Atidal bore,[1] often simply given asbore in context, is atidal 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.
Bores occur in relatively few locations worldwide, usually in areas with a large tidal range (typically more than 6 meters (20 ft) between high and low tide) and where incoming tides are funneled into a shallow, narrowing river or lake via a broad bay.[2] The funnel-like shape not only increases the tidal range, but it can also decrease the duration of theflood 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 theebb tide.
Undular bore and whelps near the mouth ofAraguari River in northeastern Brazil. The view is oblique towards the mouth from airplane at approximately 30 m (100 ft) altitude.[3]
A tidal bore may take on various forms, ranging from a single breaking wavefront with aroller —somewhat like ahydraulic jump[4][5]—toundular bores, comprising a smooth wavefront followed by a train of secondarywaves known aswhelps.[6] Large bores can be particularly unsafe for shipping but also present opportunities forriver surfing.[6]
Two key features of a tidal bore are the intense turbulence andturbulent 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.[7][8] 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.[9]
Tidal bores can be dangerous. Certain rivers such as theSeine inFrance, thePetitcodiac River inCanada, and theColorado River inMexico to name a few, have had a sinister reputation in association with tidal bores. In China, despite warning signs erected along the banks of theQiantang River, a number of fatalities occur each year by people who take too much risk with the bore.[2] The tidal bores affect the shipping and navigation in the estuarine zone, for example, inPapua New Guinea (in theFly andBamu Rivers),Malaysia (the Benak in theBatang Lupar), andIndia (theHooghly River bore).
On the other hand, tidal bore-affectedestuaries are rich feeding zones and breeding grounds of several forms of wildlife.[2] The estuarine zones are the spawning and breeding grounds of several nativefish species, while theaeration induced by the tidal bore contributes to the abundant growth of many species of fish andshrimp (for example in theRokan River,Indonesia). The tidal bores also provide opportunity for recreational inlandsurfing, such as the Seven Ghosts bore on theKampar River,Indonesia.
Scientific studies have been carried out at theRiver Dee[10] in Wales in the United Kingdom, theGaronne[11][12][13][14][15] andSélune[16] in France, theDaly River[17] in Australia, and theQiantang River estuary[18] 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,[10] Rio Mearim, Daly River,[17] and Sélune River.[16]
Qiantang River,China, which has the world's largest bore,[2][18] up to 9 m (30 ft) high, traveling at up to 40 km/h (25 mph)
Batang Lupar or Lupar River, nearSri Aman,Malaysia. The tidal bore is locally known asbenak.[6]
Batang Sadong or Sadong River, Sarawak, Malaysia.
Bono,Kampar River, at Meranti Bay, Pelalawan,Indonesia. The phenomenon is feared by the locals to sink ships.[citation needed] It is reported to break up to 130 km (81 mi) inland, but usually up to 40 km (25 mi) with 6 m (20 ft) height.[20]
River Mersey. The second highest tidal bore after the Severn bore, up to 1.7 meters (6 ft) high. The bore tends to form around theManchester Ship Canal.
ThePetitcodiac River formerly had the highest bore in North America at over 2 metres (6.6 ft) in height, butcauseway construction betweenMoncton andRiverview 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.[24] The restoration of the bore has been sufficient that in July 2013, professional surfers rode a 1 metre (3.3 ft)-high wave 29 kilometres (18.0 mi) up the Petitcodiac River from Belliveau Village toMoncton to establish a new North American record for continuous surfing.[25]
TheShubenacadie 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.[citation needed]Tour boat operators offer rafting excursions in the summer.
Historically, there was a tidal bore on theGulf of California in Mexico at the mouth of theColorado River. It formed in the estuary aboutMontague 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.
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.
Nitinat Lake onVancouver 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.
^abSimpson, 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.60 (4):619–27.Bibcode:2004ECSS...60..619S.doi:10.1016/j.ecss.2004.03.006.during this […] deployment, the [ADCP] instrument was repeatedly buried in sediment after the 1st tidal cycle and had to be dug out of the sediment, with considerable difficulty, at the time of recovery.{{cite journal}}: CS1 maint: multiple names: authors list (link)
^"Wairoa Tidal Bore".New Zealand Herald. No. 15560. 18 March 1914. Retrieved25 November 2024.
^p. 159, Barrie R. Bolton. 2009.The Fly River, Papua New Guinea: Environmental Studies in an Impacted Tropical River System. Elsevier Science.ISBN978-0444529640.
^(in English)"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 12.5 kilometers (7.8 mi)."
