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S. K. Dube
&
Tad Murty
Indian Institute of technology
Kharagpur
Highlight the current activity in
surge modelling and related area in
the Bay of Bengal
Describe the development of
location specific real time stand
alone prediction system for
providing effective and timely surge
forecasts
Effect of local Tides
Effect of local
Coastal
Configuration
Low Atmospheric
Pressure in the Centre
Wind
Rain
Storm Surge
Flooding
Loss of
Human
Life:
Injuries
Damage to
structures &
Continent
Flooding of Low-
Lying Coastal Areas
Erosion of Beaches
Damage to onshore
& offshore
installations
Damage to Shipping
& Fishing Facilities
Loss of
Communications
& Power
Urban
Bushfire
Loss of Soil
Fertility
from Saline
Intrusion
Land
Subsidence
Contaminati
on of
Domestic
Water
Supply
Destruction
of
Vegetation,
Crops,
Livestock
Potential Impact upon Landfall of a Tropical Cyclone
DEATHS IN TROPICAL CYCLONES
YEAR COUNTRIES DEATHS
1970 Bangladesh 300,000
1737 India 300,000
1886 China 300,000
1923 Japan 250,000
1876 Bangladesh 200,000
1897 Bangladesh 175,000
1991 Bangladesh 140,000
1833 India 50,000
1864 India 50,000
1822 Bangladesh 40,000
1780 Antilles(West Indies) 22,000
1965 Bangladesh 19,279
1999 India 15,000
1963 Bangladesh 11,520
1961 Bangladesh 11,466
1985 Bangladesh 11,069
1971 India 10,000
1977 India 10,000
1966 Cuba 7,196
1900 USA 6,000
1960 Bangladesh 5,149
1960 Japan 5,000
1972 India 5,000
Factors Contributing to Disastrous Surge in
the Bay of Bengal
• Convergence of the Bay
Large bottom friction
• Shallow Water
Retards return undercurrent
• Thickly Populated Low Lying Islands
(Ramgati, Sandwip, Hatiya, Bhola & Kutubdia)
• High Astronomical Tides
• Inlets & Estuaries
Review of storm surges in the
Bay of Bengal
Ali (1979)
Rao (1982)
Roy (1984)
Murty (1984)
Murty et al. (1986)
Das (1994)
Dube et al. (1997, 1999, 2000, 2001)
Chittibabu (1999)
Real Ocean Real Ocean Model
Mathematical Model
Results
Idealization & Approximation
Based on experience &
understanding of the problem Abstract
symbolic
Representation
Based on
Mathematical
Experience
Solution based on
Mathematical Experience
C
O
M
P
A
R
I
S
O
N
Location Specific Input
Meteorological Input
Oceanographic &
Hydrological Input
Dynamic Storm Model
Wind Stress Associated with Cyclones
Storm Surge Model Equations
•Vertically Integrated Mass Continuity (1)
•Vertically Integrated Momentum (2)
Numerical Solution
Results
•Sea Surface Elevations
•Extent of Coastal Inundation
IIT Storm Surge Model
Operating Procedure
 Setup forecast domain by executing an appropriate
window
 Provide an arbitrary number of stations around the
forecasted place of landfall of the cyclone for peak
surge display
 Provide duration of forecast
 Provide tropical cyclone characteristics
(preferable six hourly observations)
 Cyclone positions (lat – long)
 Pressure Drop (Hpa)
 Radii of Maximum Winds (m)
 Run storm Model & Surge Model
Ability to investigate multiple
forecast scenario in real time
Updates cyclone track as the
cyclonic storm approaches
the coast and meteorological
forecast become more accurate
Significant
Features
Surge Envelope Scenario I: Actual Landfall
Distance along East Coast of India (km)
Surge Envelope Scenario II: Landfall at Puri
Distance along East Coast of India (km)
Surge Envelope Scenario III: Landfall at Balasore
Distance along East Coast of India (km)
Andhra Pradesh
Track of 1990 Andhra Cyclone
Surge Envelope Scenario I: Actual Landfall
Distance along East Coast of India (km)
§ Place of Landfall
Surge Envelope Scenario II: Landfall (100 km to left)
Distance along East Coast of India (km)
Surge Envelope Scenario III: Landfall (100 km to right)
Distance along East Coast of India (km)
Track of 1977 Andhra Cyclone
Peak Surge Envelope
Distance along East Coast of India (km)
Bangladesh
Bangladesh
Track of 1970 Bangladesh Cyclone
Surge along Bangladesh Coast
Track of 1982 GWA Cyclone
Myanmar
Peak Surge Envelope 1982 Cyclone
Track of 1964 Sri Lanka Cyclone
 A real time storm surge prediction systems
is proposed for India, Bangladesh, Myanmar
& Sri Lanka, which can be run in a few
minutes on a PC
 Only meteorological inputs required for the
model are positions of the cyclone, pressure
drop and radii of maximum winds at any
fixed interval of times
• The system is operated via a terminal menu
and the output consists of the 2-D and 3-D
views of peak sea surface elevations with the
facility of zooming the region of interest
• The system can handle multiple forecast
scenarios
• The model has extensively been tested with
severe cyclonic storms of the last three
decades, which have affected the coastal
regions in the Bay of Bengal
Global Storm Surges:
Theory, Observations and Applications
G. Gönnert, S. K. Dube, Tad Murty and W. Siefert
CONTENTS
Introduction and General
Considerations
The Basic Storm Surge Equations and
Standard Methods of Solutions
Finite Element Models
Special Hydrodynamic Problems
Meteorological Aspects
Storm Surges Generated by Tropical
Cyclones - Case Studies
Storm Surges generated by
Extratropical Cyclones - Case Studies
Impact of Climate Change and Sea level
Rise on Storm Surges
Die Küste Germany, 2001
`

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12a_Dube.ppt

  • 1. S. K. Dube & Tad Murty Indian Institute of technology Kharagpur
