A tsunami is a series of waves generated by the displacement of water, usually caused by earthquakes, volcanic eruptions, landslides or other disturbances. The International Tsunami Warning System monitors for tsunamis in the Pacific Ocean and issues warnings to local authorities. The best sources of information during a tsunami are the two Tsunami Warning Centers and local emergency management agencies who provide warning messages to notify the public of any tsunami risks.
A tsunami is a series of waves generated by large displacements of water, typically caused by earthquakes, volcanic eruptions, landslides, or meteorite impacts under water or along coastlines. Common triggers include large earthquakes, volcanic eruptions, and landslides. When a major earthquake or landslide occurs near or undersea, it can displace enough water to cause a destructive tsunami. Coastal areas are most at risk from tsunamis, as the waves travel inland rapidly.
Tsunami is a Japanese word meaning harbor wave. Tsunamis are series of large waves generated by earthquakes, landslides, volcanic eruptions, or other disturbances that displace large volumes of water. The first recorded tsunami was in 1480 BC in the Mediterranean. Tsunamis cause devastating damage when they reach coastal areas due to their ability to flood large areas inland with fast-moving water. Proper warning systems and evacuation of coastal areas can help reduce loss of life from tsunamis.
The document provides safety tips for tsunamis, including making an evacuation plan and list of essential items, elevating coastal homes above 10 feet to avoid most tsunami waves, taking precautions to prevent flooding, using local media for updates, and following instructions from local authorities. It advises that if a warning is issued, families in tsunami-prone areas should evacuate to higher ground and stay away from rivers and streams, while those on beaches should move to high ground if they feel the earth shaking.
The Science Applications for Risk Reduction Tsunami Scenario. Perspectives on what can be done to become tsuanmi disaster resilient. Presentation courtesy of Dr Walter Hays, Global Alliance for Disaster Reduction
The document discusses tsunamis, their causes, effects, and history. Tsunamis are caused by underwater earthquakes, volcanic eruptions, landslides, or meteor impacts displacing large volumes of water. They have struck coastlines throughout history, including the 2004 Indian Ocean tsunami that killed over 118,000 people across several countries. Early warning systems and evacuation to higher ground can help reduce loss of life from future tsunamis.
An undersea earthquake near Indonesia on December 26, 2004 triggered a devastating tsunami that caused over 131,000 deaths in Indonesia due to its proximity to the epicenter. The shape of the beach affected the size of incoming waves, with shallow waters allowing waves to grow larger before reaching shore. While scientists detected unusual wave activity, they did not predict the scale of destruction and most people received no warning due to the unexpected size of the earthquake. Future precautions discussed include tsunami walls, mangrove trees, sirens, and warning signs.
Tsunamis are caused by large displacements of water, usually in oceans, that can be triggered by earthquakes, volcanic eruptions, landslides or meteorite impacts. While tsunamis have extremely long wavelengths and periods in deep ocean waters, they can travel very fast at over 600 mph. When they reach shallow coastal waters, their energy causes the sea level to rise dramatically and flood inland areas. Proper planning, awareness of warning signs and evacuation routes can help minimize damage and save lives during a tsunami.
TSunami - A natural Disaster which is like a Giant devil galloping the whole world. A Tsunami is a series of ocean waves that are usually caused by seismic events.
The word Tsunami is a Japenese word and is pronounced as ‘soo-nah-mee.’
It means ‘harbour wave’ with ‘tsu’ meaning harbour and ‘nami’ meaning wave A Tsunami is a series of ocean waves that are usually caused by seismic events.
A tsunami is a series of waves generated by large displacements of water, typically caused by earthquakes, volcanic eruptions, landslides, or meteorite impacts under water or along coastlines. Common triggers include large earthquakes, volcanic eruptions, and landslides. When a major earthquake or landslide occurs near or undersea, it can displace enough water to cause a destructive tsunami. Coastal areas are most at risk from tsunamis, as the waves travel inland rapidly.
Tsunami is a Japanese word meaning harbor wave. Tsunamis are series of large waves generated by earthquakes, landslides, volcanic eruptions, or other disturbances that displace large volumes of water. The first recorded tsunami was in 1480 BC in the Mediterranean. Tsunamis cause devastating damage when they reach coastal areas due to their ability to flood large areas inland with fast-moving water. Proper warning systems and evacuation of coastal areas can help reduce loss of life from tsunamis.
The document provides safety tips for tsunamis, including making an evacuation plan and list of essential items, elevating coastal homes above 10 feet to avoid most tsunami waves, taking precautions to prevent flooding, using local media for updates, and following instructions from local authorities. It advises that if a warning is issued, families in tsunami-prone areas should evacuate to higher ground and stay away from rivers and streams, while those on beaches should move to high ground if they feel the earth shaking.
The Science Applications for Risk Reduction Tsunami Scenario. Perspectives on what can be done to become tsuanmi disaster resilient. Presentation courtesy of Dr Walter Hays, Global Alliance for Disaster Reduction
The document discusses tsunamis, their causes, effects, and history. Tsunamis are caused by underwater earthquakes, volcanic eruptions, landslides, or meteor impacts displacing large volumes of water. They have struck coastlines throughout history, including the 2004 Indian Ocean tsunami that killed over 118,000 people across several countries. Early warning systems and evacuation to higher ground can help reduce loss of life from future tsunamis.
