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.
A tsunami is a giant wave caused by sudden movement under the ocean. Tsunamis travel very fast, like jet planes, so there is little time to escape when they hit shorelines. They can cause widespread death, homelessness, and economic problems. The most destructive tsunami was in 2004 in the Indian Ocean, where an earthquake in Indonesia generated waves that killed thousands across 11 countries. This document provides information about tsunamis, their effects, terminology, safety, detection methods, history in the US, and recent events.
Presentation highlighting tsunami lessons from key scenes in "The Impossible" to the Get Ready Ewa Beach Emergency Preparedness Fair on September 5, 2015
The document discusses tsunami warning systems. It provides details on:
1) How tsunami warning systems detect tsunamis using networks of seismic stations, sea level monitoring stations like tide gauges and DART buoys, and issue warnings.
2) The two main types of warning systems - international systems that cover ocean basins and national systems that provide very quick, localized warnings.
3) How seismic data, tide gauge data and DART buoy data are used to detect tsunamis, characterize earthquake sources, monitor tsunami progress, and issue or cancel warnings.
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 and tsunami warning systems. It explains that tsunamis are caused by large displacements of water, often due to earthquakes, landslides, or volcanic eruptions. It then describes how tsunami warning systems work, including how the Meteorological Agency issues warnings within three minutes of an earthquake with estimates of tsunami arrival times and heights. However, it notes shortcomings in that actual tsunami heights and times may differ from forecasts. It suggests developing more accurate forecasts based on observed data while still issuing warnings that assume maximum tsunami scales.
The Indian Ocean tsunami warning system detects tsunamis and issues warnings to prevent loss of life and property. The Pacific Tsunami Warning Center and Japan Meteorological Agency are responsible for warnings in the Indian Ocean. Warnings are delivered by radio, TV, SMS, email and sirens. The 2004 Indian Ocean tsunami that killed 230,000 people exposed deficiencies in the early warning system, leading to improvements with more seismic and ocean monitoring stations across the region.
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.
A tsunami is a giant wave caused by sudden movement under the ocean. Tsunamis travel very fast, like jet planes, so there is little time to escape when they hit shorelines. They can cause widespread death, homelessness, and economic problems. The most destructive tsunami was in 2004 in the Indian Ocean, where an earthquake in Indonesia generated waves that killed thousands across 11 countries. This document provides information about tsunamis, their effects, terminology, safety, detection methods, history in the US, and recent events.
Presentation highlighting tsunami lessons from key scenes in "The Impossible" to the Get Ready Ewa Beach Emergency Preparedness Fair on September 5, 2015
The document discusses tsunami warning systems. It provides details on:
1) How tsunami warning systems detect tsunamis using networks of seismic stations, sea level monitoring stations like tide gauges and DART buoys, and issue warnings.
2) The two main types of warning systems - international systems that cover ocean basins and national systems that provide very quick, localized warnings.
3) How seismic data, tide gauge data and DART buoy data are used to detect tsunamis, characterize earthquake sources, monitor tsunami progress, and issue or cancel warnings.
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 and tsunami warning systems. It explains that tsunamis are caused by large displacements of water, often due to earthquakes, landslides, or volcanic eruptions. It then describes how tsunami warning systems work, including how the Meteorological Agency issues warnings within three minutes of an earthquake with estimates of tsunami arrival times and heights. However, it notes shortcomings in that actual tsunami heights and times may differ from forecasts. It suggests developing more accurate forecasts based on observed data while still issuing warnings that assume maximum tsunami scales.
The Indian Ocean tsunami warning system detects tsunamis and issues warnings to prevent loss of life and property. The Pacific Tsunami Warning Center and Japan Meteorological Agency are responsible for warnings in the Indian Ocean. Warnings are delivered by radio, TV, SMS, email and sirens. The 2004 Indian Ocean tsunami that killed 230,000 people exposed deficiencies in the early warning system, leading to improvements with more seismic and ocean monitoring stations across the region.
This document summarizes the findings of an impact survey conducted along the Tamil Nadu coast that was affected by the 2004 Indian Ocean tsunami. Key findings include:
- The Nagapattinam to Point Calimere sector experienced the highest loss of life and damage due to dense populations and low-lying topography. It was classified as the most vulnerable zone.
- The Ramanathapuram to Tuticorin sector had less impact as it was protected by offshore islands and coral reefs that dissipated wave energy. Most areas were classified as safe.
- The Tuticorin to Tiruchendur sector also experienced limited damage due to protection from the Tambraparni River estuary and
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.
This document summarizes a presentation about tsunami warning systems. It defines what a tsunami is, noting that it is a large wave created by undersea disturbances that can cause massive destruction. It then explains that the 2004 Indian Ocean tsunami that killed 80,000 could have been less devastating if an effective warning system had been in place. Such a system uses detectors on the seafloor to detect disturbances, sends data to buoys at the surface which transmit to satellites and then ground stations, allowing for warnings. It also briefly describes how tsunamis propagate and grow in size as they reach shallow coastal waters.
Earthquakes, landslides, volcanic eruptions and other disturbances can cause tsunamis by displacing large amounts of water. Tsunamis are a series of long sea waves that can travel across entire oceans within hours. Three-quarters of tsunamis occur in the Pacific Ocean due to high seismic activity along subduction zones that make up the Pacific Ring of Fire. When tsunamis reach land, they can devastate coastal areas by destroying homes and infrastructure and endangering human life. On average, two tsunamis occur globally each year, with about 80% originating in the Pacific Ocean.
This document discusses tsunamis and tsunami warning systems. It defines a tsunami as a series of ocean waves generated by earthquakes or other disturbances under the sea. It then provides examples of historic tsunamis in locations like Lisbon, Japan, and India. The document goes on to explain that tsunami warning systems were first attempted in Hawaii in the 1920s and have since been improved. Major warning centers include the Pacific Tsunami Warning Center and the National Tsunami Warning Center. After the devastating 2004 Indian Ocean tsunami, several regional warning systems were also established.
The document describes a tsunami warning system, explaining that tsunamis are large ocean waves usually caused by undersea earthquakes, volcanic eruptions, or landslides. The system uses seismometers to detect earthquakes, tide gauges to measure changes in sea level, and NOAA and DART stations that can detect tsunamis, allowing warnings to be issued to protect coastal areas from potential damage from an approaching tsunami.
