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Tidal bore

Tidal bore is a physics topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Tidal bore rather than just read about it. In short: 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.

Tidal bore — main illustration
Tidal bore — illustration

Key takeaways

  • Tidal bore belongs to physics; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Tidal bore to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Tidal bore from memory before moving on to harder problems.

Reference excerpt

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.

Description 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. 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.

A tidal bore may take on various forms, ranging from a single breaking wavefront with a roller — somewhat like a hydraulic jump⁠— to 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

Ganges–Brahmaputra, India and Bangladesh Indus River, India and Pakistan Sittaung River, Burma Qiantang River, China, which has the world's largest bore, up to 9 m (30 ft) high, traveling at up to 40 km/h (25 mph) Batang Lupar or Lupar River, near Sri Aman, Malaysia. The tidal bore is locally known as benak. 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. 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.

Oceania

Australia Styx River, Queensland Daly River, Northern Territory

New Zealand Wairoa River, Northland Region

Papua New Guinea Fly River Turama River

Europe

Ireland River Shannon, up the Shannon Estuary to Limerick, Ireland: 21 September 2013

United Kingdom

River Dee, Wales and England 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 the Manchester Ship Canal. The Severn bore on the River Severn, Wales and England, up to 2 meters (7 ft) high The Trent Aegir on the River Trent, England, up to 1.5 meters (5 ft) high. Also other tributaries of the Humber Estuary. River Parrett River Welland The Arnside Bore on the River Kent River Great Ouse River Ouse, Yorkshire. Like the Trent bore, this is also known as "the Aegir". River Eden River Esk River Nene. This was also known as the Eagre. River Nith River Lune, Lancashire River Ribble, Lancashire River Yealm, Devon River Leven, Cumbria

Belgium Durme, Flanders

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

Seine had a significant bore until the 1960s, locally named la barre. Since then, it has been practically eliminated by dredging and river training. Bay of Mont-Saint-Michel including Couesnon, Sélune, and Sée Arguenon Frémur (baie de la Fresnaye) Vire Sienne Vilaine, locally named le mascarin Dordogne Garonne

North America

United States

… excerpt ends here. Continue reading the full article.

Illustrations

Tidal bore: A bore in Morecambe Bay, in the United Kingdom
A bore in Morecambe Bay, in the United Kingdom
Tidal bore: The tidal bore in Upper Cook Inlet, in Alaska
The tidal bore in Upper Cook Inlet, in Alaska
Tidal bore: Undular bore and whelps near the mouth of Araguari River in northeastern Brazil. The view is oblique towards the mouth from airplane at approximately 30 m (100 ft) altitude.[3]
Undular bore and whelps near the mouth of Araguari River in northeastern Brazil. The view is oblique towards the mouth from airplane at approximately 30 m (100 ft) altitude.[3]
Tidal bore: The Qiantang River tidal bore overwhelming local infrastructure in 2024
The Qiantang River tidal bore overwhelming local infrastructure in 2024
Tidal bore: The Trent Aegir seen from West Stockwith, Nottinghamshire, 20 September 2005
The Trent Aegir seen from West Stockwith, Nottinghamshire, 20 September 2005

Worked examples

Example 1 — a first encounter with Tidal bore

Start with the simplest possible case. Write down what Tidal bore claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Tidal bore before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Tidal bore ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Tidal bore

In research
Tidal bore appears in physics research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Tidal bore in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Tidal bore is common in secondary-school and first-year university syllabi. It links to neighbouring topics Fluid dynamics, River surfing, Tidal bores, so understanding it makes those chapters shorter.
In everyday life
Look for Tidal bore outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Tidal bore in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Tidal bore means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Tidal bore out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Tidal bore in simple terms?

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, agai…

Why does Tidal bore matter?

Because it connects several physics ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Tidal bore?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Tidal bore.

Tags

  • Fluid dynamics
  • River surfing
  • Tidal bores
  • Wave mechanics

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