An undersea earthquake near Indonesia on December 26, 2004 triggered a devastating tsunami that caused over 131,000 deaths in Indonesia due to its proximity to the epicenter. The shape of the beach affected the size of incoming waves, with shallow waters allowing waves to grow larger before reaching shore. While scientists detected unusual wave activity, they did not predict the scale of destruction and most people received no warning due to the unexpected size of the earthquake. Future precautions discussed include tsunami walls, mangrove trees, sirens, and warning signs.
Tsunamis are caused by large displacements of water, usually in oceans, that can be triggered by earthquakes, volcanic eruptions, landslides or meteorite impacts. While tsunamis have extremely long wavelengths and periods in deep ocean waters, they can travel very fast at over 600 mph. When they reach shallow coastal waters, their energy causes the sea level to rise dramatically and flood inland areas. Proper planning, awareness of warning signs and evacuation routes can help minimize damage and save lives during a tsunami.
TSunami - A natural Disaster which is like a Giant devil galloping the whole world. A Tsunami is a series of ocean waves that are usually caused by seismic events.
The word Tsunami is a Japenese word and is pronounced as ‘soo-nah-mee.’
It means ‘harbour wave’ with ‘tsu’ meaning harbour and ‘nami’ meaning wave A Tsunami is a series of ocean waves that are usually caused by seismic events.
This document provides information about tsunamis, including what causes them, how to recognize warning signs, and safety steps to take before, during, and after a tsunami occurs. It advises people living near coastal areas to be aware of evacuation routes and plans, know their street's elevation and distance from the coast, and prepare families on how to turn off utilities and contact emergency services. The goal is to help reduce loss of life and damage from potential future tsunamis.
Tsunamis are large ocean waves caused by underwater earthquakes, landslides, volcanic eruptions, or meteorites hitting the ocean. They can travel at speeds over 500 miles per hour and reach heights over 100 feet when crashing onto land. Major tsunamis throughout history have caused tremendous loss of life, such as the 2004 Indian Ocean tsunami that killed over 230,000 people in Indonesia. It is important that those living in coastal areas learn tsunami safety measures like evacuating to higher ground if warning signs of an impending tsunami are present.
1) Tsunamis are very large sea waves caused by intense earthquakes under the sea.
2) While tsunamis travel through the open ocean they are barely noticeable, but can grow to heights of 30 meters when they reach shorelines.
3) Tsunamis have the potential to completely submerge small islands and coastal regions, such as occurred at Indira Point on the Andaman and Nicobar islands.
The document discusses various types of tsunamis including those caused by landslides, meteorological conditions, and human activities. It provides examples of destructive meteotsunamis and discusses attempts to artificially trigger tsunamis through explosions. The characteristics of tsunamis are explained, noting that while waves have short wavelengths in deep ocean, they have much longer wavelengths and travel very quickly. The document also discusses drawback effects, forecasting tsunami probability, anatomy of tsunamis, facts about tsunamis, and preparation and safety during and after tsunamis.
The document summarizes key information from a science lesson about tsunamis, including:
- Tsunamis are caused by large underwater disturbances like earthquakes, volcanic eruptions, and landslides that displace large volumes of water.
- The 2011 Tohoku earthquake in Japan caused a devastating tsunami after the earthquake displaced a large volume of water at the subduction zone where the Pacific plate meets the North American plate.
- Warning signs of tsunamis include earthquakes in coastal areas, sudden rising or receding of bay waters, and alerts from warning systems. Early warnings can help coastal communities evacuate to higher ground.
Tsunamis are caused by large displacements of water, often due to underwater earthquakes, volcanic eruptions, landslides or explosions. While tsunamis have small amplitudes offshore, their wavelengths are very long. As they approach shore and water depths decrease, their speeds slow down while amplitudes grow tremendously, sometimes taking the form of a step-like wave. Drawbacks occur when the first part of a tsunami to reach land is a trough rather than a crest, causing a dramatic water recession that can expose normally submerged areas. Brief drawbacks can serve as warnings to immediately evacuate. While tsunamis cannot be precisely predicted, automated monitoring systems provide warnings after earthquakes to save lives.
The document provides information about tsunamis, including what they are, how they are caused, common misconceptions, and details about some significant historical tsunamis. It also discusses recommendations for preparing for, responding to, and recovering from tsunamis based on guidance from organizations like the American Red Cross.
This document provides information about tsunamis and the work of the Pacific Tsunami Warning Center (PTWC). The PTWC monitors for earthquakes, landslides, and volcanic eruptions that could trigger tsunamis in the Pacific Ocean and issues warnings. The document outlines the four main steps of the PTWC's operations: 1) seismic analysis to determine earthquake details, 2) message dissemination through various channels, 3) tsunami forecasting using modeling, and 4) sea level monitoring with sensors. The goal is to detect potential tsunamis as quickly as possible and provide warnings to save lives.
Tsunamis are caused by displacement of large volumes of water, usually due to earthquakes, landslides, volcanic eruptions or other seismic events. Tsunamis have long wavelengths and can travel at high speeds across oceans before slowing down and growing taller near coastlines, sometimes resembling a rapidly rising tide. The 2004 Indian Ocean tsunami killed over 230,000 people across 14 countries due to the immense destructive power of tsunamis, which can devastate entire coastal areas through high-speed wall of water and dragging debris back out to sea. Modern technology has enabled the development of tsunami-proof buildings that are elevated on deep foundations and designed for easy water flow to withstand such events.
1. Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. While tsunami waves do not increase much in height in the deep ocean, they build up dramatically as they reach shallow coastal waters.
2. The deadliest tsunami in recent history was in 2004, when an earthquake in the Indian Ocean triggered a tsunami that killed over 230,000 people across 14 countries, including over 10,000 in India.