The document discusses the Indian Ocean Tsunami Warning System. Earthquake data is collected by agencies in Japan and Hawaii and sent to the Pacific Tsunami Warning Center (PTWC). PTWC then sends tsunami vigilance information to countries around the Indian Ocean. The system was improved after the devastating 2004 Indian Ocean tsunami. It now includes Deep-ocean Assessment and Reporting of Tsunamis (DART) stations that can detect tsunamis far from shore and send data to PTWC to help with warnings. Warnings are then disseminated to the public using methods like radio, television, SMS and email.
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
Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. They have a devastating impact on both human life and the environment. India has established a tsunami early warning system called the Indian Tsunami Early Warning System to detect tsunamis and provide timely warnings. The 2004 Indian Ocean tsunami killed over 7,000 people in Tamil Nadu, India and highlighted the need for an early warning system. Now India can detect large undersea earthquakes and provide a tsunami warning within 10-20 minutes.
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.
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
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.
This document discusses rip currents and provides safety information. It begins by defining a rip current as a strong current that pulls water away from shore. Rip currents can be very dangerous due to their speed, which can exceed 5 miles per hour. The document then provides several steps to stay safe in a rip current: remain calm, call for help if needed, float or tread water to escape the current, then swim parallel to shore and diagonally to land. It also explains how to spot potential rip currents by looking for gaps in waves or debris moving seaward. Signs are important to educate people about rip current dangers and safety.
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.
The document provides information about tsunamis, including what they are, what causes them, their effects, and detection and mitigation. It begins with objectives and an overview. It then discusses how tsunamis differ from tidal waves, describing tsunamis as seismic sea waves rather than tidal phenomena. The document outlines some of the devastating effects of tsunamis and notes they can be detected but are very difficult to mitigate against once formed and traveling at high speed.
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.
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.
this is one of my projects that I had made for my class X holiday homework, I hope this can help you gain some information about tsunamis and if you also want to make a project like this, I hope I have helped you. - mansvini
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-
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 outlines the key components needed to describe a policy problem and propose a solution. It identifies the United States' vulnerability to disasters and lack of an effective nationwide emergency alert system. This results in unnecessary loss of life and property damage due to the absence of federal leadership to coordinate existing warning agencies and work with manufacturers. The document suggests a plausible solution is for the government to encourage the production of consumer electronics that can automatically receive and announce emergency alerts.
LifeRaft is a threat detection solution that monitors social media to identify potential threats to student safety. It monitors major social media channels like Facebook, Twitter, and Instagram. When it detects posts indicating threats like bullying, violence, or criminal plans related to a school, it sends automated alerts to administrators' mobile devices. LifeRaft uses big data analytics to understand social media posts in context and locate where they are posted in real time to help schools stay informed of risks to students.
This document summarizes the findings of an impact survey conducted along the Tamil Nadu coast that was affected by the 2004 Indian Ocean tsunami. Key findings include:
- The Nagapattinam to Point Calimere sector experienced the highest loss of life and damage due to dense populations and low-lying topography. It was classified as the most vulnerable zone.
- The Ramanathapuram to Tuticorin sector had less impact as it was protected by offshore islands and coral reefs that dissipated wave energy. Most areas were classified as safe.
- The Tuticorin to Tiruchendur sector also experienced limited damage due to protection from the Tambraparni River estuary and
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.
This document summarizes a presentation about tsunami warning systems. It defines what a tsunami is, noting that it is a large wave created by undersea disturbances that can cause massive destruction. It then explains that the 2004 Indian Ocean tsunami that killed 80,000 could have been less devastating if an effective warning system had been in place. Such a system uses detectors on the seafloor to detect disturbances, sends data to buoys at the surface which transmit to satellites and then ground stations, allowing for warnings. It also briefly describes how tsunamis propagate and grow in size as they reach shallow coastal waters.
Earthquakes, landslides, volcanic eruptions and other disturbances can cause tsunamis by displacing large amounts of water. Tsunamis are a series of long sea waves that can travel across entire oceans within hours. Three-quarters of tsunamis occur in the Pacific Ocean due to high seismic activity along subduction zones that make up the Pacific Ring of Fire. When tsunamis reach land, they can devastate coastal areas by destroying homes and infrastructure and endangering human life. On average, two tsunamis occur globally each year, with about 80% originating in the Pacific Ocean.
This document discusses tsunamis and tsunami warning systems. It defines a tsunami as a series of ocean waves generated by earthquakes or other disturbances under the sea. It then provides examples of historic tsunamis in locations like Lisbon, Japan, and India. The document goes on to explain that tsunami warning systems were first attempted in Hawaii in the 1920s and have since been improved. Major warning centers include the Pacific Tsunami Warning Center and the National Tsunami Warning Center. After the devastating 2004 Indian Ocean tsunami, several regional warning systems were also established.
The document describes a tsunami warning system, explaining that tsunamis are large ocean waves usually caused by undersea earthquakes, volcanic eruptions, or landslides. The system uses seismometers to detect earthquakes, tide gauges to measure changes in sea level, and NOAA and DART stations that can detect tsunamis, allowing warnings to be issued to protect coastal areas from potential damage from an approaching tsunami.
The document discusses the Indian Ocean Tsunami Warning System. Earthquake data is collected by agencies in Japan and Hawaii and sent to the Pacific Tsunami Warning Center (PTWC). PTWC then sends tsunami vigilance information to countries around the Indian Ocean. The system was improved after the devastating 2004 Indian Ocean tsunami. It now includes Deep-ocean Assessment and Reporting of Tsunamis (DART) stations that can detect tsunamis far from shore and send data to PTWC to help with warnings. Warnings are then disseminated to the public using methods like radio, television, SMS and email.
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
Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. They have a devastating impact on both human life and the environment. India has established a tsunami early warning system called the Indian Tsunami Early Warning System to detect tsunamis and provide timely warnings. The 2004 Indian Ocean tsunami killed over 7,000 people in Tamil Nadu, India and highlighted the need for an early warning system. Now India can detect large undersea earthquakes and provide a tsunami warning within 10-20 minutes.
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.
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
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.
This document discusses rip currents and provides safety information. It begins by defining a rip current as a strong current that pulls water away from shore. Rip currents can be very dangerous due to their speed, which can exceed 5 miles per hour. The document then provides several steps to stay safe in a rip current: remain calm, call for help if needed, float or tread water to escape the current, then swim parallel to shore and diagonally to land. It also explains how to spot potential rip currents by looking for gaps in waves or debris moving seaward. Signs are important to educate people about rip current dangers and safety.
