Bhubaneswar Final Report DRM
Bhubaneswar Final Report DRM
Bhubaneswar Final Report DRM
Final Report
November 2014
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
For the attention of:
Document Control
Acknowledgements
The consulting team extends its appreciation to UNDP, India for awarding this assignment to
us. We would also like to acknowledge the valuable guidance and support of Mr. G.
Padmanabhan, Mr. Ashok Malhotra, Ms. Abha Mishra and Mr. Prasad Babu of UNDP, India
for their discussions and sharing of thoughts during the various meetings on the project.
We would also like to acknowledge our sincere gratitude to Dr. Krishan Kumar, IAS, City
Commissioner, Municipal Corporation for extending all possible support in conducting this
assignment. We extend our sincere thanks to Dr. Kamal Lochan Mishra, Chief General
Manager, OSDMA for extending all help in getting data from different departments. We
extend our sincere thanks to all the city officials for providing their valuable support during
data collection activity and final workshop and to Mr. Meghanad Behera, City Project
Coordinator, UNDP for his kind help in coordinating with various Govt. departments.
We also acknowledge GIS division of Bhubaneswar Municipal Corporation (BMC) for sharing
of the GIS data.
Executive Summary
The Hazard Risk and Vulnerability Analysis (HRVA) for the city of Bhubaneswar, Odisha has
been carried out as part of the on-going GOI-UNDP project “Enhancing Institutional and
Community Resilience to Disasters and Climate Change.” It aims to reduce disaster risks in
urban areas by enhancing institutional and community resilience to disasters and climate
change by integrating Disaster Risk Reduction (DRR) measures in the development
programs as well as to undertake mitigation activities based on scientific analysis.
This report provides findings of the hazard risk and vulnerability assessment of key natural
hazards the city is exposed to, namely – Cyclonic wind, Flood, Earthquake, Heat wave, and
Epidemics. Quantitative modeling techniques based on GIS were used for mapping and
analysis using standard public domain models. Based on these results, recommended
actions for various mitigation and adaptation measures were provided in the last section.
City Profile:
Bhubaneswar, the capital of Odisha state, is also popularly known as the "Temple City of
India". It is located on the Eastern Ghats, about 40 km west of North Bay of Bengal (with an
average elevation of 45 meters above mean sea level) in Khordha district. It lies on the west
bank of river Kuakhai, which is a tributary of River Mahanadi that flows about 30 km
southeast of Cuttack. The river Daya branches of Kathjodi and flows along the southeastern
part of the city. The city has a spatial spread 135 sq. km with 67 Census wards and a
population of more than 8 Lakhs. It has a population density of 6,228 person/ sq km.
City Asset:
The city has more than 197,000 households and about 75% of the buildings in the city are
under residential use. The city has several commercial and industrial establishments; about
14% and 2.5% of the total buildings are under commercial and industrial use, respectively.
The city has a total road network of about 1,642 km of which about 51 km is national
highway passing through the city. The total length of rail network in Bhubaneswar city is
about 34 km and the only international airport is located at a distance of 3 km from the city
center. The city has 1,171 educational institutions and 667 health centers. The city, being a
temple city, has a large number of religious places (more than 117 sites). The total estimated
value for main exposure elements for Bhubaneswar city is more than INR 151,452 Crores,
out of which Residential, Commercial, and Industrial exposure is about INR 91,085 Crores,
INR 43,707 Crores, INR 4,353 Crores, respectively. The exposure value of essential facilities
(health care centers, educational institutions, etc.), and transportation systems are estimated
at about INR 4,985 Crores, and INR 7,186 Crores, respectively.
Hazard mapping and analysis:
For the past three decades, the state of Odisha and in particular, Bhubaneswar city has
been experiencing unprecedented contrasting extreme weather conditions; from heat waves
to cyclones; from droughts to floods. In the year 1998, the State of Odisha faced an
unprecedented heat wave situation, because of which 2,042 persons lost their lives. Though
extensive awareness campaigns have largely reduced the number of casualties during post
1998 period, a good number of casualties are still reported each year. It has become a
menace during peak summer. The temporal analysis of daily temperature data for the past
three decades shows a steady increase in city temperature. During May 2013, a maximum
temperature of 47oC was recorded at Bhubaneswar. Most of the districts in Odisha, on an
average, recorded 40ºC during April 2014 and, the temperature across a few districts in
coastal Odisha reached 46ºC by the end of May. Very severe heat stress conditions
prevailed in May / June in 2014. In fact, Bhubaneswar has become one of the hottest Indian
cities in recent times.
1
The economic loss numbers presented in this report are structural losses and cost of land and content values
are not taken in such analyses.
∙ Enforce building codes (byelaws) for various types (residential, commercial, and
industrial) of buildings in general and residential buildings in particular, to reduce the
cyclonic wind risk in the city.
∙ Significant damage to buildings also happens due to fallen trees/their branches from
high cyclonic wind speeds. Hence, city administration should have a proper tree
pruning policy for the city.
∙ Evaluate tinned/asbestos roof buildings for their resistance to cyclonic wind by certified
structural engineers in a phased manner. This should be followed up by appropriate
retrofitting measures.
∙ Gradually covert the overhead lines in general, and electric power lines in particular, to
underground cables. This will help in avoiding damage and loss due to cyclonic
winds.
Earthquake risk mitigation measures: The estimated economic losses to residential
buildings are highest followed by commercial and industrial buildings. Among
schools/colleges, hospitals, and religious places, the estimated economic losses are highest
for schools/colleges followed by religious places and hospitals. Since earthquake risk
mitigation measures are directly related to life-safety, the city administration should take
these up on priority for their strict compliance. The following are some of the measures to
mitigate losses to life and property from earthquakes:
∙ Create regular public awareness campaigns on “Earthquake safety - Dos and Don’ts”
through seminars and quizzes in schools/colleges, and through print and electronic
media
∙ Review and enforce strict building codes (byelaws) compliance in design and
construction of various types of new buildings and infrastructures.
∙ Evaluate old buildings from structural engineering point of view, especially starting from
schools/colleges, religious places and hospitals for their structural resistance to
earthquakes. This should be followed up by appropriate retrofitting measures.
∙ All the residential, commercial and industrial buildings should be evaluated for their
structural safety in a phased manner and appropriate retrofitting measures should be
taken up from building code perspectives.
∙ To mitigate non-structural damages, several measures can be adopted, such as: o
Fasten shelves, cupboards etc. securely to walls,
o Secure water heaters, LPG cylinders etc., by strapping them to the walls or
bolting to the floor
o Anchor overhead lighting fixtures and fans to the ceiling properly
o Secure hanging objects, such as ACs, heavy glass paintings etc., as hanging
objects may cause loss to life and property
Flood/Water logging mitigation measures: Taking into consideration the growth in the
city, the following measures are recommended for urban flood management:
∙ Remove encroachment of natural drains as this helps in mitigating flood/ water logging
problem of the city
∙ Develop and connect storm water network for the entire city including peripheral areas of
the city
∙ Develop high resolution (preferably 0.5 m) Digital Elevation Model (DEM), which will be
helpful to model and predict city flooding/water-logging accurately at sub-ward level and
for planning mitigation measures.