3. It is important to evacuate coastal areas immediately when tsunami warnings are issued, as the first wave may not be the largest and tsunamis consist of multiple waves that can last for hours. Staying alert and having an evacuation plan can
Tsunamis are large ocean waves caused by underwater earthquakes, landslides, volcanic eruptions or meteor impacts. While hardly noticeable at sea, tsunami waves grow enormously in size as they reach shorelines, causing devastating damage. Tsunami inundation refers to how far inland tsunami waves penetrate, which varies in each location and is determined by bathymetry, topography, and other geological factors. Common signs of approaching tsunamis include earthquakes, receding or suddenly surging water, and unnatural ocean sounds. Immediate evacuation to high ground can save lives when these signs are noticed.
A tsunami is a series of waves generated primarily by earthquakes and underwater landslides. Tsunamis have small amplitudes in deep water but increase dramatically in height as they reach shorelines, behaving like an incoming tide that floods far inland. They are very dangerous and can destroy coastal infrastructure, contaminate drinking water, and cause many casualties. Detection systems and public education on evacuation procedures can help reduce loss of life from tsunamis. Tsunamis are characterized by their long wavelengths, which can exceed 100km, and their ability to travel at high speeds across oceans before growing in destructive power near coastlines.
Presentation highlighting tsunami lessons from key scenes in "The Impossible" to the Get Ready Ewa Beach Emergency Preparedness Fair on September 5, 2015
Tsunamis are caused by the displacement of large volumes of water, generally in oceans or large lakes. Earthquakes, volcanic eruptions, and underwater explosions can displace water and generate tsunamis in the form of a series of waves. The document discusses plate tectonic theory, noting that Earth's outer shell is made up of rigid plates that move relative to each other, causing deformation at their boundaries through earthquakes, volcanism, and other phenomena. It provides details on modeling of seismograms from a large earthquake, finding slip occurred over a 400km long fault area, with maximum slip of around 20m. Entire 1200km of the aftershock zone is estimated to have slipped based on ultra-
1) Tsunamis are a series of massive ocean waves caused by earthquakes, volcanic eruptions, landslides, or meteorite impacts underneath or near the ocean.
2) Tsunamis have extremely long wavelengths and periods, allowing them to travel hundreds of miles per hour across the ocean with barely a visible wave, but grow drastically in size and power as they reach shore.
3) Warning signs of an impending tsunami include strong earthquakes near coastal areas, an unusual rapid retreat or advancement of ocean water from the shoreline, and a series of surging water waves rather than a single wave.
NATURAL DISASTER TSUNAMI AND ITS RISK REDUCTION MEASURESABUL HASAN
1. The document discusses natural hazards, specifically focusing on tsunamis - their causes, characteristics, warning systems, and potential risk reduction measures.
2. Tsunamis are caused by earthquakes, volcanic eruptions, and landslides under the sea. They differ from ordinary waves by traveling much faster in deep waters.
3. International and regional warning systems use seismic data to detect tsunamis and issue warnings to communities, with regional systems providing alerts within 15 minutes.
This document discusses tsunamis, including what causes them, how they travel, and their impacts. Some key points:
- Tsunamis are seismic sea waves caused by earthquakes, volcanic eruptions, landslides, or meteor impacts that displace large volumes of water.
- They can travel at high speeds of 400-500 mph in deep ocean water but slow down and grow taller in shallower coastal areas, causing flooding and damage on land.
- Their long wavelengths mean they lose little energy even over long distances, allowing tsunamis generated in one area to impact landmasses many hours or days away.
- Tsunami warning centers monitor seismic activity and tide gaug
Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. They can take less than an hour to reach nearby coasts within 100km, 1-3 hours to reach coasts 100-1000km away, or more than 3 hours to cross oceans and strike coasts over 1000km from the quake epicenter. Signs of an approaching tsunami include strong ground shaking, unusual sea level changes, an abnormally large first wave that may not be the biggest, and a loud ocean roar. Tsunamis consist of a series of waves that can last up to 30 minutes each and pose a danger that may persist for hours or even days. People in coastal areas should immediately evac
The document discusses a classroom lesson on tsunamis. It covers defining tsunamis and distinguishing them from tidal waves and storm surges. It discusses natural warning signs of an impending tsunami and creating a plan for before, during, and after a tsunami. The lesson includes activities to recognize tsunami signs and develop evacuation plans. It stresses the importance of evacuating inland or to higher ground if an earthquake is felt near the coast.
Earthquakes, tsunamis, volcanic eruptions, cyclones, and floods are some of the major natural hazards discussed in the document. For earthquakes, the document describes what they are, how they are measured, and their typical causes from tectonic plate movement. For tsunamis, it notes they are large sea waves caused by seismic events. Key steps outlined for preparing for tsunamis include learning about risk, developing evacuation plans, and moving quickly inland to higher ground if one occurs. Volcanic eruptions and cyclones are also briefly mentioned. Floods are described as overflowing of water beyond normal boundaries, with heavy rain, dam breaches, or tidal waves listed as common
An earthquake at the edge of a tectonic plate can displace large amounts of water and generate a tsunami. When the ocean floor suddenly rises or drops, it throws the water above it into large waves that travel towards the shore. Most tsunamis occur in the Pacific Ocean, called the "Ring of Fire", where there is frequent seismic and volcanic activity. The Japanese word "tsunami" means "harbor wave" and describes the huge waves that can overwhelm coastal areas, as seen in the devastating 2004 Indian Ocean tsunami that killed over 280,000 people.