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.
The document provides information about tsunamis, including what they are, what causes them, their effects, and detection and mitigation. It begins with objectives and an overview. It then discusses how tsunamis differ from tidal waves, describing tsunamis as seismic sea waves rather than tidal phenomena. The document outlines some of the devastating effects of tsunamis and notes they can be detected but are very difficult to mitigate against once formed and traveling at high speed.
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.
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.
this is one of my projects that I had made for my class X holiday homework, I hope this can help you gain some information about tsunamis and if you also want to make a project like this, I hope I have helped you. - mansvini
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-
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 outlines the key components needed to describe a policy problem and propose a solution. It identifies the United States' vulnerability to disasters and lack of an effective nationwide emergency alert system. This results in unnecessary loss of life and property damage due to the absence of federal leadership to coordinate existing warning agencies and work with manufacturers. The document suggests a plausible solution is for the government to encourage the production of consumer electronics that can automatically receive and announce emergency alerts.
LifeRaft is a threat detection solution that monitors social media to identify potential threats to student safety. It monitors major social media channels like Facebook, Twitter, and Instagram. When it detects posts indicating threats like bullying, violence, or criminal plans related to a school, it sends automated alerts to administrators' mobile devices. LifeRaft uses big data analytics to understand social media posts in context and locate where they are posted in real time to help schools stay informed of risks to students.
The document discusses the need for a strategic framework and policy for public warning against terrorism threats in the United States. It examines existing warning systems and recommends establishing a national commission to develop an operational strategy that incorporates these systems and eliminates barriers to information sharing between agencies. The strategy would aim to enable preemption, prevention and mitigation of terrorist threats through early detection, notification, and warning to the public.
Building a Threat Hunting Practice in the CloudProtectWise
Building a Threat Hunting Practice Using the Cloud
James Condon, Director of Threat Research and Analysis ProtectWise and Tom Hegel, Senior Threat Researcher ProtectWise
Topics:
Threat Hunting 101
Requirements for Effective Threat Hunting
How the Cloud Can Help
Threat Hunting Best Practices
Questions
Next Steps
The function of the Laser Warning Sensor is to detect the laser threat, determine Pulse Repletion Frequency (PRF) and generate an edge matching signal to give firing command to the decoy laser. It comprises of number of laser warning sensors and a master controller. The laser warning sensors detects the laser radiation processes, determine the PRF and edge matching signals. It comprises of opto-electronic front end, signal processing and onditioning, embedded module for PRF decoding, and edge matching signal.
The pattern of violent incidents attributed to Salafist groups in Libya from March 2012 to September 2012 indicate that security across the country, and particularly in Benghazi, had deteriorated prior to the attack on the U.S. Consulate in Benghazi.
New technology - the threat to our informationnormanlamont
The document discusses the threat posed by new telephone technology to corporate information security and compliance. It notes that telephone conversations can now occur across long distances and to many people at once, allowing wrong or misleading information to spread within and outside a company undetected. The document warns that without proper controls and monitoring of telephone usage, companies face risks to their accurate information, compliance, values, and reputation from the uncontrolled spread of communications via this new technology.
This document discusses application threat modeling (ATM) as a systematic approach to identifying security risks in software applications. It describes how ATM can be used at different stages of the software development lifecycle, from requirements to design to testing. The key steps of ATM include decomposing the application, identifying threats and vulnerabilities, analyzing attack vectors, and determining mitigation strategies. ATM helps prioritize risks and supports decision making around risk acceptance, avoidance, or mitigation.
The document discusses a presentation on threat hunting with Splunk. It provides an agenda that includes topics like threat hunting basics, data sources for threat hunting, using Sysmon endpoint data, the cyber kill chain framework, and doing an advanced threat hunting walkthrough using Splunk. It also discusses applying machine learning and data science techniques to security. The presentation aims to help attendees build their threat hunting methodology and drive maturity in their threat hunting practices.
SearchLove London | Will Critchlow, 'The Threat of Mobile' Distilled
Our focus on responsive websites and our fascination with app store rankings may be blinding us to the real threats and opportunities of the mobile revolution. In particular, as Google continues to ratchet up its mobile-first approach to design and Facebook looks more and more like a mobile channel, what should we be changing in our campaigns and strategies?
This document discusses techniques for optimizing threat modeling to require fewer resources. It proposes using templates and risk patterns to generate threats and countermeasures for common application components and use cases. This allows for more efficient "just enough" threat modeling compared to traditional manual methods. The document demonstrates how to decompose templates into reusable risk patterns and generate threat models through a rules engine. It also introduces the open source IriusRisk tool for implementing this approach.
Opportunity and Threat of External EnvironmentNoonamsom
The document discusses analyzing an organization's external environment. It defines the external environment and different types of external factors that can influence an organization. These include the general environment, industry environment, and competitor environment. The document provides details on how to analyze each of these environments, including using Porter's Five Forces model to analyze the industry environment. It also discusses using SWOT analysis to understand an organization's opportunities and threats in the external environment. The overall aim is to help organizations understand external factors they don't control but must adapt to in order to survive and grow.
This document discusses Russia's assessment of missile threats. It notes that most current missile threats are shorter-range tactical missiles spread around the world. For some countries, missiles are used to gain international recognition or dominance over neighbors rather than direct attack threats against major powers. The document concludes that at present, the risk of direct missile attack against states like NATO members is very low. It recommends addressing proliferation through preventive diplomacy, arms control, and reducing weapons systems rather than expensive missile defense or force.
This document discusses the importance of early warning systems for facilitating evacuation and site-specific preparedness during natural disasters. It provides examples of where early warning was critical, such as facilitating evacuation during hurricanes, floods, tsunamis and volcanic eruptions. Early warning involves real-time monitoring of hazards and messaging to at-risk communities when threats are present, in order to activate evacuation plans and accelerate preparedness to protect lives and property.
The ballistic missile threat is increasing both quantitatively and qualitatively and will likely continue to do so over the next decade. Missile systems are becoming more advanced with greater range, accuracy, mobility, and effectiveness against missile defenses. Several states are developing nuclear, chemical, and biological warheads for their missiles, posing military and coercive threats. Regional actors like North Korea and Iran continue developing long-range missiles threatening the US, though the maturity of this threat is uncertain. In the near term, the growing threat of short and medium-range missiles in regions where the US has forces and allies presents a clear danger.