∙ Periodically clean existing storm drains, which are clogged due to waste dumping and
indiscriminate developmental activities
∙ Improve the existing solid-waste disposal system and enforce non-dumping of solid waste
in drains
cover should be further improved in the city in a phased manner ∙ Increase awareness in
people to take pre-emptive measures during heat waves, for
example, drinking enough water, avoiding alcohol consumption, etc. and in
understanding warning symptoms of heat exhaustion and how best to keep cool. ∙
Training masons for constructing buildings following building codes and design
specifications that cover features of green buildings
Epidemics adaptation and mitigation measures: Health is a key sector that needs priority
considerations as part of DRR activities in both short and medium-term planning. These
include:
∙ Monitoring of commercial eating places to enforce quality standards and ensuring good
supply of quality drinking water
∙ Imparting hygiene and sanitation education in schools
∙ Land use planning needs to take into consideration water logging issues during and
after construction and development activities
∙ Coordinate with the railways and PWD to regularly fumigate railway yards and trains in
train yards, particularly during rainy seasons
∙ The drinking water supply department to the city should test water system for adequate
chlorination levels and for bacterial and viral counts
∙ Inspection across the City to identify potential mosquito breeding grounds and take
necessary steps before and during rainy season
Climate change adaptation measures
∙ Land use and infrastructure development plans of the city need to take into
consideration the short and long- term climate change trends
∙ Low-lying areas of city can be best protected from water logging by developing suitable
drainage system. The storm water drainage system of the city need to be
2
GRIHA – green building ‘design evaluation system’– A tool to design, operate, evaluate and maintain resource
efficient ‘healthy’ and ‘intelligent’ building
(http://www.cccindia.co/corecentre/Database/Docs/DocFiles/rating_system.pdf)
∙ The city Municipality and Bhubaneswar Development Authority has some GIS data of
the city. ORSAC and OSDMA are other State agencies who have/are developing GIS
data for the entire Odisha state. These agencies should develop the Utility network
layers (electricity network, drinking water network, storm water network, sewerage
network, and communication network) in GIS platform to help various decision
makers to integrate DRR activities. There should be a central database, which is
accessible to various departments through defined data sharing policies
∙ The city needs to have a mechanism to develop disease incidence data from both
government and private hospitals. This can be done through an online module in the
city portal where access can be given to users (government and private hospitals) to
enter tested and positively identified cases at their institutions with their spatial
locations. Similar to birth and death registry, registering disease incidence for
identified diseases needs to be made mandatory.
∙ Health contingency planning should be based on disease incidence data ∙ Damage
assessment reports need to follow the format developed and circulated by NDMA and
need to be decentralized. In the case of the City, it should be at ward level. Mobile based
applications can be developed for ward officials to make online entry of damage
information.
∙ The city master plan needs to consider hazard risks from various natural hazards and
integrate mitigation measures in its vision document
∙ City, with the support of the political representatives, needs to enforce land use zoning
and building codes based on hazard and risk maps
∙ Implement incentives and disincentives for climate proofing – tax subsidies for houses
with climate proofing and disincentives like climate risk penalties for people
encroaching hazard prone areas.
∙ Awareness of political representatives will help regulate community encroachment in
hazard prone areas
∙ As a medium and long-term measure, the city should build a storm water drainage
system for entire city to avoid urban flash floods/water-loggings.
Risk Atlas: The outcomes of the study are presented in graphic form in a Risk Atlas and
provided as a separate document. The atlas is a compilation of all the base and analytical
maps generated as part of this study. The risk atlas is presented at ward level, which would
help in understanding the spatial distribution of hazards, exposure and risks.
Final Report Confidential Page 11 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
Table of Contents
Document Control................................................................................................................. 3
Acknowledgements............................................................................................................... 4
Executive Summary .............................................................................................................. 5
Table of Contents................................................................................................................ 12
List of Figures ..................................................................................................................... 15
List of Tables ...................................................................................................................... 19
Abbreviations Used............................................................................................................. 20
1 Background.................................................................................................................. 22
1.1 Scope of the Assignment..................................................................................... 23 1.2
Bhubaneswar City Profile .................................................................................... 24 2 Multi
Hazard Mapping and Analysis ............................................................................. 25 2.1
Cyclonic Wind Hazard ......................................................................................... 25 2.1.1
Cyclone hazard in city of Bhubaneswar ........................................................... 25 2.1.2 Data
availability and sources ........................................................................... 30 2.1.3
Methodology for cyclone hazard assessment .................................................. 30 2.1.4 GIS
Mapping and Analysis of Cyclonic Wind hazard........................................ 32
2.1.5 Application of Cyclonic Wind Hazard Maps in Disaster Management and City
Planning....................................................................................................................... 36
2.2 Flood Hazard Assessment................................................................................... 37
2.2.1 Hydrology of Floods......................................................................................... 37
2.2.2 Probabilistic Simulation of Runoff .................................................................... 39
2.2.3 Hydraulic Modeling (Inundation Model)............................................................ 40
2.2.4 Mapping of Flood Extents ................................................................................ 41
2.2.5 Analysis of Flood Hazard................................................................................. 42
2.2.6 Localized Flooding/Water logging .................................................................... 42
2.3 Earthquake Hazard.............................................................................................. 44
2.3.1 Seismotectonics of the area around Bhubaneswar .......................................... 44
2.3.2 Seismic hazard at rock level ............................................................................ 45
2.3.3 Modeling Soil Amplification .............................................................................. 46
2.3.4 Application of Earthquake Hazard Maps in Disaster Management and City
Planning....................................................................................................................... 50
2.4 Heat Wave Hazard .............................................................................................. 51
2.4.1 Data source ..................................................................................................... 51
2.4.2 Methodology .................................................................................................... 51
2.4.3 Analysis results................................................................................................ 51
List of Figures
Figure 2-1: Storm tracks of past events from year 1877 – 2013 (Source: IMD and JTWC)..
29 Figure 2-2: Flowchart showing approach for cyclone hazard
assessment ........................... 31 Figure 2-3: Average Wind Speed Vs Return Period based
on Gumbel Distribution............. 32 Figure 2-4 : Steps for cyclone hazard
assessment.............................................................. 32 Figure 2-5: Cyclone hazard Map for
5-year return period .................................................... 33 Figure 2-6: Cyclone hazard Map for
100-year return period ................................................ 34 Figure 2-7: Basin Boundary Map of
Mahanadi with Location of Bhubaneswar .................... 38 Figure 2-8: Flood hazard
assessment framework................................................................ 39 Figure 2-9: Annual
Maximum Discharge for Tikarapara Flow Gauge Station ...................... 40 Figure 2-10:
Simulated Return Period Discharges .............................................................. 40 Figure 2-11:
HEC RAS model for Mahanadi Delta .............................................................. 41 Figure 2-12:
Flood Hazard Map for 100-year return period along with 2003 event flooding. 42 Figure 2-
13: Wards reported water logging problems during the 2014 ................................ 43 Figure
2-14: Seismotectonic map of areas around Bhubaneswar ....................................... 45 Figure
2-15: Ward level PGA map of Bhubaneswar city at hard rock-level (after GSHAP).. 46 Figure
2-16: Spatial variation of (a) Vs30 values and (b) Soil-Index for Bhubaneswar city .. 48
Figure 2-17: Site Amplification Factors for different Soil Index Values (=Vs30 Values) .......
