for 2025
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19001950
1970
2003 2015
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Damage due to urban flooding
• Rs. 255 crore (US$40million) - Cost of inaction-Public Utilities
• 700 km of water supply line damaged
• 350 km of open drains and UGD line damaged
• Water supply affected with failure of electricity supply and non-availability of generator sets
• Groundwater withdrawal not possible due to no power supply
• Shortage lasted for a week in some areas
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Primary reasons of urban flooding
• Typical topographical set up of city due to which high velocity water gushes from surrounding hills
• Low elevation coastal areas making city vulnerable to storm surge inundation during high cyclonic winds
• Poor coverage of storm water drainage network
• Ignorance of local water bodies in urban planning
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City Sector Planning Infrastructure Institutions FinanceImplementation/
O&M
Vishakhapatnam
Water Average Very Good Very Good Good very good
Sewage Average Poor Very Good Good Poor
Solid waste Poor Very Poor Very Good Good Poor
Storm water
Average Average Very Good Good average
Appraisal of Vishakhapatnam for urban flood resilience
Overall - Vishakhapatnam seems comparatively better positioned to adopt flood resilient measures as the Infra and Finances are good.
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Challenges & Key Learning
• Poor information availability from small and medium sized cities so size range increased
• Lack of systematic documentation of infrastructure damage in cities due to floods
• Lack of information on infrastructure damage/repair and O&M for urban floods . It is mixed and not separated
• No collated information on expenditure to analyze financial cost of resilience
• Lack of awareness on flood resilience among city officials• Projects prepared with engineering solutions and lack eco -system based
holistic / integrated approach• Need for wider outreach of climate resilience knowledge
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Financial cost of resilience
• Five years city budgets were analyzed to see revenue receipts from different sources like own and external sources like central, state and other grants and loans from financial institutions.
• The revenue expenditure for WSS sectors were analyzed for capital, O&M and other expenditure.
• Infrastructure gaps in WSS sectors (critical infrastructure) are important in determining cost of flood resilient WSS sectors.
• Cost of resilience is higher for those cities which have wider infrastructure gaps because this will be over and above the infrastructure gap filling cost.
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Comparison
• In Guwahati there are multiple agencies that manages WSS sectors in the city. Budgets of all the agencies are separately done and there is no collated data available with single agency on income and expenditure incurred by different agencies for new infrastructure projects, O&M etc.
• The data indicates that share of water sector for capital and O&M is quite negligible when compared to entire GMC budget. All new infrastructure projects are being constructed international financial support on loan basis.
• Since there are multiple agencies doing O&M and absence of collated data precise conclusion on financial aspect is difficult.
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Comparison cont..
• In Vishakhapatnam, analysis of budgets was easy as there are no multiple agency
• Per capita annual capital expenditure in WSS sectors infrastructure projects is only 9% considering HPEC
• Per capita annual O&M cost is only 52% of recommendations by HPEC
• This indicates that the O&M is comparatively better in the city and also validates benefit of having single agency in managing city
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Concluding remarks
• The appraisal of three pillars infrastructure, institutions and finance of study cities indicates that the financial cost to make WSS sector flood resilient will include costs for filling existing and future infrastructure gaps.
• In addition to this, the resilience costs will include cost of innovative Green Infrastructure, Institutional strengthening by capacity building to implement new cost effective options and relying on own financial strength.
• City can only afford to spend additional infrastructure expenditure for resilience, if its existing financial burden is low.
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IMPACT OF CLIMATE CHANGE ON
AGRICULTURAL, METEOROLOGICAL, AND
HYDROLOGICAL DROUGHTS
IN THE CENTRAL HIGHLANDS OF VIETNAM
Dao Nguyen Khoi
VNUHCM – University of Science, Vietnam
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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Outline
1. Background and objectives
2. Study area
3. Methodology
4. Result and discussions
Calibration and validation of the SWAT model
Climate change scenarios
Analysis of changes in SDF of the hydro-meteorological and agricultural
droughts
5. Conclusions
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Background In recent years, the frequency and severity of the flood and drought due to climate
change have considerably increased (IPCC, 2013)
Under the impact of climate change, studies on monitoring and predicting droughts on along-term scale are necessary to find countermeasures to cope with extreme droughtconditions that may occur in the future (Kim et al., 2014).
The method to monitor and predict drought is using observed hydro-meteorological dataand projected data through outputs of the general circulation models (GCMs) andhydrological model.