This document provides information about tsunamis, including what causes them, how to recognize warning signs, and safety steps to take before, during, and after a tsunami occurs. It advises people living near coastal areas to be aware of evacuation routes and plans, know their street's elevation and distance from the coast, and prepare families on how to turn off utilities and contact emergency services. The goal is to help reduce loss of life and damage from potential future tsunamis.
Tsunamis are large ocean waves caused by underwater earthquakes, landslides, volcanic eruptions, or meteorites hitting the ocean. They can travel at speeds over 500 miles per hour and reach heights over 100 feet when crashing onto land. Major tsunamis throughout history have caused tremendous loss of life, such as the 2004 Indian Ocean tsunami that killed over 230,000 people in Indonesia. It is important that those living in coastal areas learn tsunami safety measures like evacuating to higher ground if warning signs of an impending tsunami are present.
1) Tsunamis are very large sea waves caused by intense earthquakes under the sea.
2) While tsunamis travel through the open ocean they are barely noticeable, but can grow to heights of 30 meters when they reach shorelines.
3) Tsunamis have the potential to completely submerge small islands and coastal regions, such as occurred at Indira Point on the Andaman and Nicobar islands.
The document discusses various types of tsunamis including those caused by landslides, meteorological conditions, and human activities. It provides examples of destructive meteotsunamis and discusses attempts to artificially trigger tsunamis through explosions. The characteristics of tsunamis are explained, noting that while waves have short wavelengths in deep ocean, they have much longer wavelengths and travel very quickly. The document also discusses drawback effects, forecasting tsunami probability, anatomy of tsunamis, facts about tsunamis, and preparation and safety during and after tsunamis.
The document summarizes key information from a science lesson about tsunamis, including:
- Tsunamis are caused by large underwater disturbances like earthquakes, volcanic eruptions, and landslides that displace large volumes of water.
- The 2011 Tohoku earthquake in Japan caused a devastating tsunami after the earthquake displaced a large volume of water at the subduction zone where the Pacific plate meets the North American plate.
- Warning signs of tsunamis include earthquakes in coastal areas, sudden rising or receding of bay waters, and alerts from warning systems. Early warnings can help coastal communities evacuate to higher ground.
Tsunamis are caused by large displacements of water, often due to underwater earthquakes, volcanic eruptions, landslides or explosions. While tsunamis have small amplitudes offshore, their wavelengths are very long. As they approach shore and water depths decrease, their speeds slow down while amplitudes grow tremendously, sometimes taking the form of a step-like wave. Drawbacks occur when the first part of a tsunami to reach land is a trough rather than a crest, causing a dramatic water recession that can expose normally submerged areas. Brief drawbacks can serve as warnings to immediately evacuate. While tsunamis cannot be precisely predicted, automated monitoring systems provide warnings after earthquakes to save lives.
The document provides information about tsunamis, including what they are, how they are caused, common misconceptions, and details about some significant historical tsunamis. It also discusses recommendations for preparing for, responding to, and recovering from tsunamis based on guidance from organizations like the American Red Cross.
This document provides information about tsunamis and the work of the Pacific Tsunami Warning Center (PTWC). The PTWC monitors for earthquakes, landslides, and volcanic eruptions that could trigger tsunamis in the Pacific Ocean and issues warnings. The document outlines the four main steps of the PTWC's operations: 1) seismic analysis to determine earthquake details, 2) message dissemination through various channels, 3) tsunami forecasting using modeling, and 4) sea level monitoring with sensors. The goal is to detect potential tsunamis as quickly as possible and provide warnings to save lives.
Tsunamis are caused by displacement of large volumes of water, usually due to earthquakes, landslides, volcanic eruptions or other seismic events. Tsunamis have long wavelengths and can travel at high speeds across oceans before slowing down and growing taller near coastlines, sometimes resembling a rapidly rising tide. The 2004 Indian Ocean tsunami killed over 230,000 people across 14 countries due to the immense destructive power of tsunamis, which can devastate entire coastal areas through high-speed wall of water and dragging debris back out to sea. Modern technology has enabled the development of tsunami-proof buildings that are elevated on deep foundations and designed for easy water flow to withstand such events.
1. Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. While tsunami waves do not increase much in height in the deep ocean, they build up dramatically as they reach shallow coastal waters.
2. The deadliest tsunami in recent history was in 2004, when an earthquake in the Indian Ocean triggered a tsunami that killed over 230,000 people across 14 countries, including over 10,000 in India.
3. It is important to evacuate coastal areas immediately when tsunami warnings are issued, as the first wave may not be the largest and tsunamis consist of multiple waves that can last for hours. Staying alert and having an evacuation plan can
Tsunamis are large ocean waves caused by underwater earthquakes, landslides, volcanic eruptions or meteor impacts. While hardly noticeable at sea, tsunami waves grow enormously in size as they reach shorelines, causing devastating damage. Tsunami inundation refers to how far inland tsunami waves penetrate, which varies in each location and is determined by bathymetry, topography, and other geological factors. Common signs of approaching tsunamis include earthquakes, receding or suddenly surging water, and unnatural ocean sounds. Immediate evacuation to high ground can save lives when these signs are noticed.
A tsunami is a series of waves generated primarily by earthquakes and underwater landslides. Tsunamis have small amplitudes in deep water but increase dramatically in height as they reach shorelines, behaving like an incoming tide that floods far inland. They are very dangerous and can destroy coastal infrastructure, contaminate drinking water, and cause many casualties. Detection systems and public education on evacuation procedures can help reduce loss of life from tsunamis. Tsunamis are characterized by their long wavelengths, which can exceed 100km, and their ability to travel at high speeds across oceans before growing in destructive power near coastlines.
