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The second "secret" is to write \(g'(x)\) in terms of \(g\) (because that makes the calculation of \(g'(g^{-1}(x))\) easy, since \(g(g^{-1}(x)) = x\).
Here's the graph of the derivative mentioned in the activity: \[ g'(x) = \frac{(x+4)(x-1)^2}{x-2} \]
What does the graph of the derivative look like as \(x \rightarrow \pm \infty\)?
We'll go over the solutions on Wednesday, before your quiz. These functions are a little tricky: it pays to have something to help you graph them as you work on these exercises.
We might expect that "the arrival of spring" is the big indicator: when the climate is screaming that spring has arrived, things begin happening such as the arrival of robins and the blooming of cherry trees.
There are perhaps a lot of "sub-climatic things" (such as total rainfall, or average cloud cover, or average temperature) that will impact the blossoming, but there is assumed to be some "trend" function that captures the overarching pattern.
(the red line is the average across all years)
Ah ha! We see "to minimize" -- we seek an extremum.
The problem here is that the objective function is a function of two variables (\(m\) and \(b\)); we're doing "univariate calculus".
What we know, however, is that this procedure will lead to a choice of \(b\) so that the line passes through the mean of the data: \((\overline{x},\overline{y})\). This allows us to determine one of the parameters (we choose \(b\)), so it reduces to something like \[ E(m) = \sum_{i=1}^{n} (y_i - f(m;x_i))^2 \]
But it makes no sense as time continues to go further back: the blooming dates wouldn't have continued getting later and later, if the climate were relatively stable.