Vietnam has faced severe and prolonged droughts, which causes water scarcity and lossof agricultural production with damaged costs of hundreds of billion Vietnamese Dong.
• In the dry season 2015-2016 with the effects of El Niño phenomenon, the CentralHighlands region has faced the most severe droughts in the past 100 years, causingsevere damage to agriculture (FAO, 2016)
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Background (cont.)
Objective
To investigate the impacts of climate change on meteorological, agricultural, andhydrological droughts in the Srepok River Basin in the Central Highlands of Vietnam
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Study area
Area: 12,000 km2;
Climate: tropical climate monsoon,
with 2 seasons: rainy season (May-
Oct) and dry season (Nov – Apr);
Annual rainfall: 1,700-2,400 mm
Soil: 75% basalt soil;
Population: 2.5 million inhabitants
(2013).
Srepok River Basin
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Methodology
Observed climate data
5 GCMs(IPCC-AR5)
RCP 4.5
RCP 8.5Downscaling
(Bias-correction)
Climate change scenarios
(Precip and tmp)
Drought indices(SPI, SSWI, SRI)
Change in SDF of droughts
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Methodology (cont.)Input data
Data type Data description Scale Data sources
DEM Topographical features 90m USGS
Land-use Land-use classification such as
agricultural land, forest, and urban, 2003
1km MRC
Soil Soil types and physical properties 10km FAO
Meteorology Daily precipitation, min and max
temperature in the 1981-2009 period at 9
stations
Daily Hydro-Meteorological Data
Centre (HMDC)
Hydrology Streamflow in the period 1981-2000 Daily Hydro-Meteorological Data
Centre (HMDC)
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Results and discussion
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Calibration and validation of the SWAT model
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Climate change scenarios• In this study, GHG emission scenarios
adopted RCP4.5 (middle) and RCP8.5(high) were used.
• GCM simulation outputs ofSEACLID/CORDEX member countrieswithin the SEA
Centre, country developed GCMs Centre abbreviationCountry used
GCMs
Canadian Centre for Climate Modeling & Analysis, Canada CanESM2 Malaysia
Centre national de Recherches Meteo., France CNRM-CM5 Vietnam
Hadley Centre, UKMO HadGEM2-AO South Korea
Institute Pierre-Simon Laplace, France IPSL-CM5A-LR Malaysia
Max Planck Institute for Meteorology MPI-ESM-MR Thailand
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Climate change scenarios (cont.)
(a) RCP 4.5 scenario
(b) RCP 8.5 scenario
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Analysis of changes in the drought SDF
Historical time series of SPI, SSWI, and SRI
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Analysis of changes in the drought SDF (cont.)
(a) SPI (b) SSWI (c) SRI
Future changes in the severity, duration, and
frequency of the droughts in the RCP 4.5 and 8.5
scenarios
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Conclusions
Climate change scenarios (precipitation and temperature) were generated for the period2045-2070. It is indicated that the climate in the study area would generally warmer andwetter in the future;
Under the possible climate change, the annual and seasonal streamflow would increasesignificantly in the future;
The drought events would generally increase in the future, while the drought severityand frequency would decrease.
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Thank you for your attention!
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ASSESSMENT OF STORM SURGE HAZARD,
VULNERABILITY AND RISK OF THE
AGRICULTURAL SECTOR IN LEYTE, PHILIPPINESEngr. Jon H. Gaviola, The Oscar M. Lopez Center
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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INTRODUCTION
http://images.gmanews.tv/v3/webpics/v3/2014/10/640_2014_10_17_09_38_36.jpg
http://www.mb.com.ph/wp-content/uploads/2014/08/1_fish-edt.jpg
This sector shares about 10% of the country’s gross domestic product (GDP)and around 30% for its work force (Philippine Statistics Authority, 2016).
Agriculture plays a significant role in the Philippines.
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http://irri.org/images/blogs/20131113-typhoon-impact.jpg
http://philnews.ph/wp-content/uploads/2013/11/NN1.jpg
Typhoon Haiyan (local name Yolanda)
• 600 fatalities (91% from Leyte) and
• damage exceeding US$ 2 billion
Specific to the agricultural sector
• damage exceeding US$ 200 M
• about 77 000 hectares of land
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DOST Project NOAH (2014)
Most vulnerable coastal areas
Samar, Leyte, Iloilo, Palawan, Cebu, Negros, Bohol, Bicol, Quezon, Metro Manila, Bulacan, and Surigao
Recommendation from this study
DETAILED STORM SURGE STUDIESTO IMPLEMENT APPROPRIATESITE SPECIFIC SOLUTIONS
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• This study utilizes light detection andranging (LiDAR) technology in modellingthe storm surge hazards
• It targets to produce high resolution stormsurge model and maps that will help invisualizing the hazard, vulnerability andrisk.
