Abstract
Extremely large seiche oscillations are regularly observed in some specific areas around the world even in the absence of any seismic forcing. These seiches have been successfully associated with strong atmospheric pressure perturbations inducing sea level oscillations at the open ocean, before entering the inlet, which are in turn resonantly amplified by the geometric characteristics of the inlet. The coastal behaviour of such waves, although of different origin, is similar to tsunami waves behaviour, and is sometimes referred to as meteotsunamis. In some specific places, such as Ciutadella inlet, Balearic Islands, western Mediterranean, these seiche oscillations are stronger than expected, even taking into account the large amplification factor by resonance of the inlet. For these cases, some external amplification, before entering the inlet, is necessary to explain the phenomenon. In this paper, it is numerically shown how the phase speed of the atmospheric pressure disturbance generating the surface waves is a critical factor in the energy transfer between the atmosphere, and the ocean.
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References
Honda, K., Terada, T., Yoshida, Y., and Isitani, D. (1908) An investigation on the secondary undulations of oceanic tides, J. College Sci., Imp. Univ. Tokyo, 108 p.
Hibiya, T., and Kajiura, K. (1982) Origin of Abiki’ phenomenon (a kind of seiches) in Nagasaki Bay, J. Oceanogr. Soc. Japan, 38, 172–182.
Wang, X., Li, K., Yu, Z., and Wu, J. (1987) Statistical characteristics of seiches in Longkou Harbour, J. Phys. Oceanogr., 17, 1063–1065.
Hodvzic, M. (1979) Exceptional oscillations in the Bay of Vela Luka, and meteorological situation on the Adriatic, International School of Meteorology of the Mediterranean, 1 Course, Erice, Italy.
Papadopoulos, G. A. (1993) Some exceptional seismic (?) sea-waves in the Greek Archipelago, Science of Tsunami Hazards, 11, 25–34.
Gomis, D., S. Monserrat, J. Tintoré (1993) Pressure-forced seiches of large amplitude in inlets of the Balearic Islands, J. Geophys. Res., 98, 14437–14445
Monserrat, S., A.B. Rabinovich, B. Casas (1998) On the Reconstruction of the Transfer Function for Atmospherically Generated Seiches, Geophys. Res. Let., 25, 2197–2205
Monserrat, S., A.J. Thorpe (1992) Gravity wave observations using an array of microbarographs in the Balearic Islands, Q. J. R. Meteor. Soc., 118, 259–282.
Smagorinsky, J. (1963) General circulation experiments with the primitive equations, Mon. Weather Rev., 91, 99–165
Jin, X., Kronenburg, C. (1993) Quasi-3D numerical modelling of shallow water circulation, Journal of Hydraulic Engineering, Vol 119,4, 458–472
Mellor, G.L. (1991) An equation of state for numerical models of oceans, and estuaries, J. Atmos. Oceanic. Technol., 8, 601–611
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© 2003 Springer Science+Business Media Dordrecht
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Marcos, M., Monserrat, S., Medina, R., Vidal, C. (2003). Influence of the Atmospheric Wave Velocity in the Coastal Amplification of Meteotsunamis. In: Yalçiner, A.C., Pelinovsky, E.N., Okal, E., Synolakis, C.E. (eds) Submarine Landslides and Tsunamis. NATO Science Series, vol 21. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0205-9_25
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DOI: https://doi.org/10.1007/978-94-010-0205-9_25
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-1349-2
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