Publication Date:
2020-02-24
Description:
After an earthquake, rapid, real-time assessment of hazards such as ground shaking and
tsunami potential is important for early warning and emergency response. Tsunami potential
depends on seafloor displacement, which is related to the length, L, width, W, mean slip, D,
and depth, z, of earthquake rupture. Currently, the primary discriminant for tsunami potential
is the centroid-moment tensor magnitude, MCMT, representing the seismic potency LWD, and w
estimated through an indirect, inversion procedure. The obtained MCMT and the implied LWD w
value vary with the depth of faulting, assumed earth model and other factors, and is only
available 30 min or more after an earthquake. The use of more direct procedures for hazard
assessment, when available, could avoid these problems and aid in effective early warning.
Here we present a direct procedure for rapid assessment of earthquake tsunami potential
using two, simple measures on P-wave seismograms—the dominant period on the velocity
records, Td, and the likelihood that the high-frequency, apparent rupture-duration, T0, exceeds
50–55 s. T0 can be related to the critical parameters L and z, while Td may be related to
W, D or z. For a set of recent, large earthquakes, we show that the period-duration product
T T gives more information on tsunami impact and size than MCMT and other currently used d0w
discriminants. All discriminants have difficulty in assessing the tsunami potential for oceanic
strike-slip and backarc or upper plate, intraplate earthquake types. Our analysis and results
suggest that tsunami potential is not directly related to the potency LWD from the ‘seismic’
faulting model, as is assumed with the use of the MCMT discriminant. Instead, knowledge of w
rupture length, L, and depth, z, alone can constrain well the tsunami potential of an earthquake, with explicit determination of fault width, W, and slip, D, being of secondary importance. With available real-time seismogram data, rapid calculation of the direct, period-duration discriminant can be completed within 6–10 min after an earthquake occurs and thus can aid in effective and reliable tsunami early warning.
Description:
Published
Description:
283-291
Description:
JCR Journal
Description:
restricted
Keywords:
earthquake dynamics
;
earthquake source observation
;
04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
Repository Name:
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Type:
article
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