Presentation highlighting tsunami lessons from key scenes in "The Impossible" to the Get Ready Ewa Beach Emergency Preparedness Fair on September 5, 2015
Tsunamis are caused by the displacement of large volumes of water, generally in oceans or large lakes. Earthquakes, volcanic eruptions, and underwater explosions can displace water and generate tsunamis in the form of a series of waves. The document discusses plate tectonic theory, noting that Earth's outer shell is made up of rigid plates that move relative to each other, causing deformation at their boundaries through earthquakes, volcanism, and other phenomena. It provides details on modeling of seismograms from a large earthquake, finding slip occurred over a 400km long fault area, with maximum slip of around 20m. Entire 1200km of the aftershock zone is estimated to have slipped based on ultra-
1) Tsunamis are a series of massive ocean waves caused by earthquakes, volcanic eruptions, landslides, or meteorite impacts underneath or near the ocean.
2) Tsunamis have extremely long wavelengths and periods, allowing them to travel hundreds of miles per hour across the ocean with barely a visible wave, but grow drastically in size and power as they reach shore.
3) Warning signs of an impending tsunami include strong earthquakes near coastal areas, an unusual rapid retreat or advancement of ocean water from the shoreline, and a series of surging water waves rather than a single wave.
NATURAL DISASTER TSUNAMI AND ITS RISK REDUCTION MEASURESABUL HASAN
1. The document discusses natural hazards, specifically focusing on tsunamis - their causes, characteristics, warning systems, and potential risk reduction measures.
2. Tsunamis are caused by earthquakes, volcanic eruptions, and landslides under the sea. They differ from ordinary waves by traveling much faster in deep waters.
3. International and regional warning systems use seismic data to detect tsunamis and issue warnings to communities, with regional systems providing alerts within 15 minutes.
This document discusses tsunamis, including what causes them, how they travel, and their impacts. Some key points:
- Tsunamis are seismic sea waves caused by earthquakes, volcanic eruptions, landslides, or meteor impacts that displace large volumes of water.
- They can travel at high speeds of 400-500 mph in deep ocean water but slow down and grow taller in shallower coastal areas, causing flooding and damage on land.
- Their long wavelengths mean they lose little energy even over long distances, allowing tsunamis generated in one area to impact landmasses many hours or days away.
- Tsunami warning centers monitor seismic activity and tide gaug
Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. They can take less than an hour to reach nearby coasts within 100km, 1-3 hours to reach coasts 100-1000km away, or more than 3 hours to cross oceans and strike coasts over 1000km from the quake epicenter. Signs of an approaching tsunami include strong ground shaking, unusual sea level changes, an abnormally large first wave that may not be the biggest, and a loud ocean roar. Tsunamis consist of a series of waves that can last up to 30 minutes each and pose a danger that may persist for hours or even days. People in coastal areas should immediately evac
The document discusses a classroom lesson on tsunamis. It covers defining tsunamis and distinguishing them from tidal waves and storm surges. It discusses natural warning signs of an impending tsunami and creating a plan for before, during, and after a tsunami. The lesson includes activities to recognize tsunami signs and develop evacuation plans. It stresses the importance of evacuating inland or to higher ground if an earthquake is felt near the coast.
Earthquakes, tsunamis, volcanic eruptions, cyclones, and floods are some of the major natural hazards discussed in the document. For earthquakes, the document describes what they are, how they are measured, and their typical causes from tectonic plate movement. For tsunamis, it notes they are large sea waves caused by seismic events. Key steps outlined for preparing for tsunamis include learning about risk, developing evacuation plans, and moving quickly inland to higher ground if one occurs. Volcanic eruptions and cyclones are also briefly mentioned. Floods are described as overflowing of water beyond normal boundaries, with heavy rain, dam breaches, or tidal waves listed as common
An earthquake at the edge of a tectonic plate can displace large amounts of water and generate a tsunami. When the ocean floor suddenly rises or drops, it throws the water above it into large waves that travel towards the shore. Most tsunamis occur in the Pacific Ocean, called the "Ring of Fire", where there is frequent seismic and volcanic activity. The Japanese word "tsunami" means "harbor wave" and describes the huge waves that can overwhelm coastal areas, as seen in the devastating 2004 Indian Ocean tsunami that killed over 280,000 people.
The document provides information about disaster management and tsunamis. It defines different types of disasters and outlines the multidisciplinary and multi-sectoral nature of disaster management. Disaster management involves forecasting, warning, evacuation, search and rescue, relief, and reconstruction during pre-disaster, during disaster, and post-disaster periods. The document also describes what a tsunami is, how earthquakes can cause tsunamis, tsunami behavior as it approaches land including shoaling effect, and guidelines for preparing for, responding to, and recovering from tsunamis.
This document provides information about different natural disasters including earthquakes, landslides, tsunamis, and mine disasters. It defines each disaster, describes how they occur, how they are measured or classified, safety precautions to take during each one, and methods to prevent or mitigate future risks. Key details covered include how seismic waves cause earthquakes, common causes and types of landslides, how tsunamis are generated by earthquakes and volcanic eruptions under water, and important accident causes and prevention recommendations for mine disasters.
This document discusses tsunamis, including their causes, characteristics, and safety precautions. Tsunamis are caused primarily by earthquakes, volcanic eruptions, landslides, or meteor impacts under water. They can travel at high speeds and have successive waves that increase in height. Regions at greatest risk include areas along the Pacific Ocean's "Ring of Fire." To stay safe during a tsunami, people should move to higher ground, listen to emergency information, and never go to the shore to watch a tsunami.
