Periodic quantities such as tides, daylight, or rotating motion can be represented by sinusoidal functions of the form or cosine equivalents, with amplitude , period , horizontal shift , and midline interpreted in the context’s units; the model’s range and repeated behavior must agree with the phenomenon and data or graph. The focus is on constructing, comparing, and interpreting these models, not on Fourier analysis, differential-equation models, or other more advanced periodic-function theory.
Periodic phenomena repeat in regular cycles, so they can be modeled with a sine or cosine function:
or
The important features are:
The depth of water at a harbour varies periodically. At low tide, the depth is m at 3:00 a.m. At high tide, the depth is m at 9:00 a.m. The pattern repeats every hours. Create a model for the water depth.
Let be the number of hours after midnight, and let be the water depth in metres.
The maximum is and the minimum is , so
The water depth varies m above and below its midline.
The midline is the average of the maximum and minimum:
Thus, the average water depth is m.
The period is hours. Since
we have
Solving gives
At , the water is at its maximum of m. Cosine starts at a maximum, so use a cosine model shifted to :
This is a model for the water depth.
At high tide, :
At low tide, :
The model gives the correct high and low tides.
Therefore,
where is the water depth in metres and is the number of hours after midnight.
Its range is
and it repeats every hours, matching the situation.
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