2269:
Cook, Kristen L.; Glimsdal, Sylfest; Løvholt, Finn; Van Noten, Koen; Assink, Jelle D.; Marboeuf, Alexis; Lomax, Anthony; Vanneste, Kris; Taira, Taka’aki; Spagnolo, Matteo; De Plaen, Raphael; Koelemeijer, Paula; Ebeling, Carl; Cannata, Andrea; Harcourt, William D.; Cornwell, David G.; Caudron, Corentin; Poli, Piero; Bernard, Pascal; Larose, Eric; Stutzmann, Eleonore; Voss, Peter H.; Lund, Bjorn; Cannavo, Flavio; Castro-Díaz, Manuel J.; Chaves, Esteban; Dahl-Jensen, Trine; Pinho Dias, Nicolas De; Déprez, Aline; Develter, Roeland; Dreger, Douglas; Evers, Läslo G.; Fernández-Nieto, Enrique D.; Ferreira, Ana M. G.; Funning, Gareth; Gabriel, Alice-Agnes; Hendrickx, Marc; Kafka, Alan L.; Keiding, Marie; Kerby, Jeffrey; Khan, Shfaqat A.; Dideriksen, Andreas Kjær; Lamb, Oliver D.; Larsen, Tine B.; Lipovsky, Bradley; Magdalena, Ikha; Malet, Jean-Philippe; Myrup, Mikkel; Rivera, Luis; Ruiz-Castillo, Eugenio; Wetter, Selina; Wirtz, Bastien (13 September 2024). "A rockslide-generated tsunami in a
Greenland fjord rang Earth for 9 days".
716:
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617:. The low pressure of the cyclone draws greater-than-normal quantities of water into the virtually landlocked Baltic. As the cyclone continues inland, long, low-frequency seiche waves with wavelengths up to several hundred kilometres are established in the Baltic. When the waves reach the narrow and shallow Neva Bay, they become much higher—ultimately flooding the Neva embankments. Similar phenomena are observed at Venice, resulting in the
161:
343:
3255:
4164:
441:, are significantly at risk from seiches. Geological evidence indicates that the shores of Lake Tahoe may have been hit by seiches and tsunamis as much as 10 metres (33 ft) high in prehistoric times, and local researchers have called for the risk to be factored into emergency plans for the region.
675:
is about thirty minutes. That meant that every second wave was in phase with the bay, creating a seiche. As a result, Hilo suffered worse damage than any other place in Hawaii, with the combined tsunami and seiche reaching a height of 26 feet (7.9 m) along the
Bayfront, killing 96 people in the
299:
Seiches have been observed on both lakes and seas. The key requirement is that the body of water be partially constrained to allow formation of standing waves. Regularity of geometry is not required; even harbours with exceedingly irregular shapes are routinely observed to oscillate with very stable
191:
Vertical harmonic motion results, producing an impulse that travels the length of the basin at a velocity that depends on the depth of the water. The impulse is reflected back from the end of the basin, generating interference. Repeated reflections produce standing waves with one or more nodes, or
2268:
Svennevig, Kristian; Hicks, Stephen P.; Forbriger, Thomas; Lecocq, Thomas; Widmer-Schnidrig, Rudolf; Mangeney, Anne; Hibert, Clément; Korsgaard, Niels J.; Lucas, Antoine; Satriano, Claudio; Anthony, Robert E.; Mordret, Aurélien; Schippkus, Sven; Rysgaard, Søren; Boone, Wieter; Gibbons, Steven J.;
1034:
turbulence by convective overturning, whereas the falling thermocline experiences greater stratification and low turbulence at the lake bed. Internal waves can also degenerate into non-linear internal waves on sloping lake-beds. When such non-linear waves break on the lake bed, they can be an
711:
about 200 metres (660 ft) high. This was followed by a seiche with waves up to 7 metres (23 ft) high oscillating within the fjord. This seiche lasted nine days, reflecting the avalanche's large size and the fjord's long, narrow shape. During that period, it generated unusual seismic
632:, most often in the spring. During a seiche event on 31 March 1979, a water-level displacement of 2.78 metres (9.1 ft) was recorded at Nagasaki tide station; the maximum displacement in the whole bay is thought to have reached as much as 4.70 metres (15.4 ft). Seiches in Western
699:
in eastern Canada, where seiches cause some of the highest recorded tidal fluctuations in the world. A dynamical mechanism exists for the generation of coastal seiches by deep-sea internal waves. These waves can generate a sufficient current at the shelf break to excite coastal seiches.
409:
caused the water level to fall and then rise again by three feet (one metre) within fifteen minutes, leaving some boats hanging from the docks on their mooring lines when the water retreated. The same storm system that caused the 1995 seiche on Lake
Superior produced a similar effect in
1986:
199:
of a seiche is the period associated with the fundamental resonance for the body of water—corresponding to the longest standing wave. For a surface seiche in an enclosed rectangular body of water this can be estimated using Merian's formula:
901:
1144:
has a period similar to the natural frequency of the harbour, each wave will amplify the seiche's intensity, resulting in rougher waters within the harbour compared to the surrounding sea, which can create problems for shipping. The
1821:
where incoming tides are funneled into a shallow, narrowing river via a broad bay. The funnel-like shape increases the height of the tide above normal, and the flood appears as a relatively rapid increase in the water
1124:
may be severely affected even by small fluctuations in water levels, and therefore historical and predicted water level fluctuations are crucial data for any coastal design. Information on seiches, along with
378:
is particularly prone to wind-caused seiches because of its shallowness and its elongation on a northeast–southwest axis, which frequently matches the direction of prevailing winds and therefore maximises the
1029:
moves up and down a sloping lake bed, it creates a 'swash zone', where temperatures can vary rapidly, potentially affecting fish habitat. As the thermocline rises up a sloping lake bed, it can also cause
2115:
263:
176:
The effect is caused by resonances in a body of water that has been disturbed by one or more factors, most often meteorological effects (wind and atmospheric pressure variations), seismic activity, or
291:
Higher-order harmonics are also observed. The period of the second harmonic will be half the natural period, the period of the third harmonic will be a third of the natural period, and so forth.
1554:
327:
found the longitudinal period to have a 73-minute cycle, and the transversal seiche to have a period of around 10 minutes. Another lake well known for its regular seiches is New
Zealand's
2863:
1495:
1411:
As an example, the period for a seiche wave in a body of water 10 meters deep and 5 kilometers long would be 1000 seconds or about 17 minutes, while a body about 300 km long (such as the
1120:), potable water storage basins, harbours, and even spent nuclear fuel storage basins. Structures and beach-dune systems are particularly vulnerable to damage from high water levels.
1008:
778:
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1796:
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points, that experience no vertical motion. The frequency of the oscillation is determined by the size of the basin, its depth and contours, and the water temperature.
783:
390:
like that caused by hurricanes along ocean coasts, but the seiche effect can cause oscillation back and forth across the lake for some time. In 1954, the remnants of
308:
Low rhythmic seiches are almost always present on larger lakes. They are usually unnoticeable among the common wave patterns, except during periods of unusual calm.
173:
Seiches are often imperceptible to the naked eye, and observers in boats on the surface may not notice that a seiche is occurring due to the extremely long periods.
1741:
1521:
2595:
2300:
1892:
Giese, Graham S.; R. B. Hollander; J. E. Fancher; B. S. Giese (1982). "Evidence of coastal Seiche excitation by tide-generated internal solitary waves".
1349:
Tsunamis are normally associated with earthquakes, but landslides, volcanic eruptions and meteorite impacts all have the potential to generate a tsunami.
2424:"The Interaction of Large Amplitude Internal Seiches with a Shallow Sloping Lakebed: Observations of Benthic Turbulence in Lake Simcoe, Ontario, Canada"
1546:
640:
of about 30 to 40 minutes. Locally, seiches have caused floods, destroyed port facilities and damaged the fishery: hence the local word for seiche, あびき
104:. The key requirement for formation of a seiche is that the body of water be at least partially bounded, allowing the formation of the standing wave.