1) Tsunamis are large ocean waves caused by sudden displacement of water, often due to earthquakes, landslides or volcanic eruptions.
2) Upon reaching shore, tsunami waves can break and reach heights far exceeding normal sea levels, potentially causing coastal inundation of tens of meters.
3) To escape a tsunami, take earthquakes occurring near shore as an alert to immediately evacuate to high ground, bringing a survival kit and staying away from evacuation routes exposed to tsunami waves or secondary hazards.
The document discusses disasters caused by natural hazards such as earthquakes and tsunamis. It provides details about the 2011 earthquake and tsunami in Japan, including that an earthquake of magnitude 9 struck off the coast, generating a devastating tsunami. This caused widespread damage and led to a nuclear emergency at the Fukushima power plant. The document also outlines different types of natural disasters and provides information on tsunami formation, preparedness, and response.
This document discusses tsunamis, which are giant waves caused by earthquakes or volcanic eruptions under the sea. Tsunamis can cause massive damage and loss of life by destroying homes and infrastructure. While impossible to prevent, their effects can be minimized through preparation measures like building in safe areas, establishing evacuation routes, and early warning systems. The document outlines dos and don'ts for before, during, and after a tsunami and emphasizes the importance of quickly evacuating coastal areas if a tsunami is detected or warned.
This document discusses cyclones/hurricanes/tornadoes and was created by group members Jems, Kayosh, Kristina, Krishna, and Khusika. It defines a hurricane as a tropical cyclone that forms over warm ocean waters and affects countries near the equator. Hurricanes are destructive and can cause storm surges that produce floods, sink ships at sea, induce landslides, and bring heavy rain. They form due to interactions between warm, moist air near the surface and cooler air above. The document recommends safety measures like early warning systems, strong coastal infrastructure, emergency shelters, public education, and response preparedness.
1) A disaster is a natural or man-made hazard that causes substantial damage, loss of life, or environmental change. Tsunamis are a specific type of natural disaster caused by large displacements of water.
2) Tsunami waves can reach over 100 feet tall and travel at speeds up to 500-800 km/hr. The 2004 Indian Ocean tsunami caused over 283,000 deaths across 11 countries.
3) Warning signs of an approaching tsunami include rapid sea level changes and strong earthquakes. Construction practices like building on high ground and using drainage systems can help reduce tsunami damage.
The document discusses natural disasters that occur in India such as earthquakes and tsunamis. It defines earthquakes as the shaking of the ground caused by movements in the earth's crust. Tsunamis are defined as large sea waves caused by underwater seismic events like volcanic eruptions and earthquakes. The document emphasizes the importance of taking precautions such as evacuating to higher ground when an earthquake or tsunami is detected. The Richter scale is introduced as a measurement tool for earthquake magnitudes, with higher numbers indicating larger, more damaging quakes.
- The document announces Tornado and Severe Weather Awareness Week in Wisconsin from April 19-23, 2010 and encourages schools to review safety procedures and participate in a statewide tornado drill on April 22.
- Wisconsin averages 21 tornadoes per year, with 16 confirmed in 2009 causing over $150,000 in property damage but no injuries.
- Schools are asked to support Tornado and Severe Weather Awareness Week by going over safety plans and preparing students.
Storm surges are increases in seawater levels caused by intense winds and low pressure from tropical cyclones. They are the primary cause of casualties and property damage in coastal areas during tropical cyclones. The Philippines is highly prone to storm surges due to its location and extensive coastline. Storm surge height depends on factors like storm intensity, size, forward speed, angle of approach, and local geography. Preparing for surges involves securing property, creating emergency plans and kits, and evacuating if instructed.
This document discusses tsunamis, including their generation, propagation, hazards, and mitigation strategies. It defines tsunamis and distinguishes them from tidal waves and storm surges. It then discusses tsunami hazards in the Philippines and the science behind tsunami formation, movement, and inundation. The remainder of the document outlines strategies for tsunami hazard assessment, warning systems, education, and land use planning to reduce risks from these deadly waves.
1. The document outlines the objectives, topics, learning tasks and activities for a lesson on the Philippine Public Storm Warning Signals.
2. It describes the five different storm warning signals issued by PAGASA including the expected wind speeds and impacts for each. Signal No. 1 indicates winds 30-60 kph while Signal No. 5 signals winds over 220 kph.
3. The lesson explains how the storm signals help inform the public of potential threats from tropical cyclones and allow people to take appropriate precautionary measures for their safety.
Volcanic eruptions can be dangerous, so it's important to prepare. Build an emergency supply kit with food, water, masks and radios. Make a family plan to contact each other if separated. During an eruption, follow evacuation orders and avoid rivers, valleys or low areas, which can experience mudflows. After, go to a public shelter if told to evacuate or it's unsafe to stay home, and listen for official instructions on weather radios or online.
The document discusses tsunamis, including their causes, effects, and methods for prevention and preparedness. Tsunamis are generated by earthquakes, landslides, volcanic eruptions and other events that displace large volumes of water. They can travel hundreds of miles and reach heights over 30 feet. Impacts include destruction of infrastructure, loss of life and property, and contamination of water supplies. Prevention focuses on early warning systems and evacuation plans, while adaptations aim to rebuild communities and implement child protection and new livelihood strategies.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
Exploiting Artificial Intelligence for Empowering Researchers and Faculty, In...Dr. Vinod Kumar Kanvaria
Exploiting Artificial Intelligence for Empowering Researchers and Faculty,
International FDP on Fundamentals of Research in Social Sciences
at Integral University, Lucknow, 06.06.2024
By Dr. Vinod Kumar Kanvaria
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
How to Fix the Import Error in the Odoo 17Celine George
An import error occurs when a program fails to import a module or library, disrupting its execution. In languages like Python, this issue arises when the specified module cannot be found or accessed, hindering the program's functionality. Resolving import errors is crucial for maintaining smooth software operation and uninterrupted development processes.
