Tidal Bores
نویسنده
چکیده
We huddled together on the bank of the river in the cool spring night, drinking tea and warming our hands at the fire. The full moon shone intermittently through the clouds, illuminating the river below. Suddenly from downstream came the cry "Flood-O!" We ran higher up the bank with a low, rumbling sound in our ears. As we reached the top of the bank a wall of water four feet high passed be low us, moving faster than we could run. The wave was moving upstream, carry ing with it pieces of wood and other de bris. In the few minutes it took for the wave to move out of range of our hear ing the water level rose another two feet. Gradually the turbulence subsided into gentle eddies, and after an hour the river began flowing toward the sea again. Thus in 1978 did I get my first sight of the tidal bore on the River Severn in southwestern Britain. A tidal bore is a remarkable hydrodynamic phenome non: it is the incoming tide in the form of a wave going up a river that empties into the sea. After the bore passes, the river flows upstream for some time before the current reverses again. For a river to have a bore two conditions must be met. The tides in the adjoining tidal body must be exceptionally high; a difference of more than 20 feet between high and low water is generally required. In addi tion the river must be shallow with a gently sloping bottom and a broad, fun nel-shaped estuary. As the incoming tide is forced into the narrowing river mouth it builds in height until a single wave materializes and moves upstream. A bore is a member of the class of solitary waves. Such waves appear in many forms and in many mediums be sides water; they are even observed in the atmosphere of Mars. Their most in triguing property is that they do not dis perse. Like all waves, a tidal bore is made up of many sinusoidal waves with many different wavelengths. In deep wa ter the component waves move with dif ferent speeds and separate from one an other. Because of the way shallow-water waves interact with the bottom in the
منابع مشابه
Unsteady Turbulence in Tidal Bores: Effects of Bed Roughness
A tidal bore is a wave propagating upstream as the tidal flow turns to rising. It forms during spring tide conditions when the flood tide is confined to a narrow funneled channel. To date, theoretical and numerical studies rely upon physical experiments to validate the developments, but the experimental data are limited mostly to visual observations and sometimes free-surface measurements. Here...
متن کاملEnvironmental Impact of Undular Tidal Bores in Tropical Rivers
A tidal bore impacts significantly on the estuarine ecosystem, although little is known on the flow field, mixing and sediment motion beneath tidal bores. In the absence of detailed systematic field measurements, a quasi-steady flow analogy was applied to investigate undular tidal bores with inflow Froude numbers between 1.25 and 1.6. Experimental results indicated that rapid flow redistributio...
متن کاملAtmospheric noise of a breaking tidal bore.
A tidal bore is a surge of waters propagating upstream in an estuary as the tidal flow turns to rising and the flood tide propagates into a funnel-shaped system. Large tidal bores have a marked breaking roller. The sounds generated by breaking tidal bores were herein investigated in the field (Qiantang River) and in laboratory. The sound pressure record showed two dominant periods, with some si...
متن کاملUnsteady Turbulence in a Shock: Physical and Numerical Modelling in Tidal Bores and Hydraulic Jumps
A turbulent flow is characterised by an unpredictable behaviour, a broad spectrum of length and time scales, and its strong mixing properties. Turbulent flows have a great mixing potential involving a wide range of vortical length scales. In steady flows, the turbulence measurements must be conducted at high frequency to resolve the small eddies and the viscous dissipation process. They must al...
متن کاملTurbulent Advances of Breaking Bores: Physical Modelling in a Large Facility
In an estuarine system, the flood tidal wave may become a tidal bore during the early flood tide in a narrow funnelled channel under large tidal ranges. Herein new experiments were conducted in a large flume to investigate breaking tidal bores and the bore roller propagation. The results demonstrated several key features of tidal bores propagating in rectangular channels. The propagation of the...
متن کاملTurbulent mixing of particles under tidal bores: an experimental analysis
A tidal bore develops in an estuary when the tidal range exceeds 4.5–6 m and the estuarine bathymetry amplifies the tidal wave. The bore is an abrupt rise in water depth associated with a discontinuity in velocity and pressure fields at the front. Herein the free-surface properties and the turbulent mixing of light-weight particles were investigated during the passage of tidal bores. The free-s...
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تاریخ انتشار 2008