地震
峡湾
地质学
海洋学
巡航
山崩
地震学
水深测量
气候变化
港口
事件(粒子物理)
海岸带
冰期
作者
Dan H. Shugar,Katherine R. Barnhart,Mira Berdahl,Jacqueline Caplan-Auerbach,Göran Ekström,Aram Fathian,Marten Geertsema,Stephen Hicks,Bretwood Higman,Erin K. Jensen,Ezgi Karasözen,Patrick Lynett,John Lyons,Thomas Monahan,Gerard Roe,Kristian Svennevig,L. Toney,Maximillian Van Wyk de Vries,Michael E. West
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2026-05-06
卷期号:: eaec3187-eaec3187
被引量:1
标识
DOI:10.1126/science.aec3187
摘要
. The landslide was preceded by several days of microseismicity, which increased in rate and magnitude until ~1 hour before failure. The landslide produced globally observed long-period seismic waves equivalent in size to a M5.4 earthquake. A long-period (~66 s) global seismic signal, produced by a landslide-induced seiche trapped within the fjord, persisted for up to 36 hours, the second time a days-long seiche has been thus observed. With fjord regions increasingly visited by cruise ships, and climate change making similar events more likely, this unanticipated, near-miss event highlights the growing risk from landslides and tsunamis in coastal environments.
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