This document outlines a presentation on threat hunting with Splunk. The presenter is Ken Westin, a security strategist at Splunk with over 20 years of experience in technology and security. The agenda includes an overview of threat hunting basics and data sources, examining the cyber kill chain through a hands-on attack scenario using Splunk, and advanced threat hunting techniques including machine learning. Log-in credentials are provided for access to hands-on demo environments related to the presentation.
The Cuban Missile Crisis erupted in October 1962 when U.S. reconnaissance flights discovered that the Soviet Union was installing nuclear-armed missiles in Cuba, just 90 miles from Florida. This posed an immediate threat to the U.S. as missiles stationed so close could strike targets across much of America without warning. In response, President Kennedy imposed a naval blockade around Cuba and demanded that the Soviets remove the missiles. The crisis intensified as Soviet ships approached the blockade but negotiations continued. Ultimately, the Soviets agreed to withdraw the missiles in exchange for assurances from the U.S. that it would not invade Cuba, helping to resolve the crisis peacefully.
Assessment of missile defence global capabilitiesRussian Embassy
The document summarizes an assessment of global ballistic missile defense (BMD) capabilities presented at a 2012 conference in Moscow. It describes BMD information systems and assets deployed by the US and its allies that monitor ballistic missile threats. Hypothetical scenarios show trajectories of missiles launched from Russia that could be intercepted by BMD systems in Poland and Romania. The conclusion is that current and planned BMD systems pose a threat to Russia's strategic nuclear forces and limit its deterrent capabilities. Cooperation is suggested to develop an effective joint European BMD system.
The UK Missile Defence Centre is seeking innovative solutions to defending against threats like ballistic missiles, cruise missiles, and hypersonic munitions through a competition with 3 challenges: developing defence without interceptor missiles, improving kill assessment for non-destructive defences, and increasing efficiency of existing defences. Proposals are due by July 3rd, 2014 and successful concepts may receive up to £500k for further development work. The goal is to explore new technical approaches for air and missile defence.
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The Indian Ocean tsunami in 2004 killed almost 230,000 people. In response, the United Nations created an early warning system across the Indian Ocean involving seismographic centers, national warning centers, and more to detect potential tsunamis. When an earthquake occurs, data is transmitted to warning centers in Hawaii and Japan which then determine if a tsunami could occur and send watch alerts to countries in the Indian Ocean. Warnings are issued through radio, TV, SMS, email, bells, megaphones and loud speakers. The system defends communities and further improvements could allow more exact predictions.
The document describes the tsunami warning system. It discusses how tsunamis are detected using seismic alerts, tide gauges, and DART buoys. The system issues alarms that are checked by experts to determine if a tsunami exists. It then provides details on NOAA and the international/regional warning systems used in various ocean basins.
This document summarizes techniques for tsunami safety and early warning systems. It discusses how tsunamis are generated by earthquakes, landslides, volcanic eruptions and impacts. It then describes the key components of tsunami warning systems, including seismic and water level monitoring networks, modeling scenario databases, vulnerability maps, and decision support software to generate advisories. The software allows acquisition, analysis and display of real-time and modeled data, and generates advisories based on preset criteria like travel times to issue watches, warnings or alerts.
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Earthquake Early Warning (EEW) provides the ability to give warnings seconds to tens of seconds prior to the arrival of strong shaking from a major earthquake allowing the initiation of protective actions. EEW is available in many earthquake-prone countries around the world including Japan, Turkey, Mexico, and the United States. Natural Resources Canada is developing a national earthquake early warning system for Canada to cover the west coast of BC, the corridor from Ottawa to Quebec City, and other areas in Canada. The system will involve the installation of 400-600 new sensor stations, fast communication links, and new data centres for the creation of alert messages. The Canadian EEW system will be closely integrated with that operated by the US Geological Survey and use the same software packages; this will ensure consistent cross border alerts, which is particularly important in SW British Columbia. Alert messages will be distributed to the Canadian public via the National Public Alerting System. In addition, customized alerts will be available for the use of critical infrastructure operators and others to allow them to implement automated protective actions for facilities and equipment. The system is currently under development and expected to be producing alerts in 2024.
Henry Seywerd, Program Manager for the Earthquake Early Warning at Natural Resources Canada, is heading a project to establish a national system for providing rapid warnings to mitigate the effects major earthquakes. He has been involved in emergency management at NRCan for over ten years including managing the refurbishment of the Canada’s seismic monitoring network, and leading its nuclear emergency response team. Prior to joining NRCan Henry has held diverse positions in industry and research including the development of equipment for medical imaging and performing fundamental research in high energy physics.
This document outlines the history of natural disasters in India and agencies responsible for monitoring hazards such as cyclones, floods, earthquakes, and tsunamis. It discusses the need for and elements of early warning systems for natural disasters. Case studies are provided on India's tsunami warning system and how early warning systems have helped in earthquake and flood events.
This document summarizes a seminar presentation on tsunami warning systems. It discusses how tsunami warning systems work using networks of sensors like seismometers, tidal gauges, and DART buoys. DART buoys in particular detect tsunamis by measuring small changes in deep ocean water levels. Data from these sensors is communicated to warning centers to analyze earthquake data and issue tsunami warnings. The document also outlines advantages like early warning but also challenges like high costs of operating these sensor networks.
This document discusses tsunami detection systems. It begins by explaining the differences between regular wind waves and tsunamis, including size and speed. It then describes current tsunami detection methods using deep-sea buoys connected to satellites and hydrophones. The document proposes new coastal and offshore tsunami alert systems that are lower cost and have fewer points of failure. The coastal system would use anchored buoys to detect the receding water that precedes a tsunami wave and trigger alarms. The offshore system would use detachable pressure sensors dropped below the surface after seismic events to detect tsunami pressure changes. Both are presented as supplements to more advanced detection networks.
This document discusses tsunami detection systems. It begins by explaining the differences between regular wind waves and tsunamis, including size and speed. It then describes current tsunami detection methods using deep-sea buoys connected to satellites and hydrophones. The document proposes new coastal and offshore tsunami alert systems that are lower cost and have fewer points of failure. The coastal system would use anchored buoys to detect the receding water that precedes a tsunami wave and trigger alarms. The offshore system would use detachable pressure sensors dropped below the surface after seismic events to detect tsunami pressure changes. Both are presented as supplements to more advanced detection networks.
