Final answer:
To model the water depth in the Bay of Fundy as a function of time, we can use a cosine function with a time offset of 6.75 hours. The function is Dstd = (12-2)cos((2π/12)(t - 6.75)) + 2.
Step-by-step explanation:
To model the water depth Dstd (in meters) as a function of time t (in hours after midnight) on June 30, 2009, we can use a cosine function. The cosine function represents a periodic oscillation, which aligns with the natural period of oscillation of 12 hours.
Since high tide occurred at 6:45 am, we need to account for the time offset. We can express this offset as (t - 6.75), which gives us the time in hours after high tide. Multiplying this by 2π/12 gives us the angular frequency of the oscillation.
Putting these pieces together, the function that models the water depth Dstd is: Dstd = (12-2)cos((2π/12)(t - 6.75)) + 2, where Dstd represents the water depth, t represents the time in hours after midnight, and 2 and 12 are the maximum and minimum depths respectively.