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High-accuracy age estimations of tsunami deposits are very important for tsunami deposit research because the recurrence interval and frequency of tsunami deposits allow us to assess the devastating impacts of tsunamis in a populated country such as Japan.
Upcoming M9-class events should occur in regions other than the six known areas because the recurrence interval of each M9-class event should be longer than several hundred years.
In Fig. 2(c), the stress drops of the slip events become smaller just before a megathrust earthquake, because the recurrence interval of SA to heal the frictional strength (represented by the state value θ) in Eq. (4)) becomes shorter due to the higher loading rate of shear stress driven by preseismic slip.
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The recurrence interval was much shorter than pre-M9 period because of the fast loading rate.
The recurrence interval for an earthquake of that magnitude is every 50 years, and we are overdue.
We therefore suggest that silica precipitation in the accretionary wedge controls the recurrence interval of large earthquakes in subduction zones.
The former and latter sealing timescales correspond to the extensional stress period (~3 × 101 years) and the recurrence interval of megaearthquakes in the Nankai Trough (~3 × 102 years), respectively.
Other concerns of hydrometeorologists include the determination of rainfall probabilities, the space and time distribution of rainfall and evaporation, the recurrence interval of major storms, snow melt and runoff, and probable wind tides and waves in reservoirs.
The increase in the recurrence interval decreased the critical storm duration while increasing the peak flow rates.
The recurrence interval itself is important for forecast.
The recurrence interval is estimated at 400 600 years.
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