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MATERIALS AND METHODS
Study Area
The study was conducted in Palo, one of the forty municipalities
of the province of Leyte. Located in the northeastern section of
the province and south of the capital city of Tacloban, it has a
total area of 22127 hectares with an estimated population of
70,052 as of 2016 (Philippine Statistics Authority, 2016). The
farming barangays (villages) are Baras, Candahug, Cogon,
Guindapunan, Salvacion, San Fernando, San Joaquin and
Tacuranga.
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Data Used
1 meter resolution 1 km resolution
ELEVATION DATA
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Haiyan as meteorological dataFrom JWTC Best Track Data
+
Other Data Used
spatially-varying amplitudes and phases of tidal forces
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The development of the storm surge models for the study site
was done using Delft3D. Computational grids along the
coastline of the study area were used to set-up the
hydrodynamic model. Delft3D-RGFGRID was used to generate
and refine the grids using splines. The bathymetric and
topographic elevation data were then interpolated on the
computational grids using Delft3D-QUICKIN.
Storm Surge Modeling
Finally, using DELFT3D-FLOW, the flow of water in the
coastal area was simulated. It was generally dictated by the tidal
forces on the open boundaries as well as wind stress of the
meteorological data.
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Hazard
The results of the modeling phase were then exported into an
ArcGIS format for the post processing and analysis. To
transform the depth values into a hazard level, the classification
of storm surge heights was implemented. This was in reference
to an average height of a Filipino.
Height
(m)
Class GIS Value
0-0.50 Low 1
0.51-1.50 Medium 2
> 1.5 High 3
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Vulnerability
• Vulnerability (V) is a function of exposure (E), adaptive
capacity (AC), and sensitivity (S) (IPCC, 2014).
• ArcGIS Spatial Analyst will be used to facilitate the rating
procedure involving ranking of multiple datasets into one
representative dataset which would be the final output, the
vulnerability map.
• Each barangay will then be rated and ranked according to
their exposure, adaptive capacity and sensitivity scores.
• Sources for these data will be focus group discussions (FGD)
to be conducted as well as secondary data obtained from
barangays and locality concerned.
V = % E + % AC + % S
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• Adaptive capacity will be rated based on focus group
discussions involving the smallholder farmers and fisher
folks exposed to storm surge hazards.
• General questions regarding awareness of climate change,
access to climate and weather information, access to capacity
building programs, among others will be asked to the
participants.
• The answers will be patterned to the description and rank
prepared for them for uniformity and standardization of
answers.
• After post-processing of FGD results, fields for each
question shall be added to the attribute table barangay
shapefile and be ranked based on the table.
Rank GIS Value
Not at all (No) 5
A little 4
Somewhat 3
A lot 2
Extremely (Yes) 1
Ranking of data for adaptive capacity measure
Value Class
1 Very High
2 High
3 Moderate
4 Low
5 Very Low
Adaptive Capacity Index
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The indicators to be considered in exposure index were
distance from coast and elevation of the barangays.
These factors will be based from the spatial data available for
analysis such as LiDAR data, base maps and administrative
boundaries of barangays in the locality.
For the sensitivity index, series of informant interviews (KII)
and secondary data gathering will be conducted to collect
necessary data such as percentage of agricultural land, fraction
of household engaged in the agriculture sector, crops and
fishery among others.
𝐈𝐢 =𝐗𝐢 −𝐌𝐢𝐧𝐗𝐢
𝐌𝐚𝐱𝐗𝐢 −𝐌𝐢𝐧𝐗𝐢
Normalized
Value, %
GIS Value
(exposure)
GIS Value
(sensitivity)
Class
0-20 5 1 Very Low
21-40 4 2 Low
41-60 3 3 Moderate
61-80 2 4 High
81-100 1 5 Very High
Exposure and Sensitivity Indices.
V = % AC + % E + % S
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Risk
• Since storm surge risk is a function of storm surge hazard
and storm surge vulnerability, the formula will be used below
to finally determine the risk values for each barangay.
• It will finally be classified into specific risk level based on
the table.
RiskSS = Hazardss * Vulnerabilityss
Range Classification
0-3 Very Low
4-6 Low
7-9 Moderate
10-12 High
13-15 Very High
Storm surge risk classification.
