Tidal bore

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Water wave traveling up a river or narrow bay because of an incoming tide

title: "Tidal bore" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["tidal-bores", "fluid-dynamics", "wave-mechanics", "river-surfing", "articles-containing-video-clips"] description: "Water wave traveling up a river or narrow bay because of an incoming tide" topic_path: "general/tidal-bores" source: "https://en.wikipedia.org/wiki/Tidal_bore" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Water wave traveling up a river or narrow bay because of an incoming tide ::

::figure[src="https://upload.wikimedia.org/wikipedia/commons/4/48/Tidal_Bore_-geograph.org.uk-_324581.jpg" caption="A bore in [[Morecambe Bay]], in the [[United Kingdom]]" alt=""] ::

::figure[src="https://upload.wikimedia.org/wikipedia/commons/3/3e/Arnside_bore.ogv" caption="Video of the [[Arnside Bore]], in the United Kingdom"] ::

::figure[src="https://upload.wikimedia.org/wikipedia/commons/3/32/Turnagain-bore.jpg" caption="The tidal bore in Upper [[Cook Inlet]], in [[Alaska"] ::

A tidal bore, often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current. It is a strong tide that pushes up the river, against the current.

{{Anchor|Whelp}} Description==

Bores occur in relatively few locations worldwide, usually in areas with a large tidal range (typically more than 6 m between high and low tide) and where incoming tides are funneled into a shallow, narrowing river or lake via a broad bay. The funnel-like shape not only increases the tidal range, but it can also decrease the duration of the flood tide, down to a point where the flood appears as a sudden increase in the water level. A tidal bore takes place during the flood tide and never during the ebb tide.

::figure[src="https://upload.wikimedia.org/wikipedia/commons/b/b4/Undular_bore_Araguari_River-Brazil-USGS-bws00026.jpg" caption="url=https://pubs.er.usgs.gov/#search:advance/page=1/page_size=100/advance=undefined/series_cd=CIR/report_number=1022:0}}"] ::

A tidal bore may take on various forms, ranging from a single breaking wavefront with a rollersomewhat like a hydraulic jump⁠to undular bores, comprising a smooth wavefront followed by a train of secondary waves known as whelps. Large bores can be particularly unsafe for shipping but also present opportunities for river surfing.

Two key features of a tidal bore are the intense turbulence and turbulent mixing generated during the bore propagation, as well as its rumbling noise. The visual observations of tidal bores highlight the turbulent nature of the surging waters. The tidal bore induces a strong turbulent mixing in the estuarine zone, and the effects may be felt along considerable distances. The velocity observations indicate a rapid deceleration of the flow associated with the passage of the bore as well as large velocity fluctuations. A tidal bore creates a powerful roar that combines the sounds caused by the turbulence in the bore front and whelps, entrained air bubbles in the bore roller, sediment erosion beneath the bore front and of the banks, scouring of shoals and bars, and impacts on obstacles. The bore rumble is heard far away because its low frequencies can travel over long distances. The low-frequency sound is a characteristic feature of the advancing roller in which the air bubbles entrapped in the large-scale eddies are acoustically active and play the dominant role in the rumble-sound generation.

Etymology

The word bore derives through Old English from the Old Norse word bára, meaning "wave" or "swell."

Effects

Tidal bores can be dangerous. Certain rivers such as the Seine in France, the Petitcodiac River in Canada, and the Colorado River in Mexico to name a few, have had a sinister reputation in association with tidal bores. In China, despite warning signs erected along the banks of the Qiantang River, a number of fatalities occur each year by people who take too much risk with the bore. The tidal bores affect the shipping and navigation in the estuarine zone, for example, in Papua New Guinea (in the Fly and Bamu Rivers), Malaysia (the Benak in the Batang Lupar), and India (the Hooghly River bore).

On the other hand, tidal bore-affected estuaries are rich feeding zones and breeding grounds of several forms of wildlife. The estuarine zones are the spawning and breeding grounds of several native fish species, while the aeration induced by the tidal bore contributes to the abundant growth of many species of fish and shrimp (for example in the Rokan River, Indonesia). The tidal bores also provide opportunity for recreational inland surfing, such as the Seven Ghosts bore on the Kampar River, Indonesia or the Severn Bore on the River Severn, England.

Scientific studies

Scientific studies have been carried out at the River Dee in Wales in the United Kingdom, the Garonne and Sélune in France, the Daly River in Australia, and the Qiantang River estuary in China. The force of the tidal bore flow often poses a challenge to scientific measurements, as evidenced by a number of field work incidents in the River Dee, Rio Mearim, Daly River, and Sélune River. In terms of physical modelling (hydrodynamics), a tidal bore often well represented by a soliton.

