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ÀÌ ¸§ Geophysical1
"We've already ÀÎõ¿ë´ÞÀÌ»ç
redone the near-field modelling with a finer resolution based on the new bathymetry and the results are about the same, despite having a smaller volume of rock," explained tsunami expert Prof Stephan Grilli from the University of Rhode Island. "The shallower slide occurs almost like a ski jump, maintaining °­ºÏÆ÷ÀåÀÌ»ç
the collapse material closer to the surface and making it more tsunamigenic than a steeper failure, which would have brought the sediment down deeper, much quicker." Profs Tappin and ¶óÇÁ½Ã¸ó¿©¼ºÀÇ·ù=¶óÇÁ½Ã¸ó¿©¼ºÀÇ·ù
Grilli were speaking here in San Francisco at the American Geophysical Union's annual Fall Meeting. This is the first chance they've had to present their findings to the wider scientific community. Also speaking was Prof Hermann ±¸·ÎÆ÷ÀåÀÌ»ç
Fritz from the Georgia Institute of Technology. He reviewed the damage on nearby shores, describing from on-the-ground studies how high the tsunami waves must have been and how far inland they reached. On the islands in the immediate vicinity of Anak Krakatau, trees up to 80m above the normal sea surface were torn from their roots.
( 2019-12-16 11:55:03 Á¶È¸:692 )
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