3894:
451:
are especially prone to seiches caused by earthquakes, as the ground tremors often match the resonant frequencies of small bodies of water. The 1994
2319:
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in
Chicago, eight fishermen were swept away from piers at Montrose and North Avenue Beaches and drowned when a 10-foot (3.0 m) seiche hit the
2875:
3884:
2943:
2211:
2860:
1507:
1329:
2841:
1970:"Estimated Speed of Aves Ridge Solitons Packets by Analysis of Sequential Images from the Moderate Resolution Imaging Spectroradiometer(MODIS)"
636:—including Nagasaki Bay—are often induced by a low in the atmospheric pressure passing South of Kyushu island. Seiches in Nagasaki Bay have a
1833:
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2826:
184:
always seeks to restore the horizontal surface of a body of liquid water, as this represents the configuration in which the water is in
1170:
1059:, about 1,500 miles (2,400 kilometres) away. Seiches were also observed in the cave after powerful earthquakes in 2012, 2018 and 2019.
1770:
1458:
2749:
2676:
601:, respectively, as both cities are constructed on former marshland. In St. Petersburg, seiche-induced flooding is common along the
118:. The word had apparently long been used in the region to describe oscillations in alpine lakes. According to Wilson (1972), this
3800:
2855:
1654:
2888:
2237:"The 16 September 2023 Greenland Megatsunami: Analysis and Modeling of the Source and a Week‐Long, Monochromatic Seismic Signal"
206:
4167:
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475:
in 1755 also caused seiches 1,300 miles (2,100 km) farther north in Loch Lomond, Loch Long, Loch
Katrine and Loch Ness in
1788:
2916:
2718:
1442:
1281:
1248:
546:, 1842 Central Bengal, 1905 Kangra, 1930 Dhubri, 1934 Nepal-Bihar, 2001 Bhuj, 2005 Nias, 2005 Teresa Island earthquakes. The
1625:
3447:
1715:
1685:
2936:
1307:
1176:
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1737:
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reverberations detected around the world, puzzling seismologists for some time before they could identify their source.
4042:
3469:
3357:
2235:
Carrillo‐Ponce, Angela; Heimann, Sebastian; Petersen, Gesa M.; Walter, Thomas R.; Cesca, Simone; Dahm, Torsten (2024).
1525:
3889:
3160:
61:
3347:
3307:
374:
issues low water advisories for portions of the Great Lakes when seiches of 2 feet or greater are likely to occur.
164:
A standing wave (black) depicted as a sum of two propagating waves traveling in opposite directions (blue and red).
1425:
Lemmin, Ulrich (2012), "Surface
Seiches", in Bengtsson, Lars; Herschy, Reginald W.; Fairbridge, Rhodes W. (eds.),
4077:
3063:
2548:
559:
542:. Other earthquakes in the Indian sub-continent known to have generated seiches include the 1803 Kumaon-Barahat,
531:
2192:
2167:
2033:
2008:
1953:
1928:
402:, causing extensive flooding, and established a seiche that subsequently caused flooding along the south shore.
4157:
3750:
2929:
1503:
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of those winds. These can lead to extreme seiches of up to 5 metres (16 ft) between the ends of the lake.
1678:"26 December 2004, M9.1 "Boxing Day" Earthquake & Tsunami/Sumatra-Andaman Earthquake/Indian Ocean Tsunami"
2490:
543:
3205:
488:
2851:
Seiche. Encyclopædia
Britannica. Retrieved January 24, 2004, from Encyclopædia Britannica Premium Service.
1306:. 1st International Conference on Coastal Engineering, Long Beach, California. Council on Wave Research,
973:
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can produce seiches as a result of local geographic peculiarities. For instance, the tsunami that hit
324:
111:
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3342:
3302:
1301:
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are often prone to small seiches with amplitudes of a few centimetres and periods of a few minutes.
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3442:
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3372:
3008:
2978:
1868:
1465:
371:
4104:
4087:
3924:
3417:
3282:
3220:
3210:
3103:
2144:
2007:
Giese, Graham S.; David C. Chapman; Margaret Goud
Collins; Rolu Encarnacion; Gil Jacinto (1998).
921:
736:
524:
332:
185:
28:
17:
896:{\displaystyle c^{2}=g{\frac {\rho _{2}-\rho _{1}}{\rho _{2}}}{\frac {h_{1}h_{2}}{h_{1}+h_{2}}}}
4099:
4037:
3464:
3150:
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1164:
959:
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Seiches are also observed beneath the surface of constrained bodies of water, acting along the
472:
460:
3932:
3914:
3422:
3317:
2952:
2099:"Tide-Generated Internal Solitons in Bay of Bengal Excite Coastal Seiches in Trincomalee Bay"
1173: – Terminology used by the National Weather Service to describe severe weather in the US
1083:
547:
452:
2713:. Advanced series on ocean engineering. Singapore ; River Edge, N.J: World Scientific.
1653:. Abridged from Earthquake Information Bulletin, January–February 1976, Volume 8, Number 1.
1469:
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2563:
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2020:
1940:
1901:
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for example, are the result of a combination of storm surge, barometric surge and seiches.
1109:
2006:
671:
in 1946 had a fifteen-minute interval between wave fronts. The natural resonant period of
447:-generated seiches can be observed thousands of miles away from the epicentre of a quake.
8:
4114:
3999:
3994:
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3392:
3352:
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by 20 centimetres in a 27-minute cycle. Seiches can also form in semi-enclosed seas; the
2645:
2636:
2620:
2567:
2517:
2509:
2439:
2390:
2363:
Mortimer, C. H. (1974). Lake hydrodynamics. Mitt. Internat. Verein. Limnol. 20, 124–197.
2183:
2073:
2024:
1944:
1905:
1738:"Arizona Geology: Video of seiche in Devils Hole pupfish pond. (Posted: April 27, 2010)"
4200:
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3770:
3760:
3725:
3625:
3610:
3507:
2800:
2658:
2587:
2529:
2466:
2423:
2038:
1860:
1675:
In fact, "one person drowned in a pond as a result of a seiche in Nadia, West Bengal".
1599:
1273:
1179: – Severe weather-related terminology used by the Meteorological Service of Canada
1019:
551:
285:
149:
2820:
2009:"The Coupling between Harbor Seiches at Palawan Island and Sulu Sea Internal Solitons"
1646:
4139:
4129:
4072:
4052:
3735:
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3635:
3615:
3605:
3487:
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3033:
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2533:
2521:
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2453:
2404:
1864:
1438:
1394:
1367:
1321:
1277:
1244:
1182:
1113:
380:
351:
2591:
2042:
1929:"Causation of Large-Amplitude Coastal Seiches on the Caribbean Coast of Puerto Rico"
1926:
4094:
4062:
4032:
3841:
3826:
3695:
3630:
3522:
3437:
3367:
3292:
3073:
3043:
2973:
2968:
2792:
2640:
2571:
2513:
2461:
2443:
2394:
2301:"A landslide linked to climate change 'rang' the Earth for 9 days, researchers say"
2278:
2248:
2187:
2105:
2077:
2028:
1976:
1948:
1909:
1852:
1591:
1430:
1311:
1269:
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1117:
1108:
Engineers consider seiche phenomena in the design of flood protection works (e.g.,
637:
598:
196:
44:
1617:
1434:
1187:
3899:
3795:
3745:
3710:
3670:
3562:
3532:
3382:
3332:
3242:
3200:
3133:
3058:
3018:
2879:
2867:
2448:
1774:
1429:, Encyclopedia of Earth Sciences Series, Springer Netherlands, pp. 751–753,
1412:
1359:
692:
688:
684:
622:
391:
2850:
2110:
1981:
1707:
1677:
1035:
important source of turbulence and have the potential for sediment resuspension
621:, a system of 79 mobile barriers designed to protect the three entrances to the
4215:
4205:
4009:
4004:
3909:
3904:
3740:
3680:
3675:
3407:
3297:
3118:
3053:
3028:
2399:
2374:
2058:"Meteorological and internal wave forcing of seiches along the Sri Lanka coast"
1240:
1137:
703:
In
September 2023, an enormous landslide resulting from a melting glacier near
606:
448:
3254:
2575:
1927:
Giese, Graham S.; David C. Chapman; Peter G. Black; John A. Fornshell (1990).
4194:
4179:
4027:
3947:
3836:
3755:
3730:
3665:
3595:
3502:
3397:
3274:
3195:
3155:
3128:
3038:
2988:
2708:
2654:
2583:
2525:
2457:
2408:
1371:
1325:
719:
Illustration of the initiation of surface and subsurface thermocline seiches.
