A tsunami is a series of immensely powerful ocean waves resulting from the rapid displacement of a large volume of water. These waves are most commonly generated by powerful underwater geological events, such as major seismic shifts, underwater landslides, or the collapse of volcanic structures. While traveling across the deep ocean, the energy of the wave is distributed over a wide area, allowing the wave height to remain relatively low and often making it difficult to detect. However, as the energy approaches shallower coastal waters, the wave slows down and compresses, causing a dramatic increase in height and power. The resulting inundation poses a severe physical hazard to coastal areas, necessitating sophisticated warning systems for timely public safety measures.