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- W2151209426 abstract "Low, neap tides occurred along the West Coast of the United States and Canada around 0500 UT January 27, 1700, a time for the last major Cascadia earthquake/tsunami based on teletsunami arrival times in Japan [Satake et al., 1996]. However, high-range perigean spring tides occurred only a week later, illustrating how accurately occurrence times must be known to constrain the region's background water levels during such events. The ranges of background water levels increase northward from 3 m at Monterey to 8.5 m at Queen Charlotte, as estimated from the amplitudes of perigean spring tides and subtidal winter fluctuations." @default.
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- W2151209426 date "1997-09-01" @default.
- W2151209426 modified "2023-10-17" @default.
- W2151209426 title "West Coast tides during Cascadia Subduction Zone tsunamis" @default.
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- W2151209426 doi "https://doi.org/10.1029/97gl02060" @default.
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