This presentation was prepared to portray vulnerability assessment and damage mitigation for RCC buildings due to Non-Seismic Hazards in Bangladesh for the internal meeting of DDC office in Dhaka, Bangladesh. This is entirely based on the PWD-JICA manual for CNCRP project. In this presentation, we emphasized wind load and flood water calculation, their impact on our regular RCC building, and mitigation measures. The excel files are not included for the confidentiality purpose. This presentation helped our colleagues who were not interested in reading the manuals. I felt joyful and curious while I worked in this presentation with my colleague.
REVIEW OF RECENT EARTHQUAKES IN THE LIGHT OF PLATE TECTONICS AND SEISMIC RISK...Johana Sharmin
This slide represents the knowledge of tectonic plates related problems and massive earthquakes affecting our lives. Here also I accumulated the relationship between geomorphological and plate tectonic aspects in Bangladesh.
This document discusses earthquake intensity and magnitude. It defines an earthquake as the sudden release of energy in the Earth's crust that creates seismic waves. Earthquake intensity is a measure of the effects on the Earth's surface based on the Mercalli scale, while magnitude measures the energy released using seismograph recordings. The document provides details on what causes earthquakes, the relationship between intensity and magnitude, and examples of intensity scales like the Modified Mercalli scale. Tables show the correlation between typical intensities and magnitudes.
The document discusses methods for predicting earthquakes, which scientists have tried with varying degrees of success. It outlines several contemporary prediction methods, such as observing unusual animal behavior, changes in water levels and radon emissions, and analyzing seismic electric signals. However, the document concludes that scientists have not achieved 100% accurate predictions yet, though prediction capabilities have improved over time as more data is collected and patterns analyzed.
This document provides an overview of basic principles of seismology. It defines key terms like frequency, wavelength, velocity and discusses wave propagation concepts such as rays, wavefronts and Huygens' principle. It describes how seismic waves (P and S waves) travel through the Earth's interior and surface, depending on properties of the medium like density, bulk modulus and shear modulus. Typical seismic velocities are provided for different earth materials. Factors that can change seismic wave direction and amplitude during propagation are also mentioned.
1) Earthquakes occur due to the constant movement of tectonic plates inside the Earth. As strain builds up along fault lines where plates meet, it is suddenly released in the form of seismic waves.
2) The Richter scale is used to measure the magnitude of earthquakes based on the energy released. Major earthquakes over magnitude 7 can cause widespread damage.
3) To prepare for earthquakes, families should identify safe spots in each room, hold regular earthquake drills, and secure heavy furniture and objects that could cause injury. Being prepared is important since earthquakes provide no warning.
Earthquakes are caused by the buildup and sudden release of stress along faults within the Earth. As tectonic plates push against each other, stress accumulates until rocks break, causing vibrations called seismic waves. There are three types of faults defined by the direction of rock movement: normal faults occur when rocks pull apart due to tension, reverse faults occur when rocks are pushed together by compression, and strike-slip faults occur when rocks slide past one another due to shear forces. Seismographs are used to measure the seismic waves and locate the epicenter, or surface point above the underground hypocenter where rock movement begins.
This document provides information about earthquakes. It defines key earthquake terms like focus, epicenter, and aftershock. It describes the two types of seismic waves that radiate from an earthquake's focus - body waves and surface waves. It discusses how seismometers and seismographs are used to locate the epicenter and measure an earthquake's magnitude on the Richter scale. The document also outlines some of the common effects of earthquakes like ground displacement, landslides, liquefaction, tsunamis, and building collapses. Finally, it discusses ways to cope with earthquakes through earthquake zone planning, reinforced structures, and contingency plans.
This document provides information about earthquakes, including what causes them, the different types of seismic waves, how the location and magnitude of earthquakes are determined, hazards associated with earthquakes such as shaking, ground displacement, tsunamis and fires, and challenges around predicting earthquakes. It describes how earthquakes occur due to the accumulation and sudden release of strain energy in rocks under stress. There are two main types of seismic waves - body waves that travel through the interior of the earth and surface waves that travel along the surface. The location of earthquakes is determined through measuring the time delay between arrival of P and S waves at multiple seismograph stations and triangulating the epicenter. Magnitude is a measure of the
REVIEW OF RECENT EARTHQUAKES IN THE LIGHT OF PLATE TECTONICS AND SEISMIC RISK...Johana Sharmin
This slide represents the knowledge of tectonic plates related problems and massive earthquakes affecting our lives. Here also I accumulated the relationship between geomorphological and plate tectonic aspects in Bangladesh.
This document discusses earthquake intensity and magnitude. It defines an earthquake as the sudden release of energy in the Earth's crust that creates seismic waves. Earthquake intensity is a measure of the effects on the Earth's surface based on the Mercalli scale, while magnitude measures the energy released using seismograph recordings. The document provides details on what causes earthquakes, the relationship between intensity and magnitude, and examples of intensity scales like the Modified Mercalli scale. Tables show the correlation between typical intensities and magnitudes.
The document discusses methods for predicting earthquakes, which scientists have tried with varying degrees of success. It outlines several contemporary prediction methods, such as observing unusual animal behavior, changes in water levels and radon emissions, and analyzing seismic electric signals. However, the document concludes that scientists have not achieved 100% accurate predictions yet, though prediction capabilities have improved over time as more data is collected and patterns analyzed.
This document provides an overview of basic principles of seismology. It defines key terms like frequency, wavelength, velocity and discusses wave propagation concepts such as rays, wavefronts and Huygens' principle. It describes how seismic waves (P and S waves) travel through the Earth's interior and surface, depending on properties of the medium like density, bulk modulus and shear modulus. Typical seismic velocities are provided for different earth materials. Factors that can change seismic wave direction and amplitude during propagation are also mentioned.
1) Earthquakes occur due to the constant movement of tectonic plates inside the Earth. As strain builds up along fault lines where plates meet, it is suddenly released in the form of seismic waves.
2) The Richter scale is used to measure the magnitude of earthquakes based on the energy released. Major earthquakes over magnitude 7 can cause widespread damage.
3) To prepare for earthquakes, families should identify safe spots in each room, hold regular earthquake drills, and secure heavy furniture and objects that could cause injury. Being prepared is important since earthquakes provide no warning.
Earthquakes are caused by the buildup and sudden release of stress along faults within the Earth. As tectonic plates push against each other, stress accumulates until rocks break, causing vibrations called seismic waves. There are three types of faults defined by the direction of rock movement: normal faults occur when rocks pull apart due to tension, reverse faults occur when rocks are pushed together by compression, and strike-slip faults occur when rocks slide past one another due to shear forces. Seismographs are used to measure the seismic waves and locate the epicenter, or surface point above the underground hypocenter where rock movement begins.
This document provides information about earthquakes. It defines key earthquake terms like focus, epicenter, and aftershock. It describes the two types of seismic waves that radiate from an earthquake's focus - body waves and surface waves. It discusses how seismometers and seismographs are used to locate the epicenter and measure an earthquake's magnitude on the Richter scale. The document also outlines some of the common effects of earthquakes like ground displacement, landslides, liquefaction, tsunamis, and building collapses. Finally, it discusses ways to cope with earthquakes through earthquake zone planning, reinforced structures, and contingency plans.
This document provides information about earthquakes, including what causes them, the different types of seismic waves, how the location and magnitude of earthquakes are determined, hazards associated with earthquakes such as shaking, ground displacement, tsunamis and fires, and challenges around predicting earthquakes. It describes how earthquakes occur due to the accumulation and sudden release of strain energy in rocks under stress. There are two main types of seismic waves - body waves that travel through the interior of the earth and surface waves that travel along the surface. The location of earthquakes is determined through measuring the time delay between arrival of P and S waves at multiple seismograph stations and triangulating the epicenter. Magnitude is a measure of the
This presentation includes introduction to Earthquakes, Seismic Waves, Shallow Focus and Deep Focus Earthquakes, Aftershocks, Earthquake Storms, Effects/Impacts of Earthquakes, Earthquake Predictions.
1) Most earthquakes originate from a sudden release of energy at the focus or hypocenter located beneath the earth's surface.
2) Faults are fractures in the earth's crust where movement has occurred. The 1906 San Francisco earthquake involved slippage of 4.7 meters along the San Andreas Fault.
3) Earthquake waves spread out from the focus in all directions. P and S waves can be used to locate the earthquake's epicenter through triangulation of arrival times at multiple stations.
Earthquakes are caused by a sudden release of energy in the Earth's crust that creates seismic waves. The largest recorded earthquakes include a 9.5 magnitude quake in Chile in 1960 and a 9.0 magnitude quake in Japan in 2011. Earthquakes can cause significant damage through ground shaking, fault ruptures, landslides, fires, liquefaction, tsunamis, and floods. Proper construction and seismic building codes can help reduce damage from earthquakes.
1) An earthquake is caused by a sudden release of energy in the Earth's crust that creates seismic waves. Different types of seismic waves include P waves, S waves, and surface waves.
2) Earthquakes can be shallow or deep, with shallow quakes occurring less than 70 km below the surface and deep quakes occurring 300-700 km down. Aftershocks are smaller quakes that follow the main shock.
3) The effects of earthquakes include ground shaking, landslides, fires, soil liquefaction, tsunamis, and damage to infrastructure and loss of human life. While prediction of specific earthquakes remains difficult, scientists can estimate probability of quakes in active fault zones.
Most earthquakes occur along fault lines in the earth's crust due to the buildup and sudden release of strain energy. There are approximately 500,000 earthquakes detected around the world each year, with about 100,000 able to be felt. Major quakes of magnitude 7.0 or greater occur on average 18 times per year. The circum-Pacific seismic belt sees 90% of the world's quakes due to tectonic plate movement. Human activities such as dam building and fluid injection can also induce seismic activity in rare cases.
1) The document discusses key concepts related to earthquakes including their location, cause, measurement, and impact.
2) Major concepts explained include the focus (where pressure is released underground), epicenter (location directly above the focus where damage is greatest), and Richter scale (method for measuring earthquake magnitude).
3) The document provides a table listing details of significant earthquakes from 1923 to 2008 including location, year, magnitude on the Richter scale, and deaths.
The document discusses earthquakes, including what causes them, how they are measured, their effects, and statistics on major earthquakes around the world. Specifically, it defines an earthquake as rapid shaking caused by the sudden release of energy along fault lines. It describes the movement of tectonic plates and how this results in earthquakes. Key points covered include earthquake magnitude scales, the different types of seismic waves generated, and data on some of the largest earthquakes by magnitude and their impacts.
Scientists measure the magnitude of an earthquake using the Richter scale, which quantifies the amount of energy released by the earthquake based on the amplitude of seismic waves recorded by seismographs. The larger the amplitude, the higher the magnitude.
This document summarizes information about earthquakes, including the different types of stresses that cause faulting, the three main types of faults, and how the movement of tectonic plates over millions of years can change landscapes. It also describes the different types of seismic waves, how seismographs are used to measure seismic waves and earthquakes, and how data from past earthquakes can help estimate future earthquake risks. The document provides information on efforts to monitor faults and reduce earthquake damage through improved building design.
On January 17, 1995, a magnitude 7.2 earthquake struck Kobe, Japan, the second most populated area after Tokyo. Over 5,000 people were killed, more than 300,000 became homeless, and $100 billion in damage was caused during the brief 20 second shaking. The earthquake was caused by two blocks of the earth suddenly slipping past one another along a fault line.