How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
This presentation was provided by Steph Pollock of The American Psychological Association’s Journals Program, and Damita Snow, of The American Society of Civil Engineers (ASCE), for the initial session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session One: 'Setting Expectations: a DEIA Primer,' was held June 6, 2024.
it describes the bony anatomy including the femoral head , acetabulum, labrum . also discusses the capsule , ligaments . muscle that act on the hip joint and the range of motion are outlined. factors affecting hip joint stability and weight transmission through the joint are summarized.
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
General Data Protection Regulation (GDPR) - Training Courses - EN | PECB
Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
-------------------------------------------------------------------------------
For more information about PECB:
Website: https://pecb.com/
LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
How to Manage Your Lost Opportunities in Odoo 17 CRMCeline George
Odoo 17 CRM allows us to track why we lose sales opportunities with "Lost Reasons." This helps analyze our sales process and identify areas for improvement. Here's how to configure lost reasons in Odoo 17 CRM
How to Manage Your Lost Opportunities in Odoo 17 CRM
Safety techniques on tsunami
1. • A tsunami also known as a seismic sea wave, is a series of waves in
a water body caused by the displacement of a large volume of
water, generally in an ocean or a large lake.
• Earthquakes, volcanic eruptions and other underwater explosions
(including detonations, landslides, glacier calvings, meteorite
impacts and other disturbances above or below water all have the
potential to generate a tsunami.
• Unlike normal ocean waves, which are generated by wind, or tides,
which are generated by the gravitational pull of the Moon and the
Sun, a tsunami is generated by the displacement of water.
2. What is the best source of information in a tsunami situation?
The International Tsunami Warning System monitors ocean waves after any
Pacific earthquake with a magnitude greater than 6.5. If waves are detected,
warnings are issued to local authorities who can order the evacuation of low-
lying areas if necessary. The National Oceanic and Atmospheric
Administration (NOAA)’s National Weather Service operates two tsunami
warning centers:
1. West Coast/Alaska Tsunami Warning Center (WC/ATWC),
Palmer, Alaska. Serves Alaska, Washington, Oregon, California, the U.S.
Atlantic and Gulf of Mexico coasts, Puerto Rico, the U.S. Virgin Islands and
Canada.
2. Pacific Tsunami Warning Center (PTWC), Ewa Beach, Hawaii.
Serves Hawaii and the U.S. Pacific territories, and as an international
warning center for the Pacific and Indian oceans and the Caribbean Sea.
3. Tsunami Fact vs Fiction
1. Fiction
Tsunamis are giant walls of water.
Fact
Occasionally, tsunamis can form walls of water (known as tsunami bores) but
tsunamis normally have the appearance of a fast-rising and fast-receding flood.
They can be similar to a tide cycle occurring in just 10 to 60 minutes instead of
12 hours.
2. Fiction
A tsunami is a single wave.
4. Fact
A tsunami is a series of waves. Often the initial wave is not the largest. In fact,
the largest wave may not occur for several hours. There may also be more than
one series of tsunami waves if a very large earthquake triggers local landslides
which in turn trigger additional tsunamis.
3. Fiction
Boats should move to the protection of a bay or harbor during a tsunami.
Fact
Tsunamis are often most destructive in bays and harbors, not just because of
the waves but because of the violent currents they generate in local waterways.
Tsunamis are least destructive in deep, open ocean waters.
5. 4. Fiction
A tsunami is the same thing as a tidal wave.
Facts
Tidal waves are regular ocean waves, and are caused by the tides. These
waves are caused by the interaction of the pull of the moon’s gravity on
the earth. A “tidal wave” is a term used in common folklore to mean the
same thing as a tsunami, but is not the same thing.
Be aware of the signs of a tsunami:
•A strong earthquake lasting 20 seconds or more near the
coast.
•A noticeable rapid rise or fall in coastal waters.
6. Developing and Delivering Effective Warning Messages
• The likelihood of individuals responding to tsunami warnings depends on
the quality, clarity, and accuracy of the official warning messages they
receive from the two Tsunami Warning Centers (TWCs) and/or local and
state emergency management agencies.
• An effective message contains the necessary information to motivate
individuals to take self-protective action and must reach at-risk people in
a timely fashion.
• It is critical that warning messages: are accurate and consistent; use
language that allows a person to visualize the proper response; make
clear when recommended actions should begin and finish.
• identify who needs to evacuate and who does not.
• explain how taking the protective action will reduce the pending
consequences of not taking action at all.
7. Preparing in Advance Through a Consistent Public Education Campaign
Surviving a tsunami depends on the:
• ability of an individual in the hazard zone to recognize warning signals
• make correct decisions
• act quickly.
For near-field tsunamis
waves will arrive within minutes after generation; therefore, at-risk
individuals will need to recognize natural cues such as the ground
shaking or the receding of the water line as the primary warning.
Knowledge and readiness gained through pre-event education may save
lives.
8. For far-field tsunamis
waves will arrive several hours after generation, and individuals need
to understand official warnings and follow instructions given by local
agencies.
Tips
•To escape a tsunami, go as high and as far as you can –
feet above sea level or 2 miles away.