  • 2. Highlight the current activity in surge modelling and related area in the Bay of Bengal Describe the development of location specific real time stand alone prediction system for providing effective and timely surge forecasts
  • 3. Effect of local Tides Effect of local Coastal Configuration Low Atmospheric Pressure in the Centre Wind Rain Storm Surge Flooding Loss of Human Life: Injuries Damage to structures & Continent Flooding of Low- Lying Coastal Areas Erosion of Beaches Damage to onshore & offshore installations Damage to Shipping & Fishing Facilities Loss of Communications & Power Urban Bushfire Loss of Soil Fertility from Saline Intrusion Land Subsidence Contaminati on of Domestic Water Supply Destruction of Vegetation, Crops, Livestock Potential Impact upon Landfall of a Tropical Cyclone
  • 4. DEATHS IN TROPICAL CYCLONES YEAR COUNTRIES DEATHS 1970 Bangladesh 300,000 1737 India 300,000 1886 China 300,000 1923 Japan 250,000 1876 Bangladesh 200,000 1897 Bangladesh 175,000 1991 Bangladesh 140,000 1833 India 50,000 1864 India 50,000 1822 Bangladesh 40,000 1780 Antilles(West Indies) 22,000 1965 Bangladesh 19,279 1999 India 15,000 1963 Bangladesh 11,520 1961 Bangladesh 11,466 1985 Bangladesh 11,069 1971 India 10,000 1977 India 10,000 1966 Cuba 7,196 1900 USA 6,000 1960 Bangladesh 5,149 1960 Japan 5,000 1972 India 5,000
  • 5. Factors Contributing to Disastrous Surge in the Bay of Bengal • Convergence of the Bay Large bottom friction • Shallow Water Retards return undercurrent • Thickly Populated Low Lying Islands (Ramgati, Sandwip, Hatiya, Bhola & Kutubdia) • High Astronomical Tides • Inlets & Estuaries
  • 6. Review of storm surges in the Bay of Bengal Ali (1979) Rao (1982) Roy (1984) Murty (1984) Murty et al. (1986) Das (1994) Dube et al. (1997, 1999, 2000, 2001) Chittibabu (1999)
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12.
  • 13.
  • 14. Real Ocean Real Ocean Model Mathematical Model Results Idealization & Approximation Based on experience & understanding of the problem Abstract symbolic Representation Based on Mathematical Experience Solution based on Mathematical Experience C O M P A R I S O N
  • 15. Location Specific Input Meteorological Input Oceanographic & Hydrological Input Dynamic Storm Model Wind Stress Associated with Cyclones Storm Surge Model Equations •Vertically Integrated Mass Continuity (1) •Vertically Integrated Momentum (2) Numerical Solution Results •Sea Surface Elevations •Extent of Coastal Inundation
  • 16. IIT Storm Surge Model Operating Procedure  Setup forecast domain by executing an appropriate window  Provide an arbitrary number of stations around the forecasted place of landfall of the cyclone for peak surge display  Provide duration of forecast  Provide tropical cyclone characteristics (preferable six hourly observations)  Cyclone positions (lat – long)  Pressure Drop (Hpa)  Radii of Maximum Winds (m)  Run storm Model & Surge Model
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  • 18. Ability to investigate multiple forecast scenario in real time Updates cyclone track as the cyclonic storm approaches the coast and meteorological forecast become more accurate Significant Features
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  • 23. Surge Envelope Scenario I: Actual Landfall Distance along East Coast of India (km)
  • 24. Surge Envelope Scenario II: Landfall at Puri Distance along East Coast of India (km)
  • 25. Surge Envelope Scenario III: Landfall at Balasore Distance along East Coast of India (km)
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  • 64. Track of 1990 Andhra Cyclone
  • 65. Surge Envelope Scenario I: Actual Landfall Distance along East Coast of India (km) § Place of Landfall
  • 66. Surge Envelope Scenario II: Landfall (100 km to left) Distance along East Coast of India (km)
  • 67. Surge Envelope Scenario III: Landfall (100 km to right) Distance along East Coast of India (km)
  • 68. Track of 1977 Andhra Cyclone
  • 69. Peak Surge Envelope Distance along East Coast of India (km)
  • 72. Track of 1970 Bangladesh Cyclone
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  • 76. Track of 1982 GWA Cyclone
  • 78. Peak Surge Envelope 1982 Cyclone
  • 79. Track of 1964 Sri Lanka Cyclone
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  • 81.  A real time storm surge prediction systems is proposed for India, Bangladesh, Myanmar & Sri Lanka, which can be run in a few minutes on a PC  Only meteorological inputs required for the model are positions of the cyclone, pressure drop and radii of maximum winds at any fixed interval of times
  • 82. • The system is operated via a terminal menu and the output consists of the 2-D and 3-D views of peak sea surface elevations with the facility of zooming the region of interest • The system can handle multiple forecast scenarios • The model has extensively been tested with severe cyclonic storms of the last three decades, which have affected the coastal regions in the Bay of Bengal
  • 83. Global Storm Surges: Theory, Observations and Applications G. Gönnert, S. K. Dube, Tad Murty and W. Siefert CONTENTS Introduction and General Considerations The Basic Storm Surge Equations and Standard Methods of Solutions Finite Element Models Special Hydrodynamic Problems Meteorological Aspects Storm Surges Generated by Tropical Cyclones - Case Studies Storm Surges generated by Extratropical Cyclones - Case Studies Impact of Climate Change and Sea level Rise on Storm Surges Die Küste Germany, 2001
  • 84. `