Tsunami warning systems (TWS) detect tsunamis and issue warnings to minimize casualties and property damage. They consist of sensor networks for detection and communication infrastructure for timely alerts. International and regional systems utilize seismic alerts to initiate warnings, confirmed by sea level data. Proposed enhancements include analyzing t-wave energy for assessing tsunami potential.
On April 1, 1946, the Aleutian Islands earthquake triggered a tsunami that caused significant devastation in Hilo, Hawaii, leading to the development of more advanced tsunami warning systems.
On May 23, 1960, the Valdivia earthquake caused a tsunami that further highlighted the need for improved tsunami warning systems, particularly in Hilo, Hawaii, which experienced severe damage.
On July 12, 1993, a devastating tsunami struck the small island of Okushiri, Hokkaido, Japan, just minutes after a major earthquake. The close proximity of the island to the epicenter left little time for warning or evacuation, resulting in 202 fatalities and hundreds of others missing or injured. Many victims were caught by the wave while seeking safety after the initial earthquake.
Following the devastating tsunami that hit India's coasts after the Sumatra earthquake in 2004, the Indian government established the Indian National Centre for Ocean Information Services (INCOIS).
The 2004 Indian Ocean Tsunami, which resulted in nearly 250,000 fatalities, prompted the establishment of the Indian Ocean Tsunami Warning System.
In June 2005, the Intergovernmental Coordination Group for the Tsunami Early Warning and Mitigation System in the North Eastern Atlantic, the Mediterranean and connected Seas (ICG/NEAMTWS) was established by UNESCO.
The first session of the ICG/NEAMTWS took place in Rome on November 21 and 22, 2005.
In 2005, Chile began implementing the Integrated Plate boundary Observatory Chile (IPOC) to monitor seismic activity.
In March 2008, representatives of Caribbean nations met in Panama City to plan a Caribbean-wide tsunami warning system, aiming for implementation by 2010.
Barbados planned to review and test its tsunami protocol in February 2010 as a regional pilot project.
Japan's tsunami warning system issued a warning within 3 minutes of the 2011 Tōhoku earthquake and tsunami, leading to the development and implementation of an improved system in 2013.
Indonesia's tsunami warning system became non-operational in 2012 due to the failure of its detection buoys, limiting predictions to seismic activity only.
On March 7, 2013, Japan unveiled an improved tsunami warning system following the 2011 disaster.
In October 2013, the Oceansat 2 system was successfully used to predict the landfall and mitigate the impact of Cyclone Phailin.
Simulations conducted in 2013 on historical data demonstrated the value of tiltmeters and broadband seismometers for monitoring tsunamis, complementing tide gauge arrays. The 2010 Maule earthquake data showed tilt-sensors detected a signal 20 minutes before the tsunami's arrival.
After tsunamis hit Indonesia in September and December 2018, including one caused by a volcano, the Indonesian government installed sea level sensors to improve tsunami prediction.
India officially the Republic of India is a South Asian...
Japan is an East Asian island country in the Pacific...
An earthquake is the shaking of the Earth's surface caused...
A tsunami is a series of powerful waves caused by...
Hawaii is a U S state located in the Pacific...
Indonesia is a Southeast Asian and Oceanian country the world's...
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