48
Figure 2-18: Ward level PGA based Probabilistic Seismic Hazard Map For 10% Probability in
50 Years (475-Year Return Period) for Bhubaneswar city ....................................... 49
Figure 2-19: Temporal trends in observed annual mean surface air temperatures at
Bhubaneswar, India................................................................................................. 52
Figure 2-20: Temporal trends in observed annual mean maximum (day-time high) surface air
temperature at Bhubaneswar, India......................................................................... 52
Figure 2-21: Temporal trends in observed annual mean minimum (night-time low) surface air
temperature at Bhubaneswar, India......................................................................... 53
Figure 2-22: Anomalies in observed maximum (day-time high) surface air temperature during
summer season (with respect to the 1951-1980 mean) at Bhubaneswar. An
accelerated increasing trend is evident in recent decades....................................... 54
Figure 2-23: Anomalies in observed minimum (night-time low) surface air temperature during
summer season (with respect to the 1951-1980 mean) at Bhubaneswar. The
increasing trend in recent decades is not pronounced as the observed maximum
temperature trend.................................................................................................... 54
Figure 2-24: Percent deviation in observed rainfall with respect to 1991-2010 mean at
Bhubaneswar during monsoon season.................................................................... 55
Figure 2-25: Incidence of ADD cases across the year in Bhubaneswar city (derived from
district level data). ................................................................................................... 58
Figure 2-26: Seasonal incidence of malaria in Odisha State ............................................... 58
Figure 2-27: Malaria incidence trend during the last three years in Bhubaneswar city.........
58
List of Tables
Table 2-1: India Meteorological Department cyclone classification by sustained wind
speed ............................................................................................................................
.... 25
Table 2-2: List of storm events used for the study (1877-2013)........................................... 26
Table 2-3: List of notable cyclones, areas affected and lives lost (SMRC 1998 & IMD)...... 29
Table 2-4: Ward-wise cyclonic wind hazard statistics .......................................................... 35
Table 2-5: Soil Classification Scheme based on Shear Wave Velocities .............................
47 Table 3-1: Building Categories by construction materials and Structural Types ..................
76 Table 3-2: Residential built-up area by structural types .......................................................
79 Table 3-3: Unit Replacement Cost of Different Building Types ............................................
94
Table 4-1: Growth in population and slum population in Bhubaneswar city during the last 5
decade .................................................................................................................. 101
Table 4-2: Social indicators selected for social vulnerability analysis ................................ 103
Table 4-3: Incidence of major diseases across various income groups .............................
105
Table 5-1: Probable Maximum Losses (PML) for the Earthquake Hazard in Bhubaneswar
city......................................................................................................................... 115
Table 5-2: Estimation of projected losses to various sectors for the earthquake hazard for a
475-year return period hazard ............................................................................... 119
Table 5-3: PML for the Cyclonic Wind Hazard in Bhubaneswar city .................................. 119
Table 5-4: Estimation of projection of losses to various sectors for the Cyclonic Wind
hazard ...........................................................................................................................
... 127
Table 5-5: Summary of health effects of weather and climate, IPCC (2007) and WHO
(2009) ...........................................................................................................................
... 128
Table 5-6: Estimated numbers of affected people and causalities (serious injuries including
fatalities) for 475 years return-period earthquake hazard scenario event............... 129
Table 9-1: Ward-wise distribution of population................................................................. 145
Table 9-2: Ward-wise distribution of population based on literacy rate ..............................
147 Table 9-3: Distribution of the Census houses based on the condition of the
houses ......... 149 Table 9-4: Ward-wise distribution of Census houses based on
uses................................. 152 Table 9-5: Ward-wise distribution of Census houses by
building structural types .............. 155 Table 9-6: Estimated built-up floor area for different
housing types (in sq. m.) .................. 158 Table 9-7: Unit replacement costs of different
building/ infrastructure types ...................... 159
Table 9-8: Ward-wise estimated exposure value for different houses by occupancy and uses
(INR in Crores) ...................................................................................................... 160
Table 9-9: Ward-wise estimated length and exposure values for different types of roads..
163 Table 9-10: Ward-wise estimated length and exposure values for railway
network ........... 166 Table 9-11: Infrastructure details and estimated exposure value for
Bhubaneswar Airport 167 Table 9-12: Ward-wise estimated length and exposure values for
bridges and flyovers .... 168
Abbreviations Used
DM Disaster Management
EP Exceedance Probability
km Kilometer
mm Millimeter
UN United Nations
1 Background
India has experienced exponential urban growth in the last few decades with more than 70%
of its urban population residing in Class-I cities. As per 2011 Census, there are 468 Class-I
cities compared to 399 such cities in 2001. Fast growth in these urban centers also leads to
increased exposure of the urban population and infrastructure to natural hazards. The
impact of climate change has accentuated the risk of urban centers to natural hazards,
particularly, the hazards related to hydro-meteorological phenomena.
Bhubaneswar, the capital city of Odisha, has a population of about 8,40,834 with a
population density of 6,228 per sq km (Census, 2011). The city is experiencing very high
growth both in terms of urban built as well as population. The city is exposed to various key
hazards- cyclonic winds, floods, earthquakes, heat waves, and epidemics. As per the
Bureau of Indian Standards (BIS) code IS:1893 (2002) and BMTPC Atlas (2006), the city is
located in the seismic zone III that is a moderate earthquake risk zone class.
In addition, to support and be part of the State Disaster Risk Reduction (DRR) activities, the
city administration is active in developing measures towards a climate risk resilient urban
center. The city is part of the UNISDR global campaign of “The Making Cities Resilient
Campaign” and is Recipient of “SASAKAWA Recognition 2011” and Role Model for
Community Preparedness.
The city has taken several proactive steps towards climate change adaption, in particular to
the power, roads, and drainage infrastructure development activities. The new building
byelaws are in place with design safety norms (BDA, 2008). Development plans also look
into the risk zones of the city while considering any new development projects.
Bhubaneswar City has been selected as one of the eight cities in India for implementing the
Climate Risk Management Project on a pilot basis under the framework of the Urban
Disaster Risk Reduction project of GOI-UNDP.
The ongoing Government of India (GOI)-UNDP Disaster Risk Reduction (DRR) program aims
to strengthen the capacities of government, communities and institutional structures by
undertaking DRR activities at various levels and develop preparedness for recovery. Under
this program, eight cities (including Bhubaneswar) prone to multi-hazards in the country
were identified, and selected for detailed hazard vulnerability and risk assessment studies.