704:
504:
419:
406:
328:
85:
73:
69:
2728:
2282:
1913:
1891:
1398:
491:
caused seiches in standing water bodies in many Indian states as well as in
128:
meaning "dry", i.e., as the water recedes, the beach dries. The French word
114:
in 1890, who was the first to make scientific observations of the effect in
4134:
4082:
4022:
3973:
3851:
3846:
3821:
3805:
3780:
3497:
3387:
3327:
3113:
3023:
2998:
2475:
696:
629:
618:
586:
566:
459:
caused swimming pools to overflow across southern California. The massive
395:
359:
119:
2168:"A Model for the Generation of Coastal Seiches by Deep-Sea Internal Waves"
4124:
3856:
3785:
3650:
3590:
3557:
3547:
3542:
3427:
3362:
3322:
3312:
3287:
3170:
3143:
3123:
3083:
3048:
2373:
Cossu, R.; Ridgway, M.S.; Li, J.Z.; Chowdhury, M.R.; Wells, M.G. (2017).
2347:
2343:
2082:
2057:
1297:
1141:
1126:
1044:
1043:
On September 19, 2022, a seiche reaching 4 feet (1.2 metres) occurred at
1026:
967:
911:
729:
708:
512:
468:
405:
Lake seiches can occur very quickly: on July 13, 1995, a large seiche on
387:
320:
115:
2921:
2212:"Bizarre, nine-day seismic signal caused by epic landslide in Greenland"
1071:
676:
city alone. Seiche waves may continue for several days after a tsunami.
342:
3942:
3790:
3765:
3660:
3640:
3567:
3552:
3537:
3527:
3492:
3412:
3232:
3227:
3190:
3185:
3180:
3078:
2804:
2351:
2320:"A rumble echoed around the world for nine days. Here's what caused it"
2253:
2236:
1856:
1818:
1603:
1193:
963:
614:
602:
590:
520:
508:
492:
456:
444:
434:
430:
415:
411:
339:
often experiences a lengthwise seiche with a period of about 36 hours.
4174:
2873:
Great Lakes Storms Photo Gallery Seiches, Storm Surges, and Edge Waves
1316:
4014:
3876:
3861:
3775:
3620:
3459:
3454:
3237:
3165:
3093:
3013:
3003:
2960:
2549:"The degeneration of internal waves in lakes with sloping topography"
1578:
1133:
1011:
555:
375:
347:
336:
313:
154:
108:
81:
2900:
2796:
1595:
1231:
Rabinovich, Alexander B. (2018). "Seiches and Harbor Oscillations".
605:
in the autumn. The seiche is driven by a low-pressure region in the
418:
changed by 6 feet (1.8 m) over two hours. On June 26, 1954, on
157:, having periods longer than the accompanying wind-generated waves.
4109:
3831:
3690:
3582:
3572:
3517:
2993:
2681:
2234:
2098:
1969:
1158:
562:
produced large seiches that quickly became an internet phenomenon.
500:
476:
153:, which are due to subharmonic nonlinear wave interaction with the
2055:
1268:. Advances in Hydroscience. Vol. 8. Elsevier. pp. 1–94.
1196:, Disused gravity arch dam in Italy, destroyed by a seiche in 1963
160:
3978:
3968:
3138:
3108:
1121:
1031:
680:
664:
610:
539:
423:
399:
309:
181:
177:
2621:"Sediment Resuspension and Transport by Internal Solitary Waves"
1468:, Office of Climate, Water, and Weather Services. Archived from
739:, the expected period of the internal wave can be expressed as:
34:
Standing wave in an enclosed or partially enclosed body of water
3685:
2375:"Wash-zone dynamics of the thermocline in Lake Simcoe, Ontario"
1056:
668:
633:
594:
570:
535:
484:
464:
438:
93:
4047:
3866:
3645:
3600:
2889:
Shelf Response for an identical pair of incident KdV solitons
2819:
2758:
2677:"Mexico earthquake caused waves at California's Death Valley"
2267:
516:
496:
480:
76:. Seiches and seiche-related phenomena have been observed on
1547:"Huge Lake Wave Hits Chicago; Four Drowned, Ten Are Missing"
1496:"Bonanza for Lake Superior: Seiches Do More Than Move Water"
565:
Seiches up to at least 1.8 m (6 feet) were observed in
3479:
2883:
2193:
10.1175/1520-0485(1990)020<1459:AMFTGO>2.0.CO;2
2034:
10.1175/1520-0485(1998)028<2418:TCBHSA>2.0.CO;2
1954:
10.1175/1520-0485(1990)020<1449:COLACS>2.0.CO;2
1459:"Marine and Coastal Services Abbreviations and Definitions"
1146:
672:
280:
are the length and average depth of the body of water, and
97:
77:
50:
2861:
Bonanza for Lake Superior: Seiches Do More Than Move Water
258:{\displaystyle T={\frac {\ \ 2L\ \ }{\!\!\!{\sqrt {gh}}}}}
53:
2547:
Boegman, L.; Ivey, G. N.; Imberger, J. (September 2005).
2056:
Wijeratne, E. M. S.; P. L. Woodworth; D. T. Pugh (2010).
683:) can excite coastal seiches at the following locations:
101:
89:
467:
in 1964 caused seiches in swimming pools as far away as
2372:
1387:
Ueber die Bewegung tropfbarer Flüssigkeiten in Gefässen
958:
the average thicknesses of the two layers separated by
2165:
1415:) and somewhat deeper has a period closer to 12 hours.
1831:
976:
924:
786:
748:
209:
62:
47:
1789:"Japanese earthquake literally made waves in Norway"
1062:
2785:
Journal of the Royal Geographical Society of London
2546:
1218:
The Tides and Kindred Phenomena in the Solar System
2783:Jackson, J. R. (1833). "On the Seiches of Lakes".
2710:Introduction to coastal engineering and management
2311:
2205:
2203:
1577:
1393:] (thesis) (in German). Basel: Schweighauser.
1002:
950:
895:
772:
534:is known to have generated seiches as far away as
257:
3895:North West Shelf Operational Oceanographic System
2210:Hicks, Steven; Svennevig, Kristian (2024-09-14).
1136:of a seiche depends on the size and depth of the
346:Differences in water level caused by a seiche on
241:
240:
239:
4192:
1391:On the motion of drippable liquids in containers
1167: – Study of earthquake-resistant structures
660:, meaning 'the dragging-away of a fishing net'.
3885:Deep-ocean Assessment and Reporting of Tsunamis
2200:
1553:. Vol. 103, no. 35218. 27 June 1954.
585:Seiches have been observed in seas such as the
2618:
2489:Bouffard, Damien; Wüest, Alfred (2019-01-05).
2209:
1838:Phenomenon (a kind of Seiche) in Nagasaki Bay"
723:
653:
643:
2937:
2488:
2619:Boegman, Leon; Stastna, Marek (2019-01-05).
2422:Cossu, Remo; Wells, Mathew G. (2013-03-05).
2346:is the boundary between colder lower layer (
2096:
1967:
1487:
135:
129:
2757:(EM 1110-2-1607 ed.). Washington, DC:
2166:Chapman, David C.; Graham S. Giese (1990).
1845:Journal of Oceanographical Society of Japan
1832:Hibiya, Toshiyuki; Kinjiro Kajiura (1982).
429:Lakes in seismically active areas, such as
123:
2944:
2930:
2906:"The Legend of the Lake Champlain Monster"
2421:
2294:
2292:
1767:tr. "The fjord swayed from the earthquake"
1230:
1171:Severe weather terminology (United States)
1161: – Non-breaking standing wave pattern
2951:
2644:
2465:
2447:
2398:
2252:
2191:
2109:
2081:
2032:
1980:
1952:
1315:
1233:Handbook of Coastal and Ocean Engineering
2706:
2298:
1708:"M7.6 Kashmir-Kohistan Earthquake, 2005"
1358:
714:
679:Tide-generated internal solitary waves (
628:In Japan, seiches have been observed in
558:, with a height of around 0.5 feet. The
341:
159:
2782:
2289:
2062:Journal of Geophysical Research: Oceans
1817:This behaves in a fashion similar to a
1786:
1129:, and tidal fluctuations is essential.
122:dialect word comes from the Latin word
14:
4193:
3216:one-dimensional Saint-Venant equations
1968:Alfonso-Sosa, Edwin (September 2012).
1522:"Lake Huron Storm Surge July 13, 1995"
1493:
1456:
1424:
1384:
1263:
1235:. World Scientific. pp. 243–286.
1220:. London: John Murray. pp. 21–31.
1212:
580:
394:piled up water along the northwestern
2925:
2830:. Vol. 24 (11th ed.). 1911.
