This smaller volume might <a href="https://kklweiwe9o.tistory.com/91" target="_blank">°ø¸ªµ¿¿ë´ÞÀÌ»ç</a><br /> have
presented something of a problem for tsunami modellers.
Their original simulations <a href="https://hkrielfde33.tistory.com/133" target="_blank">½Å³»µ¿Æ÷ÀåÀÌ»ç</a><br /> of how the
waves generated in the collapse moved across the Sunda Strait had already proved a good match for what had been
observed <a href="https://nnbjurw345.tistory.com/140" target="_blank">Á¾·Î¿ë´ÞÀÌ»ç</a><br /> at tide gauges and from what
was known of the extent of damage along nearby coasts.
Now, the models are <a href="https://www.pinterest.co.kr/hyepyo56/%EC%97%AC%EC%84%B1%EB%A0%88%ED%94%8C%
EB%A6%AC%EC%B9%B4-httpreplicamallme/" target="_blank">¿©¼º·¹Çø®Ä«</a>=¿©¼º·¹Çø®Ä«<br /> having to be re-run but
with a smaller input.
The simulations still work, however - and with good reason. Prof Tappin's team has also discovered that the failure plane on
the volcano - the angle of slope along which the rock mass slid - was shallower than earlier assumptions.
Whereas it was once thought the failure plane cut down steeply into the basin created when the old volcano on the site blew
its top in 1883, it's now obvious the collapse slope entered the water much nearer the surface. |