These studies will support the local administration and the community to develop risk
resilience through understanding of hazards, vulnerability and risk and integrate appropriate
mitigation and management practices to protect the community and its assets. The project
emphasizes a participatory approach for developing the capacity of the cities in integrating
Climate Change Adaptation (CCA) and DRR concerns at city level plans.
The main objective of the proposed multi-hazard risk and vulnerability analysis assignment is
to assess the extent of risk and the vulnerabilities of Bhubaneswar city particularly to climate
related hazards. The outcome of the exercise is expected to help identify a set of structural
and non-structural steps that UNDP, City Administration and other stakeholders can take to
mitigate the risks posed by various hazards. It also aims to consider the future climate
change scenarios such that the development activities accommodate this understanding to
reduce the impact in the medium and long- terms.
The present study provide quantified hazard, vulnerability and risk of prominent hazards
prevalent in the city; development of short, medium and long term mitigation strategies for
DRR in the city and develop capacity of city stakeholders in mainstreaming DRR activities in
the city development activities.
Area 135 sq km
Number of wards 67
Slum details
Weather characteristics
Infrastructure
Table 2-1: India Meteorological Department cyclone classification by sustained wind speed
Sl. No. Storm category (Intensity) Abb. Wind speed (knots) Wind speed (kmph)
Table 2-2: List of storm events used for the study (1877-2013)
Sl. No. Day Month Year Category/Grade
46 15 7 1920 Depression
78 28 9 1945 Depression
79 16 8 1946 Depression
81 12 9 1949 Depression
83 1 9 1954 Depression
86 28 8 1958 Depression
88 3 7 1959 Depression
89 29 6 1960 Depression
90 4 8 1964 Depression
91 16 7 1966 Depression
92 2 9 1966 Depression
93 30 7 1967 Depression
98 25 6 1975 Depression
99 9 9 1975 Depression
The data of past cyclonic disasters was collected from India Meteorological Department
(IMD) reports, SAARC Meteorological Research Centre (SMRC, 1998), and from several
research publications and is presented in Table 2-3. These events affected Bhubaneswar
City in the last 137 years and resulted in loss of lives and property. Based on an analysis of
historical data, Bhubaneswar City witnessed several storms ranging from Tropical
Depressions (31 – 61 km/hr) to very strong storms (88-167 km/hr). The storm tracks of past
events from 1877 to 2013 are depicted in Figure 2-1.
re 2-1: Storm tracks of past events from year 1877 – 2013 (Source: IMD and JTWC)
Table 2-3: List of notable cyclones, areas affected and lives lost (SMRC 1998 & IMD)
S No. Date Description of the meteorological event
1 September 7- Crossed South Odisha coast and adjoining North Andhra coast on
14, 1971 September 10 and moved up to eastern Delhi. 90 People died and
8,000 Cattle heads perished. This system caused considerable damage
to crops, houses, telecommunications and other property in the coastal
districts of Odisha. viz., Ganjam, Puri, and Cuttack.
2 September Crossed South Odisha coast near Gopalpur on September 22. Caused
20- 25. 1971 considerable damage to crops and houses due to flood and heavy rain
at Vamsadhura village in Srikakulum and Koraput districts.
3 October 26- Crossed Odisha coast near Paradip early in the morning of October 30.
30,1971 Maximum wind speed recorded was 150-170 kmph .Lowest Pressure
recorded 966 hPa near the center of the storm. 10,000 People died and
more than one million people were rendered homeless. 50,000 Cattle
heads perished and 8,00,000 houses were damaged.
4 September Crossed extreme South Odisha coast near Gopalpur on the afternoon
20- 25, 1972 of 22nd and weakened into a depression by the morning of the 23rd.
5 November 3-9, Crossed Odisha coast close to and north of Paradip on the early
1973 morning of 9th. It weakened rapidly and lay as a trough over Odisha the
same day. Maximum wind reported was 100 kmph at Paradip and
Chandbali experienced surface winds of 100 kmph .This cyclone
caused some damage to standing crops in the coastal districts of
Odisha between Paradip and Chandbali.
6 September,2 Crossed Odisha coast near Puri on the early morning of September 26,
4- 28. 1981 weakened into a depression on that evening over interior Odisha, and
adjoining East Madhya Pradesh. 5 Launches were lost in the Bay and
many houses were damaged in Midnapur district of West Bengal and
Cuttack district of Odisha.
7 May 31 to Crossed on 3rd June near Paradip, Odisha. As a result of high tides
June 5th 1982 damage caused all along this coastal stretch. This cyclone caused
heavy damage in the coastal districts of Puri, Cuttack and Balasore.
8 October 9- Crossed North Odisha coast near Chandbali in the forenoon of 14 th. This
14.1984 system caused some damage in Cuttack and Balasore districts of
Odisha and Midnapore district of West Bengal
9 17-21 Sept. Crossed on 20th Sept. close to Puri .For three consecutive days, due to
1985 1.5 m sea-wave, Puri coast was inundation.
10 13-17 Oct. 1985 Crossed near Balasore on 16th Oct. High tidal crossed near Balasore
on16th October. High tidal wave of about 16’ to 18’ was observed.
12 23-27 May 1989 Crossed 40 km northeast of Balasore. 61 persons died in Odisha and
West Bengal.
13 26-27 Oct 1909 Ganjam district was severely affected. Puri and Balasore were less
affected with violent winds and had lower rainfall. 22 humans and many
cattle were killed. Damage ran into several lakhs of rupees. INR 15
lakhs damage was in Gopalpur alone.
14 13-18 Nov 1923 High floods occurred in the rivers in Ganjam district. Puri district was
also affected. Immense destruction to communication services including
railways. Considerable damage to crops. 20 humans and a few hundred
cattle killed. A large number of public and private properties including
irrigation works were damaged.
15 1-6 Oct 1906 Cyclonic storm crossed the coast north of Puri. Considerable damage to
trees, roads, houses, even Pucca buildings in Puri.
16 15-16 Nov 1942 Less severe than the one on 16 October 1942. The cyclone was close
to Odisha coast and weakened.