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RESULTS AND DISCUSSION
• The figure displays the storm surge
simulation results for Palo using the
parameters from Typhoon Haiyan. The
inundated area was displayed reaching
up to 2 kilometers from the shore. The
depth caused the storm surge brought
about the super typhoon has reached up
to 7.9 meters.
• The agricultural barangays namely
Baras, Candahug, Cogon,
Guindapunan, Salvacion, San
Fernando, San Joaquin and Tacuranga
were affected by the storm surge.
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• The simulated storm surge heights were
translated to a hazard map that visualize
areas that are exposed different levels of
hazards specific to storm surge.
• A flood height of 0.5 meters and below is
classified as low; 1.5 meters and above
as high; and between 0.5 and 1.5
meters as medium.
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Series of focus group discussion with the smallholder farmers and fisher folks as well as gathering of secondary data to
assess their vulnerability to the climate change and expected extreme events as manifested by stronger and higher storm
surges in the future.
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3 years after Haiyan…
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Agricultural lands and
smallholder farmers in Leyte
Damaging impacts of storm
surges
Using LiDAR technology in the
process of identifying vulnerable
areas to storm surges
Future scenarios under climate
change (how sea level rise will
intensify storm surges)
Documentation of potential
adaptation strategies
EXPECTED OUTCOMES:
Science-informed policy makingEnhanced adaptive capacity
Gender-sensitive adaptation measures
Better yield
Higher productivity
Increased income
Stabilized food supply
TARGET OUTCOMES
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CONCLUSION
This study has exhibited the use of light detection and ranging (LiDAR) technology for producing
higher resolution inundation maps to expose the agricultural areas most prone to storm surges in the
future.
The flood heights caused by the storm surge can actually be translated into hazard levels. Low, medium
and high level of hazards were mapped out to show different exposure levels to the climate risk being
studied which is storm surge.
Hazard maps can actually be analyzed with vulnerability factors such as the interaction of human
population to the physical and social environment to display the risk of the area being studied.
Vulnerability and risk assessments specific to storm surges are very important to the agricultural sector
in order for them to better adapt and prepare to the changing climate.
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for more information, contact:
Engr. Jon H. GaviolaResearcher, Oscar M. Lopez Center [email protected]
755-2332 loc. 2652
End of Presentation
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SELECTING MULTI-FUNCTIONAL GREEN
INFRASTRUCTURE TO ENHANCE RESILIENCE
AGAINST URBAN FLOODS
A. Alves, A. Sanchez, B. Gersonius, Z. Vojinovic
UNESCO-IHE, Delft, The Netherlands
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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• BACKGROUND
• CONCEPTUAL FRAMEWORK
• MEASURES SELECTION TOOL
• SELECTION TOOL APPLICATION AND PRELIMINAR RESULTS
• NEXT STEPS
• CONCLUSION
OUTLINE
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BACKGROUND
Urbanization growth:
Climate Change:
Projections of relative changes in runoff by the end of 21st century (IPCC, 2007)
Main urban agglomerations, with more 50% of world population (WB, 2007; UN, 2014)Runoff increment as a consequence of urbanization
Changing trends of precipitation
Number of reported flood events per year (WB, 2012)
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Traditional approach:
• Mainly based on grey infrastructure.
• Single oriented approach, focused on removing water from streets as fast as possible.
• Not flexible systems, based on design event methods which offer low future adaptation capacity.
• Reliable and largely tested systems.
• Enough methods, tools and resources for designing.
• High technical and social acceptability.
BACKGROUND
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Sustainable approach:
• Based on green infrastructure.
• Multiple benefits approach, focused on runoff reduction besides other co-benefits for the urban environment.
• Flexible systems, present high adaptation capacity under uncertain future.
• Lower reliability in front of extreme events.
• Tools, design methods and performance evaluation still under development.
• Are not easily chosen by decision makers.
