Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
Determination of initial tsunami wave shape at sea surface. / Lavrentiev, Mikhail M.; Romanenko, Alexey A.; Kuzakov, Dmitry E. et al.
OCEANS 2017 - Aberdeen. Vol. 2017-October Institute of Electrical and Electronics Engineers Inc., 2017. p. 1-7 (OCEANS-IEEE).Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
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TY - GEN
T1 - Determination of initial tsunami wave shape at sea surface
AU - Lavrentiev, Mikhail M.
AU - Romanenko, Alexey A.
AU - Kuzakov, Dmitry E.
AU - Vazhenin, Alexander P.
PY - 2017/10/25
Y1 - 2017/10/25
N2 - Any Tsunami Early Warning System (TEWS) should provide reliable prediction of the wave parameters as early as possible. Numerical calculation of the tsunami wave propagation over the particular part of the ocean can be implemented rather efficiently using modern high-performance system. It is possible when the initial wave shape at tsunami source is given. In this paper we discuss and show the fast algorithm for reconstructing the initial sea surface displacement at tsunami source. Based on the Fourier approximation theory, the presented algorithm treats the measured wave profile as a linear combination of synthetic (calculated) waves from the so-called unit sources. Using an artificial bathymetry, we evaluate the algorithm parameters focusing on its precision and performance. Moreover, a large tsunami sources (several hundred kilometers long) are also simulated.
AB - Any Tsunami Early Warning System (TEWS) should provide reliable prediction of the wave parameters as early as possible. Numerical calculation of the tsunami wave propagation over the particular part of the ocean can be implemented rather efficiently using modern high-performance system. It is possible when the initial wave shape at tsunami source is given. In this paper we discuss and show the fast algorithm for reconstructing the initial sea surface displacement at tsunami source. Based on the Fourier approximation theory, the presented algorithm treats the measured wave profile as a linear combination of synthetic (calculated) waves from the so-called unit sources. Using an artificial bathymetry, we evaluate the algorithm parameters focusing on its precision and performance. Moreover, a large tsunami sources (several hundred kilometers long) are also simulated.
KW - Numerical Tests
KW - Orthogonal Decomposition
KW - Tsunami Initial Sea Surface Displacement
KW - SYSTEM
KW - INDONESIA
UR - http://www.scopus.com/inward/record.url?scp=85044784854&partnerID=8YFLogxK
U2 - 10.1109/OCEANSE.2017.8084933
DO - 10.1109/OCEANSE.2017.8084933
M3 - Conference contribution
AN - SCOPUS:85044784854
VL - 2017-October
T3 - OCEANS-IEEE
SP - 1
EP - 7
BT - OCEANS 2017 - Aberdeen
PB - Institute of Electrical and Electronics Engineers Inc.
T2 - OCEANS 2017 - Aberdeen
Y2 - 19 June 2017 through 22 June 2017
ER -
ID: 12670946