Titlebook: Global Tsunami Science: Past and Future, Volume I; Eric L Geist,Hermann M. Fritz,Yuichiro Tanioka Book Apr 20171st edition Springer Intern

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innovation

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Kreditwirtschaftliche Wertermittlungenontinental slope and in the Canary Islands. Using a new PTHA methodology that is closely linked to well-established PSHA methodology combined with tide stage probability, we calculated that the return period for a wave runup exceeding the tidal range of +4 m level above mean sea level (highest astro

needle

https://doi.org/10.1007/978-3-663-13220-2rposes. We use a multidisciplinary approach bringing together geological information with modelling to construct a Probabilistic Tsunami Hazard Assessment of submarine landslide-generated tsunami. Although there are many simplifying assumptions used in this assessment, it suggests that the Cook Stra

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Kreditwirtschaftliche Wertermittlungenributions for the study test-site considering 100- and 500-year exposure times. We find that the probability that maximum wave amplitude exceeds 1 m somewhere along the Sines coasts reaches about 60 % for an exposure time of 100 years and is up to 97 % for an exposure time of 500 years. The probabil

不成比例

Modernisierung eines alten Mietshauses and photographic imagery from Google Earth and further validated by field surveys. We have explored three inundation scenarios corresponding to a constant-level tsunami flooding with assumed sea level rise of 1, 3 and 5 m, and evaluated the damage to the town buildings using both methods that make

GNAW

,Grundlagen Künstlicher Neuronaler Netze,ymetry and topography data for the entire Marmara Sea region and validated with historical observations from the 1509 and 1894 earthquakes. This study implements TUNAMI model with a two-layer model to conduct numerical tsunami simulations, and the numerical results show that the maximum tsunami heig

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https://doi.org/10.1007/978-3-322-99501-8mplitudes exceeding 50 cm can be expected, which would be dangerous in harbors and beach areas especially. The main contribution of these results is the establishment of specific thresholds of magnitude for the tsunami warning along the French coasts, 7.8 for the advisory level (coastal marine threa

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,Die Kreiselgebläse und Kreiselverdichter,g wave physics is such that tsunami currents will only rise above noise and background currents (i.e., be at least 10–15 cm/s), and become detectable, in fairly shallow water which would limit the direct detection of tsunami currents by HF radar to nearshore areas, unless there is a very wide shallo