Rivers and bays with tidal bores

Rivers and bays that have been known to exhibit bores include those listed below.

Asia

::figure[src="https://upload.wikimedia.org/wikipedia/commons/4/49/20240921钱江潮冲上之江路.png" caption="The [[Qiantang River]] tidal bore overwhelming local infrastructure in 2024"] ::

Oceania

Australia

New Zealand

Papua New Guinea

Europe

Ireland

United Kingdom

::figure[src="https://upload.wikimedia.org/wikipedia/commons/9/92/Trent_Aegir_2.JPG" caption="The Trent Aegir seen from West Stockwith, [[Nottinghamshire]], 20 September 2005"] ::

::figure[src="https://upload.wikimedia.org/wikipedia/commons/4/46/Trent_Aegir_3.JPG" caption="The Trent Aegir at [[Gainsborough, Lincolnshire]], 20 September 2005"] ::

Belgium

France

The phenomenon is generally named un mascaret in French. but some other local names are preferred.

North America

United States

::figure[src="https://upload.wikimedia.org/wikipedia/commons/a/ab/Tidal_bore.jpg" caption="Tidal bore on the [[Petitcodiac River"] ::

  • The Turnagain Arm of Cook Inlet, Alaska. Up to 2 m and 20 km/h.
  • Historically, the Colorado River had a tidal bore up to 6 feet, that extended 47 miles up river.
  • The Savannah River up to 10 mi inland.
  • Small tidal bores, only a few inches in height, have been observed advancing up tidal bayous on the Mississippi Gulf Coast.
  • The bay inlet of the Crissy Field Marsh, in San Francisco, California, can exhibit tidal bores near high tide.

Canada

With the Bay of Fundy having the highest tidal range in the world, most rivers draining into the upper bay between Nova Scotia and New Brunswick have significant tidal bores. They include:

  • The Petitcodiac River formerly had the highest bore in North America at over 2 m in height, but causeway construction between Moncton and Riverview in the 1960s led to subsequent extensive sedimentation which reduced the bore to little more than a ripple. After considerable political controversy, the causeway gates were opened on April 14, 2010, as part of the Petitcodiac River Restoration Project and the tidal bore began to grow again. The restoration of the bore has been sufficient that in July 2013, professional surfers rode a 1 m-high wave 29 km up the Petitcodiac River from Belliveau Village to Moncton to establish a new North American record for continuous surfing.
  • The Shubenacadie River in Nova Scotia. When the tidal bore approaches, completely drained riverbeds are filled. It has caused the deaths of several tourists who were in the riverbeds when the bore came in. Tour boat operators offer rafting excursions in the summer.
  • The bore is fastest and highest on some of the smaller rivers that connect to the bay including the River Hebert and Maccan River on the Cumberland Basin, the St. Croix and Kennetcook rivers in the Minas Basin, and the Salmon River in Truro.

Mexico

Historically, there was a tidal bore on the Gulf of California in Mexico at the mouth of the Colorado River. It formed in the estuary about Montague Island and propagated upstream. It was once very strong, but diversions of the river for irrigation have weakened the flow of the river to the point the tidal bore has nearly disappeared.

South America

Brazil

  • Amazon River in Brazil, up to 4 m high, running at up to 13 mph. It is known locally as the pororoca.
  • Mearim River in Brazil
  • Araguari River in Brazil. Very strong in the past, it is considered lost since 2015, due to buffaloes farming, irrigation, and dam construction along the river, leading to substantial loss of water flow.

Venezuela

Chile

Lakes with tidal bores

Lakes with an ocean inlet can also exhibit tidal bores.

North America

  • Nitinat Lake on Vancouver Island has a sometimes dangerous tidal bore at Nitinat Narrows where the lake meets the Pacific Ocean. The lake is popular with windsurfers due to its consistent winds.