2702:
2700:
2317:
1575:
331:, which varies its surface height at
143:Seiches in harbours can be caused by
72:in an enclosed or partially enclosed
4163:
2299:Chappell, Bill (13 September 2024).
1688:from the original on 21 January 2007
1427:Encyclopedia of Lakes and Reservoirs
1296:
1190: – Tourist village in Argentina
1066:
473:earthquake that hit Lisbon, Portugal
168:
2669:
2646:10.1146/annurev-fluid-122316-045049
2518:10.1146/annurev-fluid-010518-040506
1557:from the original on 2 October 2021
1308:American Society of Civil Engineers
1290:
1177:Severe weather terminology (Canada)
1140:in which it occurs. If an incoming
1003:{\displaystyle \rho _{1},\rho _{2}}
107:The term was promoted by the Swiss
24:
4043:National Oceanographic Data Center
3470:World Ocean Circulation Experiment
3358:Global Ocean Data Analysis Project
2895:Relationship to aquatic "monsters"
2776:
2697:
2141:Parks Canada - Fundy National Park
2097:Alfonso-Sosa, Edwin (April 2014).
1787:Johnson, Scott K. (30 June 2013).
1657:from the original on 20 April 2017
1366:. London: Methuen. §117 (p. 225).
1274:10.1016/b978-0-12-021808-0.50006-1
593:. This results in the flooding of
548:February 27, 2010 Chile earthquake
25:
4227:
3890:Global Sea Level Observing System
2812:
1799:from the original on 30 July 2022
1063:Engineering for seiche protection
918:is the length of the water body,
773:{\displaystyle T={\frac {2L}{c}}}
503:. Seiches were again observed in
4173:
4162:
4153:
4152:
3348:Geochemical Ocean Sections Study
3264:
3253:
2625:Annual Review of Fluid Mechanics
2498:Annual Review of Fluid Mechanics
2137:"The Bay of Fundy's Giant Tides"
1718:from the original on 6 June 2017
1070:
519:as well as in many locations in
43:
4078:Ocean thermal energy conversion
3801:Vine–Matthews–Morley hypothesis
2742:
2612:
2601:from the original on 2019-04-29
2540:
2482:
2415:
2379:Journal of Great Lakes Research
2366:
2357:
2336:
2261:
2228:
2159:
2129:
2118:from the original on 2022-07-30
2090:
2049:
2000:
1989:from the original on 2022-07-30
1961:
1920:
1885:
1825:
1811:
1780:
1756:
1744:from the original on 2014-12-19
1730:
1700:
1669:
1651:USGS Earthquake Hazards Program
1639:
1628:from the original on 2019-01-26
1610:
1576:Brown, Kathryn (10 June 2000).
1569:
1539:
1514:
1450:
1332:from the original on 2017-01-11
1038:
609:moving onshore, giving rise to
560:2010 Sierra El Mayor earthquake
303:
272:is the longest natural period,
140:(dry) descends from the Latin.
1504:University of Minnesota Duluth
1418:
1405:
1378:
1352:
1343:
1303:Origin and generation of waves
1257:
1224:
1206:
1147:levels of high water in Venice
414:, in which the water level at
13:
1:
1494:Korgen, Ben (February 2000).
1435:10.1007/978-1-4020-4410-6_226
1014:of these two same layers and
294:
3338:El Niño–Southern Oscillation
3308:Craik–Leibovich vortex force
3064:Luke's variational principle
2449:10.1371/journal.pone.0057444
2143:. 2017-03-28. Archived from
1894:Geophysical Research Letters
489:2004 Indian Ocean earthquake
7:
2318:Patel, Kasha (2024-09-14).
2111:10.13140/RG.2.2.32105.70242
1982:10.13140/RG.2.2.14561.45929
1457:Pierce, T. (July 5, 2006).
1152:
951:{\displaystyle h_{1},h_{2}}
724:Underwater (internal) waves
532:1950 Assam–Tibet earthquake
386:The effect is similar to a
10:
4232:
3403:Ocean dynamical thermostat
3251:
2556:Limnology and Oceanography
2400:10.1016/j.jglr.2017.05.002
2350:) and warmer upper layer (
1763:Fjorden svinga av skjelvet
1241:10.1142/9789813204027_0011
1101:
1049:Death Valley National Park
26:
4148:
3987:
3961:
3938:Ocean acoustic tomography
3923:
3875:
3814:
3751:Mohorovičić discontinuity
3709:
3581:
3478:
3343:General circulation model
3273:
2979:Benjamin–Feir instability
2959:
2576:10.4319/lo.2005.50.5.1620
1579:"Tsunami! At Lake Tahoe?"
1264:Wilson, Basil W. (1972).
707:in Greenland triggered a
695:in Sri Lanka, and in the
4068:Ocean surface topography
3443:Thermohaline circulation
3433:Subsurface ocean current
3373:Hydrothermal circulation
3206:Wave–current interaction
2984:Boussinesq approximation
2707:Kamphuis, J. W. (2000).
1777:Retrieved on 2011-03-17.
1466:National Weather Service
1200:
1053:7.6-magnitude earthquake
372:National Weather Service
319:The original studies in
4105:Sea surface temperature
4088:Outline of oceanography
3283:Atmospheric circulation
3221:shallow water equations
3211:Waves and shallow water
3104:Significant wave height
2827:Encyclopædia Britannica
2283:10.1126/science.adm9247
1914:10.1029/GL009i012p01305
1020:acceleration of gravity
525:2005 Kashmir earthquake
325:François-Alphonse Forel
286:acceleration of gravity
186:hydrostatic equilibrium
112:François-Alphonse Forel
29:Seiche (disambiguation)
4100:Sea surface microlayer
3465:Wind generated current
2911:The Skeptical Inquirer
1712:Amateur Seismic Centre
1682:Amateur Seismic Centre
1524:. NOAA. Archived from
1385:Merian, J. R. (1828).
1364:Dynamical oceanography
1165:Earthquake engineering
1004:
952:
897:
774:
720:
654:
644:
575:2011 Tōhoku earthquake
461:Good Friday earthquake
367:
366:) on November 14, 2003
259:
165:
136:
130:
124:
3933:Deep scattering layer
3915:World Geodetic System
3423:Princeton Ocean Model
3303:Coriolis–Stokes force
2953:Physical oceanography
2491:"Convection in Lakes"
1714:. Pune. 31 Oct 2008.
1684:. Pune. 22 Feb 2008.
1005:
953:
898:
775:
718:
550:produced a seiche on
453:Northridge earthquake
345:
260:
163:
3953:Underwater acoustics
3513:Perigean spring tide
3378:Langmuir circulation
3089:Rossby-gravity waves
2685:. September 21, 2022
2083:10.1029/2009JC005673
1622:www.soest.hawaii.edu
1110:Saint Petersburg Dam
1051:in the U.S. after a
974:
922:
784:
746:
735:In analogy with the
207:
195:The longest natural
27:For other uses, see
4115:Science On a Sphere
3721:Convergent boundary
3393:Modular Ocean Model
3353:Geostrophic current
3069:Mild-slope equation
2637:2019AnRFM..51..129B
2568:2005LimOc..50.1620B
2510:2019AnRFM..51..189B
2440:2013PLoSO...857444C
2391:2017JGLR...43..689C
2277:(6714): 1196–1205.
2184:1990JPO....20.1459C
2074:2010JGRC..115.3014W
2025:1998JPO....28.2418G
1945:1990JPO....20.1449G
1906:1982GeoRL...9.1305G
1104:Coastal engineering
691:in Palawan Island,
581:Sea and bay seiches
350:, recorded between
3771:Seafloor spreading
3761:Outer trench swell
3726:Divergent boundary
3626:Continental margin
3611:Carbonate platform
3508:Lunitidal interval
2878:2009-08-25 at the
2866:2011-09-28 at the
2254:10.1785/0320240013
2241:The Seismic Record
1857:10.1007/BF02110288
1773:2011-03-18 at the
1551:The New York Times
1082:. You can help by
1000:
948:
893:
770:
721:
552:Lake Pontchartrain
368:
255:
166:
150:infragravity waves
4188:
4187:
4180:Oceans portal
4140:World Ocean Atlas
4130:Underwater glider
4073:Ocean temperature
3736:Hydrothermal vent
3701:Submarine volcano
3636:Continental shelf
3616:Coastal geography
3606:Bathymetric chart
3488:Amphidromic point
3176:Wave nonlinearity
3034:Infragravity wave
2856:Seiche calculator
2720:978-981-02-3830-8
2172:J. Phys. Oceanogr
2104:. pp. 1–16.
