Mechanism of tsunami_
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The document discusses the mechanism of tsunami warning systems in the Indian Ocean region. Data about earthquakes is sent to warning centers like PTWC and JMA, who analyze the data to determine the earthquake's size and predict when tsunami waves will arrive. They then send alerts to countries in the region, who warn local populations using methods like radio, television, SMS, loudspeakers or bells. While technology has improved warning systems, some remote areas still lack sufficient coverage, and warnings do not always reach all people at risk.
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The document discusses the tsunami early warning system in the Indian Ocean. The system works by having centers in the Pacific and Indian Oceans receive earthquake data and tidal gauge information to determine if a quake could produce a tsunami. If so, they issue watches to countries which then alert their populations through various methods like radio, SMS, or evacuation drills. However, some remote areas still lack robust warning systems.
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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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The document describes how the tsunami warning system in the Indian Ocean works. It consists of sensors to detect tsunamis, centers to analyze earthquake data (PTWC, JMA), and regional watch providers (RTWPs) that issue warnings. When an earthquake occurs, data is sent to analysis centers, which determine the tsunami risk and send warnings to affected regions via email and news. This system was developed after the devastating 2004 Indian Ocean tsunami, and aims to protect lives by alerting people of impending tsunamis.
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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.
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An earthquake of magnitude 7.8 occurred off the coast of the Kermadec Islands on July 7th. The U.S. Pacific Tsunami Warning Center and New Zealand's Civil Defense issued tsunami warnings for the Kermadec Islands, New Zealand, Tonga, and several regions of New Zealand's North Island due to the potential for destructive tsunami waves. The document emphasizes the importance of tsunami warning systems and the need to educate other countries about them.
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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.
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The document discusses the tsunami early warning system in the Indian Ocean. The system works by having centers in the Pacific and Indian Oceans receive earthquake data and tidal gauge information to determine if a quake could produce a tsunami. If so, they issue watches to countries which then alert their populations through various methods like radio, SMS, or evacuation drills. However, some remote areas still lack robust warning systems.
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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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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.
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An earthquake of magnitude 7.8 occurred off the coast of the Kermadec Islands on July 7th. The U.S. Pacific Tsunami Warning Center and New Zealand's Civil Defense issued tsunami warnings for the Kermadec Islands, New Zealand, Tonga, and several regions of New Zealand's North Island due to the potential for destructive tsunami waves. The document emphasizes the importance of tsunami warning systems and the need to educate other countries about them.
Tsunami warning system udit dixit
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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.
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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.
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This document summarizes a seminar on tsunami warning systems. It discusses how tsunamis are generated by undersea earthquakes and can cause widespread destruction. It then describes how modern tsunami warning systems use pressure sensors on the seafloor called tsunameters to detect changes in water pressure above a threshold that may indicate an incoming tsunami. If detected, data is transmitted to surface buoys and can be used to forecast tsunamis and give warnings to save lives. The system is critical infrastructure that can help mitigate loss from tsunamis.
Tsunami warning system
tsunami warning system is a system which is used to detect tsunami and issue a warning which is used to prevent loss of life and property.
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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.
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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.
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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.
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This paper describes the system components that make up the second-generation Deep-Ocean Assessment and Reporting of Tsunamis system, known as DART II1.
Tsunami data from the DART system can be combined with seismic data ingested into a forecast model to generate accurate tsunami forecasts for coastal areas2.
The motivation for developing a transportable, real-time, deep ocean tsunami measurement system was to forecast the impact of tsunamis on coastal areas in time to save lives and protect property. Over the past 20 years, PMEL has identified the requirements of the tsunami measurement system through evolution in both technology and knowledge of deep ocean tsunami dynamics. The requirement for transportability was a conservative approach to a phenomenon that had little data to guide strategies for choosing deployment sites. The requirement for real time was to provide data in time to create a forecast. The first-generation DART design featured an automatic detection and reporting algorithm triggered by a threshold wave-height value. The DART II design incorporates two-way communications that enables tsunami data transmission on demand, independent of the automatic algorithm; this capability ensures the measurement and reporting of tsunamis with amplitude below the auto-reporting threshold. For more accurate forecast modeling and subsequent, more reliable decision-making, this capability is very important because (a) a very large, destructive tsunami may, in fact, have a very small amplitude at any particular DART station position, and (b) small, deep-ocean tsunami amplitudes can reach destructive values, due to large, localized, shallow-water amplification factors. This latter concern was dramatically affirmed and demonstrated after measurement of a 2cm wave of a tsunami generated in Alaska was amplified to become a 40cm tsunami on the north shore of Oahu, Hawaii.