Earthquakes occur due to the sudden release of built-up energy along fault lines in the earth's crust. They produce three types of seismic waves that radiate out from the hypocenter or focus of the earthquake. The location and magnitude of earthquakes can be measured using seismographs located around the world. Major effects of earthquakes include shaking, ground rupture, landslides, fires, liquefaction, tsunamis, and structural damage to buildings and infrastructure. Proper construction techniques and emergency preparedness can help reduce risks from earthquakes.
Earthquakes occur when tectonic forces cause rocks underground to break, releasing seismic waves. The focus is where the rocks break, and the epicenter is the point directly above on the surface. Different types of faults are caused by tension, compression, and shear forces. Earthquakes are measured by their magnitude using the Richter scale and by their intensity of shaking. Locating the epicenter involves measuring seismic wave arrival times at different stations. Earthquake dangers include falling objects, fires, tsunamis, liquefaction, and landslides.
This document provides an overview of earthquakes, including key vocabulary terms. It describes how earthquakes are caused by movement along faults in the earth's lithosphere. When seismic waves from an earthquake are detected by seismometers, seismologists can use the timing of the waves to triangulate the earthquake's epicenter via its focus point below the surface. The magnitude scales help describe the intensity and energy released by earthquakes.
This document provides information about earthquakes. It begins by defining key earthquake terms like epicenter, hypocenter, foreshocks, aftershocks, and magnitude. It then explains that earthquakes are caused by the sudden slipping of fault blocks within the earth, as the plates of the earth's crust shift. The document discusses how seismographs are used to measure and locate earthquakes by recording seismic waves. It also describes the different scales used to measure earthquake size and intensity. Finally, it provides references for additional information.
1. Earthquakes are caused by movements in the Earth's crust along fault lines and plate boundaries. The most severe earthquakes typically occur at destructive and conservative plate boundaries.
2. Scientists can measure earthquakes using seismographs, which detect seismic waves. The Richter scale is used to quantify the magnitude or strength of an earthquake based on the seismograph recording.
3. In addition to the Richter scale, the Mercalli scale is used to describe the intensity or amount of damage caused by an earthquake based on observations of its effects.
1) Earthquakes are caused by the sudden release of stored elastic energy in the Earth's crust. They generate different types of seismic waves that propagate outward from the earthquake focus.
2) The location and type of earthquake is determined by the surrounding tectonic environment. Convergent plate boundaries experience deep earthquakes along subduction zones, while divergent and transform boundaries have shallower quakes.
3) Earthquake magnitude is measured on different scales but all aim to characterize the energy released by the quake. Intensity scales describe perceived shaking and damage at a given location.
Earthquake seismology uses seismic waves generated by earthquakes to study the interior of the Earth. Seismic waves are detected by seismographs and include P-waves, S-waves, and surface waves. The location and depth of the initial rupture point within the Earth is known as the hypocenter and epicenter, respectively. Larger earthquakes with shallower depths typically cause more damage. Earthquake magnitude represents the energy released while intensity refers to the strength of shaking experienced at a particular location.
An earthquake is caused by a sudden release of energy in the Earth's crust that generates seismic waves. Faults in the crust result from tectonic plate movements and cause earthquakes when the rocks on either side slip past each other due to accumulated elastic strain. The focus is the point where slippage originates underground, while the epicenter is the point directly above on the surface. Seismographs installed worldwide record earthquake ground motions to study seismic activity.
An earthquake is caused by the sudden release of energy from two parts of rock masses moving suddenly along a fault. This energy is released in different types of waves that originate from the focus or epicenter of the earthquake. Earthquakes can be classified based on their mode of origin such as volcanic, tectonic, or surface causes, or based on the depth of their focus as shallow, intermediate, or deep. The effects of earthquakes can be devastating, so earthquake resistant structures should be designed through careful study of past records and use of techniques like foundations on hard rock, wider streets, and steel or reinforced concrete frames.
The document provides an overview of damage assessment methodology for various structures after a disaster. It discusses that damage assessment has short, medium and long-term objectives. For buildings, it proposes a three step methodology for damage assessment including rapid safety assessment, detailed safety assessment, and engineering evaluation. Similar methodologies are discussed for assessing damage to other structures like bridges, roads, reservoirs, irrigation structures and more.
10_BADIU Bratucu_07.04 THE EFFECTS OF WIND ON ROOF SYSTEMS FOR BUILDINGSEDUARD C BADIU
This document discusses how wind can affect roof systems on buildings. It examines various factors that influence wind resistance, such as basic wind speed, wind-building interactions, topography, and internal pressure. The highest wind pressures typically occur at edges of roofs, ridges, and corners. These localized pressures can damage roof components and cladding and lead to further structural failure if not properly designed and constructed to withstand anticipated wind loads. The document also provides examples of wind pressure calculations and zones on buildings based on standards to help design roof systems that can resist damage from wind events.
This presentation includes introduction to Earthquakes, Seismic Waves, Shallow Focus and Deep Focus Earthquakes, Aftershocks, Earthquake Storms, Effects/Impacts of Earthquakes, Earthquake Predictions.
1) Most earthquakes originate from a sudden release of energy at the focus or hypocenter located beneath the earth's surface.
2) Faults are fractures in the earth's crust where movement has occurred. The 1906 San Francisco earthquake involved slippage of 4.7 meters along the San Andreas Fault.
3) Earthquake waves spread out from the focus in all directions. P and S waves can be used to locate the earthquake's epicenter through triangulation of arrival times at multiple stations.
Earthquakes are caused by a sudden release of energy in the Earth's crust that creates seismic waves. The largest recorded earthquakes include a 9.5 magnitude quake in Chile in 1960 and a 9.0 magnitude quake in Japan in 2011. Earthquakes can cause significant damage through ground shaking, fault ruptures, landslides, fires, liquefaction, tsunamis, and floods. Proper construction and seismic building codes can help reduce damage from earthquakes.
1) An earthquake is caused by a sudden release of energy in the Earth's crust that creates seismic waves. Different types of seismic waves include P waves, S waves, and surface waves.
2) Earthquakes can be shallow or deep, with shallow quakes occurring less than 70 km below the surface and deep quakes occurring 300-700 km down. Aftershocks are smaller quakes that follow the main shock.
3) The effects of earthquakes include ground shaking, landslides, fires, soil liquefaction, tsunamis, and damage to infrastructure and loss of human life. While prediction of specific earthquakes remains difficult, scientists can estimate probability of quakes in active fault zones.
Most earthquakes occur along fault lines in the earth's crust due to the buildup and sudden release of strain energy. There are approximately 500,000 earthquakes detected around the world each year, with about 100,000 able to be felt. Major quakes of magnitude 7.0 or greater occur on average 18 times per year. The circum-Pacific seismic belt sees 90% of the world's quakes due to tectonic plate movement. Human activities such as dam building and fluid injection can also induce seismic activity in rare cases.
1) The document discusses key concepts related to earthquakes including their location, cause, measurement, and impact.
2) Major concepts explained include the focus (where pressure is released underground), epicenter (location directly above the focus where damage is greatest), and Richter scale (method for measuring earthquake magnitude).
3) The document provides a table listing details of significant earthquakes from 1923 to 2008 including location, year, magnitude on the Richter scale, and deaths.
The document discusses earthquakes, including what causes them, how they are measured, their effects, and statistics on major earthquakes around the world. Specifically, it defines an earthquake as rapid shaking caused by the sudden release of energy along fault lines. It describes the movement of tectonic plates and how this results in earthquakes. Key points covered include earthquake magnitude scales, the different types of seismic waves generated, and data on some of the largest earthquakes by magnitude and their impacts.
Scientists measure the magnitude of an earthquake using the Richter scale, which quantifies the amount of energy released by the earthquake based on the amplitude of seismic waves recorded by seismographs. The larger the amplitude, the higher the magnitude.
This document summarizes information about earthquakes, including the different types of stresses that cause faulting, the three main types of faults, and how the movement of tectonic plates over millions of years can change landscapes. It also describes the different types of seismic waves, how seismographs are used to measure seismic waves and earthquakes, and how data from past earthquakes can help estimate future earthquake risks. The document provides information on efforts to monitor faults and reduce earthquake damage through improved building design.
On January 17, 1995, a magnitude 7.2 earthquake struck Kobe, Japan, the second most populated area after Tokyo. Over 5,000 people were killed, more than 300,000 became homeless, and $100 billion in damage was caused during the brief 20 second shaking. The earthquake was caused by two blocks of the earth suddenly slipping past one another along a fault line.
Earthquakes occur due to the sudden release of built-up energy along fault lines in the earth's crust. They produce three types of seismic waves that radiate out from the hypocenter or focus of the earthquake. The location and magnitude of earthquakes can be measured using seismographs located around the world. Major effects of earthquakes include shaking, ground rupture, landslides, fires, liquefaction, tsunamis, and structural damage to buildings and infrastructure. Proper construction techniques and emergency preparedness can help reduce risks from earthquakes.
Earthquakes occur when tectonic forces cause rocks underground to break, releasing seismic waves. The focus is where the rocks break, and the epicenter is the point directly above on the surface. Different types of faults are caused by tension, compression, and shear forces. Earthquakes are measured by their magnitude using the Richter scale and by their intensity of shaking. Locating the epicenter involves measuring seismic wave arrival times at different stations. Earthquake dangers include falling objects, fires, tsunamis, liquefaction, and landslides.
This document provides an overview of earthquakes, including key vocabulary terms. It describes how earthquakes are caused by movement along faults in the earth's lithosphere. When seismic waves from an earthquake are detected by seismometers, seismologists can use the timing of the waves to triangulate the earthquake's epicenter via its focus point below the surface. The magnitude scales help describe the intensity and energy released by earthquakes.
This document provides information about earthquakes. It begins by defining key earthquake terms like epicenter, hypocenter, foreshocks, aftershocks, and magnitude. It then explains that earthquakes are caused by the sudden slipping of fault blocks within the earth, as the plates of the earth's crust shift. The document discusses how seismographs are used to measure and locate earthquakes by recording seismic waves. It also describes the different scales used to measure earthquake size and intensity. Finally, it provides references for additional information.
1. Earthquakes are caused by movements in the Earth's crust along fault lines and plate boundaries. The most severe earthquakes typically occur at destructive and conservative plate boundaries.
2. Scientists can measure earthquakes using seismographs, which detect seismic waves. The Richter scale is used to quantify the magnitude or strength of an earthquake based on the seismograph recording.
3. In addition to the Richter scale, the Mercalli scale is used to describe the intensity or amount of damage caused by an earthquake based on observations of its effects.
1) Earthquakes are caused by the sudden release of stored elastic energy in the Earth's crust. They generate different types of seismic waves that propagate outward from the earthquake focus.
2) The location and type of earthquake is determined by the surrounding tectonic environment. Convergent plate boundaries experience deep earthquakes along subduction zones, while divergent and transform boundaries have shallower quakes.
3) Earthquake magnitude is measured on different scales but all aim to characterize the energy released by the quake. Intensity scales describe perceived shaking and damage at a given location.