This document discusses early warning systems for natural disasters. It describes how early warning systems work for earthquakes, floods, tsunamis, and cyclones. For earthquakes, sensors detect preliminary waves and use those to estimate location, magnitude, and expected shaking to warn communities. Flood systems use automated sensors to monitor water levels and send warnings. Tsunami systems use seismic and sea level sensors to detect potential tsunamis and issue warnings. Cyclone detection algorithms identify developing storms to provide more lead time for warnings and research. The purpose of all these systems is to generate and disseminate timely warnings to protect lives and property.
DSD-INT 2017 Keynote: Coastal Inundation Hazards on Fringing Coral Reefs and ...Deltares
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The document discusses how tsunami early warning systems have been developed since the devastating 2004 Indian Ocean tsunami. It describes how, prior to 2004, few monitoring instruments or warning agencies existed in the Indian Ocean. Now, two warning centers in Hawaii and Japan receive earthquake data to assess tsunami potential and alert national agencies, though technology has still not reached all areas vulnerable to tsunamis.
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2. PTWC History
▶ Established in 1949
(following 1946 tsunami)
▶ International center for
Pacific since 1968
(following 1960 tsunami)
▶ Interim center for Indian
Ocean 2005-2013
(following 2004 tsunami)
▶ Interim center for
Caribbean Sea
(since 2007)
▶ Moved from Ewa
Beach to Ford Island
(in 2015)
1946 Tsunami in Hilo1960 Tsunami in Japan2004 Tsunami in ThailandCaribbean Tsunami PotentialPTWC’s Old Location
PTWC scientist staff tripled to 12 in 2005,
allowing for 24x7 shift/standby operation.
5. Types of PTWC Messages
Domestic (U.S.)
▶ Hawaii
▶ American Samoa
▶ Guam and CNMI
▶ Puerto Rico and VI
(NTWC currently)
International
▶ Pacific Ocean
countries
▶ Caribbean Sea
countries
Tsunami Warning
Tsunami Advisory
Tsunami Watch
Tsunami Information
Statement
Tsunami Threat Message
(major threat)
Tsunami Threat Message
(coastal threat)
Tsunami Threat Message
(marine threat)
Tsunami Information
Statement (no threat)
6. Domestic Messages
Tsunami Warning Potential tsunami with significant widespread
inundation (forecast >1 m) is expected in < 3 hr.
• Actions: Evacuate low-lying coastal areas, move
ships to deep water if there is time to safely do so.
Tsunami Advisory Potential tsunami may produce strong currents or
waves dangerous to those in or near the water
(forecast 0.3-1 m).
• Actions: Close beaches, evacuate harbors, move
ships to deep water if there time to safely do so.
Tsunami Watch Issued for an event which may later impact the area
in 3-6 hr.
• Actions: Be prepared to act in case the event is
upgraded.
Tsunami Information
Statement
An earthquake has occurred with no destructive
tsunami threat (forecast <0.3 m) or is expected >6 hr.
• Actions: None
7. International Messages
Tsunami Threat
Message
(major threat)
Issued to areas having a coastal forecast > 3 m
within 3 hr from earthquake magnitude >=7.9.
• Actions: Evacuate low-lying coastal areas, move
ships to deep water if there is time to safely do so.
Tsunami Threat
Message
(coastal threat)
Issued to areas having a coastal forecast 1-3 m
within 1000 km of the earthquake magnitude 7.6-7.8.
• Actions: Evacuate low-lying coastal areas, move
ships to deep water if there is time to safely do so.
Tsunami Threat
Message
(marine threat)
Issued to areas having a coastal forecast 0.3-1 m
within 300 km of the earthquake magnitude 7.1-7.5.
• Actions: Close beaches, evacuate harbors, move
ships to deep water if there time to safely do so.
Tsunami Information
Statement
(no threat)
Issued to areas having a coastal forecast < 0.3 m
and a preliminary earthquake magnitude 6.5-7.0.
• Actions: None
8. Int’l Messages Then & Now
Before Oct 2014
▶ Text only
▶ Forecast tsunami
arrival times
▶ Places assigned
Warning or Watch
alert status
▶ Some conflict with
national alert levels
▶ General response
guidance
▶ Very conservative
(over-warning)
After Oct 2014
▶ Text, graphics, & stats
▶ Forecast tsunami times
& coastal amplitudes
▶ Only Threat Level
information given (no
alert status)
▶ Reduces conflict with
national alert levels
▶ More specific
response guidance
▶ More precise
(less over-warning)
10. Inouye Regional Center
▶ Ford Island,
Pearl Harbor
(35 acres)
▶ 2 historical
hangers
joined by a
modern
structure
▶ 315,000 ft2
space with
large atrium
▶ Exhibits
▶ 700 staff
▶ LEED certified PTWC is located on the third floor.
PTWC
11. PTWC Operations Process
TWC’s prioritize speed over accuracy to determine
preliminary earthquake parameters as rapidly as possible.
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
12. Preliminary Seismic Analysis
>600 stations
from IRIS,
USGS, IMS, etc.
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
13. Stations and Response Time
Sardina et al. 2011
from >70 min in 1992 …
… to <5 min in 2015
0
10
20
30
40
50
60
70
80
90
100
1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011
PTWCMessageDelay(min) The US tsunami warning centers’ (TWCs) have as their official primary
responsibility to warn the public about the threat of tsunamis potentially
generated worldwide. For this purpose they operate similarly to a
seismological observatory in that scientists locate seismic events and
estimate their magnitude. Unlike traditional seismic observatories,
however, their mission requires the TWCs to determine the earthquake
parameters as rapidly as technically possible. Estimation of the
earthquakes’ location and magnitude subsequently leads to both the
evaluation of their tsunami generating potential and a course of action
based on pre-established criteria, as illustrated in Table 1 for the Pacific
Basin. Relying on these criteria means that to issue a tsunami warning for
the Pacific region it suffices to determine whether or not a shallow (less
than 100 km depth) earthquake’s epicenter lies under or near the sea, and if
its magnitude crosses the warning threshold, in this case magnitude 7.6 and
above for the Pacific Basin.