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The document discusses tsunami detection methods including:
1. Current methods use deep water pressure sensors anchored to the seafloor which can detect tsunami-induced pressure changes but have high costs and maintenance needs.
2. A proposed coastal alert system uses anchored buoys that detect the receding water of an approaching tsunami wave and trigger alarms to warn local communities.
3. Another proposal involves deployable underwater sensors that are dropped from buoys after seismic events to take pressure readings at multiple depths in a lower-cost and more redundant method.
Report
The 2004 Indian Ocean earthquake and tsunami killed over 230,000 people due to the lack of an early warning system. In response, countries around the Indian Ocean established a Regional Tsunami Watch Providers system to detect tsunamis and quickly notify member countries within 10 minutes. However, challenges remain in fully informing all at-risk populations and strengthening cooperation between countries. Effective tsunami warning systems require sustained funding, public education, and regional coordination.
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The document describes a tsunami warning system. It discusses how tsunamis are caused by underwater earthquakes or volcanic eruptions. It then outlines the objectives, hardware, software, and current status of a student project to build a system using pressure sensors to detect simulated tsunamis created in a hydrology lab and communicate warnings. The system aims to study how turbulence affects tsunami force and use additional sensors to monitor environmental factors when tsunamis arrive on shore.
Tsunami warning system
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The Indian Ocean tsunami warning system relies on two centers, the Pacific Tsunami Warning Center and a center in Japan, to analyze earthquake data and determine if a tsunami will occur and when it will arrive. If a tsunami is predicted, warnings are sent to countries in the Indian Ocean region through organizations like the Asian Disaster Preparedness Center to allow time for evacuation. This system was implemented after the deadly 2004 Indian Ocean tsunami to help detect future tsunamis and save lives through early warning.
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The document describes how the tsunami warning system in the Indian Ocean works. It consists of sensors to detect tsunamis, centers to analyze earthquake data (PTWC, JMA), and regional watch providers (RTWPs) that issue warnings. When an earthquake occurs, data is sent to analysis centers which determine the tsunami risk and send warnings to RTWPs. These regional groups then disseminate alerts to the public via email and news to help protect lives. The 2004 Indian Ocean tsunami that killed over 200,000 people showed the need for an improved warning system.
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The document discusses tsunami warning systems. It provides details on:
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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.
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This paper describes the system components that make up the second-generation Deep-Ocean Assessment and Reporting of Tsunamis system, known as DART II1.
Tsunami data from the DART system can be combined with seismic data ingested into a forecast model to generate accurate tsunami forecasts for coastal areas2.
The motivation for developing a transportable, real-time, deep ocean tsunami measurement system was to forecast the impact of tsunamis on coastal areas in time to save lives and protect property. Over the past 20 years, PMEL has identified the requirements of the tsunami measurement system through evolution in both technology and knowledge of deep ocean tsunami dynamics. The requirement for transportability was a conservative approach to a phenomenon that had little data to guide strategies for choosing deployment sites. The requirement for real time was to provide data in time to create a forecast. The first-generation DART design featured an automatic detection and reporting algorithm triggered by a threshold wave-height value. The DART II design incorporates two-way communications that enables tsunami data transmission on demand, independent of the automatic algorithm; this capability ensures the measurement and reporting of tsunamis with amplitude below the auto-reporting threshold. For more accurate forecast modeling and subsequent, more reliable decision-making, this capability is very important because (a) a very large, destructive tsunami may, in fact, have a very small amplitude at any particular DART station position, and (b) small, deep-ocean tsunami amplitudes can reach destructive values, due to large, localized, shallow-water amplification factors. This latter concern was dramatically affirmed and demonstrated after measurement of a 2cm wave of a tsunami generated in Alaska was amplified to become a 40cm tsunami on the north shore of Oahu, Hawaii.
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The document discusses tsunami detection methods including:
1. Current methods use deep water pressure sensors anchored to the seafloor which can detect tsunami-induced pressure changes but have high costs and maintenance needs.
