Harridan 发表于 2025-3-30 08:23:09
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Mitigation Lessons from the July 17, 1998 Papua New Guinea Tsunami, and disrupted the social and economic framework of the coastal communities of eastern Saundaun Province, Papua New Guinea. Initial response to the disaster was delayed 16 hours because of the failure to communicate the magnitude of the impact outside the affected area. Once the scope of the disasteCougar 发表于 2025-3-30 20:19:27
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http://reply.papertrans.cn/59/5809/580832/580832_54.pngoblique 发表于 2025-3-31 01:03:05
Re-examination of the Source Mechanism of the 1998 Papua New Guinea Earthquake and Tsunami,d adding bathymetric data at depths less than 60 m is carried out, reproducing the tsunami energy focus into Warapu and Arop along the Sissano Lagoon. However, the computed runup heights in the lagoon are still lower than those measured. Even if the error in estimating the fault parameters is takenMechanics 发表于 2025-3-31 06:35:12
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Field Survey and Numerical Simulations: A Review of the 1998 Papua New Guinea Tsunami,e discussion of the field survey explores a number of possible misinterpretations of the recorded data. The survey data are then employed by a numerical model as a validation tool. A Boussinesq model and a nonlinear shallow water wave (NLSW) model are compared in order to quantify the effect of freqNebulizer 发表于 2025-3-31 15:49:24
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http://reply.papertrans.cn/59/5809/580832/580832_59.pngambivalence 发表于 2025-3-31 23:26:22
A Theoretical Comparison of Tsunamis from Dislocations and Landslides,underwater slumps. We conclude that the two sources can generate tsunamis of comparable total energy. However, the slumping source is shown to be fundamentally dipolar in nature, which results in a low-frequency deficiency in the far-field. These simple conclusions corroborate the interpretation of