Earthquake seismology uses seismic waves generated by earthquakes to study the interior of the Earth. Seismic waves are detected by seismographs and include P-waves, S-waves, and surface waves. The location and depth of the initial rupture point within the Earth is known as the hypocenter and epicenter, respectively. Larger earthquakes with shallower depths typically cause more damage. Earthquake magnitude represents the energy released while intensity refers to the strength of shaking experienced at a particular location.
An earthquake is caused by a sudden release of energy in the Earth's crust that generates seismic waves. Faults in the crust result from tectonic plate movements and cause earthquakes when the rocks on either side slip past each other due to accumulated elastic strain. The focus is the point where slippage originates underground, while the epicenter is the point directly above on the surface. Seismographs installed worldwide record earthquake ground motions to study seismic activity.
An earthquake is caused by the sudden release of energy from two parts of rock masses moving suddenly along a fault. This energy is released in different types of waves that originate from the focus or epicenter of the earthquake. Earthquakes can be classified based on their mode of origin such as volcanic, tectonic, or surface causes, or based on the depth of their focus as shallow, intermediate, or deep. The effects of earthquakes can be devastating, so earthquake resistant structures should be designed through careful study of past records and use of techniques like foundations on hard rock, wider streets, and steel or reinforced concrete frames.
The document provides an overview of damage assessment methodology for various structures after a disaster. It discusses that damage assessment has short, medium and long-term objectives. For buildings, it proposes a three step methodology for damage assessment including rapid safety assessment, detailed safety assessment, and engineering evaluation. Similar methodologies are discussed for assessing damage to other structures like bridges, roads, reservoirs, irrigation structures and more.
10_BADIU Bratucu_07.04 THE EFFECTS OF WIND ON ROOF SYSTEMS FOR BUILDINGSEDUARD C BADIU
This document discusses how wind can affect roof systems on buildings. It examines various factors that influence wind resistance, such as basic wind speed, wind-building interactions, topography, and internal pressure. The highest wind pressures typically occur at edges of roofs, ridges, and corners. These localized pressures can damage roof components and cladding and lead to further structural failure if not properly designed and constructed to withstand anticipated wind loads. The document also provides examples of wind pressure calculations and zones on buildings based on standards to help design roof systems that can resist damage from wind events.
This document discusses landslide risk mapping for the entire Swiss national road network. It describes the Swiss Federal Roads Office's (FEDRO) risk management process, which includes creating intensity maps to assess hazard likelihood and attributes. FEDRO then uses its GIS-based tool called RoadRisk to overlay the maps with road segments and calculate segment-specific risks of impacts like human death, property damage, and closure costs from various natural hazards such as landslides, floods, and rockfalls. The goal is to produce a Swiss-wide risk map to help prioritize risk reduction measures across the national road network.
Assam is the biggest of the ‘Seven Sisters’ in the North-Eastern region1 of India. Th e uniqueness of this region-- as well as most of its troubles--is determined by several factors, not least of which is the fact that more than 2000 km of the country’s boundary fall here and is shared with as many as fi ve countries--Nepal, China, Bhutan, Myanmar and Bangladesh. Also, the land-locked region is ethnically and linguistically diff erent from the rest of India.
HAQ: Center for Child Rights
B1/2, Ground Floor,
Malviya Nagar
New Delhi - 110017
Tel: +91-26677412,26673599
Fax: +91-26674688
Website: www.haqcrc.org
FaceBook Page: https://www.facebook.com/HaqCentreForChildRights
1) A structural test exhibition was held on November 19-20, 2012 by JICA experts to evaluate the seismic performance of existing reinforced concrete frame buildings in Bangladesh.
2) A scaled 1-story, 1-span reinforced concrete frame model was tested under constant vertical and incremental horizontal loads to observe its strength, ductility, and failure behavior.
3) The results would provide data on factors like stiffness, strength, and ductility to assess existing buildings and aid in retrofitting design, filling gaps not covered by design codes.
Seismic vulnerability assessment using field survey and Remote Sensing techni...Beniamino Murgante
Seismic vulnerability assessment using field survey and Remote Sensing techniques
Paolo Ricci, Gerardo Mario Verderame, Gaetano Manfredi - Department of
Structural Engineering (DIST) - University of Naples Federico II
Maurizio Pollino, Flavio Borfecchia, Luigi De Cecco, Sandro Martini - National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA, UTMEA-TER)
Carmine Pascale, Elsabetta Ristoratore, Valentina James - Consortium T.R.E. Technologies for Building Rehabilitation
Development of-fragility-curves-for-seismic-vulnerability-assessment-of-high-...Leahcim Nolyab
This document summarizes Esra Mete Güneyisi's 2007 doctoral thesis on developing fragility curves to assess the seismic vulnerability of high-rise reinforced concrete (R/C) buildings retrofitted with added viscous dampers. The thesis describes selecting a 12-story non-ductile R/C office building in Istanbul as a case study, and retrofitting it with passive fluid viscous damper systems or shear walls to provide different levels of effective damping. 240 artificially generated ground motions were used to develop fragility curves representing the probability of exceeding damage states at various seismic intensities. The fragility curves, combined with seismic hazard analysis, allowed evaluating the effectiveness and cost-benefit of retrofitting using dampers
Probabilstic seismic risk evaluation of rc buildings eSAT Journals
Abstract As more and more emphasis is being laid on non-linear analysis of RC framed structures subjected to earthquake excitation, the research and development on both non-linear static (pushover) analysis as well as nonlinear dynamic (time history)analysis is in the forefront. Due to prohibitive computational time and efforts required to perform a complete nonlinear dynamic analysis, researchers and designers all over the world are showing keen interest in non-linear static pushover analysis. The paper considers two statistical random variables namely characteristic strength of concrete (fck) and yield strength of steel (fy) as uncertainties in strength. Using Monte Carlo simulation 100 samples of each of random variable were generated to quantify effect of uncertainties on prediction of capacity of structure. Based on these generated samples different models were created and static pushover analysis was performed on RC (Reinforced Concrete) Building using SAP2000. Lastly, the main objective of this article is to propose a simplified methodology to assess the expected seismic damage in reinforced concrete buildings from a probabilistic point of view by using Monte Carlo simulation and probability of various damage states were evaluated. Index Terms: Seismic Vulnerability, Probabilistic Seismic Risk Evaluation, Fragility Analysis and Pushover Analysis
A presentation on current scenario of Earthquake vulnerability of Dhaka City. The presentation shows the possible solutions of risk disaster management .
This document provides an overview of laminated glass, including its construction using polyvinyl butyral (PVB) interlayers sandwiched between two pieces of glass. It discusses the benefits of laminated glass in providing safety, sound reduction, security, solar control, and aesthetic appeal. Examples of architectural applications where laminated glass is commonly used are also presented.
This document provides an overview of the geography, climate, river systems, and floods of Bangladesh. It begins with the objectives of understanding Bangladesh's geographical location and settings, climate, major river systems, and patterns of flooding. Bangladesh is located in South Asia on the northern coast of the Bay of Bengal, surrounded by India. It has a tropical monsoon climate with three seasons: summer, winter, and rainy season. Major river systems include the Ganges, Brahmaputra, and Surma-Meghna rivers. Bangladesh is prone to frequent and devastating floods during the rainy monsoon season due to its low-lying geography and location at the end of major river systems.
The document discusses different types of wind resistant building structures that could help withstand hurricanes, including spiral, dome, pyramid, and egg-shaped designs. It also covers the devastating effects of Hurricane Katrina in 2005, which caused over 1,800 deaths and $81 billion in damages in New Orleans. The document suggests that building more wind and hurricane resistant structures, as well as stronger dams, could help mitigate damage from future storms.
As we know that in today’s world terrorists’ attacks are common and not a single country is completely safe. High-explosive detonations propagate blast energy in all directions, causing extensive damage to both the target structure and nearby buildings. Structural damage and the glass exposure have been major contributors to death and injury for the targeted buildings. If the structures are properly designed for these abnormal loads damage can be controlled. Within the Indian Standard Codes these types of situations are not dealt with and they need further explanation as the engineers have no guidelines on how to design or evaluate structures for the blast phenomenon for which a detailed understanding of structural behavior as well as effects of different kinds of blast load is required. The calculation of blast load is studied in this report using various parameters.
Seminar on Bomb Blast Resistant Structure by Shantanu PatilShantanu Patil
The design of civilian or commercial buildings to withstand the effects of a terrorist blast is unlike the design of military installations or the design of embassy buildings. The objectives of the “Structural Engineering Guidelines” for the Design of New Embassy Buildings are to prevent heavy damage to components and structural collapse. Adherence to the provisions of the guidelines will minimize injuries and loss of life and facilitate the evacuation and rescue of survivors. The blast-protection objective of any commercial or public building must be similar to those of embassy structures, that is to prevent structural collapse, to save lives, and to evacuate victims.
The document provides an introduction to BLAST (Basic Local Alignment Search Tool), which is an algorithm used to compare gene and protein sequences to those in public databases. It discusses the types of BLAST programs, the BLAST algorithm, input/output, how to perform a BLAST search, and the functions and objectives of BLAST. Specifically, BLAST is faster than previous sequence comparison methods, it outputs alignments and statistical values to evaluate matches, and its main objectives are to identify related sequences and locate domains through local alignments.
This document discusses blast load analysis and design of blast resistant structures. It begins by outlining the need for blast resistant design due to increasing terrorist attacks. It then defines what a blast is and describes the blast wave pressure time history. Different types of blast resistant structures are discussed. Empirical relationships are provided for calculating reflected blast pressures. The document provides examples of calculating the impulse of a blast load on a building and using it to determine base shear and moment. Plots of reflected pressure versus time are given for different charge weights and standoff distances. The scope of work for designing a G+6 storey building considering blast loads is also summarized.
Seismic analysis of multi storey reinforced concrete buildings frame”ankialok
The opinion that designing new buildings to be Earthquake resistant will cause substantial additional costs is still among the constructional professionals. In a country of moderate seismicity adequate seismic resistance of new buildings may be achieved at no or no significant additional cost however the expenditure needed to ensure adequate seismic resistance may depend strongly on the approach selected during the conceptual design phase and the relevant design method. Regarding the conceptual design phase early collaboration between the architect and civil engineering is crucial.
Architectural And Structural Design Of Blast Resistant Buildings - PRESENTATIONPaul Jomy
This document provides information on blast resistant building design. It discusses the objectives of blast design which are to reduce injury, facilitate rescue, expedite repair and return to full operations. It describes major causes of life loss after a blast like flying debris, smoke, and progressive structural collapse. Principles of blast resistant design are outlined such as maintaining standoff zones and limiting localized damage. Various structural elements are described for improving blast resistance, including connections, column wrapping, shear walls, glazing, and miscellaneous measures. Case studies on the WTC collapse and Israeli buildings adapted for military blast design are presented. The conclusion states that while withstanding any attack isn't practical, performance can be improved through an appropriate threat-based design process.
This document provides information on blast resistant design of structures. It discusses the objectives of blast resistance, types of blast resistant structures, and outlines the basic design process. The design process involves calculating blast loads, determining member properties, modeling the structure, selecting trial member sections, performing dynamic analysis using single-degree-of-freedom or multi-degree-of-freedom methods, checking deformation criteria, designing connections, and designing foundations. Dynamic analysis methods like equivalent static method, SDOF, and MDOF are described for evaluating structural response to blast loads.