Creation of Historical
Event Catalogue
Development of
Probabilistic Scenarios
Application of Hazard
Models for probabilistic
Scenarios
)r
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100
Y
i
75
r
50
p
25
r
0
R
150
0 25 50 75 100 125 150 175 200 225 Wnd Speed (kmph)
125
Step 2
Distribution Step 1 Step 3
• Storm Parameters Before Landfall – Duration of the storm cell of the grid
• Wind Foot Print ‒ Calibration
– Track (Lat, Long)
– Pressure drop ‒ 250 m grid cells over area of interest ▪ Hazard mapping
– Radius of maximum wind – Forward ‒ Simulate storm motion using time
step process ‒ Repeat step 2 for all storms
velocity
‒ Record maximum wind speed in each‒ Generate wind hazard map
1 66 69 78 113 165
2 65 69 78 113 166
3 65 69 78 115 170
4 66 69 78 117 178
5 66 69 77 117 174
6 65 69 77 113 166
7 65 69 77 113 165
8 65 69 77 113 165
9 66 69 76 115 169
10 66 69 77 116 172
11 65 69 77 115 169
12 66 69 77 115 169
13 65 69 77 114 165
14 65 68 77 113 164
15 65 69 78 113 164
16 65 69 77 114 165
17 65 69 77 116 170
18 65 69 76 117 175
19 65 68 77 116 173
20 65 69 77 113 164
21 65 69 77 113 163
22 65 69 78 112 159
23 65 70 78 112 159
24 65 69 78 113 161
25 65 69 78 113 163
26 65 69 77 114 164
27 65 69 77 114 165
28 65 68 77 115 167
29 65 68 77 115 168
30 65 68 77 116 170
31 65 68 77 116 171
32 65 68 77 117 173
33 65 68 77 116 171
34 65 68 77 116 170
35 65 68 77 115 168
36 65 69 78 115 166
37 65 69 78 114 165
38 65 69 78 114 164
39 65 69 78 114 165
40 65 69 78 115 167
41 65 69 78 116 169
42 65 69 78 116 170
43 65 68 77 116 170
44 66 69 78 117 172
45 65 68 78 116 168
46 65 69 78 115 165
47 65 69 78 114 164
48 65 69 78 114 162
49 65 70 78 112 160
50 65 69 78 113 162
51 65 69 78 114 163
52 65 69 78 115 165
53 65 69 78 115 166
54 65 69 78 115 165
55 65 69 78 115 167
56 65 69 78 116 168
57 65 69 78 116 169
58 65 69 78 116 168
59 65 69 78 115 166
60 65 69 78 115 166
61 65 69 78 115 164
62 65 69 78 114 162
63 65 69 78 113 160
64 65 69 78 113 161
65 65 69 78 113 159
66 65 69 78 113 159
67 65 70 79 115 163
∙ Cyclonic wind hazard maps will help the policymakers and decision makers to understand
the severity of potential storms and allow them to take necessary action to ensure
sustainable development by introducing necessary programs and measures.
∙ All the map results would be useful for the planning and design department to make
decisions. These maps would provide a basis for the government for storm prediction
and estimation of damage due to cyclonic winds.
∙ Most important sectors like education, health, housing, lifelines and transportation need
special attention for storm safety. The cyclonic windstorm zones will provide fair
understanding about expected performance of structures during cyclonic windstorms and
necessary measures to protect the structures.
∙ The zones will further help the local urban government to introduce and enforce building
byelaws and building codes to protect the urban infrastructure.
∙ These maps will also be helpful to national and international NGOs to prioritize disaster risk
reduction strategies.
∙ The cyclonic wind hazard assessment maps will help policy makers, planners, decision
makers, and related actors to better plan and implement an effective system related to
storm hazard management. However, to get a clear and more detailed picture of the
cyclonic wind hazard assessment in Bhubaneswar, it is recommended to integrate and
utilize the networking system of storm monitoring and observations, which include the
neighboring districts of Bhubaneswar.
2.2 Flood Hazard Assessment
The flood hazard assessment evaluates the frequency and severity of various flood events
at different recurrence intervals or return periods ranging from more frequent to rare events,
based on hydrological and physical information. Due to various flood control measures in
upstream areas, overall flood risk for city of Bhubaneswar is very low. In fact, flood resilience
of the city area was one of the driving factors for shifting the capital from Cuttack.
Continuous heavy rainfall during the monsoon season can cause water logging in some
areas of the city. A comprehensive modeling approach has been adopted for examining the
riverine flood hazard for city areas.
2.2.1 HYDROLOGY OF FLOODS
The city of Bhubaneswar is situated on one of the anabranch of river Mahanadi in its delta
area. The Mahanadi River forms the northern boundary of the city. The Mahanadi basin
extends over an area of 1,41,589 km2, which is nearly 4.3% of the total geographical area of
the country and drains across Chhattisgarh, Odisha, Bihar, and Maharashtra (Figure 2-7).
About 46% of the drainage area of Mahanadi lies within Odisha State. The upper basin is
saucer shaped and mostly lies in Chhattisgarh state. Complete Mahanadi river basin is
almost circular in shape with a diameter of about 400 km and an exit passage of about 160
km length and 60 km breadth. Mahanadi River discharges into the Bay of Bengal in Odisha
forming significantly larger delta area. The annual average rainfall in the basin is about 1,500
mm. The heavy rainfall received by the basin during the monsoon months is mostly caused
by the monsoon depressions. The depressions often cause heavy to very heavy rainfall
along and near their tracks. These depressions originate in the Bay of Bengal, cross the
eastern coast of the country, and move further inland in a west to northwesterly direction.
The mean annual rainfall over the entire basin is around 1,400 mm and more than 60% of it
is contributed by the southwest monsoon season.
As described above floods due to overflow from Mahanadi River is a major cause of flooding
in the entire Mahanadi Delta including Cuttack. This section examines the flood hazard for
the city of Bhubaneswar.
∙ Identification, acquisition, compilation and review of all relevant hydro meteorological and
biophysical data. These data includes terrain, soil, land use land cover, runoff/river
discharge and flood protection measures to form the input for the model.
∙ Probabilistic analysis of runoff to simulate various return period events (from frequent to
rare events) for flow gauge station upstream of the city.
∙ Hydraulic modeling to estimate flood levels throughout the flood plain areas in the city for
various flows generated from key return period events
∙ Flood hazard mapping to show flood extent and flood depth for a range of events, which is
the end result of hazard assessment.
Final Report Confidential Page 38 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
∙ Review of published probabilistic seismic hazard analyses for a key return periods and
choose the hazard value(s) at hard rock level
∙ Model the soil-amplification on a finer grid cell of 0.1 km x 0.1 km using NEHRP
(2007)/HAZUS-MH soil classification scheme
∙ Convolute the hazard value(s) at hard rock level with soil amplification factors, and
generate earthquake hazard maps for 10% probability of exceedance (475 year return
period)
∙ Compute the seismic hazard values at Uniform Resolution Grids (URG) at 0.1 km x 0.1 km
for Bhubaneswar city
∙ Generate GIS based seismic hazard map at ward level
Seismic hazard mapping to show expected peak ground motion (Peak Ground Acceleration,
PGA) for 10% probability of exceedance (475 year return period), which is the end result of
hazard assessment.
2.3.1 SEISMOTECTONICS OF THE AREA AROUND BHUBANESWAR
In areas around Bhubaneswar, several faults have been identified in the region and some
have shown evidence of movement during the Holocene epoch (SEISAT, 2000). The
Brahmani Fault in the vicinity of Bonaigarh is one among them (SEISAT, 2000). The
Mahanadi River also flows through a graben structure. As per Seismotectonic Atlas of India
(SEISAT, 2000), several deep-seated faults are situated beneath the Mahanadi delta.
The Mahanadi and Brahmani graven, Mahanadi delta and parts of Balasore and Mayurbhanj
districts come under earthquake risk zone –III (moderate damage risk zone) as per the
earthquake risk zonation map prepared by Bureau of Indian Standards and published by
Building Material Technology Promotion Council of India (BMTPC, 2006). As per Seismic
Zoning Map of India (IS: 1893, 2002, 2014), Bhubaneswar city is located in Seismic Zone-III.