2019:(12): 2418–2426.
2013:J. Phys. Oceanogr
1975:. pp. 1–11.
1933:J. Phys. Oceanogr
1900:(12): 1305–1308.
1647:"Seismic Seiches"
1444:978-1-4020-4410-6
1317:10.9753/icce.v1.1
1283:978-0-12-021808-0
1250:978-981-320-401-0
1183:Tsunamis in lakes
1100:
1099:
891:
840:
768:
352:Buffalo, New York
253:
250:
236:
233:
224:
221:
169:Causes and nature
16:(Redirected from
4223:
4178:
4177:
4166:
4165:
4156:
4155:
4095:Pelagic sediment
4033:Marine pollution
3827:Deep ocean water
3696:Submarine canyon
3631:Continental rise
3523:Rule of twelfths
3438:Sverdrup balance
3368:Humboldt Current
3293:Boundary current
3268:
3257:
3074:Radiation stress
3044:Iribarren number
3019:Equatorial waves
2974:Ballantine scale
2969:Airy wave theory
2946:
2939:
2932:
2923:
2922:
2831:
2823:
2808:
2771:
2770:
2768:
2766:
2756:
2751:Tidal Hydraulics
2746:
2740:
2739:
2737:
2735:
2704:
2695:
2694:
2692:
2690:
2673:
2667:
2666:
2648:
2616:
2610:
2609:
2607:
2606:
2600:
2562:(5): 1620–1637.
2553:
2544:
2538:
2537:
2495:
2486:
2480:
2479:
2469:
2451:
2419:
2413:
2412:
2402:
2370:
2364:
2361:
2355:
2340:
2334:
2333:
2331:
2330:
2315:
2309:
2308:
2296:
2287:
2286:
2265:
2259:
2258:
2256:
2232:
2226:
2225:
2223:
2222:
2207:
2198:
2197:
2195:
2178:(9): 1459–1467.
2163:
2157:
2156:
2154:
2152:
2133:
2127:
2126:
2124:
2123:
2113:
2103:
2094:
2088:
2087:
2085:
2053:
2047:
2046:
2036:
2004:
1998:
1997:
1995:
1994:
1984:
1974:
1965:
1959:
1958:
1956:
1939:(9): 1449–1458.
1924:
1918:
1917:
1889:
1883:
1882:
1880:
1879:
1873:
1867:. Archived from
1842:
1829:
1823:
1815:
1809:
1808:
1806:
1804:
1784:
1778:
1760:
1754:
1753:
1751:
1749:
1734:
1728:
1727:
1725:
1723:
1704:
1698:
1697:
1695:
1693:
1673:
1667:
1666:
1664:
1662:
1643:
1637:
1636:
1634:
1633:
1614:
1608:
1607:
1581:
1573:
1567:
1566:
1564:
1562:
1543:
1537:
1536:
1534:
1533:
1518:
1512:
1511:
1506:. Archived from
1500:seagrant.umn.edu
1491:
1485:
1484:
1482:
1480:
1474:
1463:
1454:
1448:
1447:
1422:
1416:
1409:
1403:
1402:
1382:
1376:
1375:
1356:
1350:
1347:
1341:
1340:
1338:
1337:
1319:
1294:
1288:
1287:
1261:
1255:
1254:
1228:
1222:
1221:
1210:
1118:Grand Coulee Dam
1116:and dams (e.g.,
1095:
1092:
1074:
1067:
1009:
1007:
1006:
1001:
999:
998:
986:
985:
957:
955:
954:
949:
947:
946:
934:
933:
902:
900:
899:
894:
892:
890:
889:
888:
876:
875:
865:
864:
863:
854:
853:
843:
841:
839:
838:
829:
828:
827:
815:
814:
804:
796:
795:
779:
777:
776:
771:
769:
764:
756:
687:in Puerto Rico,
659:
657:
649:
647:
599:Saint Petersburg
264:
262:
261:
256:
254:
252:
251:
243:
237:
234:
231:
222:
219:
217:
139:
133:
127:
65:
60:
59:
56:
55:
52:
49:
21:
4231:
4230:
4226:
4225:
4224:
4222:
4221:
4220:
4191:
4190:
4189:
4184:
4172:
4144:
3983:
3957:
3919:
3900:Sea-level curve
3871:
3810:
3796:Transform fault
3746:Mid-ocean ridge
3712:
3705:
3671:Oceanic plateau
3577:
3563:Tidal resonance
3533:Theory of tides
3474:
3383:Longshore drift
3333:Ekman transport
3269:
3263:
3262:
3261:
3260:
3259:
3258:
3249:
3201:Wave turbulence
3134:Trochoidal wave
3059:Longshore drift
2955:
2950:
2917:Geological page
2880:Wayback Machine
2868:Wayback Machine
2818:
2815:
2797:10.2307/1797612
2779:
2777:Further reading
2774:
2764:
2762:
2761:. 15 March 1991
2754:
2748:
2747:
2743:
2733:
2731:
2721:
2705:
2698:
2688:
2686:
2675:
2674:
2670:
2617:
2613:
2604:
2602:
2598:
2551:
2545:
2541:
2493:
2487:
2483:
2420:
2416:
2371:
2367:
2362:
2358:
2341:
2337:
2328:
2326:
2324:Washington Post
2316:
2312:
2297:
2290:
2266:
2262:
2233:
2229:
2220:
2218:
2208:
2201:
2164:
2160:
2150:
2148:
2135:
2134:
2130:
2121:
2119:
2101:
2095:
2091:
2054:
2050:
2005:
2001:
1992:
1990:
1972:
1966:
1962:
1925:
1921:
1890:
1886:
1877:
1875:
1871:
1840:
1834:"Origin of the
1830:
1826:
1816:
1812:
1802:
1800:
1785:
1781:
1775:Wayback Machine
1761:
1757:
1747:
1745:
1736:
1735:
1731:
1721:
1719:
1706:
1705:
1701:
1691:
1689:
1676:
1674:
1670:
1660:
1658:
1645:
1644:
1640:
1631:
1629:
1616:
1615:
1611:
1596:10.2307/4012358
1590:(24): 378–380.
1574:
1570:
1560:
1558:
1545:
1544:
1540:
1531:
1529:
1520:
1519:
1515:
1492:
1488:
1478:
1476:
1475:on May 17, 2008
1472:
1461:
1455:
1451:
1445:
1423:
1419:
1413:Gulf of Finland
1410:
1406:
1383:
1379:
1357:
1353:
1348:
1344:
1335:
1333:
1298:Munk, Walter H.