Tropical cyclones form over tropical ocean waters and affect agriculture in Tamil Nadu. They cause heavy rainfall, strong winds, and storm surges that can damage or destroy crops. A case study on Cyclone Thane found it caused over Rs. 5,250 crore in total losses, with over Rs. 4,000 crore in Cuddalore district alone due to damage to agricultural and horticultural crops across 200,000 hectares. Cyclones of increasing intensity can have increasingly catastrophic impacts like total crop destruction and uprooting of large trees. Rainfall distribution depends on cyclone size and speed, with more rainfall occurring close to the center.
Cyclones are intense low pressure areas characterized by very strong circulating winds. They develop over warm tropical oceans and are classified as extra-tropical or tropical depending on location. Tropical cyclones bring heavy rainfall, strong winds over 100 km/h, and storm surges which can flood coastal areas. India's east coast is most vulnerable as the Bay of Bengal sees several cyclones each year. Early warning systems and evacuation plans are needed to minimize loss of life and property when cyclones make landfall. Proper construction and site selection above flood levels can strengthen buildings to withstand cyclone winds and rains.
This document provides an overview of various types of hydro-meteorological disasters including floods, cyclones, avalanches, lightning, heat waves, cold waves, droughts, and thunderstorms. It describes the causes and effects of each type of disaster, highlighting that hydro-meteorological disasters result from the interaction of atmospheric and hydrological systems and can threaten lives and property. Precautions are outlined for many of the disasters to help people protect themselves during events.
This document discusses cyclones, including their formation, classification, and impacts. It notes that cyclones are intense low pressure systems that form over warm ocean waters and are driven by evaporation and convection. They are given different names in different regions, such as hurricanes, typhoons, and tropical cyclones. Cyclones are classified based on wind speed and damage potential. Major hazards include strong winds, heavy rainfall, storm surges, and flooding. The Indian subcontinent is highly impacted by cyclones that form in the Bay of Bengal and Arabian Sea.
A cyclone is a low pressure system surrounded by high pressure with winds spiraling inward toward the center. There are two main types: temperate and tropical cyclones. Characteristics of tropical cyclones include inward spiraling surface winds, tight elliptical isobar patterns, minimal surface temperature drop near the center, heavy spiral cloud bands including the distinctive eye, and central pressures well below average. Tropical cyclones are classified based on sustained wind speeds and can cause heavy rain, strong winds, storm surges, flooding, infrastructure damage, and loss of life both at sea and on land when making landfall.
The document provides information about natural disasters, specifically earthquakes and tropical cyclones. It defines earthquakes and tropical cyclones, describes their causes and effects, and lists measures to minimize damage. For example, it explains that earthquakes are caused by plate tectonic movement and can cause infrastructure damage, while tropical cyclones derive energy from warm ocean waters and can bring strong winds and flooding to coastal areas.
The document discusses various hydrometeorological hazards such as tropical cyclones, thunderstorms, floods, droughts, and heat waves. It provides descriptions of different hazards, including cyclones, typhoons, floods, storm surges, and tornadoes. The document also outlines preparedness, response, and rehabilitation strategies for hazards like tropical cyclones, thunderstorms, floods, and storm surges. These include developing family plans, securing property, sheltering safely during events, and assisting in recovery efforts after hazards pass.
Disaster is a serious, dangerous and intolerable phenomena on the planet earth. Thousands of people die in a moment. Many people may become homeless and parentless. Valuable properties get damaged within no time. Disasters are events shocking the whole world and making the humanity to feel very sad. All life support systems are affected by these incidences.
What is required to minimize the effects is the application of certain management practices. Disaster management is an essential component of our development works. Let us see the aspects of Disaster Management in this module.
On May 30, 2016, ICLR conducted a webinar providing a forecast for the 2016 hurricane season. The Webinar was conducted by Bob Robichaud, Warning Preparedness Meteorologist, Canadian Hurricane Centre. Bob Robichaud received his B.Sc. in meteorology from Lyndon State College, Vermont in 1995. After a few years as a weather forecaster in the private sector, he joined Environment Canada in 1998 as an aviation forecaster in Gander NL where he eventually became aviation weather program manager for Atlantic Canada.
Robichaud moved to Halifax in 2004 to fill the new warning preparedness meteorologist role in Atlantic Canada where his primary focus is working closely with emergency management officials on a variety of different weather related issues including training, exercising and support during actual weather events.
if you are finding about cyclones this the best you can get.
it is not as colourful as the others, but i promise you that you will not get more information about them in ppts.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM ATMOSPHERIC DISTURBANCES. It contain case studies: Hurricane Katrina 2005, Cloud Seeding in New Zealand 1950-1970.
The document discusses various types of natural and man-made disasters including earthquakes, tsunamis, cyclones, hurricanes, and industrial/structural accidents. It provides definitions and descriptions of different disasters, their causes, effects, and mitigation strategies. Specific examples discussed include the 1952 Great Smog of London that killed 12,000, the 1987 sinking of the ferry MV Doña Paz in the Philippines that caused over 4,000 deaths, and the 1626 Wanggongchang Explosion in Beijing that killed 20,000.
This document discusses typhoons, including their formation, causes, effects, and mitigation measures. It defines a typhoon as a large storm system with violent winds circulating around a low pressure center. Typhoons form over warm ocean waters, with energy derived from evaporating water that rises and condenses into clouds. Stronger typhoons develop an eye with calm winds at the center. Typhoons are classified into 5 categories based on wind speed, from a tropical depression to a super typhoon with winds over 249 km/h. The document outlines the key stages in a typhoon's formation and lists objectives for students to understand typhoons and their impacts.
Hydrometeorological hazard is a process or phenomenon of atmospheric, hydrological or oceanographic nature that may cause loss of life, injury or other health impacts, property damage, loss of livelihoods and services, social and economic disruption, or environmental damage.
This document defines and describes various hydrometeorological hazards such as tropical cyclones, thunderstorms, floods, droughts, heat waves, cold spells, avalanches, and blizzards. It then focuses on specific hazards like tropical cyclones/typhoons/hurricanes, thunderstorms, tornadoes, flash floods, and floods. For each hazard, the document discusses characteristics, causes, classification (for tropical cyclones), and potential impacts. It also covers monitoring technologies like satellites and Doppler radar. Finally, it provides strategies for preparedness, response, and rehabilitation related to tropical cyclones.
This document provides information about three types of severe weather associated with cumulonimbus clouds: thunderstorms, tornadoes, and hurricanes. It examines how each forms from different lifting mechanisms in the atmosphere and discusses their characteristics. Thunderstorms form from warm, moist air that is lifted violently by cold fronts. Tornadoes are rotating columns of air that form from wind shear. Hurricanes are intense rotating storms that form over tropical oceans from converging winds and require warm ocean waters to strengthen. The document outlines the damage potential of each, including lightning, hail, strong winds, and flooding from thunderstorms; winds and rotation from tornadoes; and winds, storm surge, and inland flooding from hurricanes.
1) Hurricanes form over warm ocean waters and require specific conditions including high heat, humidity, and low wind shear.
2) Hurricanes develop through several stages from formative to mature as the eye forms and winds intensify.
3) Hurricanes can cause both short term damage through winds and flooding as well as long term destruction through landscape alterations.
This document discusses various hydrometeorological hazards such as tropical cyclones, thunderstorms, floods, droughts, and more. It provides definitions and descriptions of different types of hazards like tropical cyclones, typhoons, hurricanes, thunderstorms, tornadoes, flash floods, floods, storm surges, El Niño and La Niña. The document also discusses how different hazards are monitored and forecasted using tools like satellites, Doppler radar, and preparedness and mitigation strategies to adopt before, during, and after hazards occur.
A hurricane is a severe tropical storm that forms in the North Atlantic Ocean, the Northeast Pacific Ocean east of the dateline, or the South Pacific Ocean east of 160E. Hurricanes need warm tropical oceans, moisture and light winds above them Typhoon — (the Northwest Pacific Ocean west of the dateline)
Severe Tropical Cyclone — (the Southwest Pacific Ocean west of 160E or Southeast Indian Ocean east of 90E)
Severe Cyclonic Storm — (the North Indian Ocean)
Tropical Cyclone — (the Southwest Indian Ocean)
High and low air pressure areas At sea level, air pressure averages 1,013 millibars.Coriolis
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VULNERABILITY ASSESSMENT AND DAMAGE MITIGATION FOR RCC BUILDINGS DUE TO NON SEISMIC HAZARDS IN BANGLADESH
1. VULNERABILITY ASSESSMENT AND DAMAGE
PREDICTION OF REINFORCED CONCRETE
BUILDINGS AGAINST NON-SEISMIC HAZARDS
WELCOME TO OUR
PRESENTATION ON
2. PRESENTED BY:
ENGR. JOHANA SHARMIN
ENGR. SOUPTIK BARMAN TIRTHA
AND
ENGR. KAZI WALIUL HASAN
Date: 20th July, 2016
T H I S P R E S E N T A T I O N I S C O M P L E T E L Y B A S E D
O N M A N U A L O F P W D A N D J I C A P R E P A R E D
U N D E R T H E P R O J E C T F O R C N C R P .
3. CONTENTS
INTRODUCTION
VULNERABILITY ASSESSMENT
NON-SEISMIC NATURAL HAZARDS
BUILDING ELEMENTS
POTENTIAL DAMAGE DUE TO NON SEISMIC FORCES
VULNERABILITY ASSESSMENT GUIDELINES (CYCLONE)
VULNERABILITY AND DAMAGE PREDICTION OF BUILDING
ENVELOPE BY ‘WIND DAMAGE BAND’ MODEL
STRENGTH EVALUATION OF MWFRS
LOAD COMBINATION
WIND LOAD ANALYSIS
ILLUSTRATIVE EXAMPLE
INUNDATION DEPTH DUE TO STORM SURGE AND TSUNAMI
BUILDING DAMAGE ASSESSMENT DUE TO FLOOD, TIDAL SURGE AND
TSUNAMI
MITIGATION MEASURES
4. • The purpose of this manual is to establish a
method of vulnerability assessment of RCC
building against non-seismic natural hazards
so that an appropriate cost effective scheme of
retrofitting may be designed for improved
resistance to non-seismic natural disaster.
5. • Vulnerability assessment of buildings other
than RCC frame structure with in-filled walls
is not within the scope of this manual and is
limited to only non-seismic natural hazards.
• Assessment and load calculation of tornado,
landslide and lightning and thunderstorm are
not considered in this manual.
6. • A systematic examination of a building or
structure through which crucial components
of the structure or building are defined,
identified and assessed that may be at risk
against natural disaster like earthquake,
cyclone, flood, tsunami, cyclone/tsunami
induced storm/ tidal surge etc.
• It also determines appropriate procedure or
countermeasures and evaluates their actual
effectiveness in reducing or removing the risk
after they are put into use.
7. Define Project
Form planning group
Identify and describe probable hazards
Define and classify major components of the structure/ building
Assign relative level of important to the components
Identify potential risk to each component
Describe effects
Set a strategy to deal with most serious potential problem first followed
by natural sequence
Define ways to minimize consequence
Recommend action
Implement action
8. NON SEISMIC NATURAL HAZARDS
Cyclone
Flood
Cyclone induced
storm surge
Tornado
Tsunami
Lighting and
Thunderstorm
Landslide
9. CYCLONE
• In the Atlantic ocean and Eastern Pacific tropical cyclones are
known as- hurricanes.