In spite of the moderate, non-damaging earthquakes observed so far in and near
Bhubaneswar, it cannot be confidently said that higher intensity earthquakes are unlikely.
Recently, on May 21, 2014 an earthquake of magnitude 6 occurred in the Bay of Bengal,
which was severely felt in different parts of Bhubaneswar city. However, there was no report
Using Wald et al. (2004) and Wald and Allen (BSSA, 2007) approach, gridded (0.1 km x 0.1
km) Vs30 map and corresponding soil-index map have been generated using NEHRP
(Figure 2-16) classification.
The site–dependent amplification factors followed the non-linear two-dimensional soil
amplification factors modified from Choi and Stewart (2005); and Walling, M, Walter Silva,
and Norman Abrahamson (2008), which relate non-linear multipliers based on the level of
ground motion (PGA) and averaged soil index assigned for a given location.
Final Report Confidential Page 47 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
Figure 2-16: Spatial variation of (a) Vs30 values and (b) Soil-Index for Bhubaneswar city
The plot of amplification factors for different soil index classes (corresponding to respective
Vs30 values) normalized by the amplification for reference BC soil Vs30=760 m/s (soil index
1.5), used in the study is shown in Figure 2-17.
Figure 2-17: Site Amplification Factors for different Soil Index Values (=Vs30 Values)
Final Report Confidential Page 48 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
The site amplification factors were then calculated based on the high resolution Vs30 based
soil index map, and these have been multiplied with the PGA Rock values derived (as given
in Figure 2-15) for the study area.
The final seismic hazard map generated at ward level contains seismic ground motion
estimates at surface level, by taking into account the local soil-amplification factors in
different parts of Bhubaneswar city (Figure 2-18).
Figure 2-18: Ward level PGA based Probabilistic Seismic Hazard Map For 10% Probability in
50 Years (475-Year Return Period) for Bhubaneswar city
As discussed earlier, from Figure 2-18 it is clear that different parts of the city are expected
to experience different levels of ground motion due to local soil amplification.
Figure 2-20: Temporal trends in observed annual mean maximum (day-time high) surface air
temperature at Bhubaneswar, India
It is interesting to note from Figure 2-20 and Figure 2-21 that the rate of increase in daytime
maximum temperature at Bhubaneswar is higher in comparison to the nighttime minimum
temperatures meaning thereby that the diurnal temperature range at this site is increasing in
recent decades. This is further illustrated in Figure 2-22 and Figure 2-23 wherein the trends
in summer time maximum and minimum temperatures at Bhubaneswar are shown.
Figure 2-23: Anomalies in observed minimum (nighttime low) surface air temperature during
summer season (with respect to the 1951-1980 mean) at Bhubaneswar. The increasing
trend in recent decades is not pronounced as the observed maximum temperature trend
Figure 2-24: Percent deviation in observed rainfall with respect to 1991-2010 mean at
Bhubaneswar during monsoon season
Urban heat islands increase overall electricity demand, as well as peak demand, which
generally occurs on hot summer weekday afternoons, when offices and homes are running
cooling systems, lights, and appliances. During extreme heat events, which are exacerbated
by urban heat islands, the resulting demand for cooling can overload systems and require a
utility to institute controlled rolling brownouts or blackouts to avoid power outages.
Apart from impact on energy-related emissions, elevated temperatures can directly increase
the rate of ground-level ozone formation. Ground-level ozone is formed when NOx (mono
nitrogen oxides NO and NO2) and volatile organic compounds (VOCs) react in the presence
of sunlight and hot weather. If all other variables are equal, such as the level of precursor
emissions in the air and wind speed and direction, more ground-level ozone will form as the
environment becomes sunnier and hotter.
In 2010, there was an epidemic outbreak of High incidence of disease recorded in the slum
Influenza H1N1 reported in Khordha district with pockets of the city
32 persons killed in the State (IDSP 2012). Malaria cases are dipping while there is an
However, the city did not report any alarming increase in waterborne diseases
numbers. In 2012, the Central Poultry
Development Organization (CPDO) located in Warns take adequate preventive steps to avoid
disease outbreak
and the city declared a 3 km radius as surveillance zone. The Salia Sahi, the biggest slum in
Odisha, falls under the alert zone and the alter zone spreads across 21 of the 67 wards in
the city. One person was reported H1N1 positive in the city in 2012.
The incidence of water borne and vector borne diseases has correlation with heavy rainfall.
However, there is a high incidence of water borne diseases across the year (Figure 2-25)
and also malaria incidence (Figure 2-26), even though reported cases of both these
diseases are high during July and August months.
s
3500 3000 2500 2000 1500 1000 500 Jan Feb Mar Apr May Jun Jul Aug Sep Oct
a
Nov Dec
0
c
2012
r
2013
b
Figure 2-25: Incidence of ADD cases across the year in Bhubaneswar city (derived from
district level data).
Figure 2-27: Malaria incidence trend during the last three years in Bhubaneswar city
The state level statistics on malaria show a decreasing trend.
It is interesting to note that there is no hotspot for any of the diseases in the city; rather the
whole city has high incidence of water borne diseases and malaria. All the wards surveyed
irrespective of income/economic classes and house types they are living in reported high
incidence of both water borne diseases and malaria.
12 10
p
8
Diarrhea Gastroenteritis Jaundice malaria
6
s
s
4
a
2
d
0
e
4 9 10 14 16 20 21 22 50 53 Wards
Figure 2-29: Distribution of disease cases reported across the wards of Bhubaneswar city
The city Capital hospital records document reported cases like snake bite, accidental
injuries, ADD, measles and acute respiratory infections. Monthly sex-wise data is available
for these diseases for the last 5 years. However, spatial distributions of the disease cases
are not available for spatial analysis. There is an increase in accident injuries during the last
three years and more male cases have been reported as compared to female cases.
s
2001-5000
a
c
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d
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Figure 2-30: Disease incidence across income group (household survey 2014)
3
WMO, 2013: The Global climate 2001-2010: A decade of climate extremes, WMO No. 1103, 61 pp.
4
State of the Climate report - 2012: NOAA’s National Climatic Data Center, Published August 2013.
1.6
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Bhubaneswar Odisha India
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2.0
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Figure 2-31: A comparison of rate of increasing trends in surface air temperature since
historical times in Bhubaneswar, Odisha and India.
∙ Historical weather data was collected from the India Meteorological Department (IMD)
and other available sources.
∙ Projected climate data obtained from one of the state-of-the-art Global Climate Models,
namely HadGEM2-ES model (UK). The reason for selection of this GCM is that this
model has demonstrated reasonable degree of skill in simulating the baseline
climatology over the Indian region. The emission scenario considered for
development of future climate change scenarios is RCP 6.0 (Representative
Concentration Pathways) emission pathways and identified as modest future
emission scenario bracketing plausible future climate change without stringent
mitigation policies.
∙ Temporal trends in rainfall and surface air temperature were assessed using historical
weather data.
