Lagrange Point

When Tsunami's strike, every extra minute of notice can help save lives. How can scientists better predict the height and journey of a tsunami? We look at the ways scientists can use tectonic plates or magnetic fields to improve tsunami predictions. Where an earthquake occurs can make a big difference to the size of a tsunami. The shallower an earthquake in a thinner sub-ducting plate can lead to higher tsunamis. When you move a large amount of sea-water the earths magnetic field changes, just enough to detect. Like reading the vibrations in seismic waves, earth's magnetic field changes enough for you to identify a tsunami. Using magnetic fields you can measure and asses the height of a tsunami much faster. Zhiheng Lin, Hiroaki Toh, Takuto Minami. Direct Comparison of the Tsunami‐Generated Magnetic Field With Sea Level Change for the 2009 Samoa and 2010 Chile Tsunamis. Journal of Geophysical Research: Solid Earth, 2021; 126 (11) DOI: 10.1029/2021JB022760 Kwok Fai Cheung, Thorne Lay, Lin Sun, Yoshiki Yamazak