BACKGROUND
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STORAGE MEASURES
GREENINFRASTRUCTURE
BLUE INFRASTRUCTURE
BUFFERING AND INFILTRATION
BUILDINGS FLOOD PROOFING
TRADITIONAL MEASURES
Knowledge Base PEARL Project – All possible measures
Local constraints analysis:• Soil type• Groundwater depth• Drainage area slope• Type of sewer system• Urban configuration
Hazards Analysis
Flood Type: • Fluvial• Pluvial• Coastal• Flash• Groundwater
Measures Screening
Suitability analysis:• Public spaces• Population density• Land use• Treatment plant /
CSO
Multiple benefits /Local preferences:• Water quantity reduction• Water quality improvement• Environmental benefits• Liveability enhancement• Cost minimization• Economic benefits• Socio-cultural benefits
Measures Ranking
CONCEPTUAL FRAMEWORK FOR MEASURES SELECTION
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MEASURES SELECTION TOOL: SCREENING
Flood type
Local constraints for measures application
Shorter list of measures
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MEASURES SELECTION TOOL: SUITABILITY RANKING
Local characteristics for suitability analysis
First ordered list of measures
Scores
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MEASURES SELECTION TOOL: BENEFITS/PREFERENCES RANKING
Co-Benefits weights according to local preferences
Second ordered list of measures
Scores
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SELECTION TOOL APPLICATION AND PRELIMINARY RESULTS
Ayutthaya
Medium population density, heritage and touristic site, fluvial and pluvial floods.
(Meesuk et al., 2015)
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SELECTION TOOL APPLICATION AND PRELIMINARY RESULTS
SukhumvitHigh urbanization and population density, mainly commercial and business area, frequent pluvial floods.
(Shrestha, 2013)
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NEXT STEPS
How to combine selected measures?
• Type of applicability: permanent or temporal measures.
• Implementation scale: centralized or decentralized approach.
• Hydrological impact: source control or end of pipe solutions.
• Main runoff reduction process: storage, evapotranspiration, infiltration, etc.
Criteria for measures combination:
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CONCLUSIONS
• This work presents a methodology for screening and ranking measures against urban floods.
• The screening process is based on the analysis of local flood problems and local conditions and
features of the urban space.
• The method also considers the co-benefits achievable through the implementation of green
infrastructure and local preferences for those benefits.
• In order to facilitate the implementation of the developed methodology, a decision support tool
has been developed.
• This tool was applied in two different study areas, obtaining different preferred measures which
are in accordance with the characteristics of each case.
• The outcome of this work is seen as useful for helping decision making processes focused on
reducing urban flood risk in a sustainable way, allowing the improvement of other
environmental aspects.
• Further work will continue with the validation and improvement of the process, as well as with
the analysis of measures combination in order to develop long term sustainable strategies.
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THANK YOU!!
Alida Alves: [email protected]
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ADAPTATION TO CLIMATE CHANGE IN AREAS
WITH CULTURAL HERITAGE
Z. Vojinovic1, D. Golub1, W. Keerakamolchai1, 2, W. Meesuk1, A.
Sanchez Torres1, S. Weesakul 2
1UNESCO-IHE, Delft, The Netherlands2 Asian Institute of Technology, Pathumthani, Thailand
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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• FRAMEWORK
• PROJECT
• STAKEHOLDER ANALYSIS
• HAZARDS, VULNERABILITIES, RISK
• MEASURES
OUTLINE
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• Flood risk analysis for urban areas with cultural objects
• Tangible and Intangible aspects
• Social and cultural contexts
Framework
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Framework
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N Limit: 14 ⁰ 23’26”S Limit: 14 ⁰ 18’49”E Limit: 100 ⁰ 35’20”W Limit: 100 ⁰38’00”
Slide 12
Project Area – Ayutthaya Island
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2011 Rainfall Analysis: 5 storms occurred, namely: HAIMA (26 Jun.), NOCK-TEN (31 Jul.),
HAITANG (28 Sep.), NESAT (30 Sep.) and NALGAE (5 Oct.)
HAIMA
NOCK-TEN
HAITANGNESAT
NALGAEAyutthaya
Rainfall from HAIMA (25 June 11)
Rainfall from NOCK-TEN (31 July 11)
Source : Hydro and Agro Informatics Institute, Thailand
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2011 Floods - Ayutthaya
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2011 Floods - Ayutthaya
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Framework - steps
Stakeholder analysis Risk analysis Communication
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identification → categorisation → interdependencies analysis
Stakeholder Analysis
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Hazard AssessmentModels 1 & 2:1 . Tachin and Chao Phraya River.2. Only Chao Phraya River.
New 1D Model (3):3. Ayutthaya Heritage Site and proximities.
1 2
3
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Water depth (m)
1D/2D: Maximum Flood-depth Resultswith bypass
Improvement options 1
Current situation
Animation!!!