• In the Western Pacific ocean- typhoons
• In the Indian ocean- cyclones
• Cyclones are normally straight line wind event. Wind speeds range
from very low to very high. High winds associated within tense low
pressure can last for days at a given location.
10. CYCLONE
• A tropical cyclone needs
warm ocean temperature (at
least 28 degree Celsius) in
order to form.
• Heat is drawn up from the
oceans creating heat engine.
• Tall convective tower of
clouds are formed within the
storm as warm ocean water
evaporates.
• As the air rises higher it cools
and condenses releasing latent
heat which causes even more
clouds to form and feed the
storm.
11. CYCLONE
• The coastal regions of
Bangladesh are subject to
damaging cyclones almost
every year.
• They generally occur in
early summer (April-May)
or late rainy season
(October-November).
• Cyclones originate from
low atmospheric pressures
over the Bay of Bengal.
12. WIND INTENSITY SCALES
• Five types of Wind Intensity Scales:
▫ Beaufort Scale (B- Scale)- 1805 and 1921
▫ TORRO Tornado Intensity Scale (T-Scale)- Purely wind speed scale
▫ Fujita Scale or Enhanced Fujita Scale (F or EF)- Rates the strength of
tornadoes based on the damage they cause
▫ The Saffir-Simpson Hurricane Wind Scale
▫ Integrated Kinetic Energy Scale
• Relation between B-scale, T-scale and wind velocity:
▫ B=2(T+4) and conversely, T=(B/2-4)
B 8 10 12 14 16 18 20 22 24 26 28 30
T 0 1 2 3 4 5 6 7 8 9 10 11
v m/s 19.00 26.50 34.80 43.80 53.60 64.00 75.00 86.40 98.40 111.00
124.0
0
137.5
0
v
mph
42.40 59.40 78.00 98.00
120.0
0
143.4
0
168.0
0
193.2
1
220.1
4
248.2
2
277.3
9
307.6
5
v
km/h
68.43 95.63
125.3
4
157.8
0
192.9
3
230.2
3
269.6
1
311.5
0
354.4
3
399.6
3
446.5
9
495.3
2
16. WIND INTENSITY SCALES
• Integrated Kinetic Energy (IKE)
▫ A new scale patented by US Government in 2007 designated to
better convey the destructive power from both hurricane wind
and storm surge.
▫ It has the ability to more accurately predict
How big the hurricane is
How strong it is
What the storm surge may be
so that the emergency management officials can make an
informed decision on whether to evacuate people before the
hurricane gets close to landfall.
▫ The IKE scale measures in a continuous scale from 0-5.99.
17. WIND INTENSITY SCALES
Table: Nomenclature of cyclone in Bangladesh
Nomenclature
Wind speed
km/h
Wind speed
mph
Wind speed m/s
Depression Up to 51 Up to 31.7 Up to 14.17
Deep Depression 52-61 32.3-37.90 14.44-16.94
Cyclonic Storm 62-88 38.5-54.65 17.22-24.44
Severe Cyclonic Storm 89-117 55.28-72.67 24.72-32.50
Severe Cyclonic Storm of hurricane
intensity
>117 >72.67 >32.50
• Bangladesh also uses a 1 to 10 scale to classify tropical cyclones with 10 being
the most severe.
• Alert stage: Signal No. I, II and III
• Warning Stage: Signal No. IV
• Disaster Stage: Signal No. V, VI, VII and VIII, IX, and X
• The most severe cyclones of recent memory since 1970 are November ‘70
(v=222km/h) and April ‘91 (v= 235km/h).
18. FLOOD
• Bangladesh is in the low-
laying Ganges-Brahmaputra
river delta, with many
tributaries flowing into the
Bay of Bengal.
• About 75% of Bangladesh is
less than 10m (33 feet)
above sea level and 80% is
flood plain.
• It is believed that about 10%
of the land shall be under
water, if the sea levels were
to rise 1 m (3.3 feet).
19. TYPES OF FLOODS
• Monsoon Flood
▫ From the major rivers generally rises slowly and the period of rise and
fall may extend from 10 to 20 days or more.
• Flash Flood
▫ In the eastern and northern rivers is characterized by a sharp rise
followed by a relatively rapid recession, often causing high flow
velocities that damage crops and property.
• Local Flood
▫ Due to high localized rainfall of long duration in the monsoon season
often generate water volume in excess of the local drainage capacity.
• Floods due to storm surges
▫ These cyclones predominate during the post monsoon (October-
November) and pre-monsoon (April-June) period.
20.
21.
22. CYCLONE INDUCED STORM SURGE
• A tidal surge is the bulge of
water that washes onto shore
during a storm, measured as a
difference between the height of
storm tide and the predicted
astronomical tide.
• It is driven by wind and low
atmospheric pressure and is
influenced by waves, tides and
uneven bathymetric and
topographic surface.
• Storm surge can reach height of
12m near the center of Category
5 hurricane and fan out across
several hundred miles of coast
line.
23. RELATION BETWEEN WIND VELOCITY, STORM SURGE AND
LIMIT OF INUNDATION IN COASTAL AREAS OF BANGLADESH
Wind
velocity
(km/h)
Storm
surge
height (m)
Wind
velocity
(mph)
Storm
surge
height (ft)
Limit of
inundation
from
coastline
(km)
Limit of
inundation
from
coastline
(miles)
85 1.5 52.80 4.92 1.0 0.62
115 2.5 71.43 8.2 1.0 0.62
135 3.0 83.90 9.84 1.5 0.93
165 3.5 102.50 11.48 2.0 1.24
195 4.8 121.12 5.74 4.0 2.48
225 6.0 140.00 19.68 4.5 2.8
235 6.5 146.00 21.32 5.0 3.11
260 7.8 161.50 25.58 5.5 3.42
24. TORNADO
• A tornado is a powerful column of winds spiraling around a centre of low
atmospheric pressure. It looks like a large black funnel hanging down from a
storm cloud.
• Most tornados have wind speeds less than 177 km/h (110 mph), are
approximately 80 m across, travel several km, lasts less than 20 mins before
dissipating.
• Tornado falls under the category of ‘Extraordinary events’ and ASCE7
considered probability of occurrence of extraordinary events as 10^-6 through
10^-4 per year or greater.
25.
26. TSUNAMI
• The term tsunami comes from the Japanese, composed of the two kanji ‘tsu’
meaning harbour and ‘nami’ meaning wave.
• The principal generation mechanism of a tsunami is the displacement of a
substantial volume of water or perturbation of sea.
• Tsunami can be generated when thrust faults associated with plate boundaries
move abruptly, resulting in water displacement.
27.
28.
29.
30. LIGHTNING AND THUNDERSTORM
• Lightning
▫ A massive electrostatic discharge
between electrically charged regions
within clouds, or between a cloud and
the Earth’s surface.
▫ Lighting occurs approximately 40-50
times a second worldwide, resulting
in nearly 1.4 billion flashes per year.
▫ Lighting primarily occurs when warm
air is mixed with colder air masses
resulting in atmospheric disturbances
necessary for polarizing the
atmosphere.
▫ Objects struck by lightning
experience heat and magnetic forces
of great magnitude.
31. LIGHTNING AND THUNDERSTORM
• Three primary types: from a cloud to itself ( intra-cloud or IC), from
one cloud to another cloud (CC), and finally between a cloud to the
ground (CG).
32. LIGHTNING AND THUNDERSTORM
• Thunderstorm
▫ It is a form of turbulent weather
characterized by the presence of
lighting and acoustic effect on
the Earth’s atmosphere.
▫ Thunderstorm result from the
rapid upward movement of
warm, moist air.
▫ Damage that results from
thunderstorms is mainly
inflicted by downburst winds,
large hailstones, and flash
flooding caused by heavy
precipitation.
▫ The effect of thunderstorm on
RC building is insignificant.
33. LANDSLIDE
• The term landslide describes downhill earth movements that can move slowly
and cause damage gradually, or move rapidly, destroying property and taking
lives suddenly and unexpectedly.
• Most landslides are caused by natural forces or events, such as heavy rain and
snowmelt, shaking due to earthquakes, volcanic eruptions and gravity.
• Landslides are typically associated wet periods of heavy rainfall or rapid
snowmelt and tend to worsen the effects of flooding.
• This hazard is not directly related to reinforced concrete buildings.
34. BUILDING ELEMENTS
Structural Elements
• Foundation
• Column
• Slab
• Beam
• Shear Walls
Non Structural Elements
• Stairways, Doorways, Windows, Partitions, Glass, Cornices,
False ceiling, Facades, Pipes, Wall claddings, Lighting
fixtures etc.
Building Contents
• Furniture, Appliances, Electronics, Equipments, Air-
conditioners, Stored items etc.
35. POTENTIAL DAMAGES DUE TO WIND (CYCLONE)
• Major causes of damage:
Low quality of
construction
Inappropriate
techniques and
utilization of low
resistance
materials
Failure of doors
and windows due
to wind pressure
Excessive
openings in the
building envelope
Location of the
building
General
roughness of the
surrounding
terrain
Height of the
building above
ground
Height of the
building more
than surrounding
structures and
vegetation
Configuration of
the building
Surrounding
topography
36. POTENTIAL DAMAGES DUE TO WIND (CYCLONE)
• Structural damage:
Collapse of structural
elements or the entire
building along with damage
to the building envelope
Water infiltration into the
building exterior wall
Leakage between door and
frame, frame and wall and
threshold and door
37. POTENTIAL DAMAGES DUE TO FLOOD
• A building may face the following hazards due to flood:
Lateral
hydrostatic and
buoyant forces
Hydrodynamic
forces
Impact load
caused by
floating debris
Erosion and
scour
Geotechnical
considerations
Contamination
Breaking waves
with floating
debris
38. POTENTIAL DAMAGES DUE TO FLOOD
• Due to mentioned flood related hazards the building shall face
the following problems:
Settlement of
Foundation
Scouring of
wall base
Debris impact
Impact of storm
surge wave
39. POTENTIAL DAMAGES DUE TO CYCLONE
INDUCED STORM SURGE
• Bangladesh coastline including islands are densely populated and
many regions lie less than 3 m (10 ft).
• Currents created by tides combine with the waves severely erode
beaches and coastal highways.
• Buildings that survive cyclone winds can be damaged if their
foundations are undermined and weakened by erosions.
• Impact of water borne debris and logs may seriously damage a
building or structure in their path.
40. POTENTIAL DAMAGES DUE TO TSUNAMI
• Difficulty of tsunami is that it cannot be precisely predicted, even
if the magnitude and location of an earthquake is known.
• Smashing force of a wall of water travelling at high speed
destroys everything in its path.
• A series of wave trains with periods ranging from minutes to
hours arrive when tsunami strikes.
• Wave heights as high as 10m (33ft) can be generated by a large
event.
• A wave of only 0.9m (3 ft) high, 3.2 km long and 1600 km wide
contains 10 billion tons of water. A 3.0 m (10 ft) wave shall
produce water velocity of approximately 20m/s.
41. POTENTIAL DAMAGES DUE TO TORNADO
• Because of extreme high pressure and missile loads that
tornados can induce, specially building envelope may face
serious damage due to tornado.
• Most buildings experience significant building envelope
damage and damage to interior partitions and ceilings if
they are in the path of a strong or violent tornado (F4 and
F5).