1295:
1291:
1284:
1262:
1258:
1251:
1229:
1225:
1211:
1207:
1203:
1155:
1106:
1096:
1090:
1087:
1080:needs expansion
1065:
1041:
994:
990:
981:
977:
975:
972:
971:
942:
938:
929:
925:
923:
920:
919:
910:is the natural
884:
880:
871:
867:
866:
859:
855:
849:
845:
844:
842:
834:
830:
823:
819:
810:
806:
805:
803:
791:
787:
785:
782:
781:
757:
755:
747:
744:
743:
726:
693:Trincomalee Bay
689:Puerto Princesa
685:Magueyes Island
651:
641:
623:Venetian Lagoon
583:
544:1819 Allah Bund
499:, and northern
398:shoreline near
392:Hurricane Hazel
306:
297:
242:
238:
218:
216:
208:
205:
204:
171:
63:
46:
42:
35:
32:
23:
22:
15:
12:
11:
5:
4229:
4219:
4218:
4213:
4208:
4203:
4186:
4185:
4183:
4182:
4170:
4160:
4149:
4146:
4145:
4143:
4142:
4137:
4132:
4127:
4122:
4120:Stratification
4117:
4112:
4107:
4102:
4097:
4092:
4091:
4090:
4080:
4075:
4070:
4065:
4060:
4055:
4050:
4045:
4040:
4035:
4030:
4025:
4020:
4012:
4010:Color of water
4007:
4005:Benthic lander
4002:
3997:
3991:
3989:
3985:
3984:
3982:
3981:
3976:
3971:
3965:
3963:
3959:
3958:
3956:
3955:
3950:
3945:
3940:
3935:
3929:
3927:
3921:
3920:
3918:
3917:
3912:
3910:Sea level rise
3907:
3905:Sea level drop
3902:
3897:
3892:
3887:
3881:
3879:
3873:
3872:
3870:
3869:
3864:
3859:
3854:
3849:
3844:
3839:
3834:
3829:
3824:
3818:
3816:
3812:
3811:
3809:
3808:
3803:
3798:
3793:
3788:
3783:
3778:
3773:
3768:
3763:
3758:
3753:
3748:
3743:
3741:Marine geology
3738:
3733:
3728:
3723:
3717:
3715:
3707:
3706:
3704:
3703:
3698:
3693:
3688:
3683:
3681:Passive margin
3678:
3676:Oceanic trench
3673:
3668:
3663:
3658:
3653:
3648:
3643:
3638:
3633:
3628:
3623:
3618:
3613:
3608:
3603:
3598:
3593:
3587:
3585:
3579:
3578:
3576:
3575:
3570:
3565:
3560:
3555:
3550:
3545:
3540:
3535:
3530:
3525:
3520:
3515:
3510:
3505:
3500:
3495:
3490:
3484:
3482:
3476:
3475:
3473:
3472:
3467:
3462:
3457:
3452:
3451:
3450:
3440:
3435:
3430:
3425:
3420:
3415:
3410:
3408:Ocean dynamics
3405:
3400:
3395:
3390:
3385:
3380:
3375:
3370:
3365:
3360:
3355:
3350:
3345:
3340:
3335:
3330:
3325:
3320:
3315:
3310:
3305:
3300:
3298:Coriolis force
3295:
3290:
3285:
3279:
3277:
3271:
3270:
3252:
3250:
3248:
3247:
3246:
3245:
3235:
3230:
3225:
3224:
3223:
3218:
3208:
3203:
3198:
3193:
3188:
3183:
3178:
3173:
3168:
3163:
3158:
3153:
3148:
3147:
3146:
3136:
3131:
3126:
3121:
3119:Stokes problem
3116:
3111:
3106:
3101:
3096:
3091:
3086:
3081:
3076:
3071:
3066:
3061:
3056:
3054:Kinematic wave
3051:
3046:
3041:
3036:
3031:
3026:
3021:
3016:
3011:
3006:
3001:
2996:
2991:
2986:
2981:
2976:
2971:
2965:
2963:
2957:
2956:
2949:
2948:
2941:
2934:
2926:
2920:
2919:
2914:
2903:
2892:
2891:
2886:
2870:
2858:
2853:
2848:
2833:
2832:
2821:"Seiche"
2814:
2813:External links
2811:
2810:
2809:
2778:
2775:
2773:
2772:
2741:
2719:
2696:
2668:
2631:(1): 129–154.
2611:
2539:
2504:(1): 189–215.
2481:
2414:
2385:(4): 689–699.
2365:
2356:
2335:
2310:
2288:
2260:
2247:(3): 172–183.
2227:
2199:
2158:
2128:
2089:
2068:(C3): C03014.
2048:
1999:
1960:
1919:
1884:
1851:(3): 172–182.
1824:
1810:
1779:
1755:
1740:. 2010-04-27.
1729:
1699:
1668:
1638:
1609:
1568:
1538:
1513:
1510:on 2007-12-27.
1486:
1449:
1443:
1417:
1404:
1377:
1351:
1342:
1289:
1282:
1256:
1249:
1223:
1204:
1202:
1199:
1198:
1197:
1191:
1185:
1180:
1174:
1168:
1162:
1154:
1151:
1098:
1097:
1077:
1075:
1064:
1061:
1040:
1037:
997:
993:
989:
984:
980:
960:stratification
945:
941:
937:
932:
928:
904:
903:
887:
883:
879:
874:
870:
862:
858:
852:
848:
837:
833:
826:
822:
818:
813:
809:
802:
799:
794:
790:
767:
763:
760:
754:
751:
737:Merian formula
725:
722:
607:North Atlantic
582:
579:
449:Swimming pools
305:
302:
296:
293:
266:
265:
249:
246:
230:
227:
215:
212:
170:
167:
86:swimming pools
33:
9:
6:
4:
3:
2:
4228:
4217:
4214:
4212:
4209:
4207:
4204:
4202:
4199:
4198:
4196:
4181:
4176:
4171:
4169:
4161:
4159:
4151:
4150:
4147:
4141:
4138:
4136:
4133:
4131:
4128:
4126:
4123:
4121:
4118:
4116:
4113:
4111:
4108:
4106:
4103:
4101:
4098:
4096:
4093:
4089:
4086:
4085:
4084:
4081:
4079:
4076:
4074:
4071:
4069:
4066:
4064:
4061:
4059:
4056:
4054:
4051:
4049:
4046:
4044:
4041:
4039:
4036:
4034:
4031:
4029:
4028:Marine energy
4026:
4024:
4021:
4019:
4018:
4013:
4011:
4008:
4006:
4003:
4001:
3998:
3996:
3995:Acidification
3993:
3992:
3990:
3986:
3980:
3977:
3975:
3972:
3970:
3967:
3966:
3964:
3960:
3954:
3951:
3949:
3948:SOFAR channel
3946:
3944:
3941:
3939:
3936:
3934:
3931:
3930:
3928:
3926:
3922:
3916:
3913:
3911:
3908:
3906:
3903:
3901:
3898:
3896:
3893:
3891:
3888:
3886:
3883:
3882:
3880:
3878:
3874:
3868:
3865:
3863:
3860:
3858:
3855:
3853:
3850:
3848:
3845:
3843:
3840:
3838:
3835:
3833:
3830:
3828:
3825:
3823:
3820:
3819:
3817:
3813:
3807:
3804:
3802:
3799:
3797:
3794:
3792:
3789:
3787:
3784:
3782:
3779:
3777:
3774:
3772:
3769:
3767:
3764:
3762:
3759:
3757:
3756:Oceanic crust
3754:
3752:
3749:
3747:
3744:
3742:
3739:
3737:
3734:
3732:
3731:Fracture zone
3729:
3727:
3724:
3722:
3719:
3718:
3716:
3714:
3708:
3702:
3699:
3697:
3694:
3692:
3689:
3687:
3684:
3682:
3679:
3677:
3674:
3672:
3669:
3667:
3666:Oceanic basin
3664:
3662:
3659:
3657:
3654:
3652:
3649:
3647:
3644:
3642:
3639:
3637:
3634:
3632:
3629:
3627:
3624:
3622:
3619:
3617:
3614:
3612:
3609:
3607:
3604:
3602:
3599:
3597:
3596:Abyssal plain
3594:
3592:
3589:
3588:
3586:
3584:
3580:
3574:
3571:
3569:
3566:
3564:
3561:
3559:
3556:
3554:
3551:
3549:
3546:
3544:
3541:
3539:
3536:
3534:
3531:
3529:
3526:
3524:
3521:
3519:
3516:
3514:
3511:
3509:
3506:
3504:
3503:Internal tide
3501:
3499:
3496:
3494:
3491:
3489:
3486:
3485:
3483:
3481:
3477:
3471:
3468:
3466:
3463:
3461:
3458:
3456:
3453:
3449:
3446:
3445:
3444:
3441:
3439:
3436:
3434:
3431:
3429:
3426:
3424:
3421:
3419:
3416:
3414:
3411:
3409:
3406:
3404:
3401:
3399:
3398:Ocean current
3396:
3394:
3391:
3389:
3386:
3384:
3381:
3379:
3376:
3374:
3371:
3369:
3366:
3364:
3361:
3359:
3356:
3354:
3351:
3349:
3346:
3344:
3341:
3339:
3336:
3334:
3331:
3329:
3326:
3324:
3321:
3319:
3316:
3314:
3311:
3309:
3306:
3304:
3301:
3299:
3296:
3294:
3291:
3289:
3286:
3284:
3281:
3280:
3278:
3276:
3272:
3267:
3256:
3244:
3241:
3240:
3239:
3236:
3234:
3231:
3229:
3226:
3222:
3219:
3217:
3214:
3213:
3212:
3209:
3207:
3204:
3202:
3199:
3197:
3196:Wave shoaling
3194:
3192:
3189:
3187:
3184:
3182:
3179:
3177:
3174:
3172:
3169:
3167:
3164:
3162:
3159:
3157:
3156:Ursell number
3154:
3152:
3149:
3145:
3142:
3141:
3140:
3137:
3135:
3132:
3130:
3127:
3125:
3122:
3120:
3117:
3115:
3112:
3110:
3107:
3105:
3102:
3100:
3097:
3095:
3092:
3090:
3087:
3085:
3082:
3080:
3077:
3075:
3072:
3070:
3067:
3065:
3062:
3060:
3057:
3055:
3052:
3050:
3047:
3045:
3042:
3040:
3039:Internal wave
3037:
3035:
3032:
3030:
3027:
3025:
3022:
3020:
3017:
3015:
3012:
3010:
3007:
3005:
3002:
3000:
2997:
2995:
2992:
2990:
2989:Breaking wave
2987:
2985:
2982:
2980:
2977:
2975:
2972:
2970:
2967:
2966:
2964:
2962:
2958:
2954:
2947:
2942:
2940:
2935:
2933:
2928:
2927:
2924:
2918:
2915:
2913:
2912:
2907:
2904:
2902:
2899:
2898:
2897:
2896:
2890:
2887:
2885:
2881:
2877:
2874:
2871:
2869:
2865:
2862:
2859:
2857:
2854:
2852:
2849:
2847:
2845:
2840:
2839:
2838:
2837:
2829:
2828:
2822:
2817:
2816:
2806:
2802:
2798:
2794:
2790:
2786:
2781:
2780:
2760:
2753:
2752:
2745:
2730:
2726:
2722:
2716:
2712:
2711:
2703:
2701:
2689:September 22,
2684:
2683:
2678:
2672:
2664:
2660:
2656:
2652:
2647:
2642:
2638:
2634:
2630:
2626:
2622:
2615:
2597:
2593:
2589:
2585:
2581:
2577:
2573:
2569:
2565:
2561:
2557:
2550:
2543:
2535:
2531:
2527:
2523:
2519:
2515:
2511:
2507:
2503:
2499:
2492:
2485:
2477:
2473:
2468:
2463:
2459:
2455:
2450:
2445:
2441:
2437:
2434:(3): e57444.