2. A proposed coastal alert system uses anchored buoys that detect the receding water of an approaching tsunami wave and trigger alarms to warn local communities.
3. Another proposal involves deployable underwater sensors that are dropped from buoys after seismic events to take pressure readings at multiple depths in a lower-cost and more redundant method.
Report
The 2004 Indian Ocean earthquake and tsunami killed over 230,000 people due to the lack of an early warning system. In response, countries around the Indian Ocean established a Regional Tsunami Watch Providers system to detect tsunamis and quickly notify member countries within 10 minutes. However, challenges remain in fully informing all at-risk populations and strengthening cooperation between countries. Effective tsunami warning systems require sustained funding, public education, and regional coordination.
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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.
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1. The document discusses the process of introducing a tsunami warning system in the Indian Ocean after the 2004 tsunami killed over 230,000 people without a warning system.
2. The warning system collects earthquake data from sensors at warning centers in Hawaii and Japan which then provide alerts to countries in the Indian Ocean.
3. The Indian Ocean countries are responsible for alerting their populations after receiving watches from the two warning centers through methods like radio, TV, SMS, and speakers.
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1) After the deadly 2004 Indian Ocean tsunami, a warning system was established across the Indian Ocean region to detect potential tsunamis and share warnings.
2) When an earthquake occurs, data is sent to warning centers in Hawaii and Japan which analyze the data and issue watches to countries in the Indian Ocean.
3) National agencies are responsible for delivering warnings to their populations through various means like evacuation drills, but the author believes the system and understanding of tsunamis must continue to improve to help all people in earthquake-prone areas.
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The document describes how the Indian Ocean tsunami warning system works. After the devastating 2004 tsunami, countries around the Indian Ocean realized they needed a warning system like the one used in the Pacific. They installed sea level monitoring instruments that detect tsunamis and send data to the Pacific Tsunami Warning Center. The PTWC then issues warnings via radio, TV, SMS, email and other means. Education efforts teach people what to do upon receiving a warning to help minimize damage from future tsunamis.
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The document describes how the Indian Ocean tsunami warning system works. After the devastating 2004 tsunami, countries around the Indian Ocean realized they needed a warning system like the one used in the Pacific. They installed sea level monitoring instruments that detect tsunamis and send data to the Pacific Tsunami Warning Center. The PTWC then issues warnings via radio, TV, SMS, email and other means. Education efforts teach people what to do upon receiving a warning to help minimize damage from future tsunamis.
GradeAssignment6B
The document discusses the tsunami warning system in the Indian Ocean. It describes the old system, which lacked coordination between countries. This led to disasters like the 2004 Indian Ocean tsunami that killed over 230,000 people. Now, two main warning centers - the Pacific Tsunami Warning Center and Japan Meteorological Agency - work together to quickly analyze earthquakes and predict potential tsunamis. They use seismic and sea level monitoring instruments and communication networks to alert countries via radio, TV, internet, sirens and alarms.
GradeAssignment6B
The document discusses the tsunami warning system in the Indian Ocean. It describes the old warning system which lacked coordination between countries. It then discusses the devastating 2004 Indian Ocean tsunami that killed over 230,000 people and led to improvements like more sea level monitors and better international communication. Now two main warning centers, the Pacific Tsunami Warning Center and Japan Meteorological Agency, analyze earthquakes and predict potential tsunami impacts, alerting countries within 20 minutes through radio, TV, internet, sirens and other means.
The tsunami warning_system
The Indian tsunami warning system was created after the devastating 2004 Indian Ocean tsunami. It is coordinated by the UN's International Oceanographic Commission and involves national warning centers and monitoring networks set up by individual countries over five years. The system analyzes data from seismic and sea level sensors to detect potential tsunamis. Warning information is shared between the Pacific Tsunami Warning Center in Hawaii, the Japan Meteorological Agency, and Regional Tsunami Watch Providers in Indian Ocean countries. The goal is to provide accurate and timely warnings to better protect lives.
The tsunami warning_system
The Indian tsunami warning system was created after the devastating 2004 Indian Ocean tsunami. It is coordinated by the UN's International Oceanographic Commission and involves national warning centers and monitoring networks set up by individual countries over five years. The system analyzes data from seismic and sea level sensors to detect potential tsunamis. Warning information is shared between the Pacific Tsunami Warning Center in Hawaii, the Japan Meteorological Agency, and Regional Tsunami Watch Providers in other Indian Ocean countries. The goal is to provide accurate and timely warnings to better protect lives.
