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

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Tidal influence on high frequency harbor oscillations in a narrow entrance bay,y modulated response. During low tides, these sea level oscillations reach amplitudes of 10–20 cm, while during high tides they are significantly smaller. Wells Harbor is located in a low lying area with a tidal range of about 2 m and is connected to the open ocean through a narrow channel. Thus, th
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Recent observations of meteotsunamis on the Finnish coast,tnesses report unusually rapid and strong sea-level variations (up to 1 m in 5–15 min) and strong oscillating currents during these events. High-resolution sea-level measurements confirm the eyewitness observations, but the oscillations recorded by tide gauges mostly have a considerably smaller ampl
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Assessing meteotsunami potential of high-frequency air pressure oscillations observed in the middlenalysed to extract the rapid pressure changes normally found during meteotsunamis. Five-minute air pressure tendencies were used to detect an event. Wavelet and cross-wavelet analysis showed that the energies of high-frequency pressure changes that occurred during the warm part of the year were an o
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Abiki oscillations in Sakitsu Bay, west Kyushu, Japan,on characteristics of both bays are investigated by taking field measurements and conducting numerical experiments with regard to flood mitigation with the aim to reduce the flood impact during Abiki events. A continuous wavelet transform and bandpass filtering both of the pressure and water level i
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The Dwarskersbos, South Africa local tsunami of August 27, 1969: field survey and simulation as a mabsence of any seismic disturbance or major meteorological storm. A field survey, based on the interview of nine elderly witnesses still residing in the community, documented maximum run-up of 2.9 m, concentrated on an extremely short segment of coastline, less than 2 km in length. These characteris
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Simultaneous meteorological tsunamis and storm surges at Buenos Aires coast, southeastern South Amecurrence of atmospheric gravity waves during the passages of cold fronts over the Buenos Aires Province continental shelf. On the other hand, storm surges are also frequent in the region, and they are associated with strong and persistent southerlies, which are also frequent during cold front passag
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