• As wind speed rapidly decreases with increase distance
from the center of tornado, a building on the periphery of a
strong or violent tornado could be subjected to moderate to
high wind speed depending upon the distance from the
center of the tornado.
42. VULNERABILITY ASSESSMENT GUIDELINES
(CYCLONE)
• This covers the guidelines for survey and inspection of the
building for assessment of degree of vulnerability against
cyclone.
• Standard pro forma prepared for survey and inspection shall
establish
▫ Building typology, configuration, weaknesses in structural system
and elements, inadequacy in the material strength and method of
construction
so that an appropriate cost effective scheme of retrofitting may
be designed for improved cyclone resistance and thus decreasing
vulnerability to any future non-seismic natural disaster like
cyclone.
43. VULNERABILITY ASSESSMENT GUIDELINES
(CYCLONE)
• Guidelines for filling standard pro forma for field survey of
building
▫ The pro forma has been prepared on the basis of a questionnaire
presented in checklist from through which detailed information can
be gathered regarding
Building configuration, structural system, member sizes, architectural
details, construction material and building environment
▫ The pro forma contains basically two types of questions.
In the first set, multiple options are given and the surveyors have to
provide a tick on the respective box.
In other set of questions, the answer is to be provided in definite
quantitative terms on the basis of actual measurement or information at
site in the box provided.
44. VULNERABILITY ASSESSMENT GUIDELINES (CYCLONE)
• Standard Pro forma for Vulnerability Assessment of Building
▫ Pro forma A :
statistical information of the building for the purpose of characterization
of the building typology
Information about structural system, member sizes, connection details
for examining the cyclone resistance of the existing building and to
retrofit them
▫ Pro forma B:
Summary of information about building envelope collected from Pro
forma A for examining the cyclone resistance of building envelope
▫ Pro forma C:
Information collected from Pro forma A about structural system and its
components for performing structural strength analysis
45. VULNERABILITY AND DAMAGE PREDICTION OF
BUILDING ENVELOPE BY ‘WIND DAMAGE BAND’ MODEL
• The amount of damage is defined as the ratio of replacement cost of damaged
building components (due to wind pressure and wind borne missiles) to the
replacement cost of the building.
• It is necessary that a wind damage prediction model satisfies the following
criteria:
▫ The model should be capable of predicting the actual amount of damage to a building
▫ There should have some proportionality relationship between the model predictions of
damage degrees to individual buildings based upon their relative wind performance
characteristic.
• The first criterion is the desired output, upon which several decisions are ultimately
based. The second criterion enables a check to be made on the precision of the model
prediction.
46. VULNERABILITY AND DAMAGE PREDICTION OF
BUILDING ENVELOPE BY ‘WIND DAMAGE BAND’ MODEL
• Wind Damage Band:
▫ The procedure for wind damage prediction of individual building based on the
concept of wind damage bands for building occupancy classes. Wind damage bands
define the damage degree ranges bounded by a lower and upper damage threshold
for given intensities of the wind hazard.
▫ The upper boundary damage band for a class of building represents the wind
damage function of the least wind resistant building in the building class, while the
lower boundary represents the damage function of the most wind resistant building
in the building class.
▫ For individual buildings the damage degree due to the wind pressure and wind-
borne missile is given by:
47. VULNERABILITY AND DAMAGE PREDICTION OF
BUILDING ENVELOPE BY ‘WIND DAMAGE BAND’ MODEL
• Wind Damage Band:
48. VULNERABILITY AND DAMAGE PREDICTION OF
BUILDING ENVELOPE BY ‘WIND DAMAGE BAND’ MODEL
• Wind Damage Band:
•RRI= a measure of the building’s
damage resistance relative to other
buildings
•RRI very close to 1 indicates a
building whose features and
components offer very little
resistance to wind damage, while
RRI very close to zero represents a
building whose features and
components offer very high
resistance to wind damage.
49. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• Basic Requirements
• Nominal and
factored loads
in load
combination
1
• Adequate
stiffness
2 • Self
restraining
forces
arising
3
• Load
effects
4 • Resist forces
due to
earthquake
and wind.
5
50. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• Special Requirements for Coastal Saline Areas
Minimum live
load of 4.8 kN/m2
(100 lb/ft2)
No reduction in
live load
Denseness of
concrete
Clear cover to
reinforcement
Effect of chloride
on concrete
Minimum strength
of concrete shall
be 24 Mpa
No artificial
coarse aggregate
Fine aggregate
shall be 100%
coarse
Saline water
strictly prohibited
51. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• Steps for Non-Seismic Structural Strength Evaluation
Select the
building to be
analyzed
Identify
appropriate
structural
system
Determine
risk category
Collect information
related to type of
materials used & their
strength, design criteria
etc.
Determine
basic wind
speed
Determine wind
load parameters
Select
appropriate
lateral force
procedure
Select gravity,
live and wind
loads
Calculate
velocity
pressure
Calculate wind
pressure
52. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• Steps for Non-Seismic Structural Strength Evaluation
Calculate forces
acting on
MWFRS
Collect test core-
concrete
Study story drift
limitations
Design &
evaluate elements
of MWFRS
Compare
capacity of
existing MWFRS
Evaluate
overturning
effects
Verify structure’s
continuous load
path
Comment on the safety of
individual members of MWFRS
against wind load combination
53. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• The evaluation method depends on:
▫ Structural framing system
▫ Information known about its existing condition
▫ Logistic and economic consideration
• Two methods of strength evaluation of existing structures:
▫ Analytic evaluation based on member dimensions and material properties
▫ Load test (if member dimensions and material properties are not possible to
determine)
• If the dimensions and material properties are available then:
▫ Dimension of structural elements shall be established at critical sections.
▫ Location and size of the reinforcing bars shall be determined by measurement.
▫ Concrete strength shall be based on the results of cylinder tests.
▫ The number of core tests may depend on the size of the structure and sensitivity of
the structural safety to concrete strength.
54. STRENGTH EVALUATION OF MAIN WIND FORCE
RESISTING SYSTEM
• Basic parameters in determining wind loads:
• Earthquakes and wind load need not be assumed to act simultaneously. In
some instances, forces due to wind might exceed those due to earthquake,
while ductility requirements might be determined by earthquake load.
Basic wind
speed
Wind
directionality
factor
Building
exposure
category
Importance
factor
Topographic
factor
Gust effect
factor
Enclosure
classification
Internal
pressure
coefficient
External
pressure
coefficient
55. STRENGTH EVALUATION OF MAIN WIND FORCE RESISTING
SYSTEM
• Coastal areas subjected to flooding can be designated into two categories:
▫ Coastal A-zone (Risk area)
▫ Coastal High Hazard Area (V-zone) (High risk area)
• Coastal A-zones lie landward of V-zones. Coastal A-zones are subjected to the
effects of waves, high velocity flows, and erosion, although not to the extent
those V-zones are.
• In order for a coastal A-zone to be present, two conditions are required:
▫ A still water flood depth greater than or equal to 0.61m.
▫ Breaking wave heights greater than or equal to 0.46m.
▫ Forces generated by the impact of flood borne debris.
• Coastal V-zones extend from offshore to the inland limit of a primary frontal
dune along an open coast.
• Generally speaking, A-zones are designated where wave less than 0.9m (3ft)
is expected. V-zones are designated where wave height greater than 0.9m (3ft)
is expected.
56. LOAD COMBINATION
• Combining factored loads using strength design (BNBC15 and
ASCE7-5):
1. 1.4 (D+F)
2. 1.2(D+F+T)+1.6(L+H)+0.5(Lr or R)
3. 1.2D+1.6 (Lr or R)+ (1.0L or 0.8W)
4. 1.2D+1.6W+1.0L+0.5 (Lr or R)
5. 1.2D+1.0E+1.0L
6. 0.9D+1.6W+1.6H
7. 0.9D+1.0E+1.6H
• Load combination including flood load
▫ In V-Zones or coastal A-zones, 1.6W in combinations (4) and (6) shall be
replaced by 1.6W+2.0Fa.
▫ In non-coastal A-zones, 1.6W in combination (4) and (6) shall be replaced
by 0.8W+1.0Fa.
57. LOAD COMBINATION
• Combining nominal loads using allowable stress design:
1. D
2. D+L
3. D+F
4. D+H+F+L+T
5. D+H+F+ (Lr or R)
6. D+H+F+0.75 (L+T) +0.75 (Lr or R)
7. D+H+F+ (W or 0.7E)
8. D+H+F+ 0.75 (W or 0.7E) +0.75L+0.75 (Lr or L)
9. D+L+ (W or 0.7E)
10. 0.6D+W+H
11. 0.6D+0.7E+H
• Load combination including flood load
▫ In coastal zones vulnerable to tidal surge 1.5Fa shall be added to other loads in
combination (7), (8), (9) and (10) and E shall be set equal to zero in (7), (8) and (9).
▫ In non- coastal zone, 0.75Fa shall be added to combination (7), (8), (9) and (10) and
E shall be set equal to zero in (7), (8) and (9).
58. WIND LOAD ANALYSIS
• METHOD 1- SIMPLIFIED PROCEDURE:
▫ It can be used for determining wind forces on low rise enclosed building
with flat, gabled or hipped roof, provided it satisfied the requirements
below.
▫ Main wind force resisting system:
The building is a simple diaphragm building (no structural separation).
The building is a low rise building that complies with the following conditions:
Mean roof height h is less than or equal to 18.3m (60.0ft)
Mean roof height h does not exceed least horizontal dimension
The building does not comply with requirements for open or partially enclosed
buildings.
Open building: a building having each wall at least 80 percent open.
Partially Enclosed building:
59. WIND LOAD ANALYSIS
• METHOD 1- SIMPLIFIED PROCEDURE:
The building is a regular-shaped building having no unusual geometrical
irregularity in spatial form.
The building is not a flexible (slender) building and has a fundamental
natural frequency greater than or equal to 1Hz.
The has an approximately symmetrical cross section in each direction
with either a flat roof or a gable or hip roof with θ≤45˚.
The building does not have response characteristics.
▫ Components and claddings
The mean roof height h≤18.3m (60.0ft).
The building is enclosed, a regular shape building and does not have
response characteristics as defined earlier.
The building has either a flat roof, a gable roof with θ≤45˚ or a hip roof
with θ≤27˚.
60. WIND LOAD ANALYSIS
▫ Design procedure
▫ Design of Main Wind-force Resisting System
Ps, the combination of windward and leeward net pressure,
▫ Design of Components and Claddings
Pnet, net design wind pressure,
Basic wind
speed, V
(Table 1)
Importance
factor, I (Table
2)
Exposure
category
Height and
exposure
adjustment
coefficient λ
(Table 4)
61. WIND LOAD ANALYSIS
• METHOD 2- ANALYTICAL PROCEDURE
▫ A building whose design wind loads are determined in
accordance with this section shall meet all of the following
conditions:
The building is a regular shaped building having no unusual geometrical
irregularity in spatial form.
The building does not have response characteristics.