Working of tsunami warning system in Indian Ocean
The tsunami warning system in the Indian Ocean works by having the Japan Meteorological Agency send earthquake information to the Pacific Tsunami Warning Center, which then uses this data as well as tide indicators to evaluate the possibility of a tsunami and send warnings to coastal countries. However, prior to 2004 there was no formal warning system, resulting in over 230,000 victims from an Indian Ocean tsunami that year. The document suggests the system in the Indian Ocean could be improved.
Article3
1) The Indian Ocean tsunami warning system was established after the devastating 2004 tsunami to help detect future tsunamis and warn people.
2) The system works by sending seismic data from the Indian Ocean to warning centers in Hawaii and Japan to analyze if an earthquake could generate a tsunami, and then various methods are used to disseminate warnings to the public.
3) While the technology has not reached all regions yet, efforts by governments and community groups are helping to improve preparedness and save lives.
Presentation@roy
The United Nations began coordinating efforts after the 2004 tsunami to create an early warning system for the Indian Ocean. Previously there were no monitoring instruments and many countries lacked tsunami warning agencies. Experts say more cooperation is still needed, but the system is much improved, with networks of sensors, warning centers, and communication across the region to detect and warn of potential tsunamis. While the system has progressed, challenges remain in ensuring all systems function well and that communities receive warnings in time.
report3
The document discusses the establishment of a tsunami warning system in the Indian Ocean following the devastating 2004 Indian Ocean earthquake and tsunami. Key points include:
1) Several countries installed pressure gauges in the ocean to directly detect tsunami wave movement and share data with meteorological agencies.
2) Scientists study past earthquakes and tsunamis to simulate scenarios and choose the most appropriate forecast when a tsunami occurs.
3) The Japan Meteorological Agency initially provided tsunami forecasts for countries around the Indian Ocean, but responsibility has transitioned to Regional Tsunami Watch Providers consisting of local countries.
4) Challenges remain in fully informing all people of warnings and establishing comprehensive evacuation plans
Hw6
The Indian Ocean tsunami warning system involves several organizations working together to detect tsunamis and warn populations. The Pacific Tsunami Warning Centre monitors for tsunamis in the Indian Ocean. Regional watch providers and the Japan Meteorological Agency collect seismic and oceanographic data. The Asian Disaster Preparedness Centre, Regional Integrated Multi-Hazard Early Warning System, and Deep-ocean Assessment and Reporting of Tsunamis analyze this data to detect tsunamis and issue warnings. Warnings are then delivered to the public through methods like radio, television, SMS, email and bells.
The Indian tsunami warning system
The Indian tsunami warning system was created after the 2004 Indian Ocean tsunami killed over 230,000 people in India. Before 2004, India did not have tools to monitor or warn people about potential tsunamis. In the five years after 2004, India established a network of seismograph centers, national warning centers, and coastal and deep-ocean stations to detect tsunamis and warn coastal communities. The system utilizes data from the Pacific Tsunami Warning Center in Hawaii and the Japan Meteorological Agency to inform agencies that notify people in threatened areas to evacuate.
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The Japanese yen has strengthened against the US dollar to a 15-year high. This is causing problems for Japan's export-driven economy by decreasing competitiveness and GDP growth. The yen is strong because Japan runs a large trade surplus with more exports than imports, leading to net currency inflows. Additionally, foreign investors are demanding Japanese assets due to diversification and low domestic interest rates in Japan compared to other countries like the US. Unless Japan can decrease exports and increase imports to balance trade flows, the strong yen trend is expected to continue causing economic issues.
Why is the japanese yen so strong
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McDonald's entered the Chinese market in 1990 and has since focused on developing its services, products, and menus for Chinese tastes. While it faces competition from KFC in China, McDonald's strategies include keeping prices low, providing good customer service, and creating new products for Chinese customers. The key difference between McDonald's strategies in China versus East Asia is customer service - in East Asia, service is better as clerks clean tables and customers don't need to bus their own trays.