∙ Spatial distribution patterns in maximum and minimum surface air temperatures and
rainfall over Bhubaneswar were developed using above-mentioned HadGEM2-ES
model data in GIS platform (ArcGIS 9.2). These analyses provide the likely shifts in
spatial changes of temperature and rainfall during 2040s (2026-2055) and 2080s
(2061-2090) with respect to baseline time period (1961-1990). The results of this,
together with the trend analysis, can be used to assess the implications of climate
change on various meteorological and hydro-meteorological hazards (e.g., drought,
flood, and heat wave etc.).
2.6.4 ANALYSIS RESULTS
India, as a whole, has experienced its average annual surface air temperature rise by about
0.5°C during the past century as also observed across the continents and globe and thus
supports its attribution to anthropogenic influences on global scale. The rise in surface
temperature seems to have accelerated since 1960s and particularly so during the past
decade. Past studies5reported that surface air temperatures over India are going up at the
rate of 0.4°C per decade, with peaks during the post-monsoon and winter seasons. Summer
temperatures over the State of Odisha in India are projected to increase by 2.5°C during
2040s and 3.5°C during 2080s. Winter temperatures could increase by as much as 3.0°C
during 2040s and 4.5°C by 2080s. According to a more recent study, south Asian summer
temperatures are projected to increase by 3°C to nearly 6°C by the end of 21 st Century with
the warming most pronounced in the northwestern parts of India 6. By the time 1.5°C warming
is reached, heat extremes that are unusual or virtually absent in today’s climate in the region
are projected to cover 15% of land areas in summer. Some regions are projected to
experience unprecedented heat during more than half of the summer months.
The recent climate modeling results (CMIP5 simulations) suggest that greenhouse gases
have contributed a global mean surface warming in the range of 0.5°C to 1.3°C over the period
of 1951−2010, with the contributions from other anthropogenic forcings, including the cooling effect
of aerosols, likely to be in the range of −0.6°C to 0.1°C. On regional scales, the confidence in
model capability to simulate key climate variables remains lower than for the larger scales.
However, there is high confidence that simulation of regional-scale surface temperature has
significantly improved now than at the time of the AR4. The new versions of Earth System
Models reproduce better some important circulation features modulating the climate
anomalies. There is high confidence that the key circulation features controlling the Asian
monsoon and El Niño-Southern Oscillation (ENSO) based on multi-model simulations have
improved since AR4 (IPCC, 2013)7.
A spatial distribution of rise in annual mean maximum and minimum surface air
temperatures in Bhubaneswar City of Odisha, as downscaled from outputs from one of the
5
Lal, M. 2003: Global climate change: India’s monsoon and its variability, Jr. Environmental Studies &
Policy, 6, 1-34.
6
Rajiv Kumar Chaturvedi, Jaideep Joshi, Mathangi Jayaraman, G. Bala and N. H. Ravindranath, 2012:
Multi-model climate change projections for India under representative concentration pathways, Current
Science, VOL. 103, NO. 7, 12 pp.
7
IPCC, 2013: Summary for Policymakers, in: Stocker, T.F.; Qin, D.; Plattner, G.K.; Tignor, M.; Allen, S.K.;
Boschung, J.; Nauels, A.; Xia, Y.; Bex, V.; Midgley, P.M. (Eds.) Climate Change 2013: The Physical
Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental
Panel on Climate Change, Cambridge University Press, Cambridge, United Kingdom and New York, NY,
USA.
Final Report Confidential Page 62 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
state-of-the-art global climate model used in CMIP5 simulations (Taylor et al., 2012) 8for the
5th scientific assessment report of IPCC under RCP 6.0 scenario, is presented here. The
projected rise in maximum (day-time) and minimum (night-time) surface air temperatures in
Bhubaneswar city of Odisha state at two time slices, namely, 2040s and 2080s are
illustrated in Figure 2-32 and Figure 2-33 respectively. The plausible changes in annual
mean and monsoon season rainfall over Bhubaneswar City of Odisha for two time slices,
namely, 2040s and 2080s are depicted in Figure 2-34 and Figure 2-35 respectively. The
model used here for the purpose is HadGEM2-ES model developed by Met Office Hadley
Center (UK). The emission scenario RCP 6.0 used for these projections is identified as
modest future scenario, bracketing plausible future climate change without stringent
mitigation policies. In our previous research and analysis of model validation, this model has
demonstrated reasonable degree of skill in simulating the baseline climatology over the
Indian sub-continent (HadGEM2-ES is found to be the best-performing individual model in
simulating the annual and seasonal Indian climatological characteristics, followed closely by
a few others).
Figure 2-32: Projected rise in mean maximum and minimum surface air temperatures during
hot summer months for 2040s in Khordha District of Odisha (Bhubaneswar city is marked
with black boundary here)
Further, it is evident from Figure 2-32 that the mean maximum day-time surface air
temperatures during hot summer months in the city of Bhubaneswar is likely to rise on an
average by about 0.8°C around the middle of this century while the rise in mean night-time
minimum surface air temperature during the hot summer months could exceed 1.1°C by the
middle of this century. This illustration further suggests that the diurnal temperature range
would reduce in future in Bhubaneswar city of Odisha State. During 2080s, the maximum
day-time and minimum night-time surface air temperatures in the city of Bhubaneswar on hot
summer months mean basis are expected to rise in excess of 2.1°C and 2.3°C respectively
(Figure 2-33). These projections of rise in surface air temperatures in future suggest that the
intensity of heat waves in the city of Bhubaneswar should become stronger with time during
peak summer months and record high temperatures could be experienced here more often
in future.
8
Taylor, Karl E., Ronald J. Stouffer, Gerald A. Meehl, 2012: An Overview of CMIP5 and the Experiment
Design. Bull. Amer. Meteor. Soc., 93, 485–498.
Final Report Confidential Page 63 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
Figure 2-33: Projected rise in mean maximum and minimum surface air temperatures during
hot summer months for 2080s in Khordha District of Odisha (Bhubaneswar city is marked
with black boundary here)
An examination of the change in rainfall patterns as depicted in Figure 2-34 suggests that
the annual mean and monsoon season rainfall is projected to increase by about 0.46 mm /
day and by about 1.12 mm / day respectively (a total of about 170 mm in a year) over
Bhubaneswar city by the middle of this century. Figure 2-35 reveals that the seasonal
monsoon rainfall could increase by about 2.27 mm / day (a total of about 270 mm in the
season) over Bhubaneswar city by the end of this century. On annual basis, the rainfall
would increase over Bhubaneswar city by around 0.81 mm / day (a total of about 295 mm in
a year) by the end of this century. It is evident from Figure 2-34 and Figure 2-35 that, on an
average, Bhubaneswar city is likely to experience a significant increase in monsoon rainfall
only in the latter part of this century.
Figure 2-34: Projected change in annual and monsoon season rainfall (in mm/ day) for
2040s in Khordha District of Odisha (Bhubaneswar city is marked with red boundary
here)
While an enhanced focus has been placed in recent years on short-term climate change
projections (say 2040s), it must be acknowledged that there remain many uncertainties
regarding future climate change on local scales. This is because the future level of global
greenhouse-gas emissions is uncertain, and the available knowledge about the climate-earth
ocean system is still rather inadequate for reliably forecasting the local climate change. The
climate information and projections provided in this study should, therefore, be considered
only as indicative, not predictive.
