Tsunami Inundation Modelling in Estuaries: Sensitivity to Variation in Tide from an Emergency Management Perspective.

2016 ◽  
Vol 75 (sp1) ◽  
pp. 1262-1266
Author(s):  
Olivia A. Wilson ◽  
Hannah E. Power
2011 ◽  
Vol 9 (1) ◽  
pp. 83-98 ◽  
Author(s):  
E M Lane ◽  
P A Gillibrand ◽  
J R Arnold ◽  
R A Walters

2020 ◽  
Vol 8 ◽  
Author(s):  
Steven J. Gibbons ◽  
Stefano Lorito ◽  
Jorge Macías ◽  
Finn Løvholt ◽  
Jacopo Selva ◽  
...  

Probabilistic Tsunami Hazard Analysis (PTHA) quantifies the probability of exceeding a specified inundation intensity at a given location within a given time interval. PTHA provides scientific guidance for tsunami risk analysis and risk management, including coastal planning and early warning. Explicit computation of site-specific PTHA, with an adequate discretization of source scenarios combined with high-resolution numerical inundation modelling, has been out of reach with existing models and computing capabilities, with tens to hundreds of thousands of moderately intensive numerical simulations being required for exhaustive uncertainty quantification. In recent years, more efficient GPU-based High-Performance Computing (HPC) facilities, together with efficient GPU-optimized shallow water type models for simulating tsunami inundation, have now made local long-term hazard assessment feasible. A workflow has been developed with three main stages: 1) Site-specific source selection and discretization, 2) Efficient numerical inundation simulation for each scenario using the GPU-based Tsunami-HySEA numerical tsunami propagation and inundation model using a system of nested topo-bathymetric grids, and 3) Hazard aggregation. We apply this site-specific PTHA workflow here to Catania, Sicily, for tsunamigenic earthquake sources in the Mediterranean. We illustrate the workflows of the PTHA as implemented for High-Performance Computing applications, including preliminary simulations carried out on intermediate scale GPU clusters. We show how the local hazard analysis conducted here produces a more fine-grained assessment than is possible with a regional assessment. However, the new local PTHA indicates somewhat lower probabilities of exceedance for higher maximum inundation heights than the available regional PTHA. The local hazard analysis takes into account small-scale tsunami inundation features and non-linearity which the regional-scale assessment does not incorporate. However, the deterministic inundation simulations neglect some uncertainties stemming from the simplified source treatment and tsunami modelling that are embedded in the regional stochastic approach to inundation height estimation. Further research is needed to quantify the uncertainty associated with numerical inundation modelling and to properly propagate it onto the hazard results, to fully exploit the potential of site-specific hazard assessment based on massive simulations.


2006 ◽  
Vol 22 (2_suppl) ◽  
pp. 159-182 ◽  
Author(s):  
Lucien G. Canton

Despite a distance of 100 years the Great San Francisco Earthquake and Fire still has much to teach the emergency managers of 2006. The response to the 1906 disaster foreshadows many modern emergency management techniques and sounds a cautionary note about areas where work still needs to be done. By comparing the city's response in 1906 with modern emergency plans, this paper examines how San Francisco might deal with a similar event in 2006. While many issues that marred the 1906 response have been resolved and much has been done to build resiliency, San Francisco in 2006 is in many ways still very similar in attitude to the San Francisco of 1906. Further, the recent example of Hurricane Katrina suggests that some of the more critical issues that arose in 1906 have still not been fully resolved.


Space Weather ◽  
2014 ◽  
Vol 12 (8) ◽  
pp. 530-537 ◽  
Author(s):  
Mark H. MacAlester ◽  
William Murtagh

Author(s):  
Costas E Synolakis ◽  
Eddie N Bernard

Tsunami science has evolved differently from research on other extreme natural hazards, primarily because of the unavailability until recently of instrumental recordings of tsunamis in the open ocean. Here, the progress towards developing tsunami inundation modelling tools for use in inundation forecasting is discussed historically from the perspective of hydrodynamics. The state-of-knowledge before the 26 December 2004 tsunami is described. Remaining aspects for future research are identified. One, validated inundation models need to be further developed through benchmark testing and instrumental tsunameter measurements and standards for operational codes need to be established. Two, a methodology is needed to better quantify short-duration impact forces on structures. Three, the mapping of vulnerable continental margins to identify unrecognized hazards must proceed expeditiously, along with palaeotsunami research to establish repeat intervals. Four, the development of better coupling between deforming seafloor motions and model initialization needs further refinement. Five, in an era of global citizenship, more comprehensive educational efforts on tsunami hazard mitigation are necessary worldwide.


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