Hazard Assessment
Improvement options 2 Improvement options 3
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Hazard Assessment
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Vulnerability Assessment
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SOCIAL VULNERABILITY
Source: Google Images
- Large scale survey;
- Eight parameters were used
to calculate social vulnerability;
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SOCIAL VULNERABILITY
Source: Google Images
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PHYSICAL VULNERABILITY – vulnerability of the built environment
Cultural properties
Residential buildings
Identification of buildings' types
• residential
• commercial
• public
• cultural
Identification of vulnerability parameters
• type of structure (e.g. single or two -storey, flood protection, etc)
• condition
• building content
Categorisation
• low
• medium
• or high level of vulnerability
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IMPACT ASSESSMENT – tangible damages: depth-damage curves
0
10000
20000
30000
40000
50000
60000
70000
80000
90000
100000
0 0.5 1 1.5 2 2.5 3 3.5 4
Esti
mat
ed d
amag
es [
THB
]
Depth of inundation [m]
Single-storey houses Two-storey houses Pillar houses
Property’s area:< 50 m2 ≥ 50 m2
Type of structure
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PHYSICAL VULNERABILITY
Source: Google Images
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Social vulnerability assessment at the community level
Flood awareness
14%
Flood preparedness
16%
External Support
9%Community cohesiveness
and education11%
Health14%
Property15%
Income /livelihood12%
Vulnerable groups
9%
Cap
acity
Susc
epti
bili
ty
(flo
od
eff
ect
on
dif
fere
nt
do
mai
ns)
8 groups of social vulnerability parameters and their weights.
Identification of communities
• 33 communities
Data collection
• Focus Group Discussions with communities’ representatives
• Questionnaire
Evaluation of vulnerability
• Qualitative and quantitative analysis of questionnaire responses
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Parameters for economic vulnerability assessment:
• time period of complete shutdown of the business due to a flood event;
• time period when a business experiences downsizing caused by a flood event; and
• an operational capacity during downsizing phase.
ECONOMIC VULNERABILITY
Identification of economic activities
• tourist–oriented / non-tourist
Data collection
• Interviews with business owners
• Government and insurance
Evaluation of vulnerability
• Analysis of three parameters
VS denotes vulnerability score,
I denotes income level before the 2011 flood event [Thai Baht per month],
Tsd denotes shutdown phase [months],
Td denotes downsizing phase [months],
Cd denotes operational capacity during a downsizing phase [in comparison to I].
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ECONOMIC VULNERABILITY
Source: Google Images
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CULTURAL VULNERABILITY
59525252
5145
4342
3132
2525
2019
1513
1211
88
66
544
22
11
0 20 40 60
Chantharakasem National Museum
The Ancient Palace
Wat Phra Si Sanphet
Phet Fortress
Old City Wall
City Shrine
Wat Suwan Dararam
Somdet Phra Srinakarindra Park
Wat Rattanachai
Million Toy Museum
Wat Yan San
Wat Som
Wat Pra Sat Thong
Wat Khun Mueng Jai
Wat Je di Thong
Number of responses
The degree of a property's sensitivity to flooding
very low low medium high very high
Level of a
property's
significance
very low very low low low medium medium
low low low medium medium high
medium low medium medium high high
high medium medium high high very high
very high medium high high very high very high
A matrix which defines different levels of cultural vulnerability based on the properties' significance and their sensitivity to flooding.
Residents’ opinion about cultural significance
Assessment of individual significance of different cultural properties in Ayutthaya
(UNESCO and ICOMOS, Structural Assessment)
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CULTURAL VULNERABILITY
Source: Google Images
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COMBINED VULNERABILITY
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COMBINED VULNERABILITY
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RISK ASSESMENT
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RISK ASSESMENT - CALCULATED
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RISK PERCEPTION“Areas at higher risk of floods?”
Group mapping exercise
3 colours represent different levels of risk:
light tint – low level,
moderate tint – medium,
rich tint – high level.
“Critical depth of flood waters?”
“Acceptable levels of risk?”
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RISK PERCEPTION
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RISK COMPARISON
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RISK ASSESMENT – Calibration # 1
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RISK ASSESMENT – Calibration # 2
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RISK COMPARISON
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http://www.pearl-fp7.eu/
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THANK YOU!!
