Seiches and Harbour Oscillations



Download 235.54 Kb.
Page4/4
Date18.10.2016
Size235.54 Kb.
#2367
1   2   3   4
60, (1/4), 1-13.

Bowers, E.C., 1982: The modelling of waves and their effects in harbours, in Hydraulic Modelling in Maritime Engineering., Thomas Telford, London, 121-127.

Candela, J., Mazzola, S., Sammari, C., Limeburner, R., Lozano, C.J., Patti, B., and Bonnano, A., 1999: The “Mad Sea” phenomenon in the Strait of Sicily, J. Phys. Oceanogr., 29, 2210-2231.

Chapman, D.C., and Giese, G.S., 2001: Seiches, in: Encyclopedia of Ocean Sciences, J.H. Steele, K.K. Turekian, and S.A. Thorpe (eds.), London, Academic Press, 5: 2724-2731.

Colucci, P., and Michelato, A., 1976: An approach to study of the ‘Marubbio’ phenomenon, Boll. Geofis. Theor. Appl., 13 (69), 3-10.

Defant, A., 1961: Physical Oceanography, Vol.2, Pergamon Press, Oxford, UK.

de Jong, M. P. C., L. H. Holthuijsen, and J. A. Battjes, 2003: Generation of seiches by cold fronts over the southern North Sea, J. Geophys. Res., 108 (C4), 3117, doi:10.1029/2002JC001422.

de Jong, M. P. C., and J. A. Battjes, 2004: Low-frequency sea waves generated by atmospheric convection cells, J. Geophys. Res., 109, C01011, doi:10.1029/2003JC001931

Djumagaliev, E.A. Kulikov, and S.L. Soloviev, 1993: Analysis of ocean level oscillations in Malokurilsk Bay caused by tsunami of 16 February 1991, Science Tsunami Hazards, 11, (1), 47-58.

Djumagaliev, V.A, Rabinovich, A.B., and Fine, I.V., 1994: Theoretical and experimental estimation of transfer peculiarities of the Malokurilsk Bay coast, the Island of Shikotan, Atmosph. Oceanic Physics, 30, (5), 680-686

Donn, W.L., 1964: Alaskan earthquake of 27 March 1964: remote seiche simulation, Science, 145, 261-262.

Drago, A.F., 1999: A study on the sea level variations and the ‘Milghuba’ phenomenon in the coastal waters of the Maltese Islands, Ph.D. thesis, University of Southampton.

Fontseré, E., 1934: Les ‘seixes de la costa catalana. Servei Meteorològic de Catalunya, Notes d’Estudi, 58 (in Catalan).

Garcies, M. Gomis, D., and Monserrat, S., 1996: Pressure-forced seiches of large amplitude in inlets of the Balearic Islands. Part II: Observational study. J. Geophys. Res., 101, (C3), 6453-6467.

Giese, G.S., and Chapman, D.C.: 1993, Coastal seiches, Oceanus, spring issue, 38-45.

Giese, G.S., Chapman, D.C., Black, P.G., and Fornshell, J.A., 1990: Causations of large-amplitude harbour seiches on the Caribbean coast of Puerto-Rico, J. Phys. Oceanogr., 20, 1449-1458.

Giese, G.S., and Hollander, R.B., 1987: The relation between coastal seiches at Palawan Island and tide-generated internal waves in the Sulu Sea, J. Geophys., 92, (C5), 5151-5156.

Gomis, D., Monserrat, S., and Tintoré, J., 1993: Pressure-forced seiches of large amplitude in inlets of the Balearic Islands. J. Geophys. Res., 98, 14,437-14,445.

Goring, D.G., 2005: Rissaga (long-wave events) on New Zealand's eastern seaboard: A hazard for navigation, Proc. 17th Australasian Coastal Ocean Eng. Conf., 20-23 Sept 2005, Adelaide, Australia, 137-141.

Gossard, E.E., and Hooke B.H., 1975: Waves in Atmosphere, Elsevier, New York, 456 p.

Greenspan, H.P., 1956: The generation of edge waves by moving pressure disturbances, J. Fluid Mech., 1, 574-592.

Hamblin, P.F., 1976: Seiches, circulation and storm surges of an ice-free Lake Winnipeg, J. Fisheries Res. Board Canada, 33, 2377-2391.

Harris, D.L., 1957: The effect of a moving pressure disturbance on the water level in a lake, Meteorol. Monogr., 2 (10), 46-57.

Henry, R.F., and Murty, T.S., 1995: Tsunami amplification due to resonance in Alberni Inlet: Normal modes, in Tsunami: Progress in Prediction, Disaster Prevention and Warning, edited by Y. Tsuchiya and N. Shuto, Kluwer Acad. Publ., Dordrecht, The Netherlands, 117-128.

