Answer:
D(t) = 20 * sin(B * t - B * 3 + k * 2π) + 45 = 20 * sin(B * (t - 3) + k * 2π) + 45
Explanation:
The temperature over a day can be modeled by a sinusoidal function of the form:
D(t) = A * sin(Bt + C) + D
Where A is the amplitude (half the difference between the high and low temperatures), B is the angular frequency, C is the phase shift, and D is the vertical shift.
From the given information, we know:
The high temperature is 85 degrees.
The low temperature of 45 degrees occurs at 3 AM, or 3 hours after midnight.
So, the amplitude is (85 - 45)/2 = 20
The temperature at 3 AM can be found by setting t = 3:
D(3) = 20 * sin(B * 3 + C) + 45
So, the vertical shift is 45.
Finally, we can find the phase shift by using the fact that the low temperature occurs at 3 AM:
C = -B * 3 + k * 2π
Where k is an integer.
Putting it all together, we get:
D(t) = 20 * sin(B * t - B * 3 + k * 2π) + 45 = 20 * sin(B * (t - 3) + k * 2π) + 45
This is the equation for the temperature, D, in terms of t.