Zoran Vojinovic: [email protected]
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WHEN HAZARDS BECOME DISASTERS: THE CASE
OF COASTAL FISHING COMMUNITIES IN
BANGLADESHMAHMUDUL ISLAM, M. MOSTAFIZ, P. BEGUM Sylhet Agricultural
University
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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Background
• Bangladesh is the 5th most at risk country in the world in terms of disasters (World Risk Report 2016)
• About 97.1% of the total area of Bangladesh and 97.7% of its total population are at risk of multiple hazards (World Bank, 2005)
• Cyclones, saline water intrusion, water logging, landslides, and arseniccontamination pose substantial threats to the livelihoods of the coastal inhabitants (Lazar et al., 2015)
• 14 percent of GDP Bangladesh is exposed to disasters. Each year the country incurred 1.8 percent of GDP loss due to natural disaster (CDMP II 2016)
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Background
• About 80–90% of global losses and 53% of global cyclone-related deaths occurred in Bangladesh (GoB, 2008)
• Hazards do not necessarily cause a disaster. Instead disasters occur by a mix of physical exposure and socio economic pressures
• Small-scale fishers are among the most vulnerable professional groups . Because they
live close to coastal water, heavily dependent on climate sensitive fisheries usually “poorest of the poor” involved in “low profile” profession
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Study areas and methods
•Using DPSIR as analytical tool, this study explores the mechanism of disaster vulnerability of coastal fishers in the Southern Bangladesh
• Semi-structured interviews (59)
• Four communities (from Borguna and Patuakhali districts) dependent on Hilsa fishing
• Secondary Data from Bangladesh Meteorological Department and Department of Fisheries
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DPSIR Framework
The DPSIR (Drivers-Pressures-State-Impacts-Responses) framework was developed for assessing the causes, consequences and responses to change in a holistic way (EEA, 1999; Atkins et al. 2011).
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Drivers • River mouth system in the low-lying coastal ecosystem. Thus vulnerable to climate related hazards, coming from
both sea and catchment areas
• Majority of the interviewed households are found functionally landless, a section them live on the government (khas) land in densely settlement
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Drivers
• Repeated exposure to cyclones originating in the Bay of Bengal
• From 2007, seven cyclones made landfall on the Bangladesh coast suchThe track of major cyclones (1985-2009) (Chowdhury et al. 2012)
•
• The track of cyclone
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Drivers
• Increasing numbers of low pressure system means that increasing number of days of rough weather which hinders traditional fishing in the open sea
Total Duration of Depression Events (X axis) and Number of Total Days of Rough Sea (Y axis) per Month between 1975 and 2015 (Islam 2015)
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Drivers• Patron-client relationship is most dominant in the communities that wielded most social
power in the area
• Socio-economic profiling, for most of the respondents, monthly income is close to poverty line
• Longer distance from cyclone centers and reluctance to move
• Stability and effectiveness of the embankments in the face of repeated extreme events.
© P. Gain
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Pressures• Cyclones destroyed standing crops, productive assets for fishing, collapsed houses and other
physical infrastructures that shattered local economy,
• Frequent cyclones and depression in the bay often force fishers to abandon their fishing trip and return to coast. Incomplete fishing trips incur a substantial financial loss
• Loss to be 76,000 BDT (950 US$) for a 10-day fishing trip
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State
• The coastal population of Bangladesh has doubled since the 1980s
• Agricultural productivity drastically reduced , coastal fisheries ecosystem suffer over-exploitation
• Intense competition cause reduction in catch-per-unit-effort
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Impacts and response
• Overall ecological environment degraded
• Prolonged saline water stagnation cause agricultural land unsuitable
• Loss and damage fishing assets decimated the capacity to go for fishing and immediate survival
• Destructive fishing practices rises significantly since majority of the fishers are indebted and are desperate to restore their livelihoods
• Displacement and migration
The population density (754/square km) of the southern zone is relatively lower compared to Bangladesh (964/square km) (BBS, 2011), largely because of out migration (GoB/FAO, 2013)
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Summary
• River-mouth system in coast is particularly vulnerable to disaster coming from both sea and catchment areas
• Hazards are recurring and cumulative, making vulnerable to disaster
• Communities suffer several shocks within a short period, and/or multiple simultaneous pressures,
• The pace of change outstrips adaptive capacity of suffered population and local institutions
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Reflection• The fishing communities, by their very nature are the first victim of cyclone
and more prone to water borne hazards
• The implementation of the implementation of the Voluntary Guidelines for Securing Sustainable Small-Scale Fisheries will be a right step forward
• The Guidelines asks for urgent and ambitious action, in accordance with the objectives, principles, and provisions of the United Nations Framework Convention on Climate Change (UNFCCC)
• Better coordination, between GoB and NGOs and among the NGOs response and recovery programs could have produced better utilization of limited resources and resulted in distribution of services and resources equally to all the affected parties that would ultimately benefit the vulnerable population in the coast
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Thank you
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THE USE OF AGENT BASED MODELS FOR CLIMATE
CHANGE ADAPTATION AND DEVELOPMENT OF LARGE-
SCALE EVACUATION STRATEGIES FOR FLOOD RISK
MITIGATIONNeiler Medina (a) Arlex Sanchez (a) Zoran Vojinovic (a) Alida Alves (a)
(a) UNESCO-IHE, Westvest 7, Delft, Zuid Holland, 2611AX, The Netherlands
WATER SECURITY AND CLIMATE CHANGE:CHALLENGES AND OPPORTUNITIES IN ASIA
Asian Institute of Technology, Bangkok, Thailand
29 November - 01 December 2016
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Outline
• Motivation of the work
• Scope of the research
• Methodology
• Preliminary Results
• Conclusions
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Motivation!