Hibiya, T. and K. Kajiura, 1982: Origin of ‘Abiki’ phenomenon (kind of seiches) in Nagasaki Bay, J. Oceanogr. Soc. Japan, 38, 172-182.

Honda, K., Terada, T., Yoshida, Y., and Isitani D., 1908: An investigation on the secondary undulations of oceanic tides, J. College Sci., Imper. Univ. Tokyo, 108 p.

Hutchinson, G.E., 1957. A Treatise on Limnology. Volume 1. Geography, Physics and Chemistry. J. Wiley, New York, 1015 p.

Keulegan, G.H., and Carpenter, L.H., 1958: Forces on cylinders and plates in an oscillating fluid, J. Res. Nat. Bureau Stand., 60, 423-440.

Kinsman, B., 1965: Wind Waves: Their Generation and Propagation on the Ocean Surface, Prentice Hall, Englewood Cliffs, 676 p.

Korgen, B.J., 1995: Seiches, American Scientist, 83, 330-341.

Lamb, H., 1945: Hydrodynamics, 6th ed., Dover, New York, 738 p.

Lee, J.J., 1971: Wave induced oscillations in harbors of arbitrary geometry, J. Fluid Mech., 45, 375-394.

Le Méhauté, B., and Wilson, B.W., 1962: Harbor paradox (discussion). J. Waterways Harbor Division, ASCE, 88, 173-195.

Liu, P.L.-F., Monserrat, S., Marcos, M., and Rabinovich, A.B., 2003: Coupling between two inlets: Observation and modeling, J. Geophys. Res., 108, (C3), 3069, doi:10.1029/2002JC001478, 14-(1-10).

Longuet-Higgins, M.S., and Stewart, R.W., 1962: Radiation stress and mass transport in gravity waves, with application to ‘surf-beats’, J. Fluid Mech., 13, 481-504.

McGarr, A., 1965: Excitation of seiches in channels by seismic waves, J. Geophys. Res., 70 (4), 847-854.

Mei, C.C., 1992: The Applied Dynamics of Ocean Surface Waves, World Scientific, London, 740 p.

Merrifield, M.A., et al., 2005: Tide gage observations of the Indian Ocean tsunami, December 26, 2004, Geophys. Res. Lett. 32, L09603, doi:10.1029/2005GL022610.

Metzner, M., Gade, M., Hennings, I., and Rabinovich, A.B., 2000: The observation of seiches in the Baltic Sea using a multi data set of water levels, J. Marine Systems, 24, 67-84.

Mikishev, G.N. and Rabinovich, B.I., 1968: Dynamics of a Solid Body with Cavities Partially Filled with Liquid (in Russian), Mashinostroyeniye Press, Moscow, 532 p.

Miles, J.W., 1958: Ring damping of free surface oscillations in a circular tank, J. Appl. Mech., 25, 6, 26-32.

Miles, J.W., 1974: Harbor seiching, Ann. Rev. Fluid Mech., 6, 17-36.

Miles, J., and Munk, W., 1961: Harbor paradox, J. Waterways Harbor Division, ASCE, 87, 111-130.

Miller, G.R., 1972: Relative spectra of tsunamis: Hawaii Inst. Geophys, HIG-72-8, 7 p.

Monserrat, S., Ibberson, A., and Thorpe, A.J., 1991: Atmospheric gravity waves and the “rissaga” phenomenon, Q. J. R. Meteorol. Soc., 117, 553-570.

Monserrat, S., Rabinovich, A.B., and Casas, B., 1998: On the reconstruction of the transfer function for atmospherically generated seiches, Geophys. Res. Let., 25, (12), 2197-2200.

Monserrat S., I. Vilibić, and A.B. Rabinovich, 2006: Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band, Nat. Hazards Earth Syst. Sci., 6, 1035-1051

Munk, W.H. 1949: Surf beats, Eos, Trans. Amer. Geophys. Un., 30, (6), 849-854.

Munk, W.H. 1962: Long waves, in The Sea, J. Wiley, New York, 647-663.

Murty, T.S., 1977: Seismic Sea Waves - Tsunamis. Bull. Fish. Res. Board Canada 198, Ottawa, 337 p.

Murty, T.S., 1985: Modification of hydrographic characteristics, tides, and normal modes by ice cover, Marine Geodesy, 9 (4), 451-468.

Nakano, M., 1932: Secondary undulations in bays forming a coupled system, Proc. Phys. Math. Soc. Japan, 3, 372-380.`

Nakano, M., 1933: Possibility of excitation of secondary undulations in bays by tidal or oceanic currents, Proc. Imp. Acad. Japan, 9, 152-155.

Nakano, M., and T. Abe, 1959: Standing oscillation of bay water induced by currents, Records Oceanogr. Works in Japan, Spec. No. 3, 75-96.