62. WIND LOAD ANALYSIS
• METHOD 2- ANALYTICAL PROCEDURE
▫ Design Procedure:
Basic wind
speed, V
(Table 1)
Wind
directionality
factor (Table
5)
Importance
factor, I
(Table 2)
Exposure
category
Velocity
exposure
coefficient (Kz
or Kh)
Topographic
factor, Kzt
Gust effect
factor, G or
Gf
Enclosure
classification
Internal
pressure
coefficient,
Gcpi (Table 9)
External
pressure
coefficient,
Cp or GCpf
Velocity
pressure qz
or qh
Design
load p or F
66. TABLE 1: BASIC WIND SPEED (3-SECOND GUST SPEED)
FOR SELECTED LOCATIONS OF BANGLADESH
Location
Basic Wind Speed
m/s Km/h Mph
Sirajgonj 50.6 182.16 113.14
Srimongol 50.6 182.16 113.14
St. Martin
Island
80.0 288.0 179.0
Sunamgonj 61.1 220.0 136.62
Sylhet 61.1 220.0 136.62
Sandwip 80.0 288.0 179.00
Tangail 50.6 182.16 113.14
Teknaf 80.0 288.0 179.00
Thakurgaon 41.1 147.96 91.90
67. TABLE 2: OCCUPANCY CATEGORIES OF BUILDINGS AND OTHER
STRUCTURES FOR FLOOD, SURGE, WIND AND EARTHQUAKE LOADS
68. TABLE 3: IMPORTANCE FACTOR, I (WIND LOADS)
Category or
Importance Class
Non-cyclone Prone
Regions and Cyclone
Prone Regions with V=
38-44m/s
Cyclone Prone Regions
with V>44m/s
I 0.87 0.77
II 1.00 1.00
III 1.15 1.15
IV 1.15 1.15
69. TABLE 4: HEIGHT AND EXPOSURE ADJUSTMENT
COEFFICIENT, λ
Adjustment Factor For Building Height and Exposure, λ
Mean roof height Exposure
ft meter A B C
15 4.6 1.00 1.21 1.47
20 6.0 1.00 1.29 1.55
25 7.6 1.00 1.35 1.61
30 9.1 1.00 1.40 1.66
35 10.7 1.05 1.45 1.70
40 12.2 1.09 1.49 1.74
45 13.7 1.12 1.53 1.78
50 15.2 1.16 1.56 1.81
55 16.8 1.19 1.59 1.84
60 18.3 1.22 1.62 1.87
70. TABLE 5: WIND DIRECTIONALITY FACTOR, Kd
Structure Type Directionality Factor, Kd
Buildings
Main Wind-force-resisting system
Components and cladding
0.85
0.85
Arched roofs 0.85
Chimneys, tanks, similar structure
Square
Hexagonal
Round
0.96
0.95
0.95
Solid signs 0.85
Open Signs & Lattice Frame work 0.85
Trussed towers
Triangular, square, rectangular
All other cross sections
0.85
0.95
71. SURFACE ROUGHNESS CATEGORIES AND EXPOSURE
CATEGORIES
• Surface roughness categories
▫ Surface roughness A: urban and suburban areas,
wooded areas or other terrain with numerous closely
spaced obstructions having the size of single family
dwellings or larger
▫ Surface roughness B: open terrain with scattered
obstructions having heights generally less than 9.1m.
This category includes flat open country, grasslands,
and all water surfaces in cyclone prone regions.
▫ Surface roughness C: flat, unobstructed areas and water
surfaces outside cyclone prone areas.
73. GUST EFFECT FACTOR, G or Gf
• Frequency determination
▫ The approximate building natural frequency, na shall be
permitted to be calculated for concrete buildings meeting the
following requirements:
The building height is less than or equal to 91m (300ft).
The building height is less than 4 times its effective length Leff
The effecting length Leff in m (ft.) in the direction under consideration
shall be determined from the eqn.
• Natural Period and Frequency
▫ It is important to distinguish between the building period (Ta)
with site period or with the period of earthquake (T=1/n).
74. TABLE 6: VALUES OF APPROXIMATE PERIOD
PARAMETERS Ct AND x
Structure Type
Ct
x
SI Fps
Moment resisting frame system in which the frames
resist 100% of required seismic force and are not
enclosed or adjoined by components that are more rigid
and will prevent the frames from deflecting when
subject to seismic force:
Steel moment-resisting frame
Concrete moment resisting frame
0.0724
0.0466
0.028
0.016
0.8
0.9
Eccentrically braced steel frame 0.0731 0.03 0.75
All other structural system 0.0488 0.02 0.75
▫ But in the commentary of ASCE 07-5, it has been suggested that the above
expressions are based on recommendations for earthquake design. For wind
design applications, these values may be unconservative.
75. TABLE 7: COMPARATIVE VALUES OF FREQUENCY OF
BUILDING FOR DIFFERENT EQUATIONS
Equation (fps) Equation(SI)
N1 (Example
values)
Type
Ta = Ct hn
x
n1 = 1/Ta
Ta = Ct hn
x
n1 = 1/Ta
0.70
1.17
Flexible in E-W
Rigid in N-S
Ta = 0.1N
n1 = 1/ Ta
Ta = 0.1N
n1 = 1/ Ta
0.83 Flexible
n1 = 43.5/ H0.9 n1 = 14.3/ H0.9 0.48 Flexible
n1 = 100/H (avg
value)
n1 = 75/H (lower
bound value)
n1 = 30.49/H (avg
value)
n1 = 22.86/H
(lower bound
value)
0.68
0.51
Flexible
Flexible
fn1 = 150/H fn1 = 45.73/H 1.014 Rigid
n1 = 220/H n1 = 67/H 1.49 Rigid
76. GUST EFFECT FACTOR, G or Gf
• For rigid structures having a fundamental frequency greater than or equal
to 1Hz, the gust effect factor shall be taken as 0.85 or calculated by the
eqn:
77. TABLE 8: TERRAIN EXPOSURE CONSTANTS IN SI AND
FPS SYSTEM
Expo
sure
α zg (m)
zg
(ft)
â b ά Б c l (m)
l
(ft)
є
zmin
(m)
zmin
(ft)
A 7.0 365.76 1200 1/7 0.84 ¼.0 0.45 0.30 97.54 320 1/3.0 9.14 30
B 9.5 274.32 900 1/9.5 1.0 1/6.5 0.65 0.20 152.4 500 1/5.0 4.57 15
C 11.5 213.36 700 1/11.5 1.07 1/9.0 0.80 0.15 198.12 650 1/8.0 2.13 7
78. GUST EFFECT FACTOR, G or Gf
• For flexible or dynamically sensitive structures are those
which satisfy any one of the following conditions:
▫ A slender building or structure having a height exceeding five times the
least horizontal dimension.
▫ A building or structure that has a fundamental natural frequency less
than 1Hz.
79. ENCLOSURE CLASSIFICATION
• General
▫ All buildings shall be classified as enclosed, partially enclosed or open
• Openings
▫ A determination shall be made of the amount if openings in the building
envelope to determine the enclosure classification
• Wind borne debris
▫ Glazing in building located in wind-borne debris regions shall be
protected with an impact resistant covering or be impact resistant
glazing.
• Multiple classification
▫ If a building by definition complies with both the “open” and “partially
enclosed” definitions, it shall be classified as “open” building. A
building that does not comply with either the “open” or “partially
enclosed” definitions shall be classified as “enclosed” building.
80. TOPOGRAPHIC EFFECT
• Wind speed-up over Hill, Ridges and Escarpments
▫ The hill ridge or escarpment is isolated and unobstructed upwind by
other similar topographic features of comparable heights for 100 times
the height of the topographic feature (100H) or 3.22 km (2.0 miles,
whichever is less.
▫ The structure is located in the upper one-half of a hill or ridge or near
the crest of an escarpment.
▫ H/Lh ≥ 0.2
▫ H is greater than or equal to 4.5 m (15 ft) for exposure B and C and 18.0
m (60.0 ft) for exposure A.
• Topographic factor, Kzt
81. TABLE 9:INTERNAL PRESSURE COEFFICIENT GCpi
Enclosure Classification Gcpi
Open Building 0.00
Partially Enclosed Building
+0.55
-0.55
Enclosed Building
+0.18
-0.18
• Plus and minus signs signify pressure acting toward and away from internal
surfaces respectively.
• Values of Gcpi shall be used with qz or qh
• Two cases shall be considered to determine the critical load requirement for the
appropriate condition:
• A positive value of GCpi applied to all internal surfaces
• A negative value of Gcpi applied to all internal surfaces
82. TABLE 10: EXTERNAL PRESSURE CO-EFFICIENT, Cp OF
WALLS AND ROOF FOR ENCLOSED, PARTIALLY
ENCLOSED BUILDING
Wall Pressure Coefficient, Cp
Surface L/B Cp Use with
Windward wall All values 0.8 qz
Leeward wall
0-1 -0.5
qh2 -0.3
>4 -0.2
Side wall All values -0.7 qh
83. TABLE 10: EXTERNAL PRESSURE CO-EFFICIENT, Cp OF
WALLS AND ROOF FOR ENCLOSED, PARTIALLY
ENCLOSED BUILDING
Wind
Direction
Roof pressure coefficient Cp for use with qh
Windward Leeward
Angle, θ (degrees) Angle, θ (degrees)
normal to
ridge for
θ≥10◦
h/L 10 15 20 25 30 35 45 >60 10 15 >20
≤0.25
-0.7
-0.18
-0.5
0.0
-0.3
0.2
-0.2
0.3
-0.2
0.3
0.0
0.4
0.4 0.01θ -0.3 -0.5 -0.6
0.5
-0.9
-0.18
-0.7
-0.18
-0.4
0.0
-0.3
0.2
-0.2
0.2
-0.2
0.3
0.0
0.4
0.01θ
-0.5 -0.5 -0.6
≥1.0
-1.3
-0.18
-1.0
-0.18
-0.7
-0.18
-0.5
0.0
-0.3
0.2
-0.2
0.2
0.0
0.3
0.01θ
-0.7 -0.6 -0.6
84. TABLE 10: EXTERNAL PRESSURE CO-EFFICIENT, Cp OF WALLS
AND ROOF FOR ENCLOSED, PARTIALLY ENCLOSED BUILDING
Wind
Direction
h/L
Horizontal
distance from
windward
edge
Cp
•Value is provided for
interpolation purposes
• Value can be reduced
linearly with area over
which it is applicable as
follows
Normal to
ridge for
θ<10 and
parallel to
ridge for all θ
≤0.5
O to h/2 -0.9,-0.18
h/2 to h -0.9,-0.18
H to 2h -0.5,-0.18
>2h -0.3,-0.18
≥1.0
0 to h/2 -1.3,-0.18
Area (sqft)
Reduction
factor
≤100
(9.3sqm)
1.0
> h/2 -0.7, -0.18
200
(23.2sqm)
0.9
≥1000
(92.9sqm)
0.8
88. VELOCITY PRESSURE, qz
DESIGN WIND LOADS ON ENCLOSED AND PARTIALLY
ENCLOSED BUILDING
• Sign convention
▫ Positive pressure acts towards the surface and negative pressure
acts away from the surface.
• Critical load conditions
▫ Values of external and internal pressures shall be combined
algebraically to determine the most critical load.
• Tributary areas greater than 65m2 (700 sft.)
▫ Components and cladding elements with tributary areas greater
than 65m2 shall be permitted to be designed using the provisions
of MWFRS.