The TWCs have gradually adopted an operational model that sacrifices
some accuracy of the preliminary earthquake parameters for the needed
response speed. The critical character of their mission have also justified
the TWCs sending their preliminary event parameters even ahead of the US
institution considered authoritative regarding earthquakes, in this case the
NEIC. During the last decade the US TWCs have in fact achieved
processing and warning speeds that made some official directives obsolete
sooner than expected. As influencing these operational improvements we
can mention the following factors:
• An increasing density of the available seismic networks worldwide.
Figure 1 illustrates the number and type of seismic stations available to
the TWCs from 1992 to 2011. For many years the TWCs did not
actually import all the available seismic data into their systems. In 1998,
for instance, the PTWC ingested into its systems data from about two
dozen of the 93 seismic stations available. As shown in Figs. 1 and 2,
however, since 2004 the PTWC has more than doubled the number of
seismic stations it monitors in near-real time.
• The adoption of faster magnitude estimation methods such as the
broadband P-wave moment magnitude (Mwp) after Tsuboi et al., 1995
[1], 1999 [2]. The method has a tendency to incur larger magnitude
underestimations for great earthquakes, as documented by Whitmore et
al, 2002 [3], and Lomax and Michelini , 2009 [4]. Notwithstanding, the
Mwp magnitude scale does not in fact saturate for mega earthquakes, as
shown by Hara and Nishimura, 2011 [5], and still allows the estimation
of an earthquake’s size with sufficient accuracy to determine whether or
not its magnitude crosses the tsunami warning thresholds.
• An improved IT infrastructure, from faster computers with expanding
memory and storage, to faster and more reliable internet connections.
Most traditional seismic observatories operate guided by a set of
operational considerations that place parametric accuracy and catalog
completeness, not extra speed, as their main priority. During this inherently
hasten process, how much accuracy do the TWCs actually relinquish to
gain a lot in response speed, and vice versa? Without analyzing a data set
that allows to actually quantify and measure these variables the question
remains without a valid answer.
By operating under the imperative of speeding up their seismic analyses
a great deal, the TWCs have rather inadvertently accumulated a lot of
information characterizing the quality of increasingly faster earthquake
parametrizations. These data’s rather unique characteristics stem from the
fact that while obtaining it the TWCs have systematically violated several
of the earthquake processing rules considered as standard seismological
practice. This list of “transgressions” include using Mwp, a non-standard
magnitude estimation method, as the main technique applied to estimate
the preliminary magnitudes, and sending messages containing hypocenter
determinations with more than 180 degrees of maximum azimuth gap.
These set of conditions motivated us to seize this rare opportunity to
evaluate the quality of faster than normal earthquake parametrizations,
assess their reliability, and make some recommendations regarding the
daily operations of the tsunami warning centers.
15:00
20:00
25:00
essageDelay(mm:ss)
220
2:33
13:26
6:02
5:42
1:51
235
3:02
13:40
6:59
6:44
1:59
231
1:22
15:28
7:36
7:18
2:14
301
2:39
17:54
8:24
7:54
2:21
268
5:00
22:55
10:19
9:54
3:07
203
2:24
30:53
11:56
11:44
3:49
198
6:14
32:57
13:29
12:56
3:56
118
4:48
24:18
13:02
13:21
3:39
N 84
Min 6:00
Max 38:17
Mean 14:06
Median 13:53
Std 4:30
15:00
20:00
essageDelay(mm:ss)
N
M
M
M
M
S
05:00
10:00
15:00
20:00
25:00
PTWCMessageDelay(mm:ss)
12/31/03
12/30/04
12/30/05
12/30/06
12/30/07
12/29/08
12/29/09
12/29/10
12/29/11
05/01/03
08/31/03
04/30/04
08/30/04
04/30/05
08/30/05
04/30/06
08/30/06
04/30/07
08/30/07
04/29/08
08/29/08
04/29/09
08/29/09
04/29/10
08/29/10
04/29/11
08/29/11
2003 2004 2005 2006
220
1:53
16:14
6:29
6.05
2:20
20112010200920082007
235
3:09
16:24
8:00
7:23
2:33
231
04:08
24:18
9:23
8:45
2:48
301
4:53
34:34
10:39
10:09
3:13
268
5:19
25:16
12:36
11:56
3:25
203
5:16
31:42
13:05
12:42
3:51
196
6:54
32:18
13:03
12:48
3:22
118
6:33
29:52
13:07
12:38
4:29
N 84
Min 5:57
Max 20:17
Mean 12:51
Median 12:46
Std 3:21
More Bandwidth
00:00
05:00
10:00
15:00
20:00
PTWCMessageDelay(mm:ss)
05/01
N
M
M
M
M
S
PTWCTWC
Observatory Message Delays
Introduction
by V.H.R. Sardiña, N.C. Becker,
S.D
EPARTMENT OF COM
M
ER
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
14. Stations and Response Time
Sardina et al. 2011
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
Becker et al. 2010
15. Seismic Analysis Steps 1
1. Event detection
2. Page to duty
scientists
3. Pick review
4. Locate/relocate
5. MwP review
6. Send PDL and
observatory
message
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
16. Initial Tsunami Message
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
EQ
>100km,
inland,
or
M6.5-7.0
Information
Statement
M
7.1-7.5
<300
km
away
Marine Threat
(local)
Information
Statement
M
7.6-7.8
<1000
km
away
Coastal Threat
(region)
Information
Statement
M >=
7.9
<3 hr
away
Major Threat
(basin)
Information
Statement
Y
Y
Y
Y
Y
Y
Y
N
N
N
N
N
N
Initial tsunami
messages are
based on earthquake
information and
expected tsunami travel times only.
Domestic:
Warning <3hr
Watch 3-6hr
17. 0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
Message
Example
IOC Technical Series, 105
page 18
APPENDIX II. EXAMPLES OF PTWC NEW ENHANCED PRODUCTS FOR THE PTWS
A. Tsunami Information Statement (no tsunami threat)
a. Initial Product (text only)
i. Text Product
ZCZC
WEPA42 PHEB 010008
TIBPAC
TSUNAMI INFORMATION STATEMENT NUMBER 1
NWS PACIFIC TSUNAMI WARNING CENTER EWA BEACH HI
0008 UTC WED OCT 1 2014
...TSUNAMI INFORMATION STATEMENT...