Nakano, M., and Unoki, S., 1962: On the seiches (secondary undulations of tides) along the coast of Japan, Records Oceanogr. Works Japan, Spec. No.6, 169-214.

Nakano, M., and N. Fujimoto, 1987: Seiches in bays forming a coupled system, J. Oceanogr. Soc. Japan, 43, 124-134.

Nomitsu, T., 1935: A theory of tsunamis and seiches produced by wind and barometric gradient, Mem. Coll. Sci. Imp. Univ. Kyoto, A 18, (4), 201-214.

Okihiro, M., Guza, R.T., and Seymour, R.J., 1993: Excitation of seiche observed in a small harbor, J. Geophys. Res., 98, (C10), 18,201-18,211.

Oltman-Shay, J., and Guza, R.T., 1987: Infragravity edge wave observations on two California beaches, J. Phys. Oceanor., 17, (5), 644-663.

Orlić, M., 1980: About a possible occurrence of the Proudman resonance in the Adriatic, Thalassia Jugoslavica, 16 (1), 79-88.

Proudman, J., 1929: The effects on the sea of changes in atmospheric pressure, Geophys. Suppl. Mon. Notices R. Astr. Soc., 2 (4), 197-209.

Prandle, D., 1974: The use of wave resonators for harbour protection, Dock Harbour Author., 279-280.

Rabinovich, A.B., 1992: Possible vorticity effect in longwave motions (surging) in harbors, Trans. (Doklady) Russian Academy of Sciences, Earth Sciences Sections, 325, 224-228.

Rabinovich, A.B., 1993: Long Ocean Gravity Waves: Trapping, Resonance, and Leaking (in Russian), Gidrometeoizdat, St. Petersburg, 325 p.

Rabinovich, A.B., 1997: Spectral analysis of tsunami waves: Separation of source and topography effects, J. Geophys. Res., 102, (C6), 12,663-12,676.

Rabinovich, A.B., and Levyant, A.S., 1992: Influence of seiche oscillations on the formation of the long-wave spectrum near the coast of the Southern Kuriles, Oceanology, 32, (1), 17-23.

Rabinovich, A.B., and Monserrat, S., 1996: Meteorological tsunamis near the Balearic and Kuril Islands: Descriptive and statistical analysis, Natural Hazards, 13, (1), 55-90.

Rabinovich, A.B., and Monserrat, S., 1998: Generation of meteorological tsunamis (large amplitude seiches) near the Balearic and Kuril Islands, Natural Hazards, 18, (1), 27-55.

Rabinovich, A.B., Monserrat, S. and Fine, I.V., 1999: Numerical modeling of extreme seiche oscillations in the region of the Balearic Islands, Oceanology, 39, (1), 16-24.

Rabinovich, A.B., R.E. Thomson, and F.E. Stephenson, 2006: The Sumatra tsunami of 26 December 2004 as observed in the North Pacific and North Atlantic oceans, Surveys in Geophysics, 27, 647-677.

Rabinovich, A.B., and R.E. Thomson, 2007: The 26 December 2004 Sumatra tsunami: Analysis of tide gauge data from the World Ocean Part 1. Indian Ocean and South Africa, Pure Appl. Geophys., 164, (2/3), 261-308.

Rabinovich, A.B., Lobkovsky, L.I., Fine, I.V., Thomson, R.E., Ivelskaya, T.N., and Kulikov, E.A., 2008: Near-source observations and modeling of the Kuril Islands tsunamis of 15 November 2006 and 13 January 2007, Advances in Geosciences, 14 (1), 105-116.

Rabinovich, B.I. and Y.V. Tyurin, 2000: Numerical Conformal Mapping in Two-Dimensional Hydrodynamics, Space Research Institute RAS, Moscow, 312 p.

Raichlen, F., 1966: Harbor resonance, in Estuary and Coastline Hydrodynamics, Edited by A.T. Ippen, McGraw Hill Book Comp., New York, 281-340.

Raichlen, F., 2002: The effect of ship-harbor interactions on port operations, Maritime Technology, 11-20.

Raichlen, F., and Lee, J.J., 1992: Oscillation of bays, harbors, and lakes, in Herbich, J.B., ed., Handbook of Coastal and Ocean Engineering: Houston, Texas, Gulf Publishing Company, p. 1073-1113.

Ramis, C. and Jansà, A.: 1983: Condiciones meteorológicas simultáneas a la aparición de oscilaciones del nivel del mar de amplitud extraordinaria en el Mediterráneo occidental, Rev. Geofísica, 39, 35-42 (in Spanish).

Sawaragi, T., and Kubo, M., 1982: Long-period motions of a moored ship induced by harbor oscillations, Coast. Eng. Japan, 25, 261-275.

Schwab, D.J., and D.B. Rao, 1977: Gravitational oscillations of Lake Huron, Saginaw Bay, Georgian Bay and the North Channel, J. Geophys. Res., 82 (15), 2105-2116.

