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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Primary terms
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waves
Full-waveform inversion by model extension: Theory, design, and optimization
Full-waveform inversion by model extension: Practical applications
Wavefield simulation with the discontinuous Galerkin method for a poroelastic wave equation in triple-porosity media
Wave propagation in thermo-poroelasticity: A finite-element approach
Methane Fluxes at the Water–Atmosphere Interface and Gas-Geochemical Anomalies in the Bottom Sediments in the Northwestern Part of the Sea of Japan
Toward autonomous event identification in wave-equation traveltime inversion
On the spectral changes of seismic wave energy by a partially saturated crack due to the hysteresis of liquid bridges phenomenon
Microbially induced pseudotraces from a Pantanal soda lake, Brazil: Alternative interpretations for Ediacaran simple trails and their limits
Characterization of fluvio-deltaic gas reservoirs through AVA deterministic, stochastic, and wave-equation-based seismic inversion: A case study from the Carnarvon Basin, Western Australia
An approach for attenuation-compensating multidimensional constant- Q viscoacoustic reverse time migration
Local and global fluid-flow effects on dipole flexural waves
Application of perfectly matched layers in 3D transient controlled-source electromagnetic modeling by the rapid expansion method
New Perspectives On the Geomorphic, Sedimentologic, and Stratigraphic Signatures of Former Wave-dominated Tidal Inlets: Assateague Island, Maryland, U.S.A.
Linking the High-Resolution Architecture of Modern and Ancient Wave-Dominated Deltas: Processes, Products, and Forcing Factors
Modification of crustal seismic anisotropy by geological structures (“structural geometric anisotropy”)
Water hammers tremors during plate convergence
Random Response Spectrum Analysis of Gravity Dam Classes: Simplified, Practical, and Fast Approach
Abstract Central America is a small and culturally homogeneous region that, since the 1990s, has experienced economic and political integration of its six countries, which share the same threats of volcanic eruptions, disastrous earthquakes and tsunamis. The Pacific coastline of 1700 km is common for Guatemala, El Salvador, Honduras, Nicaragua, Costa Rica and Panama, and the Pacific subduction zone has the potential for creating huge tsunamis that threaten this coast. In addition to the natural hazard, the growing tourist industry is expanding its infrastructure along the Pacific beaches, which again enhances the exposure and tsunami risk. Even though the 1992 tsunami disaster in Nicaragua did not severely hit the tourist beaches, it raised the risk awareness, and special attention is now given to ‘slow’ earthquakes that may be modest in shaking while still having a large tsunami potential. The tsunami hazard mapping is well advanced in Nicaragua, Costa Rica and El Salvador, and initiatives are ongoing to improve the mapping in all countries. National systems for early warning were established in Nicaragua and El Salvador, while the other four countries rely on rapid information from the Pacific Tsunami Warning Center. Mitigation measures and information campaigns are presently conducted on a national basis in all countries, but a regional centre for early tsunami warning and coordinated information campaigns (CATAC) is expected to become operational in the near future.