**** NOTICE **** NOTICE **** NOTICE **** NOTICE **** NOTICE *****
THIS STATEMENT IS ISSUED FOR INFORMATION ONLY IN SUPPORT OF THE
UNESCO/IOC PACIFIC TSUNAMI WARNING AND MITIGATION SYSTEM AND IS
MEANT FOR NATIONAL AUTHORITIES IN EACH COUNTRY OF THAT SYSTEM.
NATIONAL AUTHORITIES WILL DETERMINE THE APPROPRIATE LEVEL OF
ALERT FOR EACH COUNTRY AND MAY ISSUE ADDITIONAL OR MORE REFINED
INFORMATION.
**** NOTICE **** NOTICE **** NOTICE **** NOTICE **** NOTICE *****
PRELIMINARY EARTHQUAKE PARAMETERS
---------------------------------
* MAGNITUDE 6.7
* ORIGIN TIME 0000 UTC OCT 1 2014
* COORDINATES 20.0 SOUTH 173.4 WEST
* DEPTH 178 KM / 111 MILES
* LOCATION TONGA
EVALUATION
----------
* AN EARTHQUAKE WITH A PRELIMINARY MAGNITUDE OF 6.7 OCCURRED
IN THE TONGA ISLANDS AT 0000 UTC ON WEDNESDAY OCTOBER 1 2014.
* BASED ON ALL AVAILABLE DATA... THERE IS NO TSUNAMI THREAT
FROM THIS EARTHQUAKE.
RECOMMENDED ACTIONS
-------------------
* NO ACTION IS REQUIRED.
NEXT UPDATE AND ADDITIONAL INFORMATION
--------------------------------------
* THIS WILL BE THE ONLY STATEMENT ISSUED FOR THIS EVENT UNLESS
ADDITIONAL DATA ARE RECEIVED OR THE SITUATION CHANGES.
* AUTHORITATIVE INFORMATION ABOUT THE EARTHQUAKE FROM THE U.S.
GEOLOGICAL SURVEY CAN BE FOUND ON THE INTERNET AT
EARTHQUAKE.USGS.GOV/EARTHQUAKES -ALL IN LOWER CASE-.
* FURTHER INFORMATION ABOUT THIS EVENT MAY BE FOUND AT
PTWC.WEATHER.GOV AND AT WWW.TSUNAMI.GOV.
* COASTAL REGIONS OF HAWAII... AMERICAN SAMOA... GUAM... AND
▶ Header
▶ Headline
▶ Target Area
▶ Preliminary Earthquake
Parameters
▶ Evaluation
▶ Recommended Actions
▶ Potential Impacts
▶ Additional Information
• Tsunami Forecasts
• Tsunami Observations
18. Message Dissemination
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
AFTN
airports
GTS/NMC
international
NWW
USA & Canada
Web, RSS
public
HAWAS
Hawaii
NAWAS
USA & Canada
Telephone
warning points
FAX
warning points
Soc. Media
public
Email
public
PDL
USGS, public
EMWIN
warning points
SMS
RANET
Text Phone
Internet
TEX & CAP
public
19. Seismic Analysis Steps 2
1. Event detection
2. Page to duty
scientists
3. Pick review
4. Locate/relocate
5. MwP review
6. Send PDL, Obs msg
7. Revise Location
8. Mm, Mw
9. Theta
10. W-phase CMT
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea level
gauge
monitoring
20. Tsunami Forecast Analysis
Run forecast model with W-phase CMT or other
earthquake source as input. Calculate coastal
threats and prepare to issue message update.
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
GCMT W-phase
21. Subsequent tsunami
messages are based
primarily on tsunami
forecasts.
Suppl. Tsunami Messages
CM
T
>100km,
inland, or
M6.5-7.0
Information
Statement
M >=
7.1
forecast
<0.3 m
Information
Statement
forecast
0.3-1 m
Marine Threat
(local)
forecast
1-3m
Coastal Threat
(region)
forecast
>3m
Major Threat
(basin)
Y
Y
Y
Y
Y
Y
N
N
N
N
Domestic:
Advisory <3hr
Watch 3-6hr Domestic:
Warning <3hr
Watch 3-6hr
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
22. Issue Enhanced Products
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
To Public:
▶ Text bulletin
To Tsunami Warning Focal
Points:
▶ Deep-Ocean Tsunami Amplitude
Forecast Map
▶ Coastal Tsunami Amplitude
Forecast Map
▶ Coastal Tsunami Amplitude
Forecast Polygon Map
▶ Coastal Tsunami Amplitude
Forecast KMZ
▶ Table of Forecast Statistics for
Regional Polygons
Intergovernmental Oceanographic Commission
Technical Series
105
User’s Guide
for the Pacific Tsunami Warning Center
Enhanced Products for the Pacific
Tsunami Warning System
August 2014
UNESCO
http://ptws-ptwcnewproducts.info
23. Deep-Ocean Forecast
▶ Tsunami Travel
Time contours
(assumes
point source)
▶ Color range
scaled so
red / white
show maxima
▶ Shaded
textures show
bathymetry
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
24. Coastal Forecast
▶ Green’s Law used
to propagate
deep-ocean
forecast to coast
▶ Tsunami Travel Time
contours (assumes
point source)
▶ Tsunami Wave
Amplitudes at
designated coastal
forecast points
▶ Shaded textures
show energy
distribution
▶ Regional plots too:
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
25. Coastal Forecast Polygons
▶ Threat level
for
designated
forecast zones
▶ Color range
scaled to
match threat
levels
▶ Grey textures
show
bathymetry
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
26. Coastal Forecast KMZ
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
Google Earth: User can zoom into areas of
interest and click for detailed point forecast.
27. Forecast Statistics Table
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
Max, Mean, Median, Standard deviation of
coastal and deep-ocean (offshore) forecasts.
PTWC TABLE OF FORECAST STATISTICS FOR REGIONAL POLYGONS - RUN ID 20140816233614
(for internal use only - not for distribution)
Earthquake - Origin: 10/01/2014 00:00:00 UTC Coordinates: 45.2N 151.3E Depth: 028km Magnitude: 8.6
This table is issued for information only in support the UNESCO/IOC Pacific Tsunami Warning and Mitigation System and is
meant for national authorities in each country of that system. National authorities will determine the appropriate
level of alert for each country and may issue additional or more refined information.