Sorensen, R.M. and E.F. Thompson, 2002: Harbor hydrodynamics, in Coastal Engineering Manual, Part II, U.S. Army Corps. Of Engineers, Washington, D.C., New York, Chapter 7, 1-92.

Tintoré, J., Gomis, D., Alonso, S., and Wang. D.P., 1988: A theoretical study of large sea level oscillations in the Western Mediterranean, J. Geophys. Res., 93, 10,797-10,803.

Titov, V.V., A.B. Rabinovich, H. Mofjeld, R.E. Thomson, and F.I. González, 2005: The global reach of the 26 December 2004 Sumatra tsunami, Science, 309, 2045-2048.

Thomson, R.E., P.W. Vachon, and G.A. Borstad, 1992: Airborne synthetic aperture radar imagery of atmospheric gravity waves. J. Geophys. Res. 97 (C9): 14,249-14,257.

Thomson, R.E., A.B. Rabinovich, and M.V. Krassovski, 2007: Double jeopardy: Concurrent arrival of the 2004 Sumatra tsunami and storm-generated waves on the Atlantic coast of the United States and Canada, Geophys. Res. Lett., 34, L15607, doi:10.1029/2007GL030685.

Tucker, M.J., 1950: Surf beats: Sea waves of 1 to 5 minute period, Proc. Roy. Soc. London, Ser.A., 202, 565-573.

Van Dorn, W.G., 1984: Some tsunami characteristics deducible from tide records, J. Phys. Oceanogr. 14, 353-363.

Vilibić, I., and Mihanović, H., 2003: A study of resonant oscillations in the Split Harbour (Adriatic Sea), Estuar. Coastal Shelf Sci., 56, 861-867,

Vilibić, I., Domijan, N., Orlić, M., Leder, N., and Pasarić, M., 2004: Resonant coupling of a traveling air-pressure disturbance with the east Adriatic coastal waters, J. Geophys. Res., 109, C10001, doi:10.1029/2004JC002279, 2004.

Wang, X., Li, K., Yu, Z., and Wu, J., 1987: Statistical characteristics of seiches in Longkou Harbor, J. Phys. Oceanogr., 17, 1063-1065.

Wiegel, R.L., 1964: Tsunamis, storm surges, and harbor oscillations. Ch. 5 in Oceanographical Engineering, Prentice-Hall, Englewood Cliffs, N.J., 95-127.

Wilson, B., 1972: Seiches, Advances in Hydrosciences, 8, 1-94.



Wu, J.-K., and Liu, P.L.-F., 1990: Harbour excitations by incident wave groups, J. Fluid Mech., 217, 595-613.



1 In many papers and text books [cf. Wiegel, 1964; Wilson, 1972; Chapman and Giese, 2001] this mode is considered the “first mode”. However, it is more common to count nodal lines only inside the basin (not at the entrance) and to consider the fundamental harbour mode as the “zeroth mode” [cf., Raichlen, 1966; Raichlen and Lee, 1992; Mei, 1992; Rabinovich, 1993; Sorensen and Thompson, 2002]. This approach is physically more sound because this mode is quite specific and markedly different from the first mode in a closed basin.

2 This approach is used for numerical computation of eigen modes in natural two-dimensional basins [cf. Rabinovich and Levyant, 1992].

3 This is the reason for calling this the “zeroth mode”.

4 The Russian name for these waves are ‘anemobaric’ [Rabinovich, 1993] because they are induced by atmospheric pressure(“baric”) and wind (“anemos”) stress forcing on the ocean surface

5 Figure 5 does not include all possible types of IG-waves and mechanisms of their generation; a more detailed description is presented by Bowen and Huntley [1984] and Battjes [1988].

6 A famous example of this kind is the French port Le Havre. Before World War II it was known for very common and strong surging motions that created severe problems for ships. During the war a German submarine torpedoed by mistake a rip-rap breakwater, creating a second harbour opening of 20-25 m width. After this, the surging in the port disappeared [Rabinovich, 1993].

7 The resonant characteristics of each location are always the same; however, different sources induce different resonant mode, specifically, large seismic sources generate low-frequency modes and small seismic sources generate high-frequency modes.

8 For this reason a wave specialist in New Zealand (Derek Goring) suggested to apply the term “rissaga” to all rissaga-like meteorological seiches in other areas of the World Ocean [Goring, 2005]. However, if we were to adopt this term, then we would loose information on the cause of the oscillations and the fact that they are part of a family of events that include seismically generated tsunamis, landslide tsunamis, volcanic tsunamis and meteotsunamis.

Download 235.54 Kb.

Share with your friends:
1   2   3   4




The database is protected by copyright ©ininet.org 2024
send message

    Main page