2433:
2429:
2425:
2418:
2410:
2406:
2401:
2396:
2392:
2388:
2384:
2380:
2376:
2369:
2360:
2353:
2349:
2345:
2339:
2325:
2321:
2314:
2306:
2302:
2295:
2293:
2284:
2280:
2276:
2272:
2264:
2255:
2250:
2246:
2242:
2238:
2231:
2217:
2213:
2206:
2204:
2194:
2189:
2185:
2181:
2177:
2173:
2169:
2162:
2147:on 2016-03-04
2146:
2142:
2138:
2132:
2117:
2112:
2107:
2100:
2093:
2084:
2079:
2075:
2071:
2067:
2063:
2059:
2052:
2044:
2040:
2035:
2030:
2026:
2022:
2018:
2014:
2010:
2003:
1988:
1983:
1978:
1971:
1964:
1955:
1950:
1946:
1942:
1938:
1934:
1930:
1923:
1915:
1911:
1907:
1903:
1899:
1895:
1888:
1874:on 2011-05-27
1870:
1866:
1862:
1858:
1854:
1850:
1846:
1839:
1837:
1828:
1820:
1814:
1798:
1794:
1790:
1783:
1776:
1772:
1768:
1764:
1759:
1743:
1739:
1733:
1717:
1713:
1709:
1703:
1687:
1683:
1679:
1672:
1656:
1652:
1648:
1642:
1627:
1623:
1619:
1613:
1605:
1601:
1597:
1593:
1589:
1585:
1580:
1572:
1556:
1552:
1548:
1542:
1528:on 2008-09-16
1527:
1523:
1517:
1509:
1505:
1501:
1497:
1490:
1471:
1467:
1460:
1453:
1446:
1440:
1436:
1432:
1428:
1421:
1414:
1408:
1400:
1396:
1392:
1388:
1381:
1373:
1369:
1365:
1361:
1355:
1346:
1331:
1327:
1323:
1318:
1313:
1309:
1305:
1304:
1299:
1293:
1285:
1279:
1275:
1271:
1267:
1260:
1252:
1246:
1242:
1238:
1234:
1227:
1219:
1215:
1214:Darwin, G. H.
1209:
1205:
1195:
1192:
1189:
1188:Villa Epecuén
1186:
1184:
1181:
1178:
1175:
1172:
1169:
1166:
1163:
1160:
1157:
1156:
1150:
1148:
1143:
1139:
1135:
1130:
1128:
1123:
1119:
1115:
1111:
1105:
1094:
1085:
1081:
1078:This section
1076:
1073:
1069:
1068:
1060:
1058:
1054:
1050:
1046:
1036:
1033:
1028:
1023:
1021:
1017:
1013:
995:
991:
987:
982:
978:
969:
965:
961:
943:
939:
935:
930:
926:
917:
913:
909:
885:
881:
877:
872:
868:
860:
856:
850:
846:
835:
831:
824:
820:
816:
811:
807:
800:
797:
792:
788:
765:
761:
758:
752:
749:
742:
741:
740:
738:
733:
731:
717:
713:
710:
706:
705:Dickson Fjord
701:
698:
694:
690:
686:
682:
677:
674:
670:
666:
663:On occasion,
661:
656:
646:
639:
635:
631:
626:
624:
620:
616:
612:
608:
604:
600:
596:
592:
588:
578:
576:
573:, during the
572:
568:
563:
561:
557:
553:
549:
545:
541:
538:and southern
537:
533:
528:
526:
522:
518:
514:
510:
506:
505:Uttar Pradesh
502:
498:
494:
490:
486:
482:
478:
474:
470:
466:
462:
458:
454:
450:
446:
442:
440:
436:
432:
427:
425:
421:
420:Lake Michigan
417:
413:
408:
407:Lake Superior
403:
401:
397:
393:
389:
384:
382:
377:
373:
365:
361:
357:
353:
349:
344:
340:
338:
334:
330:
329:Lake Wakatipu
326:
322:
317:
315:
311:
301:
300:frequencies.
292:
289:
287:
283:
279:
275:
271:
247:
244:
228:
225:
213:
210:
203:
202:
201:
198:
193:
189:
187:
183:
179:
174:
162:
158:
156:
152:
151:
146:
141:
138:
132:
126:
121:
117:
113:
110:
105:
103:
99:
95:
91:
87:
83:
79:
75:
74:body of water
71:
70:standing wave
67:
66:
58:
40:
30:
19:
4135:Water column
4083:Oceanography
4058:Observations
4053:Explorations
4023:Marginal sea
4016:
3974:OSTM/Jason-2
3806:Volcanic arc
3781:Slab suction
3498:Head of tide
3388:Loop Current
3328:Ekman spiral
3114:Stokes drift
3098:
3024:Gravity wave
2999:Cnoidal wave
2909:
2901:The Unmuseum
2894:
2893:
2843:
2835:
2834:
2825:
2788:
2784:
2763:. Retrieved
2750:
2744:
2732:. Retrieved
2709:
2687:. Retrieved
2680:
2671:
2628:
2624:
2614:
2603:. Retrieved
2559:
2555:
2542:
2501:
2497:
2484:
2431:
2427:
2417:
2382:
2378:
2368:
2359:
2338:
2327:. Retrieved
2323:
2313:
2304:
2274:
2270:
2263:
2244:
2240:
2230:
2219:. Retrieved
2216:Ars Technica
2215:
2175:
2171:
2161:
2149:. Retrieved
2145:the original
2140:
2131:
2120:. Retrieved
2092:
2065:
2061:
2051:
2016:
2012:
2002:
1991:. Retrieved
1963:
1936:
1932:
1922:
1897:
1893:
1887:
1876:. Retrieved
1869:the original
1848:
1844:
1835:
1827:
1813:
1801:. Retrieved
1793:Ars Technica
1792:
1782:
1766:
1758:
1746:. Retrieved
1732:
1720:. Retrieved
1711:
1702:
1690:. Retrieved
1681:
1671:
1659:. Retrieved
1650:
1641:
1630:. Retrieved
1621:
1612:
1587:
1584:Science News
1583:
1571:
1559:. Retrieved
1550:
1541:
1530:. Retrieved
1526:the original
1516:
1508:the original
1499:
1489:
1477:. Retrieved
1470:the original
1452:
1426:
1420:
1407:
1390:
1386:
1380:
1363:
1360:Proudman, J.
1354:
1345:
1334:. Retrieved
1302:
1292:
1265:
1259:
1232:
1226:
1217:
1208:
1131:
1127:storm surges
1107:
1088:
1084:adding to it
1079:
1055:hit western
1042:
1039:Cave seiches
1024:
1015:
915:
907:
905:
734:
727:
702:
697:Bay of Fundy
678:
662:
630:Nagasaki Bay
627:
619:MOSE Project
613:lows on the
587:Adriatic Sea
584:
567:Sognefjorden
564:
529:
443:
428:
426:waterfront.