According to a recent World Bank Report 9, a four degrees Celsius world would bring about
unprecedented heat waves, severe drought, and major floods in many regions, with serious
impacts on ecosystems and associated services. In a summary for policy makers report of
the Working Group 2 of the IPCC (March 2014) 10, this has been reasserted with a high
degree of confidence that globally, the impacts from recent climate-related extremes, such
as heat waves, droughts, floods, cyclones, and wildfires, reveal significant vulnerability and
exposure of some ecosystems and many human systems to current climate variability.
Impacts of such climate-related extremes include alteration of ecosystems, disruption of food
production and water supply, damage to infrastructure and settlements, morbidity and
mortality, and consequences for mental health and human well-being. For countries at all
levels of development, these impacts are consistent with a significant lack of preparedness
for current climate variability in some sectors. In such a scenario, the frequency and duration
of heat waves and extremes in daily rainfall in some States of India including Bhubaneswar
city is also likely to increase substantially, taking a toll on disruption to city life and human
health. Agriculture too would be adversely affected by the thermal stress due to rise in
temperature although part of the loss in soil evapotranspiration due to higher temperature
could be compensated by increase in rainfall. Intense rainfall spells could lead to loss of top
soils in farmlands and cause sedimentation concerns in river basins and deltas. A warming
of the global surface temperature by 4°C could lead to an associated sea level rise of one
9
World Bank, 2012: Turn Down the Heat: Why a 4°C Warmer World Must be Avoided, World Bank, Washington,
D.C.
10
IPCC, 2014: Summary for Policy Makers, in: Christopher B. Field (USA) et al., Climate Change 2014: Impacts,
Adaptation, and Vulnerability. Contribution of the Working Group II to the Fifth Assessment Report of the
Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge, United Kingdom and New
York, NY, USA.
11
IPCC, 2013: Summary for Policymakers, in: Stocker, T.F.; Qin, D.; Plattner, G.K.; Tignor, M.; Allen, S.K.; Boschung, J.;
Nauels, A.; Xia, Y.; Bex, V.; Midgley, P.M. (Eds.) Climate Change 2013: The Physical Science Basis. Contribution of Working
Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press,
Cambridge, United Kingdom and New York, NY, USA.
∙ An understanding of projected climate scenarios and potential impacts and the limitations
of the projections;
∙ Identification of who/what are the most vulnerable groups, areas, sectors, and urban
systems and how they may be affected;
∙ Identification of the range of factors that systematically combine to make them vulnerable,
including both direct (e.g. exposure to hazards) and indirect (e.g. regional or
international food security) factors; and
∙ Assessment of existing capacities to adapt
Figure 3-5: Distribution of non-working population and child population (<6 Years)
Figure 3-6 presents the density of population by municipal wards. It is observed that ward
number 21 has the highest population density of more than 54,969 persons/ sq. km.
whereas ward number 15 is the least densely populated (about 1,136 persons/ sq. km.)
amongst all the wards.
3.4.2 HOUSING
In the present study, building classification is carried out primarily based on occupancy types
and structure types. The occupancy-based classification differentiates housing into four
occupancy classes viz., residential, commercial, industrial, and others. The class named as
others comprises of occupancy classes such as schools and colleges, hospitals and
dispensaries, government offices, places of worship etc. Structure based classification,
categorizes the houses based on the construction materials used (roof and wall materials)
as per Census 2011, their architecture, and height. The analysis also considered classifying
houses into occupied and vacant (Figure 3-8). The different classifications represent
elements that are distinctly vulnerable to the same level of hazard. The determined exposure
value is used as an input to the vulnerability and risk assessment.
As mentioned above, the source of housing data is the Census of India (2011), which
provides city-level data based on the usage and construction materials. Further, the data
generated from the field survey conducted by the team and information gathered from local
builders is used for filling the data gaps and validation of information. In this process, the
city-level data is brought to the ward level using the household numbers available at ward
level in the demographic data table of Census. These statistics are then correlated with the
Final Report Confidential Page 73 of 174
Multi-Hazard Risk and Vulnerability Analysis for the City of Bhubaneswar, Odisha
housing data received from BMC and finally ward-wise distribution of houses based on their
occupancy and structural class are determined. Figure 3-7 presents the building footprints
delineated from LISS IV satellite images for Bhubaneswar city. The classifications are done
based on the tone, texture, shape, size, pattern, and associations between buildings as
present on satellite images. For example, residential strips generally have a uniform size and
spacing between structures with linear driveways and lawn areas. Commercial strips are
more likely to have buildings of different sizes with non-uniform spacing between them. They
are also characterized by the larger driveways and parking areas associated with them.
Commercial areas are often abutted by residential, agricultural, or other contrasting uses
that help in defining them. Similarly, Industrial areas are generally situated at some distance
from urban centers. The ward-wise distribution of houses based on their occupancy and
structure is given in
1 Grass/ thatch/ bamboo/ Grass/ thatch/ bamboo/ wood/ plastic/ polythene etc. used
wood/ plastic/ polythene in combination for wall and roof materials
etc.
2 Mud/ Unburnt Brick/ Stone Mud/Un-burnt brick/stone without mortar as wall materials
without mortar and grass/thatch/bamboo/ Plastic/ polythene/handmade
tiles/ machine-made tiles etc as roof materials
4 Burnt Brick/ Stone with Burnt brick/ Stone packed with mortar as wall materials
mortar with Temporary and temporary roof (tiles, wood, GI, slate, etc.)
Roof
infill
3.4.2.2 Residential
The residential houses of Bhubaneswar city are broadly classified into four categories viz.,
Villas, Apartments, Row Houses and Huts based on construction materials and structures.
Sample photographs of each category are provided in Figure 3-9. Though, in some cases,
one category of house is often found mixed up with other categories, however, in some
cases the distinct clusters can be identified. For demarcation of ward-wise residential house
clusters, interpretation of LISS IV satellite image, landmark locations received from BMC and
Census 2011 housing statistics are considered. The results obtained are then correlated and
validated against the field survey data collected by the survey team at sample wards.
Villa
Apartment
Huts
Figure 3-10: Distribution of residential houses by use (left), Condition of residential houses in
Bhubaneswar city (right)
Reinforced concrete frame (RCF) with brick infill is the dominant structural class that
comprises of about 72% of the residential houses (Table 3-2). Burnt brick (with mortar) with
temporary roof and masonry buildings are the next dominant classes that are present for
10% and 8% residential houses, respectively (Figure 3-11). The latter two types of structures
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G a
W
f
t
)
n
r
.
r
o
o
c
u
o
B
m
R
e
Total 0.37 3.26 0.05 6.44 5.51 35.35 12.88 0.59 2.02 0.12
Built-up
Area
(sq. km.)
3.4.2.3 Commercial
The data regarding the number and location of commercial buildings in Bhubaneswar city is
collected from the Census of India 2011, BMC and other internet sources. The GIS data with