89. DESIGN OF MAIN WIND-FORCE RESISTING SYSTEM
• Rigid buildings of all heights
• Flexible Buildings
• Parapets
• Design Wind Load Cases
• Components and Claddings
▫ Low rise building & building with h≤18.3m (60ft)
▫ Buildings with h> 18.3m (60ft)
93. INUNDATION DEPTH DUE TO STORM SURGE AND
TSUNAMI IN COASTAL AREAS
• Introduction
▫ Bangladesh has approximately 710 km (441 miles) coastline.
▫ 13 coastal districts vulnerable to strong tidal surge, wind action,
high waves and tropical cyclones and tsunami:
Satkhira
Khulna
Bagerhat
Perojpur
Barisal
Barguna
Patuakhali
Bhola
Lakshmipur
Noakhali
Feni
Chittagong
Cox’s Bazar
50 upazillas/ thanas are considered to be
exposed directly to vulnerability from natural
disaster.
All these areas are comparatively low in
elevation
Of these areas, about 62% of the lands
have an elevation of up to 3 meters (10ft)
and 86% up to 5 meters (16.40 ft) from mean
sea level.
94. INUNDATION DEPTH DUE TO STORM SURGE AND
TSUNAMI IN COASTAL AREAS
• Risk zone and high risk area
▫ Multipurpose Cyclone Shelter Programme (MPCSP) has
delineated the coastal belt of Bangladesh into two zones
based on the possible extent of the inland intrusion of the
cyclone storm surge.
Risk zone (RZ) and
High Risk Area (HRA)
• Inundation depth due to storm surge:
▫ IWM, while calculating inundation depth due to cyclone,
has considered the following climate change sceneries for
2050:
Sea level rise of 0.5m (1.64 ft)
10% increase in maximum wind speed of cyclone
95. INUNDATION DEPTH DUE TO STORM SURGE AND
TSUNAMI IN COASTAL AREAS
• Comparison of Inundation depths due to storm surge and
tsunami
▫ Inundation depth is higher due to tidal surge than tsunami.
▫ As the maximum water velocity in relation to depth of water is
double for tsunami compared to tidal surge, the hydrodynamic
force, debris impact force shall be same for tsunami in
comparison to tidal surge for half the water depth.
▫ For tidal surge water rises gradually with the increase of intensity
of wind velocity, whereas water forces due to tsunami is
somewhat sudden and surge volume of receding water draining
off the land has the devastating power of carrying almost
everything with it.
▫ So even with half the inundation depth compared to tidal surge,
the damage and destruction due to tsunami may be much more.
96. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Introduction
▫ Flood actions include
Hydrostatic force
Hydrodynamic force
Impact force
Breaking wave force
Time-dependent local soil scour
▫ The assessment (a stochastic methodology) is based on
both flood water depth and flood water velocity. The
methodology focuses on the vulnerability of reinforced
concrete frame building with infill concrete block
walls.
97. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Introduction
▫ Expected flood damage (EFD):
▫ Buildings are considered a total loss when EFD reaches
60%. This threshold indicates that the cost of repairing
the building is equal to the value of replacing it.
▫ Buildings located particularly in coastal areas are
frequently affected by high winds in addition to the
flood action.
▫ Although tsunami and storm surge are very different
events, the effects on the buildings or infrastructures of
the low-lying coastal zones can be very similar.
98. Load Cases and Forces for Different Flooding Conditions
Riverine
Flood
•Slow rise of water allowing
infiltration of water into the
building.
•Flood water level equal at both
sides of external wall
•Hydrodynamic force due to water
velocity on the outside of external
column/wall
•No hydrostatic force
•Flash flood
•High velocity water
Hydrostatic as well as
hydrodynamic force
Storm Surge
Depth of still water increments
gradually & flooding of coastal area
occurs hours before system landfall
•Hydrodynamic force due to storm
surge
•No hydrostatic force
Breaking wave reaches the building
located at the coast line
•Breaking wave force
•No hydrostatic force
Possibility of carrying debris Debris impact force
Tsunami
High velocity current with turbulent
bores
Hydrostatic as well as
hydrodynamic forces
Possibility of breaking waves with
direct impact on building
Breaking wave force
Possibility of carrying debris either
from sea or from coast as broken
buildings or tree trunks
Debris impact force
99. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Flood Forces and Loads
▫ Flood depth (d):
▫ Design Flood Elevation (DFE):
▫ Flood proofing design depth:
▫ Hydrostatic forces:
The pressure exerted by still and slow moving water (velocity less
than 3.0m/sec) is called hydrostatic pressure.
During any point of flood water contact with a structure, hydrostatic
pressures are equal in all direction and always act in perpendicular
direction to the surface on which they are applied.
Pressure increases linearly with depth
Four types:
Lateral hydrostatic force
Combined water and saturated soil pressure
Equivalent hydrostatic pressure due to low velocity of water
Vertical buoyancy hydrostatic pressure
102. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Flood Forces and Loads
▫ Hydrodynamic Forces:
Low velocity hydrodynamic forces
Where flood water velocities do not exceed 3m/s (10ft/s).
In this case, the hydrodynamic effects of moving water shall
be permitted to be converted to an equivalent hydrostatic
loads by increasing the DFE for design purpose by an
equivalent surcharge depth, dh.
High velocity hydrodynamic forces
for special structures and conditions and for velocity greater
than 3m/s, the basic eqn for hydrodynamic pressure is,
104. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
CONVERSION OF EQUIVALENT HEAD TO EQUIVALENT HYDROSTATIC FORCE
105. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Flood Forces and Loads
▫ Hydrodynamic Forces:
Complexities:
▫ One of the complexities when calculating forces generated by a
storm surge is determining the flood water velocity.
▫ Both the direction and velocity of flood water vary drastically
throughout the course of a storm system.
▫ FEMA (2000) recommended that flood water velocities due to
storm surge should be assumed to lie between specific lower and
upper bounds.
▫ For tsunami, the upper bound eqn is,
106. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Flood Forces and Loads
▫ Debris Impact Forces:
It is related to isolated occurrences of typically sized debris or
floating objects striking the building.
Magnitude of impact load due to a floating object:
With the coefficients set equal to 1, the eqn reduces to
▫ Breaking Wave Force:
Two wave forces:
Breaking waves on columns/piles:
Breaking waves on walls:
107. BUILDING DAMAGE ASSESSMENT DUE TO FLOOD,
TIDAL SURGE AND TSUNAMI
• Components of Buildings Affected by Flood:
▫ Foundation
▫ Reinforced concrete frame
▫ Infill external brick/ block wall
▫ Doors and windows
▫ Utility services, building contents and finishes
• Flood Damage Computation
▫ EFD defined as the expected value of flood damages, is then computed
per building unit by considering the aggregated damage to all five
building components.
108. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Planning and Site Consideration
▫ As far as possible, the building shall be on good ground.
▫ Regular plan shapes are preferred.
▫ For individual building, a circular or polygonal plan is
preferred over rectangular or square plans.
▫ Ornamental architecture involving horizontal or vertical
cantilever projections, facets etc should be avoided.
▫ Building should not be located in low-lying areas as cyclones
are invariably associated with flood & tidal surge.
▫ Long walls having lengths in access of about 3.5m shall be
provided with cross walls.
▫ In hilly regions, construction along ridges should be avoided.
▫ It is always preferable to locate the facility on a site in
Exposure A. Also where possible, avoid locating a building on
an escarpment or upper half of a hill.
▫ Trees in excess of 150mm in diameter, poles or tower should
not be placed near office or shelter buildings.
109. MITIGATION MEASURES AGAINST NON-
SEISMIC NATURAL HAZARDS
• Inspection, Periodic Maintenance, Repair and
Replacement
▫ It is important to understand that, over time, a facility’s
wind-resistance will degrade due to exposure to weather
unless it is periodically maintained and repaired.
• Exterior Doors
▫ Door assembly should be of sufficient strength to resist
negative and positive wind pressure.
▫ When corrosion is problematic, anodized aluminium or
galvanized doors and frames and stainless steel hardware
are recommended.
• Wall Opening
▫ Opening just below roof level is avoided.
▫ Percent of the total opening in the cross-section of any
wind resisting walls shall be less than 50% of the width of
the wall.
110. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Glass Paneling
▫ A wooden board may be securely fixed outside
all large size glass panels as and when cyclone/
wind storm warning is issued.
▫ Provide well-designed glass panels.
▫ Recourse may be taken to reduce the panel size
to smaller dimension.
▫ Glass panes can be strengthened by pasting thin
plastic film or paper strips.
▫ To prevent damage to glass panels from wind
borne missiles, a metallic fabric/ mesh may be
provided outside the large panels.
111. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Design Considerations
▫ Basic wind speed
▫ Pressure and Force
▫ Load Effects
▫ Wind Direction
▫ Resistance to Corrosion
• Causes of Damage Propagation
▫ Lack of general awareness among engineers that
structural integrity against collapse is important enough
to be regularly considered in design.
▫ In attempting to achieve economy in structure through
greater speed of erection and less site labor, systems may
be built with minimum continuity.
▫ Un-reinforced or lightly reinforced load bearing walls in
multistory structure may also have inadequate continuity
and joint rigidity.
112. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• General Structural Integrity
▫ Good plan layout
▫ Integrated tie system
▫ Change direction of span of floor slab
▫ A part of the detailed design effort
▫ Ductile detailing
▫ Load bearing interior partition
• Durability
▫ Special attention needs to be given to specification of
adequate protection to ferrous metals.
▫ Where termites are problematic, it is recommended that
the soil be treated with a germicide.
▫ When corrosion is problematic, anodized aluminium or
galvanized doors and frames and stainless steel hardware
are recommended.
113. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Non load bearing walls
▫ Although masonry walls are not indented to carry gravity loads,
they must be designed to resist the positive and negative wind
loads in order to avoid collapse.
• Lighting protection system
▫ It is important to adequately design the attachment of the
lightning protection system and it should be firmly fixed with the
roof system.
• Elevator Pent House
▫ Proper waterproofing membrane should be provided in external
doors and windows of elevator penthouse or machine room.
• Protection of Utility System
▫ If the lowest floor is above DFE, utility system components can
be protected from flood damage by locating them anywhere on
or above the lowest floor of the structure.
114. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Mitigation Measures for Tornado
▫ Safe room can be located anywhere in the house or even
outside.
▫ Safe room must be designed for wind speeds up to 112m/s
▫ Exposure B and exposure C
▫ Partially enclosed
▫ Structurally isolated from the main structure of the house
▫ Securely anchored to the foundation
▫ All components must be designed and tested to resist the
specified wind forces and prevent perforation by wind-
borne debris.
▫ Adequate ventilation
▫ Constructed in accordance with the perspective design of
the FEMA 320
115. MITIGATION MEASURES AGAINST NON-SEISMIC
NATURAL HAZARDS
• Mitigation Measures for Tsunami
▫ Elevate the structure above the ground floor with deeper
foundation and open ground floor
▫ The columns should be firmly fixed to the foundation, also
braced to each other.
▫ As much as possible, leave vegetations and reefs intact.
▫ Do not build building at low level on the shore line at the
top of a smooth shallow beach.
▫ Buildings should not be close together in a way that makes
a wider dam.
▫ Construct small sea walls parallel to the sea shore.
▫ Construct multi level buildings within the inundation zone
▫ Orient the building at an angle to the shore line.
▫ Construct building with reinforced concrete structures.