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The scope of this research is to explore new andnovel techniques that can be used to betterunderstand which are the key components in theformation of risk and which of those are the mostsignificant in order to reduce people’s risk tofloods. More specific the research focus on howcan we improve evacuation strategies
Scope
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Methodology
To better understand the key components of people’s risk toflood and determine which are the most sensitive parametersto have better evacuation plans we are using a state of the artAgent Base Model (ABM) to allow us to study and modelindividual and crowd behaviour under extreme Hydro-Meteorological events (Floods) in coastal Areas before andduring a disaster is unfolding.
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Methodology
The key challenge for a successfulEvacuation is Information…. In cityevacuation Not only the message contentmatters but the way the message is deliver,accepted and understood by individualsand the community plays a major role inthe effectiveness of the evacuation itself. Inaddition lead time plays a major role in theeffectiveness of the evacuation itself.
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Methodology
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Methodology
Social Model
Hydrodynamic Model
Flood Warning
How people willbehave under floodthreat
Dissemination StrategyDissemination MeansMessage Content
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MethodologyBuilding the Behavioral Model
Agent and Environment General Characterization
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Building the Behavioral ModelModel Formalization and parameterisation
Methodology
Phase 1 – Daily Behaviour
Threat
PERCEPTION SENSOR
BEHAVIOUR
Social Status
Z F
Cognition
Z F
Emotion
Z F
Physis
Z F
ACTOR
Z: State Causal DependenciesF: State Transition Function Information Flow
Phase 2 – Cognitive Behaviour
Internal structure of PECS reference model (from [1]) [1] C. Urban and S. Bernd, ‘PECS–Agent-Based Modelling of Human Behaviour’, in Emotional and Intelligent–The Tangled Knot of Social Cognition, North Falmouth, MA, 2001
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To explore and evaluate how the provision of warning information can affect theevacuation response and behaviours, 4 different scenarios were set up in the ABM builtin using Repast-Simphony:
Baseline scenario: The agents evacuate according with the initial set of rulesof the ABM, no new information is given to the agents in how to evacuateand the evacuation will be performed based on the "existing" knowledge ofthe agent.
Scenario 1: A message with the warning and evacuation was sent at thesame time to all the population in the island.
Scenario 2: A message with the warning and evacuation was send graduallyto all the population in the island, known as stage evacuation.
Scenario 3: A message with the warning and evacuation was sent only tothose inhabitants that reside and/or work in the areas to be expected beaffected by the hazard event.
Methodology - Implementation
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ABM – Sint Maarten.
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ABM – Sint Maarten.
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Preliminary Results – Scenario Analysis
ABM – Sint Maarten.
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Adjusted mortality functions based on:
People Vulnerability à F[Age(h, w, As), gender, health]
Building Vulnerability à F[Material, Year]
Car “Vulnerability” à F[Stability on Water] - Type of Car
- Terrain Slope - Hazard
“Mortality” Function
ABM – Sint Maarten.
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1. ABM has proved to be a powerful tool to test several evacuation strategiesregarding Warning messages content, dissemination Means anddissemination strategies.
2. ABM for city evacuation allows authorities to detect the need to improve(update) evacuation plans, also to identify the need to improve currentinfrastructure (roads, shelters capacity and location, etc.)
3. A good synergy between social sciences and engineers is needed to havebetter evacuation models that can be used in real life.
4. At this point a generic ABM for city evacuation seems to be an impossibletask.
Conclusions
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[email protected] Medina P.