Suppose you hike on a mountain shaped like a hemisphere
, as shown above in 3D. The contour
map representing it is at the bottom of the same figure.
You hike on a trail given by
a parametric curve
,
. This is drawn in black on the contour
map, and then lifted up to the surface. This turns z into a function
of t:
You can compute dz/dt (the rate of change of elevation) in two ways.
This is a contrived example where it is possible to do it two ways and compare
them, and the old way is easier. With other problems, the chain rule
might be easier or might be the only way to solve them.