By The Open University (Auth.)
ISBN-10: 0080363725
ISBN-13: 9780080363721
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Extra info for Waves, Tides and Shallow-Water Processes. Prepared by an Open University Course Team
Sample text
Before discussing these relationships, we shall first describe some principal features of tidal wave motions. 1 is a tidal record, showing regular vertical movements of the water surface relative to a mean level, over a period of about a month. 5 hours, at a station in the Tay estuary, Scotland. 5, you will see two important differences between wave motions resulting from the tides and those associated with wind-generated waves. 5) is typically in the order of seconds to a few tens of seconds, and both period and amplitude of the oscillations can be quite irregular.
In this case, the length of "_-hebasin (l) corresponds to a quarter of the wavelength of the seiche ~L). 18) T is here known as the resonant period. For standing waves to develop, the resonant period of the basin must be equal to the period of the wave motion or to a small whole number of nultiples of that period. 19 is an example of how the arrival of waves of a certain frequency can create problems for moored vessels in small harbours by setting up a standing wave. ish will 'slop over' if your standing wave gets too big, so a standing ,vave in a harbour may dash vessels against the harbour wall, or even throw them ashore.
13 (a) Diagram (not to scale), illustrating how the Moon (shown here in conjunction) must travel further round its orbit to return to the same position relative to both Earth and Sun, because the Earth has also moved in its orbit relative to the Sun. For simplicity both orbits are portrayed as circular. (b) Summary diagram (not to scale) of combined motions of Earth and Moon about the Sun and about the centre of mass of the Earth-Moon system. For simplicity, orbits are assumed to be circular. Note: synodic month = lunar month (see p.
Waves, Tides and Shallow-Water Processes. Prepared by an Open University Course Team by The Open University (Auth.)
by Edward
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