•Every foot inland or upward may make a difference!
•if you can see the wave, you are too close for safety.
9. Detecting and Forecasting Tsunamis
The two separate Tsunami Warning Centers monitor seismic activity to
assess the potential for tsunami threats from earthquakes.
• The content of the tsunami information statement, advisory, watch,
or warning from the TWC is decided solely on seismic parameters and
the historical record, if any, of past tsunamis generated in the area of
the earthquake.
• Based on their own data analysis, the TWCs independently decide
whether to issue alerts to the emergency managers in their respective
areas of responsibility.
10. How to Prepare for a Tsunami
Protecting your family
• Talk about tsunamis with your family so that everyone knows what
to do in a tsunami situation. Discussing ahead of time helps reduce
fear, particularly for younger children.
• Check at your workplace and your children's schools and day care
centers to learn if they are in a tsunami hazard area or inundation
zone. Learn about their evacuation plans, especially the designated
spot where you will pick up your children.
• Plan evacuation routes from your home, school, workplace and
other places you could be
11. where tsunamis present a risk.
• If possible try to pick areas 100 feet above sea level or 2 miles
inland.
• If you cannot get that high or far, go as high or far as you can.
Every foot inland or upward may make a difference. You
should be able to reach the highest ground possible on foot
within 15 minutes.
• Practice your evacuation routes. Familiarity may save your life.
Be able to follow your escape route at night and during
inclement weather.
12. Protecting your home
• Avoid building or living in buildings within several hundred feet of
the coastline. These areas are more likely to experience damage
from tsunamis, strong winds, or coastal storms.
• If you do live in a coastal area, elevate your home to help reduce
damage. Most tsunami waves are less than 10 feet (3 meters).
• Take precautions to prevent flooding.
• Have an engineer check your home and advise about ways to
make it more resistant to tsunami water. There may be ways to
divert waves away from your property. Improperly built walls
could make your situation worse.
13. Know the difference!
•A Tsunami WARNING means a tsunami may
generated and could be close to your area.
•A Tsunami WATCH means a tsunami has not
verified but could exist and may be as little
• Make a list of items to bring inside in the event of a tsunami
watch or warning being issued for your area. But remember, you
may need to evacuate immediately – don’t risk your safety to
save your belongings
14. Be sure you're Red Cross Ready.
That means:
• Assembling an emergency preparedness kit.
• Creating a household evacuation plan that includes your pets.
• Staying informed about your community’s risk and response
plans.
• Educating your family on how to use the Safe and Well
website.
• Download the Emergency App for iPhone >> or for Android >>
15. During a Tsunami
If You Feel a Strong Coastal Earthquake
• Drop, cover, and hold on to protect yourself from the earthquake.
• When the shaking stops, gather members of your household and review your
evacuation plan. A tsunami may be coming within minutes.
• Use a Weather Radio or stay tuned to a Coast Guard emergency frequency station
or a local radio or television station for updated emergency information.
• Follow instructions issued by local authorities. Recommended evacuation routes
may be different from the one you planned, or you may be advised to climb higher.
16. • Take your emergency preparedness kit. Having supplies will make you more
comfortable during the evacuation.
• Get to higher ground as far inland as possible. Watching a tsunami from the
beach or cliffs could put you in grave danger. If you can see the wave, you are too
close to escape it.
• Avoid downed power lines and stay away from buildings and bridges from
which heavy objects might fall during an aftershock.
• Do not assume that after one wave the danger is over. The next wave may be
larger than the first one.
17. •Get to higher ground as far inland as possible. Watching a tsunami
from the beach or cliffs could put you in grave danger. If you can see
the wave, you are too close to escape it.
• Avoid downed power lines and stay away from buildings and
bridges from which heavy objects might fall during an aftershock.
• Stay away until local officials tell you it is safe. A tsunami is a series
of waves that may continue for hours. Do not assume that after one
wave the danger is over. The next wave may be larger than the first
one.
18. After a Tsunami
If you do nothing else:
• Let friends and family know you’re safe.
• Register yourself as safe on the Safe and Well website.
• If evacuated, return only when authorities say it is safe to do so.
• Continue listening to local news or a NOAA Weather Radio for
updated information and instructions.
• If people around you are injured, practice CHECK, CALL, CARE. Check
the scene to be sure it’s safe for you to approach, call for help, and if
you are trained, provide first aid to those in need until emergency
responders can arrive.
19. Specific Site Planning Strategies to Reduce Tsunami Risk
• Avoid Inundation Areas: Site Buildings or infrastructure away from hazard area or locate
on a high point.
• Slow Water: Forests, ditches, slopes, or berms can slow down waves and filter out debris.
The success of this method depends on correctly estimating the force of the tsunami.
• Steering: Water can be steered to strategically placed angled walls, ditches and paved
roads. Theoretically, porous dikes can reduce the impact of violent waves.
• Blocking : Walls, hardened terraces, berms and parking structures can be built to block
waves.he house and household in a wide community context such as whether it is a
majority or minority situation, the conflict situation and ownership issues.
20. REFERENCES:
1. THE AMERICAN RED CROSS
2. Designing for Tsunamis Seven Principles for Planning and Designing
for Tsunami
Hazards. NOAA, USGS, FEMA, NSF, Alaska, California, Hawaii, Oregon,
and Washington. (2001). National Tsunami Hazard Mitigation
Program (NTHMP)
3.Tsunami Awareness Kit General Tsunami Resources.(2005). Tsunami
Mitigation Strategies. Prepared by the Pacific Disaster Center.