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Titlebook: Meteorological Tsunamis: The U.S. East Coast and Other Coastal Regions; Ivica Vilibi?,Sebastian Monserrat,Alexander B. Rab Book 2015 Sprin

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31#
發(fā)表于 2025-3-26 22:42:55 | 只看該作者
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32#
發(fā)表于 2025-3-27 01:15:56 | 只看該作者
978-3-319-36612-8Springer International Publishing Switzerland 2015
33#
發(fā)表于 2025-3-27 07:57:59 | 只看該作者
https://doi.org/10.1007/978-3-319-12712-5Air-sea Interaction and Meteorological Tsunamis; Meteorological Tsunamis; Meteotsunami; Multiresonance
34#
發(fā)表于 2025-3-27 11:06:04 | 只看該作者
35#
發(fā)表于 2025-3-27 16:52:42 | 只看該作者
en more papers are documenting meteotsunamis in various coastal areas of the world oceans. All continents, except Antarctica, have been covered, with the authors representing 11 countries. .Previously Published in Natural Hazards, Volume 74, No. 1, 2014.978-3-319-36612-8978-3-319-12712-5
36#
發(fā)表于 2025-3-27 20:16:27 | 只看該作者
nant phenomenon. Altogether an editorial and 15 contributions are part of this book; eight of the contributions deal with different aspects of meteotsunamis along the U.S. East Coast and in the region of the Great Lakes, including one paper introducing a new methodology in meteotsunami research. Sev
37#
發(fā)表于 2025-3-28 00:20:51 | 只看該作者
38#
發(fā)表于 2025-3-28 05:35:58 | 只看該作者
39#
發(fā)表于 2025-3-28 06:29:05 | 只看該作者
Recent observations of meteotsunamis on the Finnish coast,gust fronts. These fronts propagate above the sea at a resonant speed, allowing efficient energy transfer between the atmospheric disturbance and the sea wave that it generates. Thus, we interpret the observed sea-level oscillations as small meteotsunamis, long tsunami-like waves generated by meteorological processes and resonance effects.
40#
發(fā)表于 2025-3-28 13:00:40 | 只看該作者
Assessing meteotsunami potential of high-frequency air pressure oscillations observed in the middlean 1?h, while air pressure disturbances were dispersive and not coherent at shorter periods. This implies that the disturbances had little to no potential to generate meteotsunamis in the middle Adriatic area, as the eigenoscillations in bays and harbours of the region are over timescales of minutes up to a few tens of minutes.
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