Untitled presentation(1)
McDonald's entered the Chinese market in 1990 and has since focused on developing its services, products, and menus for Chinese tastes. While it faces competition from KFC in China, McDonald's strategy includes keeping prices low, providing good customer service, and creating new products for Chinese customers. The key difference between McDonald's strategy in China versus East Asia is quality of service - in East Asia, service is better as clerks clean tables and customers don't need to bus their own trays.
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1) Communication technology like email, Skype, and internet television allow for faster and easier exchange of information both within companies and with customers.
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The document summarizes damage from a major earthquake in Chile. Over 214 people were killed and many buildings were destroyed, including an important bridge. Tsunamis caused damage in Hawaii, Tahiti, and New Zealand. Aftershocks led to additional deaths in Santiago and destruction of buildings. Chemical plant fires and tsunamis from aftershocks killed more people and left some missing in Juan Fernandez islands. The earthquake and tsunamis caused widespread damage across Chile and other countries.
Issue of tsunami_warning_system
An earthquake with a magnitude of 7.6 occurred near the Kermadec Islands of New Zealand, causing concern about a potential tsunami. While the U.S. tsunami warning system did not cover the Kermadec Islands or Tonga, New Zealand's Civil Defense agency issued tsunami warnings and advised people near beaches to move to high ground. A tsunami between 60cm to 1 meter arrived as predicted, though it did little damage due to the warning. The document stresses the importance of tsunami warning systems to prevent loss of life from these dangerous waves.
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Pacific ring of_fire
The Pacific Ring of Fire is an area in the basin of the Pacific Ocean characterized by active volcanoes and frequent earthquakes. It is caused by tectonic plate movement and friction. The Ring of Fire makes up approximately 40,000 km in length and shapes a horseshoe around the Pacific basin, containing 452 volcanoes. Due to lithospheric plates colliding and rubbing against each other in this region, 80% of the world's earthquakes and over 75% of the world's active and dormant volcanoes are found near the Ring of Fire.
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Possible health
1. The document discusses the dangerousness of nuclear power plants and nuclear bombs. Radial rays emitted from nuclear power plants can cause people within 12 miles to evacuate and people within 20 miles to close windows and stay indoors.
2. There are two types of radiation: non-ionizing and ionizing. Ionizing radiation is harmful and can cause cancer, break chemical bonds, and have other adverse health effects on people.
3. Both nuclear power plants and nuclear bombs emit ionizing radiation like x-rays and gamma rays, which are dangerous and in large amounts can cause cancer, death, and the effects of the 1945 Hiroshima nuclear bombing are discussed.
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Mechanism of tsunami_
- 1. Mechanism of Tsunami warning system s1180030 Keisuke Hashimoto
- 2. Table of contents 1. Mecanism of the Tsunami Warning System 2. About PTWC and JMA 3. Indian Ocean Agency 4. How to Convey Warning 5. Actual Condition 6.Conclusion
- 3. Mecanism of The System ・Data is send to PTWC and JMA when an earthquake ocurred in the Indian Ocean region. ・ PTWC and JMA determine the size of earthquake and predict the time when the tsunami wave will arrive. ・PTWC and JMA send alarm of tsunami to some country in the Indian Ocean region. ・Those country in the Indian Ocean region accept the alarm and warn people about tsunami.
- 4. Role of PTWC and JMA ・PTWC and JMA have a responsibility of tsunami watches. ・PTWC and JMA take some data of earthquake from DART censor and buoy. ・Determine the earthquake size and predict the time when the tsunami will arrive. ・Send alarm of tsunami to some country in Indian Ocean region.
- 5. Indian Ocean Agency ・RTWPs RTWPs undertake the same role as PTWC and JMA. There is the RTWPs in Indian Ocean countries. The agency undertake the same role as PTWC and JMA. ・ADPC ADPC is a agency to watch around some region. ADPC is regional watch providers. ・RIMES RIMES is the multi - hazard early warning system.
- 6. How to convey tsunami warning ・Airwaves radio, television, SMS, email ・Mannually bell, megaphone,loud-speaker
- 7. Actual Condition ・The technology of tsunami warning system does not reach all areas. ・Some region of in Indian Ocean country, Safety exercise is done very well. ・Warning of tsunami occasionally muddle around people.
- 8. Conclusion ・There are many agency of tsunami warning system in Indian Ocean country, those agency is very important to people in Indian Ocean country. However, those agency can't save all people in Indian Ocean country. So, those agency should do effort to save many people.