References

References

  1. Sometimes also known as an '''aegir''', '''eagre''', or '''eygre''' in the context of specific instances in Britain.
  2. Chanson, H.. (2011). "Tidal Bores, Aegir, Eagre, Mascaret, Pororoca. Theory and Observations". World Scientific, Singapore.
  3. (1988). "Catalog of worldwide tidal bore occurrences and characteristics". [[United States Geological Survey.
  4. Chanson, H.. (2012). "Momentum considerations in hydraulic jumps and bores". ASCE.
  5. Chanson, H.. (2009). "Current Knowledge In Hydraulic Jumps And Related Phenomena. A Survey of Experimental Results". European Journal of Mechanics B.
  6. Chanson, H.. (2009). "Environmental, Ecological and Cultural Impacts of Tidal Bores, Benaks, Bonos and Burros". Proc. International Workshop on Environmental Hydraulics IWEH09, Theoretical, Experimental and Computational Solutions, Valencia, Spain, 29–30 October Editor P.A. Lopez-Jimenez et al., Invited keynote lecture, 20 pp. (CD-ROM).
  7. Koch, C. and [[Hubert Chanson. (2008). "Turbulent Mixing beneath an Undular Bore Front". Journal of Coastal Research.
  8. Koch, C. and [[Hubert Chanson. (2009). "Turbulence Measurements in Positive Surges and Bores". Journal of Hydraulic Research.
  9. Chanson, H.. (2009). "The Rumble Sound Generated by a Tidal Bore Event in the Baie du Mont Saint Michel". [[Journal of the Acoustical Society of America]].
  10. Simpson, J.H., Fisher, N.R., and Wiles, P.. (2004). "Reynolds Stress and TKE Production in an Estuary with a Tidal Bore". [[Estuarine, Coastal and Shelf Science]].
  11. [[Hubert Chanson. (2010). "Turbulence and Sediment Processes in the Tidal Bore of the Garonne River: First Observations". Hydraulic Model Report No. CH79/10, School of Civil Engineering, The University of Queensland, Brisbane, Australia, 97 pp..
  12. Simon, B., Lubin, P., Reungoat, D., [[Hubert Chanson. (2011). "Turbulence Measurements in the Garonne River Tidal Bore: First Observations". Proc. 34th IAHR World Congress, Brisbane, Australia, 26 June–1 July, Engineers Australia Publication, Eric Valentine, Colin Apelt, James Ball, [[Hubert Chanson]], Ron Cox, Rob Ettema, George Kuczera, Martin Lambert, Bruce Melville and Jane Sargison Editors, pp. 1141–48.
  13. [[Hubert Chanson. (2012). "High-Frequency Turbulence and Suspended Sediment Concentration Measurements in the Garonne River Tidal Bore". Estuarine, Coastal and Shelf Science.
  14. Reungoat, D., [[Hubert Chanson. (2014). "Sediment Processes and Flow Reversal in the Undular Tidal Bore of the Garonne River (France)". [[Environmental Fluid Mechanics]].
  15. Reungoat, D., [[Hubert Chanson. (2014). "Turbulence, Sedimentary Processes and Tidal Bore Collision in the Arcins Channel, Garonne River (October 2013)". Hydraulic Model Report No. CH94/14, School of Civil Engineering, the University of Queensland, Brisbane, Australia, 145 Pp..
  16. Mouazé, D., [[Hubert Chanson. (2010). "Field Measurements in the Tidal Bore of the Sélune River in the Bay of Mont Saint Michel (September 2010)". Hydraulic Model Report No. CH81/10, School of Civil Engineering, The University of Queensland, Brisbane, Australia, 72 pp..
  17. Wolanski, E., Williams, D., Spagnol, S., and [[Hubert Chanson. (2004). "Undular Tidal Bore Dynamics in the Daly Estuary, Northern Australia". Estuarine, Coastal and Shelf Science.
  18. (July 2019). "Real-time characteristics of tidal bore propagation in the Qiantang River Estuary, China, recorded by marine radar". Elsevier.
  19. Chanson, H.. (2008). "Photographic Observations of Tidal Bores (Mascarets) in France". Hydraulic Model Report No. CH71/08, Univ. of Queensland, Australia, 104 pp..
  20. Ryan Novitra. (February 3, 2017). "Riau to Introduce Bono Wave to International Tourism".
  21. (18 March 1914). "Wairoa Tidal Bore". New Zealand Herald.
  22. p. 159, Barrie R. Bolton. 2009. ''The Fly River, Papua New Guinea: Environmental Studies in an Impacted Tropical River System.'' Elsevier Science. {{ISBN. 978-0444529640.
  23. {{in lang. fr [http://www.cnrtl.fr/lexicographie/mascaret definition of mascaret]
  24. [https://www.cbc.ca/news/canada/new-brunswick/petitcodiac-river-changing-faster-than-expected-1.944296 Petitcodiac River changing faster than expected]
  25. "Surf's Up -- in Canada! Small New Brunswick Town Becomes International Surfing Hotspot".
  26. [http://ojs.library.dal.ca/NSM/article/view/3753 ''Natural History of Nova Scotia'' Vol. I, Chap. T "Ocean Currents", p. 109 ]
  27. {{in lang. en [http://fogonazos.blogspot.com/2007/03/pororoca-surfing-amazon.html "Pororoca: surfing the Amazon"] indicates that "The record that we could find for surfing the longest distance on the Pororoca was set by Picuruta Salazar, a Brazilian surfer who, in 2003, managed to ride the wave for 37 minutes and travel {{convert. 12.5. km. mi. 1

::callout[type=info title="Wikipedia Source"] This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page. ::

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