404:
396:Lake Ontario
385:
369:
363:
360:Toledo, Ohio
355:
318:
312:, bays, and
307:
304:Lake seiches
298:
290:
281:
277:
273:
269:
267:
194:
190:
175:
172:
148:
144:
142:
120:Swiss French
106:
38:
36:
4211:Water waves
4125:Thermocline
3842:Mesopelagic
3815:Ocean zones
3786:Slab window
3651:Hydrography
3591:Abyssal fan
3558:Tidal range
3548:Tidal power
3543:Tidal force
3428:Rip current
3363:Gulf Stream
3323:Ekman layer
3313:Downwelling
3288:Baroclinity
3275:Circulation
3171:Wave height
3161:Wave action
3144:megatsunami
3124:Stokes wave
3084:Rossby wave
3049:Kelvin wave
3029:Green's law
2791:: 271–275.
2348:hypolimnion
2344:thermocline
1045:Devils Hole
1027:thermocline
968:hypolimnion
780:with
730:thermocline
709:megatsunami
523:during the
513:West Bengal
469:Puerto Rico
388:storm surge
321:Lake Geneva
145:long-period
116:Lake Geneva
109:hydrologist
4195:Categories
4063:Reanalysis
3962:Satellites
3943:Sofar bomb
3791:Subduction
3766:Ridge push
3661:Ocean bank
3641:Contourite
3568:Tide gauge
3553:Tidal race
3538:Tidal bore
3528:Slack tide
3493:Earth tide
3413:Ocean gyre
3233:Wind setup
3228:Wind fetch
3191:Wave setup
3186:Wave radar
3181:Wave power
3079:Rogue wave
3009:Dispersion
2842:What is a
2605:2020-09-06
2352:epilimnion
2329:2024-09-15
2221:2024-09-15
2122:2022-07-30
1993:2022-07-30
1878:2009-02-26
1819:tidal bore
1748:17 October
1632:2019-03-12
1532:2009-03-13
1336:2017-04-19
1194:Vajont Dam
1142:wave train
1114:reservoirs
1102:See also:
964:epilimnion
650:, from 網引き
615:Baltic Sea
603:Neva River
591:Baltic Sea
577:in Japan.
521:Bangladesh
509:Tamil Nadu
493:Bangladesh
457:California
445:Earthquake
435:California
431:Lake Tahoe
416:Port Huron
412:Lake Huron
333:Queenstown
295:Occurrence
155:wind waves
82:reservoirs
4201:Limnology
3925:Acoustics
3877:Sea level
3776:Slab pull
3713:tectonics
3621:Cold seep
3583:Landforms
3460:Whirlpool
3455:Upwelling
3238:Wind wave
3166:Wave base
3094:Sea state
3014:Edge wave
3004:Cross sea
2663:126363796
2655:0066-4189
2584:0024-3590
2534:125132769
2526:0066-4189
2458:1932-6203
2409:0380-1330
1865:198197231
1561:2 October
1479:April 19,
1372:223124129
1326:2156-1028
1091:June 2008
1012:densities
992:ρ
979:ρ
832:ρ
821:ρ
817:−
808:ρ
556:Louisiana
479:, and in
463:that hit
376:Lake Erie
348:Lake Erie
337:North Sea
314:estuaries
4158:Category
4110:Seawater
3837:Littoral
3832:Deep sea
3691:Seamount
3573:Tideline
3518:Rip tide
3448:shutdown
3418:Overflow
3151:Undertow
2994:Clapotis
2876:Archived
2864:Archived
2765:2 August
2734:2 August
2729:45698321
2682:BNO News
2596:Archived
2592:55292327
2476:23472085
2428:PLOS ONE
2116:Archived
2043:55974279
1987:Archived
1803:18 April
1797:Archived
1771:Archived
1742:Archived
1722:19 April
1716:Archived
1692:19 April
1686:Archived
1661:19 April
1655:Archived
1626:Archived
1618:"Seiche"
1555:Archived
1399:46229431
1362:(1953).
1330:Archived
1300:(1950).
1216:(1898).
1159:Clapotis
1153:See also
1122:Wetlands
681:solitons
673:Hilo Bay
665:tsunamis
611:cyclonic
589:and the
501:Thailand
477:Scotland
310:Harbours
178:tsunamis
4168:Commons
4038:Mooring
3988:Related
3979:Jason-3
3969:Jason-1
3852:Pelagic
3847:Oceanic
3822:Benthic
3139:Tsunami
3109:Soliton
2836:General
2805:1797612
2633:Bibcode
2564:Bibcode
2506:Bibcode
2467:3589419
2436:Bibcode
2387:Bibcode
2271:Science
2180:Bibcode
2151:9 April
2070:Bibcode
2021:Bibcode
1941:Bibcode
1902:Bibcode
1604:4012358
1266:Seiches
1032:benthic
1025:As the
655:amibiki
540:England
424:Chicago
400:Toronto
182:Gravity
94:harbors
68:) is a
18:Seiches
3857:Photic
3686:Seabed
3099:Seiche
2844:seiche
2803:
2727:
2717:
2661:
2653:
2590:
2582:
2532:
2524:
2474:
2464:
2456:
2407:
2041:
1863:
1822:level.
1602:
1441:
1397:
1370:
1324:
1280:
1247:
1134:period
1057:Mexico
962:(e.g.
912:period
906:where
669:Hawaii
638:period
634:Kyushu
595:Venice
571:Norway
536:Norway
487:. The
485:Sweden
481:canals
471:. The
465:Alaska
439:Nevada
358:) and
268:where
235:
232:
223:
220:
197:period
125:siccus
100:, and
39:seiche
4216:Water
4206:Flood
4048:Ocean
4017:Alvin
3867:Swash
3711:Plate
3656:Knoll
3646:Guyot
3601:Atoll
3480:Tides
3243:model
3129:Swell
2961:Waves
2882:from
2801:JSTOR
2759:USACE
2755:(PDF)
2659:S2CID
2599:(PDF)
2588:S2CID
2552:(PDF)
2530:S2CID
2494:(PDF)
2102:(PDF)
2039:S2CID
1973:(PDF)
1872:(PDF)
1861:S2CID
1841:(PDF)
1836:Abiki
1600:JSTOR
1473:(PDF)
1462:(PDF)
1389:[
1201:Notes
1138:basin
645:abiki
517:India
497:Nepal
381:fetch
137:sèche
98:caves
78:lakes
64:SAYSH
4015:DSV
4000:Argo
3862:Surf
3318:Eddy
2884:NOAA
2767:2024
2736:2024
2725:OCLC
2715:ISBN
2691:2022
2651:ISSN
2580:ISSN
2522:ISSN
2472:PMID
2454:ISSN
2405:ISSN
2342:The
2153:2018
1805:2019
1750:2014
1724:2017
1694:2017
1663:2017
1563:2021
1481:2017
1439:ISBN
1395:OCLC
1368:OCLC
1322:ISSN
1278:ISBN
1245:ISBN
1132:The
1018:the
1010:the
966:and
597:and
530:The
511:and
370:The
364:blue
284:the
276:and
102:seas
90:bays
2908:in
2793:doi
2641:doi
2572:doi
2514:doi
2462:PMC
2444:doi
2395:doi
2305:NPR
2279:doi
2275:385
2249:doi
2188:doi
2106:doi
2078:doi
2066:115
2029:doi
1977:doi
1949:doi
1910:doi
1853:doi
1592:doi
1588:157
1431:doi
1312:doi
1270:doi
1237:doi
1112:),
1086:.
1047:at
970:),
515:in
483:in
455:in
433:in
356:red
323:by
147:or
134:or
131:sec
4197::
2824:.
2799:.
2787:.
2723:.
2699:^
2679:.
2657:.
2649:.
2639:.
2629:51
2627:.
2623:.
2594:.
2586:.
2578:.
2570:.
2560:50
2558:.
2554:.
2528:.
2520:.
2512:.
2502:51
2500:.
2496:.
2470:.
2460:.
2452:.
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2430:.
2426:.
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2354:).
2322:.
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2015:.
2011:.
1985:.
1947:.
1937:20
1935:.
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914:,
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625:.
569:,
554:,
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288:.
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96:,
92:,
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878:+
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