Final answer:
To model the height of the tide at West Bay, you can use the sine or cosine function with the appropriate parameters. Both equations are equivalent and can represent the same periodic motion.
Step-by-step explanation:
To model the height of the tide at West Bay in terms of time (t) since midnight on January 1st, we can use trigonometric functions. One equivalent equation can be represented by the sine function, where the height (h) is given by h = A * sin(B(t - C)) + D. Another equivalent equation can be represented by the cosine function, where the height (h) is given by h = A * cos(B(t - C)) + D. In both equations, A represents the amplitude, B represents the frequency (the number of cycles that occur within a given time period 2π), C represents the phase shift (the time it takes for the initial cycle to start), and D represents the vertical shift, which is the average height of the tide.
These two equations are equivalent because they belong to the same family of trigonometric functions and can describe the same periodic motion. The sine and cosine functions are related through a phase shift of π/2 or 90 degrees. So, when you shift one equation by π/2, it becomes equivalent to the other equation. Therefore, both equations can be used to represent the height of the tide at West Bay in terms of time since midnight.