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Precalculus I Class Notes 8/27/98

Quadratic Model of Depth vs. Clock Time (3 points, 3 simultaneous equations)


Here we

By stretching and shifting the graph of the basic parabola y = t^2, we can obtain the graph of any quadratic function y = a t^2 + b t + c. To fit a quadratic function to our depth vs. clock time data, we choose three points we believe to lie on the graph of depth vs. clock time. We substitute the coordinates of these points into the form y = a t^2 + b t + c to obtain three simultaneous linear equations in the parameters a, b and c. We solve these equations using elimination to obtain a, b and c which we then substituting to the form y = a t^2 + b t + c to obtain our quadratic model. We then evaluate the model by evaluating y each t value from our original data set, and compare these predictions of the model with the actual observe y values. The differences between predicted and observe values are called 'residuals'; we consider our model to be good if residuals are small and if there is no consistent pattern to the residuals.


The graph of y = x^2 is a parabola symmetric with respect to the x axis and with its vertex at the origin (0,0). 

We can obtain a graph which very closely models our depth vs. time data (see previous class notes) if we shift this parabola to the right and stretch it in the horizontal (right-left) direction, so it reaches its low point around t = 180 seconds, and in the vertical (up-down) direction so it passes through the y axis around y = 100.

Any parabola can be obtained in this way, and every parabola whose axis of symmetry is vertical will be represented by some quadratic function y = a t^2 + b t + c.   Furthermore every quadratic function will have a parabola as its graph.

pc01.jpg

To create a quadratic model we can choose three data points. 

From the point (11,80), we see that when we substitute 11 for t and 80 for y we obtain the equation 80 = a (11)^2 + b(11) + c. 

pc02.jpg

We can solve such a system by any of several methods.  Here we use elimination.

This system of two equations is reduced in the 'green' set of calculations. 

We solve the resulting equation for a (the 'red' calculations).

pc03.jpg

Having obtained a we proceed to obtain the values of b and c by 'back-substitution':

We substitute the values we have obtained for a and b back into the form y = a t^2 + b t + c:

pc04.jpg

We now evaluate the model to determine how well it fits our original data set:

pc05.jpg

 

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