Actual amplitudes at the coast may vary from forecast amplitudes due to uncertainties in the forecast and local
features. In particular, maximum tsunami amplitudes on atolls will likely be much smaller than the forecast indicates.
Coastal Forecast (meters) Offshore Forecast (meters) Total
Region_Name Maximum Mean Median STD Maximum Mean Median STD Points
Urup_Etorofu_Kunashiri_Shikotan_and_Habomai_Islands 20. 5.46 3.25 4.55 13. 2.55 1.84 2.49 101
Kuril_Islands 13. 3.37 2.44 2.67 5.9 1.43 1.10 1.07 95
Wake_Island 5.8 5.77 5.84 0.09 0.97 0.93 0.90 0.03 3
Society_Islands 4.4 2.24 1.89 0.88 1.8 0.57 0.48 0.33 35
Midway_Island 3.3 2.32 1.82 0.72 1.9 1.33 1.04 0.41 3
Northwestern_Hawaiian_Islands 3.1 2.07 1.98 0.58 1.4 0.90 0.99 0.41 5
East_Coast_of_Japanese_Main_Islands 3.0 1.37 1.21 0.39 3.0 0.86 0.70 0.48 407
Marshall_Islands 2.9 2.31 2.14 0.36 1.6 0.81 0.62 0.53 4
Bougainville_Papua_New_Guinea 2.9 1.49 1.09 0.82 2.0 0.74 0.60 0.43 75
Hawaii 2.8 1.27 1.21 0.40 1.4 0.45 0.42 0.20 147
Cook_Islands 2.7 1.64 1.35 0.78 0.35 0.22 0.20 0.09 3
Kosrae_State_Micronesia 2.7 2.69 2.69 0.00 0.34 0.34 0.34 0.00 1
West_Coast_of_Japanese_Main_Islands 2.7 0.56 0.20 0.70 2.1 0.34 0.12 0.42 465
Phoenix_Islands_Kiribati 2.6 2.61 2.61 0.00 0.61 0.61 0.61 0.00 1
Line_Islands_Kiribati 2.5 1.46 1.09 0.74 0.90 0.39 0.15 0.36 3
Choisel_to_Philip_Solomon_Islands 2.5 0.99 0.76 0.51 1.6 0.44 0.35 0.29 339
Sea_of_Okhotsk_Coast_of_Sakhalin_Russia 2.3 1.71 1.71 0.36 2.0 1.21 1.19 0.23 150
28. Sea Level Gauge Analysis
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
>600 stations
from GLOSS,
NOAA, etc.
Deep-Ocean Coastal
29. Sea Level Gauge Analysis
0-5 min
Preliminary
Seismic
Analysis
5-10 min
Initial
Tsunami
Message
10-20 min
Continued
Seismic
Analysis
20-30 min
Tsunami
Forecast
Analysis
30-33 min
Supplemental
Tsunami
Message
33 min - 2 hr
Sea Level
Gauge
Analysis
first arrival time
wave amplitude
wave period
can downgrade from
warning to advisory
31. Tsunami Event XML (TEX)
Problem: Legacy text bulletins are difficult and
brittle to parse.
• Solution: We have adopted an XML-based standard
called “TEX” (Tsunami Event XML).
• TEX helps integrate TWC information.
• Other products like CAP, IPAWS/WEA are easy to
generate from TEX through XSL/XSLT.
• Could be integrated with PDL and/or integrate
QuakeML into the schema
• In development since 2010
• Current version 2.0.1 (22 October 2014)
32. Tsunami Event XML (TEX)
<?xml version="1.0" encoding="UTF-8" ?>
<tsunamiEvent xmlns:geo="http://www.w3.org/2003/01/geo/wgs84_pos#">
<TWCBulletin>
<TWCEventID>803322</TWCEventID>
<WMOID source="PAAQ">WEPA40</WMOID>
<WMOCenterID>PHEB</WMOCenterID>
<WMODateTimeGroup>251907</WMODateTimeGroup>
<AWIPSID>TSUPAC</AWIPSID>
<bulletinNumber>1</bulletinNumber>
<bulletinName>Tsunami Bulletin Number 1</bulletinName>
<issuingCenter>Pacific Tsunami Warning Center/NOAA/NWS</issuingCenter>
<bulletinIssueTime>2010-10-25-T19:07:36Z</bulletinIssueTime>
<bulletinIssueTimeString>Issued at 1907Z 25 OCT 2010</bulletinIssueTimeString>
<messageUpdates></messageUpdates>
<preHeadline><![CDATA[This bulletin applies to areas within and bordering the
Pacific Ocean and adjacent seas, except Alaska, British Columbia, Washington, Oregon,
and California. ]]></preHeadline>
<bulletinAreas>
<segment id="1”>
<headline><![CDATA[A Tsunami Warning is in effect for: RUSSIA, and JAPAN. ]]></
headline>
33. Tsunami.gov
Problem: TWC websites are different and
confusing.
• Solution: Merge NOAA tsunami websites in one
place at www.tsunami.gov
• Users don’t have to know about complicated areas
of responsibility.
• Emergency mangers can log in to get our enhanced
products, and national focal points can manage
their contact information.
• Site is driven by TEX products from the TWCs.
• In development since 2011
• Contracted to ERT with planned delivery late 2015
37. RIFT Model Assumptions
RIFT = Real-time Inundation Forecast of
Tsunamis model
RIFT uses Green’s Law, which assumes:
• Acoast = Aoffshore * (Doffshore / Dcoast)1/4
• Coastline is linear and exposed to open ocean.
• Tsunami waves near coast are 1-D plane waves.
• No significant wave reflections
• No significant dissipation by turbulence
• Bathymetry varies slowly compared with tsunami
wavelength.
• Cliff boundary condition (coast is a vertical wall).
Wang et al. 2012
38. Limitations of RIFT model
Some caveats of RIFT include:
• Initial results can vary by a factor of 2 due to
uncertainties in magnitude, depth, and assumed
mechanism of earthquake. Later results contrained
by Wphase are more reliable.
• Green’s Law can overestimate coastal amplitude for
small islands (< 30 km size).
• Green’s Law can underestimate wave amplitude in
resonant harbors.
• Coastal amplitude forecast is not necessarily
indicative of inundation depth, which is a function of
local topography.
Wang et al. 2012