An ensemble forecasting method for tsunami warning
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作者:
Zhao, Guangsheng
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机构:
Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
Minist Water Resources, Key Lab Hydrosphere Sci, Beijing 100084, Peoples R China
Tsinghua Univ, Dept Hydraul Engn, Beijing 100084, Peoples R ChinaTsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
Zhao, Guangsheng
[1
,2
,3
]
Niu, Xiaojing
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机构:
Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
Minist Water Resources, Key Lab Hydrosphere Sci, Beijing 100084, Peoples R China
Tsinghua Univ, Dept Hydraul Engn, Beijing 100084, Peoples R ChinaTsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
Niu, Xiaojing
[1
,2
,3
]
机构:
[1] Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] Minist Water Resources, Key Lab Hydrosphere Sci, Beijing 100084, Peoples R China
[3] Tsinghua Univ, Dept Hydraul Engn, Beijing 100084, Peoples R China
Tsunami;
Ensemble forecasting;
South China sea;
Manila subduction zone;
Scenarios sampling;
MANILA SUBDUCTION ZONE;
PREDICTION;
SLIP;
DEFORMATION;
NCEP;
D O I:
10.1007/s11069-024-07068-0
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
Tsunami warning driven by the earthquake rapid report can provide rapid prediction of tsunami threats after an earthquake occurs. However, there is significant uncertainty in the earthquake data obtained immediately after an earthquake occurs, and further information such as slip heterogeneity cannot be obtained in a timely manner. The uncertainty of earthquake rapid report consequently results in significant uncertainty in tsunami forecasting. Thus, an ensemble forecasting method for tsunamis has been proposed to quantitatively estimate uncertainty and tsunami hazard, considering the uncertainty of magnitude, epicenter, and heterogeneous slip. The deviation distribution of magnitude and epicenter in earthquake rapid report is approximately adopted based on the historical data statistics between widely used earthquake datasets. The heterogeneous slip is generated using the well-known CERS (Codes for Earthquake Rupture and ground-motion Simulation) model. The ensemble simulation can be completed in a short period of time to obtain the probability distribution of tsunami height, using a fast simulation method based on the unit source reconstruction. Taking a hypothetical Mw 9.0 earthquake tsunami event as an example, the forecasting results and efficiency of the ensemble method have been discussed. An optimized scenario sampling has been suggested by comparing with a statistically stable results obtained from refined scenarios sampling.
机构:
ASCE, ASCE World Headquarters, 1801 Alexander Bell Drive, Reston,VA, United StatesASCE, ASCE World Headquarters, 1801 Alexander Bell Drive, Reston,VA, United States
机构:
Stanford Univ, Inst Computat & Math Engn, Stanford, CA 94305 USAStanford Univ, Inst Computat & Math Engn, Stanford, CA 94305 USA
Yang, Yuyun
Dunham, Eric M.
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机构:
Stanford Univ, Inst Computat & Math Engn, Stanford, CA 94305 USA
Stanford Univ, Dept Geophys, Stanford, CA 94305 USAStanford Univ, Inst Computat & Math Engn, Stanford, CA 94305 USA
Dunham, Eric M.
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机构:
Barnier, Guillaume
Almquist, Martin
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h-index: 0
机构:
Stanford Univ, Dept Geophys, Stanford, CA 94305 USAStanford Univ, Inst Computat & Math Engn, Stanford, CA 94305 USA